Genetic polymorphisms in folate and adenosine pathway and MTX transporters associated with MTX treatment outcome in patients with psoriasis or psoriatic arthritis.
\\n\\n
\\n"}]',published:!0,mainMedia:{caption:"Milestone",originalUrl:"/media/original/124"}},components:[{type:"htmlEditorComponent",content:'
Barely three months into the new year and we are happy to announce a monumental milestone reached - 150 million downloads.
\n\nThis achievement solidifies IntechOpen’s place as a pioneer in Open Access publishing and the home to some of the most relevant scientific research available through Open Access.
\n\nWe are so proud to have worked with so many bright minds throughout the years who have helped us spread knowledge through the power of Open Access and we look forward to continuing to support some of the greatest thinkers of our day.
\n\nThank you for making IntechOpen your place of learning, sharing, and discovery, and here’s to 150 million more!
\n\n\n\n\n'}],latestNews:[{slug:"webinar-introduction-to-open-science-wednesday-18-may-1-pm-cest-20220518",title:"Webinar: Introduction to Open Science | Wednesday 18 May, 1 PM CEST"},{slug:"step-in-the-right-direction-intechopen-launches-a-portfolio-of-open-science-journals-20220414",title:"Step in the Right Direction: IntechOpen Launches a Portfolio of Open Science Journals"},{slug:"let-s-meet-at-london-book-fair-5-7-april-2022-olympia-london-20220321",title:"Let’s meet at London Book Fair, 5-7 April 2022, Olympia London"},{slug:"50-books-published-as-part-of-intechopen-and-knowledge-unlatched-ku-collaboration-20220316",title:"50 Books published as part of IntechOpen and Knowledge Unlatched (KU) Collaboration"},{slug:"intechopen-joins-the-united-nations-sustainable-development-goals-publishers-compact-20221702",title:"IntechOpen joins the United Nations Sustainable Development Goals Publishers Compact"},{slug:"intechopen-signs-exclusive-representation-agreement-with-lsr-libros-servicios-y-representaciones-s-a-de-c-v-20211123",title:"IntechOpen Signs Exclusive Representation Agreement with LSR Libros Servicios y Representaciones S.A. de C.V"},{slug:"intechopen-expands-partnership-with-research4life-20211110",title:"IntechOpen Expands Partnership with Research4Life"},{slug:"introducing-intechopen-book-series-a-new-publishing-format-for-oa-books-20210915",title:"Introducing IntechOpen Book Series - A New Publishing Format for OA Books"}]},book:{item:{type:"book",id:"6266",leadTitle:null,fullTitle:"Marine Ecology - Biotic and Abiotic Interactions",title:"Marine Ecology",subtitle:"Biotic and Abiotic Interactions",reviewType:"peer-reviewed",abstract:"During the last decades, aquatic resources have been severely depleted due to human-induced factors such as overexploitation and pollution and more recently due to deviations in the physicochemical parameters of oceans, dramatic changes in weather patterns and melting of glaciers. The effects of these man-made factors are occurring in a relatively shorter time scale and, in many cases, are beyond the capacity of organisms to adapt to these deviations. The majority of natural aquatic resources, which are one of the most important food sources on the planet, are being used to the extent that limits their capacity for regeneration. Despite ongoing attempts towards developing strategies for long-term management of aquatic resources all over the world, efforts have met with limited success. Thus, the sustainable use of aquatic resources has become a very important reality considering a projected human population of 11 billion by the year 2100. With this reality in mind, the purpose of this book is to shed more light on the field of marine ecology by emphasizing the diversity of aquatic life on earth and its importance both as part of a balanced ecosystem and as part of critical source of food on earth. The book covers important findings, discussions and reviews on a variety of subjects on environmental and competitive interactions of marine organisms at different trophic levels and their effects on the productivity, dynamics and structure of marine ecosystems around the world. Each chapter focuses on a specific case in the field of marine ecology and was written by researchers with years of experience in their respective fields. We hope that academicians, researchers and students as well as experts and professionals working in the field of marine ecology will benefit from these contributions. We also hope that this book will inspire more studies to help better understand the marine environment and develop strategies to better protect this crucial element of life on earth.",isbn:"978-1-78923-449-7",printIsbn:"978-1-78923-448-0",pdfIsbn:"978-1-83881-368-0",doi:"10.5772/intechopen.69018",price:119,priceEur:129,priceUsd:155,slug:"marine-ecology-biotic-and-abiotic-interactions",numberOfPages:294,isOpenForSubmission:!1,isInWos:1,isInBkci:!1,hash:"9d821ed950a497c8f50de67abf419259",bookSignature:"Muhammet Türkoğlu, Umur Önal and Ali Ismen",publishedDate:"August 1st 2018",coverURL:"https://cdn.intechopen.com/books/images_new/6266.jpg",numberOfDownloads:17732,numberOfWosCitations:42,numberOfCrossrefCitations:38,numberOfCrossrefCitationsByBook:1,numberOfDimensionsCitations:57,numberOfDimensionsCitationsByBook:1,hasAltmetrics:1,numberOfTotalCitations:137,isAvailableForWebshopOrdering:!0,dateEndFirstStepPublish:"July 13th 2017",dateEndSecondStepPublish:"August 3rd 2017",dateEndThirdStepPublish:"January 9th 2018",dateEndFourthStepPublish:"February 9th 2018",dateEndFifthStepPublish:"April 9th 2018",currentStepOfPublishingProcess:5,indexedIn:"1,2,3,4,5,6,7",editedByType:"Edited by",kuFlag:!1,featuredMarkup:null,editors:[{id:"99483",title:"Prof.",name:"Muhammet",middleName:null,surname:"Turkoglu",slug:"muhammet-turkoglu",fullName:"Muhammet Turkoglu",profilePictureURL:"https://mts.intechopen.com/storage/users/99483/images/system/99483.jpeg",biography:"Dr. Muhammet TURKOGLU, completed his undergraduate education in Biology in 1988 at Hacettepe University, Faculty of Science, Department of Biology; graduate education in 1991 at Dokuz Eylul University, Marine Sciences and Technology Institute, Marine Living Resources Department (Master thesis titled 'Investigation of Chromium (Cr) Concentrations in Water, Sediments and Some Organisms of Izmir Bay'). He completed his Ph.D. at Ege University, Faculty of Science, Department of Biology, Section of Marine Biology in 1998 (Doctorate thesis (Ph.D. Thesis) titled 'Phytoplankton Composition and Effects of Bio-ecological Factors of Middle Black Sea Area (Coasts of Sinop Peninsula)'). \r\nCurrently, he is working as a full professor of Marine Science and Technology Faculty at Çanakkale Onsekiz Mart University, Turkey. Dr. Turkoglu is an oceanographer and his researches involve studies in Aegean Sea, Black Sea, Turkish Straits System (Dardanelles, Sea of Marmara and Bosphorus) and Caspian Sea. He is interested in species diversity, vertical and temporal successions of phytoplankton in marine ecosystems, especially in coastal habitats. Dr. Turkoglu is also interested in nutrient dynamics and harmful algal blooms (HABs) in marine systems. He has more than 100 scientific studies published by various reputed scientific journals and others. Dr. Turkoglu participated in various national and international marine scientific voyages throughout the academic career. \r\nHis expertise are (1) Marine Biodiversity and Ecology (Microplankton, Phytoplankton and Microzooplankton) (2) Biological Oceanography (Phytoplankton Dynamics) (3) Chemical Oceanography (Nutrient Dynamics) (4) Harmful Algal Blooms (HABs) (5) Eutrophication and Phytoplankton (6) Physical Oceanography (CTD)",institutionString:"Çanakkale Onsekiz Mart University",position:null,outsideEditionCount:0,totalCites:0,totalAuthoredChapters:"2",totalChapterViews:"0",totalEditedBooks:"1",institution:{name:"Canakkale Onsekiz Mart Universitesi Tip Fakultesi Hastanesi",institutionURL:null,country:{name:"Turkey"}}}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,coeditorOne:{id:"83707",title:"Dr.",name:"Umur",middleName:null,surname:"Önal",slug:"umur-onal",fullName:"Umur Önal",profilePictureURL:"https://mts.intechopen.com/storage/users/83707/images/5354_n.jpg",biography:"Dr. Umur ÖNAL is a full professor in the Department of Aquaculture, Marine Science and Technology Faculty, Canakkale Onsekiz Mart University, Turkey. Dr. ÖNAL received his MS and Ph.D from the Department of Fisheries and Wildlife, Oregon State University. His research interests involve larval fish and mollusc culture and mainly focuses on larval fish feeding and nutrition. In addition, he studies reproduction of fish and molluscs with emphasis on optimizing reproduction potential towards developing methods on the mass culture of early stages of commercially important species.",institutionString:null,position:null,outsideEditionCount:0,totalCites:0,totalAuthoredChapters:"0",totalChapterViews:"0",totalEditedBooks:"0",institution:{name:"Canakkale Onsekiz Mart Universitesi Tip Fakultesi Hastanesi",institutionURL:null,country:{name:"Turkey"}}},coeditorTwo:{id:"208452",title:"Dr.",name:"Ali",middleName:null,surname:"İsmen",slug:"ali-ismen",fullName:"Ali İsmen",profilePictureURL:"https://mts.intechopen.com/storage/users/208452/images/5355_n.jpg",biography:'Dr. Ali İSMEN is a full professor in Fisheries Section of Marine Science and Technology Faculty in Canakkale Onsekiz Mart University, Turkey. Dr. ISMEN has completed his undergraduate education on Fisheries in Ankara University in 1985. Then, he comleted his graduate education in 1988 in Ankara University, giving the master thesis titled \\"A comparative study of the catches in bait and non-bait pinter with freshwater lobster (Astacus leptodactylus Esch.1823)”. In 1995, he completed his PhD thesis titled “Biology and Population Parameters of whiting (Merlangus merlangus euxinus) in Turkish Coasts of the Black Sea\\" in METU, Institute of Marine Science, Department of Fisheries Biology. He is interested in marine fish species distribution, fisheries biology, stock assessment and population parameters in Turkish seas. He has scientific studies numerous published by various reputed scientific journals and others.',institutionString:null,position:null,outsideEditionCount:0,totalCites:0,totalAuthoredChapters:"0",totalChapterViews:"0",totalEditedBooks:"0",institution:null},coeditorThree:null,coeditorFour:null,coeditorFive:null,topics:[{id:"659",title:"Aquatic Ecosystem",slug:"earth-and-planetary-sciences-marine-biology-aquatic-ecosystem"}],chapters:[{id:"61795",title:"Introductory Chapter: Marine Ecology—Biotic and Abiotic Interactions",doi:"10.5772/intechopen.78296",slug:"introductory-chapter-marine-ecology-biotic-and-abiotic-interactions",totalDownloads:1103,totalCrossrefCites:0,totalDimensionsCites:2,hasAltmetrics:0,abstract:null,signatures:"Muhammet Turkoglu, Umur Onal and Ali Ismen",downloadPdfUrl:"/chapter/pdf-download/61795",previewPdfUrl:"/chapter/pdf-preview/61795",authors:[{id:"99483",title:"Prof.",name:"Muhammet",surname:"Turkoglu",slug:"muhammet-turkoglu",fullName:"Muhammet Turkoglu"}],corrections:null},{id:"61920",title:"Geo-Biological Coupling of Authigenic Carbonate Formation and Autotrophic Faunal Colonization at Deep-Sea Methane Seeps I: Geo-Biological Settings",doi:"10.5772/intechopen.76976",slug:"geo-biological-coupling-of-authigenic-carbonate-formation-and-autotrophic-faunal-colonization-at-1",totalDownloads:1040,totalCrossrefCites:2,totalDimensionsCites:2,hasAltmetrics:1,abstract:"Methane (CH4) in sub-seafloor sediment is generated both biologically and non-biologically from organic and inorganic sources. A major part of the sub-seafloor methane is oxidized before leakage via “anaerobic oxidation of methane” (AOM) in the subsurface. The AOM-survivor methane, which is relatively minor part of the subsurface methane, leaches to the overlying water column and is eventually subject to thorough anaerobic and aerobic oxidation in the water column. The AOM with sulfate results in the generation of carbon dioxide and sulfide; the former (CO2) is incorporated into authigenic carbonate and autotrophic biomass, and the autotrophy is energetically driven by oxidation of the latter (H2S). These processes are typically observed at focused sites that are generally known as “methane seeps” or hydrocarbon seeps, or occasionally called as cold seeps in comparison with hydrothermal vents. Methane seeps are typically formed in passive and active continental margins, occasionally with unique features such as exposed methane hydrates, mud volcanoes, asphalt volcanoes, salt diapirs, and brine pools. Accordingly, authigenic carbonates and unique biological communities are shaped at respective methane seeps. This chapter overviews geological and biological setting for the formation of methane seeps associated with unique landscapes of carbonates and biomes.",signatures:"Takeshi Naganuma",downloadPdfUrl:"/chapter/pdf-download/61920",previewPdfUrl:"/chapter/pdf-preview/61920",authors:[null],corrections:null},{id:"62136",title:"Geo-Biological Coupling of Authigenic Carbonate Formation and Autotrophic Faunal Colonization at Deep-Sea Methane Seeps II. Geo-Biological Landscapes",doi:"10.5772/intechopen.78978",slug:"geo-biological-coupling-of-authigenic-carbonate-formation-and-autotrophic-faunal-colonization-at-2",totalDownloads:1197,totalCrossrefCites:0,totalDimensionsCites:1,hasAltmetrics:1,abstract:"Deep-sea methane seeps are typically shaped with authigenic carbonates and unique biomes depending on methane-driven and methane-derived metabolisms. Authigenic carbonates vary in δ13C values due probably to δ13C variation in the carbon sources (directly carbon dioxide and bicarbonate, and ultimately methane) which is affected by the generation and degradation (oxidation) of methane at respective methane seeps. Anaerobic oxidation of methane (AOM) by specially developed microbial consortia has significant influences on the carbonate δ13C variation as well as the production of carbon dioxide and hydrogen sulfide for chemoautotrophic biomass production. Authigenesis of carbonates and faunal colonization are thus connected. Authigenic carbonates also vary in Mg contents that seem correlated again to faunal colonization. Among the colonizers, mussels tend to colonize low δ13C carbonates, while gutless tubeworms colonize high-Mg carbonates. The types and varieties of such geo-biological landscapes of methane seeps are overviewed in this chapter. A unique feature of a high-Mg content of the rock-tubeworm conglomerates is also discussed.",signatures:"Takeshi Naganuma",downloadPdfUrl:"/chapter/pdf-download/62136",previewPdfUrl:"/chapter/pdf-preview/62136",authors:[null],corrections:null},{id:"57495",title:"Plankton Ecology and Productivity in Jamaican Waters with New and Unique Applications",doi:"10.5772/intechopen.70663",slug:"plankton-ecology-and-productivity-in-jamaican-waters-with-new-and-unique-applications",totalDownloads:1232,totalCrossrefCites:1,totalDimensionsCites:1,hasAltmetrics:0,abstract:"Unique applications of plankton ecology and productivity in Jamaican waters are presented. While traditional indices were inadequate descriptors of mangrove lagoon water quality, planktonic indices (total Chlorophyll a, zooplankton groups and species) were more reliable. Phytoplankton biomass was used to indicate a longitudinal gradient along the Hellshire Coastline, identifying non-point sources of enrichment, and movement of water masses in the absence of expensive Eulerian current meters. Along that same coast, mean primary production, determined by 14C techniques, confirmed a gradient from the eutrophic Kingston Harbour (21.1 g C m−2year−1) to the oligotrophic control site (0.52 g C m−2 year−1). Maximum inshore station values (36.75–18.39 g C m−2 year−1) were more than 20 times greater than offshore and exceeded Harbour values, confirming non-point sources and localized mechanisms as important inshore sources of eutrophication. The novel use of Ecopath with Ecosim (EwE) software to model trophic flows within planktonic communities was done in two bays. For Discovery Bay, on Jamaica’s north coast, the model indicated a developing ecosystem with open mineral cycles and poor nutrient conservation while in Foul and Folly Bays on the southeastern coast the model indicated greater resilience and ability to recover from perturbations. These applications have facilitated informed management decisions for sustainable use in Jamaican coastal ecosystems.",signatures:"Mona K. Webber, Dale F. Webber and Gale Persad Ford",downloadPdfUrl:"/chapter/pdf-download/57495",previewPdfUrl:"/chapter/pdf-preview/57495",authors:[null],corrections:null},{id:"57518",title:"Ecology of Planktonic Atlantic Cod (Gadus morhua)",doi:"10.5772/intechopen.70661",slug:"ecology-of-planktonic-atlantic-cod-gadus-morhua-",totalDownloads:931,totalCrossrefCites:0,totalDimensionsCites:0,hasAltmetrics:0,abstract:"Atlantic cod larvae surviving the first weeks after hatching settle next years juvenile recruitment on Georges Bank (USA). It probably supports Hjort’s critical period hypothesis that effects of climate on marine biological productivity control early-life history processes and recruitment in fish populations. Climate also regulates local ultraviolet sea surface radiation, which may potentially kill microbes pathogenic to planktonic cod eggs. Survival capacities of cod larvae depend on maternal effects on egg qualities attained during oogenesis, influenced by variable food sources for female cod. Actual survival of first-feeding cod larvae requires proper abundance of preferred prey, copepod nauplii, produced by fertile females. Temporal and spatial mismatch between cod larvae and prey is normal, extensive and lethal, counteracted by opportunistic behavior that optimizes encounters. In spawning habitats of Northeast Arctic cod, the abundance of Calanus finmarchicus nauplii possibly results from coastal biological productivity in the previous year, which may explain time lags in positive correlations between vernal river discharge and NEA cod recruitment. Extensive meltwater storage for year-round hydroelectric production probably limits food web productivity, survival of NEA cod larvae and stock recruitment. Global climate change and stock management interact ecologically with other anthropogenic influences concerning sustainability of Atlantic cod population systems.",signatures:"Stig Skreslet",downloadPdfUrl:"/chapter/pdf-download/57518",previewPdfUrl:"/chapter/pdf-preview/57518",authors:[null],corrections:null},{id:"56972",title:"Encounters in the Zooplankton: Implications for Pelagic Ecosystem Dynamics",doi:"10.5772/intechopen.70662",slug:"encounters-in-the-zooplankton-implications-for-pelagic-ecosystem-dynamics",totalDownloads:1066,totalCrossrefCites:0,totalDimensionsCites:0,hasAltmetrics:0,abstract:"Many important phenomena in the plankton are driven by encounters among individuals. These encounters are mediated by the relative motion of zooplankters, either through the swimming ability of organisms, the small-scale hydrodynamic turbulence, or both. Through selected case studies, in this chapter, we illustrate how encounter rates influence the predator-prey interactions and reproduction, two of the major processes regulating the zooplankton population dynamics. Estimations on the encounter rates among zooplankters were made on the basis of the Gerritsen-Strickler and Rothschild-Osborn models, which consider non-turbulent and turbulent conditions, respectively. In a first case, we show how the predatory impact of siphonophores is over the fish larvae, in the southern Gulf of Mexico. In the absence of water turbulence, a predator encounters 38–40 prey in a day at surface waters, but under the influence of the wind, encounters can increase between 1.2 and 3.3 times depending on the wind velocity and prey speed. In a second case, we examined the encounters between a copepod predator and a cladoceran prey, the dominant groups in the meromictic lagoon of Clipperton atoll. Here, a predator can encounter a high number of prey (until 441) in a day, due to the high density of prey. Turbulence conditions enhance encounter rates, but even if encounters are high, it does not mean that a predator can ingest a high number of prey. In a third case, we analyzed the mate encounters of the holoplanktonic mollusk Firoloida desmarestia from the southern Gulf of Mexico, throughout an annual cycle. Results indicated that May is the high reproductive season, a period where a female can encounter 17 males in a day, under turbulent conditions. As F. desmarestia is a low abundant species, the role of wind-induced turbulence proved to be highly important in increasing encounters between mates. These case studies illustrate the importance of encounters among zooplankters in the growth and maintenance of populations in the plankton. Future field and experimental studies are needed to achieve a better understanding of the pelagic ecosystem dynamics.",signatures:"Laura Sanvicente-Añorve and Miguel Alatorre-Mendieta",downloadPdfUrl:"/chapter/pdf-download/56972",previewPdfUrl:"/chapter/pdf-preview/56972",authors:[null],corrections:null},{id:"59865",title:"Marine Fisheries in Nigeria: A Review",doi:"10.5772/intechopen.75032",slug:"marine-fisheries-in-nigeria-a-review",totalDownloads:3863,totalCrossrefCites:8,totalDimensionsCites:10,hasAltmetrics:1,abstract:"Fisheries production especially from marine is important for the socio-economic development of Nigerians and its contribution to the nation’s economic growth through the Gross Domestic Product (GDP). Nigeria is blessed with enough marine fisheries resources that could enhance increased fish production. Yet, fish supply from domestic production is far below the fish demand of her citizens. This chapter is therefore focused on marine fisheries in Nigeria. We adopted a desk review approach. This chapter is divided into different sections such as the Nigerian fisheries sector, marine fisheries resources in Nigeria, status of marine fisheries production in Nigeria, marine fisheries regulations, and constraints to optimal marine fisheries production in Nigeria. We concluded that the contribution of aquaculture to marine fisheries production has been low, compared to the marine capture fisheries production. Also, we noted that despite the availability of regulations, noncompliance by fisher folks has not helped to optimize marine fisheries production. We therefore recommended that the culture of marine fishes should be intensified. Marine waters should also be protected against destruction and pollution as a result of human activities. Available marine fisheries regulations should be enforced and violators of the regulations should be punished as stipulated in the regulations.",signatures:"Olalekan Jacob Olaoye and Wahab Gbenga Ojebiyi",downloadPdfUrl:"/chapter/pdf-download/59865",previewPdfUrl:"/chapter/pdf-preview/59865",authors:[null],corrections:null},{id:"60228",title:"Marine Stock Enhancement in India: Current Status and Future Prospects",doi:"10.5772/intechopen.75175",slug:"marine-stock-enhancement-in-india-current-status-and-future-prospects",totalDownloads:2115,totalCrossrefCites:0,totalDimensionsCites:0,hasAltmetrics:0,abstract:"India is a 12 mega-diversity nation known for its biodiversity richness. The geographic territory of India is an integral part of Central Indian Ocean Region consisting of three distinct marine ecosystem zones such as the Arabian Sea, Bay of Bengal and Indian Ocean. India is endowed with an exclusive economic zone of 2.02 million km2, coastline of over 8000 km and a variety of coastal ecosystems. The estimated number of marine fish species known from India constitutes 2443 species distributed in 230 families. According to the IUCN extant (2014), 50 species are threatened (6 of them critically endangered, 7 endangered and 37 vulnerable), while 45 are near-threatened. Marine fish diversity is in ever-increasing danger with depletion of resources. Overdependence on fish has led to overfishing resulting in the dwindling of diversity and abundance of stocks. Central Marine Fisheries Research Institute has initiated marine stock assessment practices in India and its present report in 2016 recorded a total of 709 species which is lower than 730 species recorded in 2015 in the landings showing an alarming situation on the exploited marine fishery resources of India. This situation demands restorative measures such as restocking, stock enhancement and sea ranching.",signatures:"Mohammad Serajuddin, Farah Bano, Madhu Awasthi, Pragya\nGupta and Graish Kumar",downloadPdfUrl:"/chapter/pdf-download/60228",previewPdfUrl:"/chapter/pdf-preview/60228",authors:[null],corrections:null},{id:"60154",title:"The Natural Ecology and Stock Enhancement of the Edible Jellyfish (Rhopilema esculentum Kishinouye, 1891) in the Liaodong Bay, Bohai Sea, China",doi:"10.5772/intechopen.75576",slug:"the-natural-ecology-and-stock-enhancement-of-the-edible-jellyfish-rhopilema-esculentum-kishinouye-18",totalDownloads:1011,totalCrossrefCites:1,totalDimensionsCites:1,hasAltmetrics:0,abstract:"Among the edible jellyfish species, Rhopilema esculentum Kishinouye, 1891, is one of the most abundant jellyfish species consumed. Therefore, this jellyfish species is an important fisheries source in China. The jellyfish fisheries in China show annually considerable fluctuations and have a very short season. In the chapter, we firstly try to review the natural ecology of R. esculentum, which includes the distribution and migration, growth model, and survival rate in the Liaodong Bay (LDB) based on the results of our field studies for more than 20 years. Secondly, we focus on reviewing the jellyfish fishery and population dynamic in the LDB. Thirdly, we emphasize the themes, including the survey methods, catch prediction, enhancement assessment, and fishery management, based on our survey results from 2005 to 2010. Finally, we present our field and experiment results of resource restoration. The high commercial value of R. esculentum enhancement in the LDB has made this a very successful enterprise.",signatures:"Jing Dong, Bin Wang, Yan Duan, Aiyong Wang, Yulong Li, Ming\nSun, Yu Chai, Xiuze Liu, Xuguang Yu, Dong Guo and Xiaolin Wang",downloadPdfUrl:"/chapter/pdf-download/60154",previewPdfUrl:"/chapter/pdf-preview/60154",authors:[null],corrections:null},{id:"60698",title:"Overview on Mediterranean Shark’s Fisheries: Impact on the Biodiversity",doi:"10.5772/intechopen.74923",slug:"overview-on-mediterranean-shark-s-fisheries-impact-on-the-biodiversity",totalDownloads:1095,totalCrossrefCites:13,totalDimensionsCites:18,hasAltmetrics:1,abstract:"Bibliographic analysis shows that the Mediterranean Sea is a hot spot for cartilaginous species biodiversity, including sharks, rays, and chimaeras; 49 sharks and 36 rays were recorded in this region. However, they are by far the most endangered group of marine fish in the Mediterranean Sea. The IUCN Red List shows clearly the vulnerability of elasmobranchs and the lack of data; 39 species (53% of 73 assessed species) are critically endangered, endangered, or vulnerable. The biological characteristics of elasmobranchs (low fecundity, late maturity, and slow growth) make them more vulnerable to fishing pressure than most teleost fish. Overfishing, the wide use of nonselective fishing practices, and habitat degradation are leading to dramatic declines of these species in the Mediterranean Sea. In general, elasmobranchs are not targeted but are caught incidentally. In many fisheries, they are, however, often landed and marketed. A decline in cartilaginous fish species landings has been observed while fishing effort has generally increased. Better understanding of the composition of incidental and targeted catches of sharks by commercial fisheries are fundamentally important for the conservation of these populations. Moreover, problems encountered by elasmobranchs in the area are highlighted, and conservation measures are suggested.",signatures:"Mohamed Nejmeddine Bradai, Bechir Saidi and Samira Enajjar",downloadPdfUrl:"/chapter/pdf-download/60698",previewPdfUrl:"/chapter/pdf-preview/60698",authors:[null],corrections:null},{id:"59954",title:"An Update on Reproduction in Ghost Shrimps (Decapoda: Axiidea) and Mud Lobsters (Decapoda: Gebiidea)",doi:"10.5772/intechopen.75067",slug:"an-update-on-reproduction-in-ghost-shrimps-decapoda-axiidea-and-mud-lobsters-decapoda-gebiidea-",totalDownloads:1217,totalCrossrefCites:5,totalDimensionsCites:9,hasAltmetrics:0,abstract:"In this report, I review the taxonomic history, body adaptations, ecology, and reproduction of the infraorders Axiidea (ghost shrimps) and Gebiidea (mud lobsters). Known until recently as the “Thalassinidea,” modern classification divided Axiidea into six families and Gebiidea into five. Ghost shrimps are characterized by having the first and second pereiopod chelate and a soft and delicate body, whereas mud lobsters possess the first pereiopod chelate or subchelate and second pereiopod subchelate or simple with a hard and heavily calcified body. Among the main body adaptations of these organisms are distinguished: (i) carapace laterally compressed, (ii) pleon longer than the cephalothorax in ghost shrimps but usually shorter in mud lobsters, and (iii) anterior feet thrown directly forward. Current accounting of axiideans and gebiideans reaches around 781 and 240 extant species, respectively, with major number of species in Callianassidae and Upogebiidae within of each clade. Male reproductive system involves paired testes linked to the vas deferens that open in gonopores on the ventral coxal segment of the fifth pereiopod. In females, the reproductive system is composed of paired and colored ovaries, one ovary shorter than another, and a pair of short and translucent oviducts linking each ovary to the gonopore, this latter located on the ventral coxal of the third pereiopod. When present in males, the first pleopod is sexually dimorphic. Most ghost shrimps show distinct sexual dimorphism in body size and the major cheliped which become them in a promising group for growth studies. Hypertrophied chelipeds in males are often used to defend galleries against invasion from other shrimps from the same or opposite sex or during the intense male-to-male competition for sexual partners. Knowledge about sexual systems of these species remains limited; however, available information suggests that hermaphroditism might be commonly present in axiideans and gebiideans. Regarding mating systems, all species of ghost shrimp and mud lobster with solitary habits and remarkable sexual dimorphism in the major cheliped are expected to be polygamous. Finally, considerable variability among Axiidea and Gebiidea species in fecundity and egg size may indicate important differences in the reproductive strategy and may also reflect a latitudinal trend as observed in other decapods.",signatures:"Patricio Hernáez",downloadPdfUrl:"/chapter/pdf-download/59954",previewPdfUrl:"/chapter/pdf-preview/59954",authors:[null],corrections:null},{id:"61371",title:"The Role of Microalgae in Renewable Energy Production: Challenges and Opportunities",doi:"10.5772/intechopen.73573",slug:"the-role-of-microalgae-in-renewable-energy-production-challenges-and-opportunities",totalDownloads:1863,totalCrossrefCites:8,totalDimensionsCites:13,hasAltmetrics:0,abstract:"Microalgae are one of the most effective sources of renewable energy production. It can grow at high rates and capable of producing oil along the year. Microalgae biomass was first suggested as a feedstock for biofuel production and received early attention for commercial application. Microalgae are expected to be a vital raw material for amino acids, vitamins and productions of valuable byproducts. The cultivation of microalgae is known to be the most gainful business in the biotechnological industry. It is a waste less, environmentally pure, energy and resource saving route. Biodiesel production from algal lipid is non-toxic and highly biodegradable. Conversion of biomass to biofuel can be achieved by different methods which are broadly classified into: thermal, chemical and biochemical methods, in addition to the large number of different agents for decomposing and hydrolysing. We can obtain the low-cost energy production from the wastewater treatment by using microalgae. Finally, biodiesel production by microalgae in Egypt is not practical at the economical level. In order to improve biodiesel fuel quality, the alga must be subjected to genetic engineering for up-regulation of fatty acid biosynthesis and/or by down-regulation of β-oxidation. Economically, the algal biomass must be processed for bio-refinery to maximize its utilization for different applications.",signatures:"Abd Ellatif Mohamed Hussian",downloadPdfUrl:"/chapter/pdf-download/61371",previewPdfUrl:"/chapter/pdf-preview/61371",authors:[null],corrections:null}],productType:{id:"1",title:"Edited Volume",chapterContentType:"chapter",authoredCaption:"Edited by"},subseries:null,tags:null},relatedBooks:[{type:"book",id:"304",title:"Sediment Transport in Aquatic Environments",subtitle:null,isOpenForSubmission:!1,hash:"0eb11af1d03ad494253c41e1d3c998e9",slug:"sediment-transport-in-aquatic-environments",bookSignature:"Andrew J. Manning",coverURL:"https://cdn.intechopen.com/books/images_new/304.jpg",editedByType:"Edited by",editors:[{id:"23008",title:"Prof.",name:"Andrew James",surname:"Manning",slug:"andrew-james-manning",fullName:"Andrew James Manning"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"6344",title:"Biological Resources of Water",subtitle:null,isOpenForSubmission:!1,hash:"ca4f407275697c7cf547debc6b1e85a9",slug:"biological-resources-of-water",bookSignature:"Sajal Ray",coverURL:"https://cdn.intechopen.com/books/images_new/6344.jpg",editedByType:"Edited by",editors:[{id:"173697",title:"Prof.",name:"Sajal",surname:"Ray",slug:"sajal-ray",fullName:"Sajal Ray"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"5765",title:"Corals in a Changing World",subtitle:null,isOpenForSubmission:!1,hash:"eed323f414d06a6bd994cc9d37ad24c4",slug:"corals-in-a-changing-world",bookSignature:"Carmenza Duque Beltran and Edisson Tello Camacho",coverURL:"https://cdn.intechopen.com/books/images_new/5765.jpg",editedByType:"Edited by",editors:[{id:"155319",title:"Emeritus Prof.",name:"Carmenza",surname:"Duque",slug:"carmenza-duque",fullName:"Carmenza Duque"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"8421",title:"Invertebrates",subtitle:"Ecophysiology and Management",isOpenForSubmission:!1,hash:"524faf733c0ebf32b356f89b2148e6de",slug:"invertebrates-ecophysiology-and-management",bookSignature:"Sajal Ray, Genaro Diarte-Plata and Ruth Escamilla-Montes",coverURL:"https://cdn.intechopen.com/books/images_new/8421.jpg",editedByType:"Edited by",editors:[{id:"173697",title:"Prof.",name:"Sajal",surname:"Ray",slug:"sajal-ray",fullName:"Sajal Ray"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"7912",title:"Biological Research in Aquatic Science",subtitle:null,isOpenForSubmission:!1,hash:"8f86a91e9a5c76a2d11a861d879bc96a",slug:"biological-research-in-aquatic-science",bookSignature:"Yusuf Bozkurt",coverURL:"https://cdn.intechopen.com/books/images_new/7912.jpg",editedByType:"Edited by",editors:[{id:"90846",title:"Prof.",name:"Yusuf",surname:"Bozkurt",slug:"yusuf-bozkurt",fullName:"Yusuf Bozkurt"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"6645",title:"Seabirds",subtitle:null,isOpenForSubmission:!1,hash:"6ce1372af411b6ada3b53e881f7b85fc",slug:"seabirds",bookSignature:"Heimo Mikkola",coverURL:"https://cdn.intechopen.com/books/images_new/6645.jpg",editedByType:"Edited by",editors:[{id:"144330",title:"Dr.",name:"Heimo",surname:"Mikkola",slug:"heimo-mikkola",fullName:"Heimo Mikkola"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"6411",title:"Mangrove Ecosystem Ecology and Function",subtitle:null,isOpenForSubmission:!1,hash:"5425ea4e90ed12b902f30186f807f8f5",slug:"mangrove-ecosystem-ecology-and-function",bookSignature:"Sahadev Sharma",coverURL:"https://cdn.intechopen.com/books/images_new/6411.jpg",editedByType:"Edited by",editors:[{id:"227169",title:"Ph.D.",name:"Sahadev",surname:"Sharma",slug:"sahadev-sharma",fullName:"Sahadev Sharma"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"9243",title:"Coastal Environments",subtitle:null,isOpenForSubmission:!1,hash:"8e05e5f631e935eef366980f2e28295d",slug:"coastal-environments",bookSignature:"Yuanzhi Zhang and X. San Liang",coverURL:"https://cdn.intechopen.com/books/images_new/9243.jpg",editedByType:"Edited by",editors:[{id:"77597",title:"Prof.",name:"Yuanzhi",surname:"Zhang",slug:"yuanzhi-zhang",fullName:"Yuanzhi Zhang"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"8882",title:"Advances in the Studies of the Benthic Zone",subtitle:null,isOpenForSubmission:!1,hash:"79f77db18a383e92371a06aa07937f90",slug:"advances-in-the-studies-of-the-benthic-zone",bookSignature:"Luis A. Soto",coverURL:"https://cdn.intechopen.com/books/images_new/8882.jpg",editedByType:"Edited by",editors:[{id:"256002",title:"Ph.D.",name:"Luis",surname:"Soto",slug:"luis-soto",fullName:"Luis Soto"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"7746",title:"Lagoon Environments Around the World",subtitle:"A Scientific Perspective",isOpenForSubmission:!1,hash:"372053f50e624aa8f1e2269abb0a246d",slug:"lagoon-environments-around-the-world-a-scientific-perspective",bookSignature:"Andrew J. Manning",coverURL:"https://cdn.intechopen.com/books/images_new/7746.jpg",editedByType:"Edited by",editors:[{id:"23008",title:"Prof.",name:"Andrew James",surname:"Manning",slug:"andrew-james-manning",fullName:"Andrew James Manning"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}}],ofsBooks:[]},correction:{item:{id:"66063",slug:"corrigendum-to-introductory-chapter-historical-perspective-and-brief-overview-of-insulin",title:"Corrigendum to: Introductory Chapter: Historical Perspective and Brief Overview of Insulin",doi:null,correctionPDFUrl:"https://cdn.intechopen.com/pdfs/66063.pdf",downloadPdfUrl:"/chapter/pdf-download/66063",previewPdfUrl:"/chapter/pdf-preview/66063",totalDownloads:null,totalCrossrefCites:null,bibtexUrl:"/chapter/bibtex/66063",risUrl:"/chapter/ris/66063",chapter:{id:"63640",slug:"introductory-chapter-historical-perspective-and-brief-overview-of-insulin",signatures:"Gaffar Sarwar Zaman",dateSubmitted:"June 29th 2018",dateReviewed:"August 28th 2018",datePrePublished:"November 5th 2018",datePublished:"February 6th 2019",book:{id:"6675",title:"Ultimate Guide to Insulin",subtitle:null,fullTitle:"Ultimate Guide to Insulin",slug:"ultimate-guide-to-insulin",publishedDate:"February 6th 2019",bookSignature:"Gaffar Zaman",coverURL:"https://cdn.intechopen.com/books/images_new/6675.jpg",licenceType:"CC BY 3.0",editedByType:"Edited by",editors:[{id:"203015",title:"Dr.",name:"Gaffar",middleName:"Sarwar",surname:"Zaman",slug:"gaffar-zaman",fullName:"Gaffar Zaman"}],productType:{id:"1",title:"Edited Volume",chapterContentType:"chapter",authoredCaption:"Edited by"}},authors:[{id:"203015",title:"Dr.",name:"Gaffar",middleName:"Sarwar",surname:"Zaman",fullName:"Gaffar Zaman",slug:"gaffar-zaman",email:"gffrzaman@gmail.com",position:null,institution:null}]}},chapter:{id:"63640",slug:"introductory-chapter-historical-perspective-and-brief-overview-of-insulin",signatures:"Gaffar Sarwar Zaman",dateSubmitted:"June 29th 2018",dateReviewed:"August 28th 2018",datePrePublished:"November 5th 2018",datePublished:"February 6th 2019",book:{id:"6675",title:"Ultimate Guide to Insulin",subtitle:null,fullTitle:"Ultimate Guide to Insulin",slug:"ultimate-guide-to-insulin",publishedDate:"February 6th 2019",bookSignature:"Gaffar Zaman",coverURL:"https://cdn.intechopen.com/books/images_new/6675.jpg",licenceType:"CC BY 3.0",editedByType:"Edited by",editors:[{id:"203015",title:"Dr.",name:"Gaffar",middleName:"Sarwar",surname:"Zaman",slug:"gaffar-zaman",fullName:"Gaffar Zaman"}],productType:{id:"1",title:"Edited Volume",chapterContentType:"chapter",authoredCaption:"Edited by"}},authors:[{id:"203015",title:"Dr.",name:"Gaffar",middleName:"Sarwar",surname:"Zaman",fullName:"Gaffar Zaman",slug:"gaffar-zaman",email:"gffrzaman@gmail.com",position:null,institution:null}]},book:{id:"6675",title:"Ultimate Guide to Insulin",subtitle:null,fullTitle:"Ultimate Guide to Insulin",slug:"ultimate-guide-to-insulin",publishedDate:"February 6th 2019",bookSignature:"Gaffar Zaman",coverURL:"https://cdn.intechopen.com/books/images_new/6675.jpg",licenceType:"CC BY 3.0",editedByType:"Edited by",editors:[{id:"203015",title:"Dr.",name:"Gaffar",middleName:"Sarwar",surname:"Zaman",slug:"gaffar-zaman",fullName:"Gaffar Zaman"}],productType:{id:"1",title:"Edited Volume",chapterContentType:"chapter",authoredCaption:"Edited by"}}},ofsBook:{item:{type:"book",id:"11454",leadTitle:null,title:"Contemporary Issues in Land Use Planning",subtitle:null,reviewType:"peer-reviewed",abstract:"
\r\n\tRapid urbanization is one of the most important global change problems that land-use planners are facing worldwide. With increased population growth and urbanization, cities around the world are becoming more affluent and putting even greater pressures on various land uses. The greatest challenges include managing traffic and transportation, the urban sprawl of cities, and affordable housing in ways that can improve people’s health and social well-being in a city-based framework, keeping in mind qualitative principles of equity, public participation, and sustainability. The proposed book hopes to bring together leading scholars in the field of transportation or engineering, land use planning, affordable housing, and smart cities growth, to discuss contemporary land use issues and challenges facing cities in both developed and developing countries. The book is also intended to serve as important reference material for academics, land use planning professionals, and students around the globe seeking to understand contemporary land-use problems and innovative solutions.
",isbn:"978-1-80356-237-7",printIsbn:"978-1-80356-236-0",pdfIsbn:"978-1-80356-238-4",doi:null,price:0,priceEur:0,priceUsd:0,slug:null,numberOfPages:0,isOpenForSubmission:!1,isSalesforceBook:!1,hash:"e669f527567e12a187e61b3dbb18155f",bookSignature:"Dr. Seth Appiah-Opoku",publishedDate:null,coverURL:"https://cdn.intechopen.com/books/images_new/11454.jpg",keywords:"Land Use, Transportation Interaction, Smart City, Housing, City Typology, Urbanization, Urban Sprawl, Affordable Housing, Transit Management, Squatter Settlement, Manufactured Home, Sustainability",numberOfDownloads:null,numberOfWosCitations:0,numberOfCrossrefCitations:null,numberOfDimensionsCitations:null,numberOfTotalCitations:null,isAvailableForWebshopOrdering:!0,dateEndFirstStepPublish:"February 9th 2022",dateEndSecondStepPublish:"March 9th 2022",dateEndThirdStepPublish:"May 8th 2022",dateEndFourthStepPublish:"July 27th 2022",dateEndFifthStepPublish:"September 25th 2022",remainingDaysToSecondStep:"2 months",secondStepPassed:!0,currentStepOfPublishingProcess:4,editedByType:null,kuFlag:!1,biosketch:"Dr. Seth Appiah-Opoku is a member of the American Institute of Certified Planners. He also served on the Technical Advisory Team that advised the government of Ghana on the preparation of a 40-year development plan for the country.",coeditorOneBiosketch:null,coeditorTwoBiosketch:null,coeditorThreeBiosketch:null,coeditorFourBiosketch:null,coeditorFiveBiosketch:null,editors:[{id:"137858",title:"Dr.",name:"Seth",middleName:null,surname:"Appiah-Opoku",slug:"seth-appiah-opoku",fullName:"Seth Appiah-Opoku",profilePictureURL:"https://mts.intechopen.com/storage/users/137858/images/system/137858.jpg",biography:"Dr. Seth Appiah-Opoku is a Professor of Geography at the University of Alabama, Tuscaloosa, AL, USA. He teaches World Regional Geography, Regional Geography of Africa, Environmental Management, Land Use Regulation, Principles of Planning, Regional Planning and Analysis, and also the Ghana Summer Abroad course. He is a member of the American Institute of Certified Planners and the editor of three books - The Need for Indigenous Knowledge in Environmental Impact Assessment: The Case of Ghana (Edwin Mellen Press, NY, June 2005), Environmental Land Use Planning (IntechOpen, 2012), and International Development (IntechOpen, 2017). His research focuses on international development, urban planning, ecotourism, environmental impact assessment, and resource development. He serves on the Editorial Boards of the Journal of Environmental Impact Assessment Review and the Environment and Social Psychology Journal. He also served as the editor of the Journal of African Geographical Review from 2016 to 2018. He has published scholarly articles in several renowned journals including Environmental Management, Society and Natural Resources, Environmental Impact Assessment Review, Journal of Cultural Geography, and Plan Canada. He served on the Technical Advisory Team that advised the government of Ghana on the preparation of a 40-year development plan for the country.",institutionString:"University of Alabama, Tuscaloosa",position:null,outsideEditionCount:0,totalCites:0,totalAuthoredChapters:"1",totalChapterViews:"0",totalEditedBooks:"3",institution:{name:"University of Alabama, Tuscaloosa",institutionURL:null,country:{name:"United States of America"}}}],coeditorOne:null,coeditorTwo:null,coeditorThree:null,coeditorFour:null,coeditorFive:null,topics:[{id:"12",title:"Environmental Sciences",slug:"environmental-sciences"}],chapters:null,productType:{id:"1",title:"Edited Volume",chapterContentType:"chapter",authoredCaption:"Edited by"},personalPublishingAssistant:{id:"429339",firstName:"Jelena",lastName:"Vrdoljak",middleName:null,title:"Ms.",imageUrl:"https://mts.intechopen.com/storage/users/429339/images/20012_n.jpg",email:"jelena.v@intechopen.com",biography:"As an Author Service Manager, my responsibilities include monitoring and facilitating all publishing activities for authors and editors. From chapter submission and review to approval and revision, copyediting and design, until final publication, I work closely with authors and editors to ensure a simple and easy publishing process. I maintain constant and effective communication with authors, editors and reviewers, which allows for a level of personal support that enables contributors to fully commit and concentrate on the chapters they are writing, editing, or reviewing. I assist authors in the preparation of their full chapter submissions and track important deadlines and ensure they are met. I help to coordinate internal processes such as linguistic review, and monitor the technical aspects of the process. As an ASM I am also involved in the acquisition of editors. Whether that be identifying an exceptional author and proposing an editorship collaboration, or contacting researchers who would like the opportunity to work with IntechOpen, I establish and help manage author and editor acquisition and contact."}},relatedBooks:[{type:"book",id:"2358",title:"Environmental Land Use Planning",subtitle:null,isOpenForSubmission:!1,hash:"45c4591d49ed3ff918fe563a30203cb2",slug:"environmental-land-use-planning",bookSignature:"Seth Appiah-Opoku",coverURL:"https://cdn.intechopen.com/books/images_new/2358.jpg",editedByType:"Edited by",editors:[{id:"137858",title:"Dr.",name:"Seth",surname:"Appiah-Opoku",slug:"seth-appiah-opoku",fullName:"Seth Appiah-Opoku"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"5468",title:"International Development",subtitle:null,isOpenForSubmission:!1,hash:"df06431aaa20f810b8d187e0db9b807d",slug:"international-development",bookSignature:"Seth Appiah-Opoku",coverURL:"https://cdn.intechopen.com/books/images_new/5468.jpg",editedByType:"Edited by",editors:[{id:"137858",title:"Dr.",name:"Seth",surname:"Appiah-Opoku",slug:"seth-appiah-opoku",fullName:"Seth Appiah-Opoku"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"8013",title:"Land Use Change and Sustainability",subtitle:null,isOpenForSubmission:!1,hash:"6b3aee3b93d95ecd84c41753486f7a83",slug:"land-use-change-and-sustainability",bookSignature:"Seth Appiah-Opoku",coverURL:"https://cdn.intechopen.com/books/images_new/8013.jpg",editedByType:"Edited by",editors:[{id:"137858",title:"Dr.",name:"Seth",surname:"Appiah-Opoku",slug:"seth-appiah-opoku",fullName:"Seth Appiah-Opoku"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"1591",title:"Infrared Spectroscopy",subtitle:"Materials Science, Engineering and Technology",isOpenForSubmission:!1,hash:"99b4b7b71a8caeb693ed762b40b017f4",slug:"infrared-spectroscopy-materials-science-engineering-and-technology",bookSignature:"Theophile Theophanides",coverURL:"https://cdn.intechopen.com/books/images_new/1591.jpg",editedByType:"Edited by",editors:[{id:"37194",title:"Dr.",name:"Theophile",surname:"Theophanides",slug:"theophile-theophanides",fullName:"Theophile Theophanides"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"3161",title:"Frontiers in Guided Wave Optics and Optoelectronics",subtitle:null,isOpenForSubmission:!1,hash:"deb44e9c99f82bbce1083abea743146c",slug:"frontiers-in-guided-wave-optics-and-optoelectronics",bookSignature:"Bishnu Pal",coverURL:"https://cdn.intechopen.com/books/images_new/3161.jpg",editedByType:"Edited by",editors:[{id:"4782",title:"Prof.",name:"Bishnu",surname:"Pal",slug:"bishnu-pal",fullName:"Bishnu Pal"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"3092",title:"Anopheles mosquitoes",subtitle:"New insights into malaria vectors",isOpenForSubmission:!1,hash:"c9e622485316d5e296288bf24d2b0d64",slug:"anopheles-mosquitoes-new-insights-into-malaria-vectors",bookSignature:"Sylvie Manguin",coverURL:"https://cdn.intechopen.com/books/images_new/3092.jpg",editedByType:"Edited by",editors:[{id:"50017",title:"Prof.",name:"Sylvie",surname:"Manguin",slug:"sylvie-manguin",fullName:"Sylvie Manguin"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"371",title:"Abiotic Stress in Plants",subtitle:"Mechanisms and Adaptations",isOpenForSubmission:!1,hash:"588466f487e307619849d72389178a74",slug:"abiotic-stress-in-plants-mechanisms-and-adaptations",bookSignature:"Arun Shanker and B. Venkateswarlu",coverURL:"https://cdn.intechopen.com/books/images_new/371.jpg",editedByType:"Edited by",editors:[{id:"58592",title:"Dr.",name:"Arun",surname:"Shanker",slug:"arun-shanker",fullName:"Arun Shanker"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"72",title:"Ionic Liquids",subtitle:"Theory, Properties, New Approaches",isOpenForSubmission:!1,hash:"d94ffa3cfa10505e3b1d676d46fcd3f5",slug:"ionic-liquids-theory-properties-new-approaches",bookSignature:"Alexander Kokorin",coverURL:"https://cdn.intechopen.com/books/images_new/72.jpg",editedByType:"Edited by",editors:[{id:"19816",title:"Prof.",name:"Alexander",surname:"Kokorin",slug:"alexander-kokorin",fullName:"Alexander Kokorin"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"314",title:"Regenerative Medicine and Tissue Engineering",subtitle:"Cells and Biomaterials",isOpenForSubmission:!1,hash:"bb67e80e480c86bb8315458012d65686",slug:"regenerative-medicine-and-tissue-engineering-cells-and-biomaterials",bookSignature:"Daniel Eberli",coverURL:"https://cdn.intechopen.com/books/images_new/314.jpg",editedByType:"Edited by",editors:[{id:"6495",title:"Dr.",name:"Daniel",surname:"Eberli",slug:"daniel-eberli",fullName:"Daniel Eberli"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"57",title:"Physics and Applications of Graphene",subtitle:"Experiments",isOpenForSubmission:!1,hash:"0e6622a71cf4f02f45bfdd5691e1189a",slug:"physics-and-applications-of-graphene-experiments",bookSignature:"Sergey Mikhailov",coverURL:"https://cdn.intechopen.com/books/images_new/57.jpg",editedByType:"Edited by",editors:[{id:"16042",title:"Dr.",name:"Sergey",surname:"Mikhailov",slug:"sergey-mikhailov",fullName:"Sergey Mikhailov"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}}]},chapter:{item:{type:"chapter",id:"54915",title:"Pharmacogenetics of Psoriasis Treatment",doi:"10.5772/intechopen.68185",slug:"pharmacogenetics-of-psoriasis-treatment",body:'\nPsoriasis is a chronic systemic immune-mediated disorder of which etiopathogenesis is not yet fully understood, though there is evidence of genetic, immunologic and environmental factors playing a role in the development and the severity of the disease. The most common symptoms involve typical inflammatory skin lesions, but systemic inflammation may also be present [1, 2]. Psoriatic arthritis (PsA) is the most frequent systemic manifestation that can accompany the skin lesions and occurs in up to 40% of patients [3]. Systemic inflammation is also one of the reasons for the occurrence of many other comorbidities in patients with psoriasis, such as metabolic syndrome which includes obesity, type 2 diabetes, hypertension and dyslipidaemia, cardiovascular diseases, chronic inflammatory bowel disease and also cancer in some cases [4]. Furthermore, lower quality of life and psychological disorders are also more frequent among psoriasis patients as compared to general population [5, 6]. It is proven that lifestyle, including diet, smoking and alcohol consumption, influences the occurrence and the course of psoriasis and the comorbidities [7]. Elevated body mass index and visceral fat can also increase the probability of more progressive course of the disease [7].
\nThe severity of the disease is evaluated by the Psoriasis Area and Severity Index (PASI) score that takes into account the area of the affected skin, the thickness of skin plaques and the severity of inflammation. PASI score is calculated before the treatment strategy is chosen and is also used to monitor the treatment response. The response to treatment is considered to be good when PASI has decreased for at least 75% from the baseline score in 3–6 months after the first dose was administered (PASI75) [8]. The minimum treatment goal is usually set at PASI decreasing for at least 50% from the baseline score (PASI50). If PASI50 is not met, the treatment plan is usually changed [9]. However, PASI only evaluates the dermatological manifestations of the disease and neglects the psychological aspect. Therefore, Dermatology Life Quality Index (DLQI) is also assessed with a questionnaire to evaluate the impact of psoriasis on a patient’s physical, psychological and social well-being. The treatment goal is to achieve DLQI of zero to one after 2–4 months of treatment, but if this cannot be achieved, at least DLQI below five should be aimed for [9].
\nThe patient’s response to systemic psoriasis treatment cannot be predicted. Furthermore, the interindividual variability in the treatment response is quite extensive and adverse events occur frequently [6]. A study conducted 3 years ago discovered that approximately 75% of traditional systemic drugs are discontinued after 143 days of treatment (
Our genetic characteristics are encoded in our genome [13]. Interindividual differences between people are due to differences in less than 1% of genomic DNA sequence between unrelated individuals. Different variants of the same gene or genetic locus are called alleles. A variant is called a polymorphism when there are at least two alleles present in the population and the frequency of the less prevalent allele is more than 1%. A great majority of variants are due to single nucleotide polymorphisms (SNPs), which means that alleles differ only in one nucleotide. In addition to SNPs, deletions, insertions, duplications of nucleotides or longer sequences, microsatellites, changes in variable number of tandem nucleotide repeats (VNTR) and others may account for genetic polymorphism. Genetic polymorphisms may influence the process of transcription, translation and/or function of proteins. If variants change the binding site for different regulatory proteins, transcription may be altered. Amino acids are encoded as a sequence of three nucleotides, called codons. If a polymorphism changes a codon, another amino acid can be incorporated into a protein, which can change the characteristics and function of a protein. Insertion of only one nucleotide causes frame shift, which results in a premature stop codon and non-functional protein. The same happens after a stop codon is formed in the middle of an exon or when SNPs alter mRNA splicing. Gene deletions may cause depletion of proteins while, on the other hand, gene duplications lead to excess of the encoded protein [14].
\nGenetic polymorphisms may also influence expression and function of proteins involved in drug metabolism and transport as well as drug targets and their effector pathways. Because of that, genetic polymorphisms may influence patients’ response to drugs and the occurrence of adverse effects. Pharmacogenetics studies the associations between genetic polymorphisms and the course of disease and response to treatment. The aim of this chapter is to summarize the current knowledge on pharmacogenetic polymorphisms that may influence the response to systemic treatment in patients diagnosed with psoriasis. Such polymorphisms have been investigated as predictive biomarkers of treatment response that would support personalized treatment approaches in patients with psoriasis.
\nMethotrexate (MTX) is an immunomodulatory drug that is widely used in the treatment of psoriasis and PsA and is frequently the first-line systemic treatment for these two indications. It is usually orally administered once per week in doses of 7.5–30 mg [9]. Good response to treatment is achieved in approximately 50% of cases [8]. On the other hand, from 10 to 30% of patients have to discontinue the treatment because of adverse drug reactions. These include nausea, malaise, gastrointestinal ulcers, depression, infections, nephrotoxicity and most importantly hepatotoxicity and bone marrow suppression [9]. Adverse events are usually mild and can be eliminated by dose reduction. However, some adverse events may be severe or even life-threatening and cannot be predicted. This is the reason why patients treated with MTX are monitored very closely, and liver and kidney functions and blood status have to be checked regularly [8]. With the low doses used for psoriasis treatment, MTX plasma concentrations are too low to be measured, so drug monitoring cannot be used to predict the occurrence of adverse events. It has been therefore proposed that genetic polymorphisms should be investigated as predictors of response to treatment, either efficacy or toxicity [15–17].
\nMTX is a folate analogue and as such inhibits folic acid metabolism. Folic acid is a donor of methyl group in the process of deoxythymidylate synthesis that is required for DNA synthesis and cell proliferation as well as donor of methyl groups for methionine synthesis that directs the methyl group towards methylation reactions [18].
\nMTX enters the cell through the reduced folate carrier SLC19A1 and is activated by folylpoly- glutamate synthase that adds glutamate moieties to the molecule. MTX polyglutamate primarily inhibits dihydrofolate reductase (DHFR), thus inhibiting also thymidylate synthase (TYMS) reaction, which results in inhibition of DNA synthesis. Indirectly it inhibits also other enzymes of folate metabolic pathway and methylation reactions, such as methylentetrahydrofolate dehydrogenase (MTHFD1), methylentetrahydrofolate reductase (MTHFR), methionine synthase (MS) and methionine-synthase reductase (MSR) (Figure 1) [19].
\nSchematic view of MTX mechanism of action on folate and adenosine pathway. SLC19A1—reduced folate carrier, MTX—methotrexate, ABC—ABC transporters (ATP dependent), FPGS—folypolyglutamate synthase, GGH—gamma-glutamyl hydrolase, MTXglu—methotrexate polyglutamate, DHFR—dihydrofolate reductase, THF—tetrahydrofolate, MTHFD1—methylentetrahydrofolate dehydrogenase, SHMT1—serine hydroxymethyltransferase, MTHFR—methylentetrahydrofolate reductase, MTR—methionine synthase, MTRR—methionine synthase reductase, TYMS—thymidylate synthase, DHF—dihydrofolate, dTMP—deoxythimidine monophosphate, dUMP—deoxyuridine monophosphate, AICAR—5-aminoimidazole-4-carboxamide ribonucleotide, ATIC—AICAR transformylase, THF—tetrahydrofolate, FAICAR—5-formamidoimidazole-4-carboxamide ribotide, ITP—inosine triphosphate, IMP—inosine monophosphate, AMP—adenosine monophosphate, AS—adenylosuccinate, AMPD1—AMP deaminase, ITPA—inosine triphosphatase, ADA—adenosine deaminase.
MTX is also adenosine pathway inhibitor. It inhibits the enzyme 5-aminoimidazole-4- carboxamide ribonucleotide (AICAR) transformylase (ATIC), which results in elevated levels of AICAR. AICAR inhibits adenosine deaminase (ADA) and this consequently leads to higher intercellular concentrations of adenosine. Adenosine is released into circulation, and its binding to adenosine receptors on the target cells contributes significantly to the anti-inflammatory effects of MTX (Figure 1) [18].
\nCells are protected from toxic effects of MTX by transmembrane transporters ABC (ATP-binding cassette), especially ABCB1, ABCC2 and ABCG2. They are ATP dependent, and they actively pump MTX out of the cell. On the other hand, solute carriers (SLC), such as SLC19A1 and SLCO1B1, facilitate MTX transport in the direction of the concentration gradient (Figure 1) [19].
\nMost of the genes coding for the enzymes in folate and adenosine pathway as well as for folate and MTX transporters are polymorphic. As genetic polymorphisms may lead to differences in expression and activity of enzymes, polymorphisms in the genes coding for the above mentioned proteins (transporters and enzymes) contribute to interindividual variability in therapeutic response and toxicity profile of drugs among patients. Several of the above mentioned polymorphic genes were already studied in relation to MTX treatment response in rheumatoid arthritis (RA) and cancer, but studies regarding psoriasis are scarce. Studies pointing out positive associations between polymorphisms and response to MTX in psoriasis and PsA are listed in Table 1.
\nGenes | \nVariants | \nPredicted effect | \nReference | |
---|---|---|---|---|
rs34743033 28-bp repeat | \n0.048 | \nCarriers of the 3R allele susceptible to poor response to MTX | \n[20] | |
rs35592 c.1219-176T>C | \n0.008 | \nHomozygotes for the major allele respond better to MTX | \n[25] | |
rs2238476 c.3391-1960G>A | \n0.02 | |||
rs28364006 c.4009A>G | \n0.02 | |||
rs13120400 c.1194+928A>G | \n0.03 | \nMinor allele associated with better response to MTX | \n[25] | |
rs17731538 c.204-1592C>T | \n0.007 | \nMajor allele associated with better response to MTX | ||
DHFR | \nrs1232027 g.80619201G>A | \n0.02 | \nMinor allele associated with better response to MTX | \n[15] |
rs1051266 c.80A>G | \n0.025 | \nA allele associated with occurrence of adverse events | \n[20] | |
0.03 | \nA allele associated with toxicity | \n[25] | ||
rs1801131 c.1298A>C Glu429Ala | \n0.042 | \nC allele associated with lower risk of hepatotoxicity | \n[20] | |
rs1801133 c.677C>T Ala222Val | \n0.04 | \nHomozygotes for the minor allele more susceptible to liver toxicity | \n[15] | |
rs34489327 nt.1494del6 | \n0.015 | \nPolymorphism increases the risk for hepatotoxicity | \n[20] | |
rs34743033 28-bp repeat | \n0.0025 | \n3R allele increased risk for adverse events in patients without folic acid supplementation | ||
rs2372536 c.347C>G | \n0.038 | \nG allele associated with increased risk for MTX discontinuation due to adverse events | \n[20] | |
0.01 | \nHomozygotes for the major allele more susceptible to MTX toxicity | \n[22] | ||
rs4672768 c.1660-135G>A | \n0.02 | \nHomozygotes for the major allele more susceptible to MTX toxicity | \n[22] | |
rs2238476 c.3391-1960G>A | \n0.01 | \nHomozygotes for the major allele more susceptible to toxicity | \n[25] | |
rs3784864 c.616-1641G>A | \n0.03 | \nCarriers of at least one major allele more susceptible to toxicity | ||
rs246240 c.616-7942A>G | \n0.0006 | \nHomozygotes for the major allele more susceptible to toxicity | ||
rs3784862 c.615+413G>A | \n0.002 | \nHomozygotes for the major allele more susceptible to toxicity | ||
rs1967120 c.489+409G>A | \n0.01 | \nCarriers of at least one major allele more susceptible to toxicity | ||
rs11075291 c.49-3198G>A | \n0.008 | \nCarriers of at least one major allele more susceptible to toxicity | ||
rs5760410 g.24815406G>A | \n0.03 | \nHomozygotes for the major allele more susceptible to toxicity | \n[25] |
Genetic polymorphisms in folate and adenosine pathway and MTX transporters associated with MTX treatment outcome in patients with psoriasis or psoriatic arthritis.
The direct target of MTX within folate pathway is DHFR that converts dihydrofolic acid into tetrahydrofolic acid (Figure 1). It is therefore surprising that the impact of
TYMS is one of the key enzymes providing deoxythymidylate for DNA synthesis, thus enabling cell proliferation. Two common functional polymorphisms in
MTHFR is the central enzyme in folate pathway as it is responsible for the conversion of 5,10-methylentetrahydrofolate, which is a substrate for TYMS, to 5-methyltetrahydrofolate, which is a substrate for homocysteine remethylation (Figure 1). The most studied polymorphisms in
Polymorphisms in
MTX directly inhibits ATIC, the key enzyme in the adenosine pathway (Figure 1). The consequent accumulation of AICAR indirectly leads to accumulation of adenosine in circulation, which acts as an anti-inflammatory factor. The most studied genetic polymorphism in
ADA is the enzyme inhibited because of accumulation of AICAR following MTX treatment. A functional polymorphism
No other polymorphic genes in adenosine metabolic pathway were investigated in psoriasis patients. However, in Slovenian patients with RA, several other genes in adenosine pathway were studied.
The anti-inflammatory effect of adenosine is directly related to its binding to the adenosine receptors (ADORA). Only one pharmacogenetic study investigated adenosine receptors so far and included 374 patients with chronic plaque psoriasis, who had been treated with MTX for at least 3 months. No significant association was detected between polymorphisms in
Polymorphisms in transporters may influence intracellular MTX levels and, thus, also influence therapeutic effect. SLC19A1 (RFC1) is a reduced folate carrier, which facilitates the MTX transport into the cell. Many studies investigated the most common functional polymorphism in
On the other hand, polymorphisms in genes coding for the efflux ABC transporters showed association with efficacy as well as toxicity. In the study by Warren et al., two polymorphic transporter genes were investigated in psoriasis patients:
Cyclosporine is an orally administered systemic immunosuppressive drug that may be used to treat the most resistant forms of psoriasis, especially the plaque-type diseases [9]. It inhibits the first phase of T-lymphocyte activation, thus decreasing the levels of inflammatory cytokines, among them interleukin-2 (IL2) and interferon- gamma (IFNG) [26]. It is usually administered in doses of 2.5–5 mg/kg of body weight/day [9]. The current knowledge on cyclosporine pharmacogenetics comes from studies in recipients of solid organ transplants. Bioavailability and clearance of the drug are influenced by polymorphic P-glycoprotein (ABCB1) in gastrointestinal tract and CYP3A4 and CYP3A5 in the liver, suggesting that these polymorphisms could also influence the response to cyclosporine treatment in psoriatic patients [27, 28]. There was only one pharmacogenetic study performed on psoriasis patients treated with cyclosporine, and it focused only on
Genes | \nVariants | \nPredicted effect | \nReference | |
---|---|---|---|---|
ABCB1 | \nrs1045642 c.3435C>T p.Ile1145= | \n0.0075 | \nMinor T allele associated with poor response to cyclosporine | \n[29] |
Genetic polymorphism associated with response to cyclosporine treatment in patients with psoriasis.
Acitretin is a vitamin A derivative that belongs to the second-generation retinoids [30]. It reduces proliferation of epidermal keratinocytes and promotes their differentiation. It is also used as an anti-inflammatory agent. It is administered orally in doses of 0.5–0.8 mg/kg daily. Usually, it is used in combination with topical treatment as well as phototherapy [9]. Studies pointing out positive associations between polymorphisms and response to acitretin in psoriasis are listed in Table 3. The most widely studied polymorphisms lie in the gene coding for vascular epidermal growth factor (
Genes | \nVariants | \nPredicted effect | \nReference | |
---|---|---|---|---|
rs833061 c.-958C>T | \n0.04 | \nTT genotype increased the risk of poor response to acitretin | \n[31] | |
0.01 | \nTC genotype increased the chance of favourable response to acitretin | \n|||
14 bp DEL | \n0.008 | \nDEL allele associated with better response to acitretin | \n[34] | |
0.05 | \nDEL/DEL genotype is associated with better response to acitretin |
Genetic polymorphisms associated with response to acitretin treatment in patients with psoriasis.
Another study performed on a group of Italian patients found an association between the
Biologic drugs specifically bind to their target, usually inflammation mediators or their receptors, and inhibit their action, which results in anti-inflammatory effect. Biologics used in treatment of psoriasis mainly inhibit tumour necrosis factor alpha (TNFα) and several interleukins (IL)—IL17, IL12 and IL23. Among the biologics used for psoriasis treatment, infliximab, adalimumab, etanercept are TNFα inhibitors, while ustekinumab is an IL12/23 inhibitor and secukinumab is IL17 inhibitor [36, 37].
\nBiologic drugs are relatively safe and well tolerated. Adverse events occur only in appro- ximately 15% of patients, but the symptoms are usually not severe and are not the reason for discontinuation [38]. The most common adverse events are injection-site reaction (pain, erythema, itching and haemorrhage) and different infections, mostly of upper respiratory tract [9]. However, according to a study performed by Levin et al., 48% of patients discontinue treatment due to reasons not related to toxicity [8].
\nA study conducted in 2015 that included 4309 patients treated with different biologics for 12 months showed that patients experienced dose escalations and discontinuations, restarting the same biologic or switching to a different one. Approximately one-third of patients had their doses increased until month 6 and 39% until month 12 of treatment. On the other hand, half of these patients also discontinued the biologic drug or reduced the dose [6]. This indicates that many patients do not achieve sufficient response or lose an initially favourable response over time. Pharmacogenetic studies have investigated several polymorphisms in genes coding for the targets of biologic drugs and their signalling pathways regarding their contribution to interpatient and intrapatient variability in treatment response to biologics in patients with RA, PsA, Chron’s disease and spondyloarthritis (SA). However, such studies have been rarely performed exclusively in psoriasis patients [39].
\nThe most widely used biologic drugs for systemic psoriasis treatment are TNFα blockers. It is therefore not surprising that the majority of pharmacogenetic studies focused on polymorphisms in the gene coding for TNFα (
Genes | \nVariants | \nPredicted effect | \nReference | |
---|---|---|---|---|
rs1799724 c.-857C>T | \n0.002 | \nC allele associated with better response to etanercept | \n[49] | |
0.004 | \nPatients with CT/TT genotypes showed greater improvements in PASI score | \n[47] | ||
rs361525 c.-238A>G | \n0.049 | \nPatients with GG genotype achieved PASI75 more frequently after 6 months of anti-TNFα therapy | \n[47] | |
0.03 | \nG allele associated with better response to etanercept | \n[48] | ||
rs1799964 c.-1031T>C | \n0.041 | \nPatients with TT genotype demonstrated superior improvements in PASI after 6 months of therapy | \n[47] | |
rs80267959 c.186+123G>A | \n0.0136 | \nG allele favours better response to etanercept in PsA patients | \n[63] | |
rs1800629 c.-308G>A | \n0.001 | \nGG genotype associated with better response to etanercept | \n[48] | |
rs1061622 c.676T>G p.Met196Arg | \n0.001 | \nT allele associated with better response to etanercept | \n[49] | |
0.05 | \nG allele associated with poor response | \n[52] | ||
rs610604 c.987-152G>T | \n0.05 | \nG allele associated with better response to anti-TNFα therapy | \n[53] | |
0.007 | \nT allele associated with better response to etanercept | \n[54] | ||
rs20575 c.626G>C p.Arg209Thr | \n0.048 | \nCC genotype associated with better response to infliximab in PsA | \n[66] | |
rs767455 c.36A>G p.Pro12= | \n0.04 | \nAA genotype associated with better response to infliximab in PsA | \n||
rs11209026 c.1142G>A p.Arg381Gln | \n0.006 | \nPatients with GG genotype achieved more frequently PASI 90 at 6 months | \n[47] | |
rs1800795 c.-237C>G | \n<0.05 | \nCarriers of t C allele respond better to therapy | \n[55] | |
rs763780 c.482T>C p.His161Arg | \n0.0044 | \nTC genotype associated with no response to adalimumab at 6 months | \n[56] | |
0.023 | \nTC genotype associated with better response to infliximab at 3 months | \n|||
0.020 | \nTC genotype associated with better response to infliximab at 6 months | \n|||
rs4819554 c.-947G>A | \n0.03 | \nAA genotype associated with better response at12 weeks | \n[67] | |
rs10484554 g.2609009C>T | \n0.007 | \nC allele associated with better response to adalimumab | \n[54] | |
rs13190932 c.220C>T p.Arg74Trp | \n0.041 | \nG allele associated with better response to infliximab | \n||
rs9260313 g.1428637T>C | \n0.05 | \nTT genotype associated with better response to adalimumab | \n||
rs1801274 c.497A>G p.His131Arg | \n0.03 | \nPatients homozygous for high-affinity allele had a higher chance of achieving PASI75 after 3 months of therapy | \n[57] | |
0.034 | \nPsA patients with high-affinity genotype respond better to anti-TNFα drugs (etanercept) after 6 months of therapy | \n[64] | ||
rs396991 c.841T>C p.Val158Phe | \n0.02 | \nPatients homozygous for high-affinity allele had a higher chance of achieving PASI75 after 3 months of therapy | \n[57] | |
0.018 | \nT allele associated with better response to etanercept | \n[58] | ||
rs3794271 c.50+1078G>A | \n0.0031 | \nAA genotype associated with better response to etanercept | \n[59] | |
0.00034 | \nA gender-specific (males) association between G allele and poor response found in PsA patients | \n[65] | ||
rs6427528 c.*1738A>G | \n0.025 | \nGA genotype associated with better response to etanercept | \n[60] | |
rs6701290 c.84-10630G>A | \n<0.05 | \nAssociated with anti-TNFα drug response in a GWAS | \n[62] | |
rs3784240 c.475+782C>T | \n\n | \n | \n | |
rs2390256 c.*2687G>A | \n\n | \n | \n | |
rs2219538 c.77+2269G>A | \n\n | \n | ||
rs10515637 c.2507-1067T>C | \n\n | \n | \n | |
rs10823825 c.2290-538T>C | \n\n | \n | \n | |
rs1927159 c.704-13438A>C | \n\n | \n | \n | |
rs7820834 g.129238197T>C | \n\n | \n | \n | |
rs553668 c.450+33966C>T | \n\n | \n | \n | |
rs4867965 c.88+96839A>C | \n\n | \n | \n | |
rs11209026 c.1142G>A p.Arg381Gln | \n0.005 | \nAG genotype associated with development of paradoxical psoriasiform reactions | \n[61] | |
rs10782001 c.1361+720G>A | \n0.028 | \nGG genotype associated with development of paradoxical psoriasiform reactions | ||
rs3087243 c.*1421G>A | \n0.012 | \nAG/GG genotype associated with development of paradoxical psoriasiform reactions | ||
rs651630 c.1706-272C>T | \n0.011 | \nTT genotype associated with development of paradoxical psoriasiform reactions | ||
rs1800453 c.1307A>G | \n0.018 | \nAG genotype associated with development of paradoxical psoriasiform reactions |
Genetic polymorphisms associated with response to anti-TNFα therapy in patients with psoriasis or psoriatic arthritis.
The most frequently investigated candidate gene is
Other
Researchers expanded their interests also to polymorphisms in other genes in TNFα pathways. A study performed on 80 Greek patients with psoriasis investigated polymorphisms in
Polymorphisms within gene coding for tumour necrosis factor alpha-induced protein 3 (
Furthermore, polymorphisms in genes encoding several interleukins and their receptors were investigated in psoriasis patients treated with anti-TNFα drugs. A study that included 109 psoriasis patients investigated polymorphisms in
Genes for Fc gamma receptors were also investigated for their association with response of psoriasis patients to anti-TNFα drugs. Patients homozygous for high-affinity alleles of two variants
A study performed by Cabaleiro et al. revealed an association between certain polymorphisms and occurrence of paradoxical psoriasiform reactions after treatment with anti-TNFα therapy. Polymorphisms in five genes:
Another approach to identify novel loci and SNPs associated with response to anti-TNFα drugs included genome-wide association study (GWAS) approach. A small GWAS study was recently performed that included 65 psoriasis patients prospectively followed for 12 weeks. This study identified 10 SNPs in 10 different genes that could be associated with drug response: cadherin-related 23 (
Several studies have also investigated association of genetic polymorphisms with anti-TNFα treatment outcome in PsA cohorts. A study investigating the association of an intronic polymorphism at the position c.+489 of
Ustekinumab is a human monoclonal antibody directed against interleukins IL12 and IL23. Studies of polymorphisms affecting patients’ response to these inhibitors are scarce, but some of them, listed in Table 5, pointed out positive associations. A cohort of 51 patients with psoriasis treated with ustekinumab was tested for three polymorphisms, including the
Genes | \nVariants | \nPredicted effect | \nReference | |
---|---|---|---|---|
rs763780 c.482T>C p.His161Arg | \n0.022 | \nTC genotype associated with no response at 3 months | \n[56] | |
0.016 | \nTC genotype associated with no response at 6 months | |||
rs3213094 c.89-432G>A | \n0.017 | \nCT genotype associated with favourable response | \n[60] | |
rs610604 c.987-152G>T | \n0.031 | \nGG genotype associated with poor response | ||
Cw6POS/NEG | \n0.008 | \nCw6POS patients respond better and faster | \n[68] | |
0.035 | \nCw6POS patients respond better | \n[69] | ||
rs1061622 c.676T>G p.Met196Arg | \n0.05 | \nG allele associated with poor response | \n[52] | |
rs151823 c.-454-1169A>C | \n0.026 | \nCC genotype associated with better response | \n[54] | |
rs26653 c.380G>C p.Arg127Pro | \n0.016 | \nGG genotype associated with better response |
Genetic polymorphisms associated with response to ustekinumab in patients with psoriasis.
Another study found association between the
Large heterogeneity in patients’ response to therapy calls for new molecular predictors of treatment response. We have searched the current literature to compile a comprehensive review of today’s knowledge on genetic variants that may influence the outcome of psoriasis systemic treatment. A rather small number of studies were performed so far, and, although some of the results are encouraging, even larger number of studies shows inconsistent or even conflicting results. The investigated patient cohorts were with a few exceptions rather small and the number of evaluated polymorphisms limited. The future studies should expand the range of polymorphisms investigated by either looking into other pathways besides the ones directly involved in drug mechanisms, such as metabolism and transport, though they certainly are important in treatment response. Great interindividual variability in treatment outcome among patients could also be associated with heterogeneous pathology. Not all of the patients have the same pathogenesis, although they present with similar symptoms. Genetic defects in various pathways could be causative of the disease or support disease occurrence, and these defects in so-called susceptibility genes should also be checked regarding their influence on treatment outcome. The heterogeneity in pathogenesis could also be the reason for inconsistency in pharmacogenetic studies conducted so far. The hypothesis-free approach of the GWAS studies could help to overcome these obstacles and help to elucidate genetic factors associated with both disease pathways and treatment responses; however, such studies should include large number of well-characterized patients. Furthermore, the identified predictors of the course of the disease and of the treatment response should be validated in independent patient samples.
\nSuch validated pharmacogenetic biomarkers would enable us to characterize patients with psoriasis by their genetic characteristics and not just their phenotype and would allow for a more targeted approach to pharmacotherapy. The patients could be stratified according to their genetic defects affecting the molecular mechanisms of the disease in combination with genetic defects in pathways of drug metabolism and transport as well as in drug targets and effector pathways. Pharmacogenetic factors should also be combined with clinical data to find the most suitable way of stratifying patients into groups eligible for certain treatment strategies. If a physician would be able to predict patient’s response based on pharmacogenetic polymorphisms, problems of inefficacy and toxicity could be overcome by choosing the right drug and dose for a particular patient. This would also help to lower the cost of the treatment and, what is more important, relieve some of the patient’s psychological burden, which is often overlooked in psoriasis. Methods for genotyping are fast, reliable, relatively cheap and suitable for use in diagnostic laboratories. Despite the costs that would be spent on implementation of new genetic analysis methods into everyday clinical practice, pharmacogenetics-based personalized treatment approach would probably lower the expenses of psoriasis treatment due to more rational pharmacotherapy.
\nPersonalized medicine is emerging as the innovative approach also in psoriasis treatment. A general belief that every drug can help every patient is getting obsolete. However, to be able to properly tailor the patient’s treatment, consistent biomarkers of the treatment outcome must be identified and validated. In psoriasis treatment, the search for such biomarkers is still in its beginnings. In this chapter, we summarized the current knowledge on genetic predictors of response to MTX, cyclosporine, acitretin and biologic drugs. Several studies have already identified some of the genetic variants associated with response to a particular drug, but none of the genetic polymorphisms within these genes were recognized as specific enough to be used in clinical practice so far. However, some promising candidates for predictors of treatment response were identified that could be used in personalized treatment of psoriasis patients if validated in further studies.
\nPeperite is a volcaniclastic rock related to
The formation of peperite is a complex process and depends, in general, on the magma and host sediment properties, their mass ratio and total volume of pore water heated during their contact and mingling. For magma, the most relevant properties are composition, the content of volatiles and rheology, and for the host sediment that is texture and water-saturation. An important stage in the process of peperite formation is magma disintegration that can be brittle or ductile and attained by quenching, hydromagmatic explosions, surface tension effects, mechanical stress related to the movement of magma and density contrast to the sediment, and magma-sediment shearing. The contact of magma and wet sediment causes heating and expansion of pore waters, and the resulting disruption of coherence and sometimes fluidisation and shear liquefaction of the host sediment facilitate dispersion of clasts derived from magma away from the site of formation. The intricate processes of intermixing finally result in the formation of peperite [4, 10, 11, 12, 13, 14].
Two textural types of peperite have been recognised on the basis of shape of clasts derived from magma. Blocky peperite consists of sharply angular, blocky or platy clasts while in globular or fluidal peperite lensoidal, lobate, ameboid or bulbous clasts occur [5]. The term peperitic hyaloclastite refers to a peperitic rock in which magma fragmentation is largely the result of quenching, mechanical stress, or pore-water steam explosions [4, 12].
Several detailed studies of peperite occurrence and formation have been carried out in the system of Pannonian basins, in particular, in the Tokaj Mountains [15] and Western Hungary at Hajagos-hegy, Kissomlyó and Ság-hegy [9, 16, 17]. Subaqueous Miocene rhyolitic dome-cryptodome complex outcropping at Pálháza, the Tokaj Mountains, is surrounded by a carapace of hyaloclastites, hyaloclastite breccia, and globular and blocky peperite. Closely packed peperite zone with jigsaw-fit juvenile clasts formed next to a rhyodacitic body, and toward the boundary with the host sediment, a transition into the clast-rotated and clast dispersed zones of peperite has been recognised [17]. In the volcanic conduits, vents and crater lakes of phreatomagmatic volcanoes in Mio/Pliocene volcanic fields of Western Hungary globular and blocky peperite occur together regardless of the grain-size and texture of host sediment [15]. The study supports conclusions that the formation of different peperite textures depends on several factors, e.g., break-down of vapour films at the magma/wet-sediment interface, viscosity of magma and/or magma flux rate, a change in temperature, microlite crystallinity and gas content of magma, thermal properties of the host sediment and steam explosions [18, 19, 20, 21, 22].
The alteration of peperite is common and may begin contemporaneously to its formation owing to the release of deuteric magmatic fluids and volatiles, transfer of heat from magma or lava to the host sediment and heating of pore-waters therein. Large magma intrusions can cause contact metamorphism along the margins and initiate or modify fluid circulation on a several-kilometre-scale that may last a long period of time after the peperite formed [23]. Lavas undergo more rapid cooling, and effective circulation of heated pore-waters can be attained only locally along the contacts with the wet sediment until thermal gradients exist. Most often, the formation of secondary minerals such as carbonates, Fe-oxides and silica along the contacts of juvenile clasts has been reported [23, 24, 25, 26, 27].
The Oligocene Smrekovec Volcanic Complex (Figures 1 and 2) located in the south-westernmost extending of the Tertiary system of Pannonian basins, is a remnant of a submarine stratovolcano. Prior to erosion, and tectonic dissection and displacement along the Periadriatic Line, the stratovolcano extended in an area of over 1000 km2. Similar large submarine volcanoes have been encountered in modern and ancient environments worldwide (e.g., [30, 31, 32]), and also, within the Carpathian-Pannonian region [33, 34, 35].
Simplified geological map of northern Slovenia after [
The study area (northern Smrekovec Volcanic Complex) after [
The stratovolcano is composed of a succession of lavas and shallow intrusive bodies, and autoclastic, pyroclastic, resedimented volcaniclastic and mixed siliciclastic-volcaniclastic deposits. Lithofacies associations change from proximal, medial and distal zones over a distance of 0-2 km, 2-5 km and 5-20 km, respectively. The proximal zone is dominated by lavas and autoclastic deposits, and in the medial-zone pyroclastic and syn-eruptive resedimented volcaniclastic deposits become abundant. The distal zone is dominated by fine-grained pyroclastic, syn-eruptive resedimented volcaniclastic and siliciclastic deposits.
Peperites are the most abundant in medial-zone lithofacies associations. The mingling lavas range in composition from andesitic to rhyodacitic and the host sediments are mixed siliciclastic-volcaniclastic silts and calcareous muds or volcaniclastic deposits of various texture and grain size, i.e., fine- and coarse-grained tuffs, lapilli tuffs, volcaniclastic breccias [36]. Blocky and fluidal peperite and peperitic hyaloclastite are common in occurrence although their formation has not been related to the texture, grain size or porosity of the host sediment.
The stratovolcano-hosted hydrothermal system with convective-advective flow regime developed, and as a result, alteration minerals formed, the most widespread assemblage being laumontite, chlorite, ordered mixed layer chlorite-smectite, quartz and albite. Despite of complex alteration that affected lithofacies associations, peperites very often contain authigenic minerals with typically higher temperature stability ranges than those in the adjacent underlying or overlying volcaniclastic deposits [37, 38]. Their formation must have occurred contemporaneously to the development of the host rock itself owing to thermal gradients originating from the parent lava or shallow intrusive body and geochemical gradients related local circulation of heated pore waters and deuteric fluids.
As the Smrekovec Volcanic Complex is a remnant of an ancient submarine composite stratovolcano the processes of alteration of peperites described herein could be recognised in, and applied to, similar environments worldwide.
The sampling was performed in the entire area of the Smrekovec Volcanic Complex, although particularly detailed study has been carried out in two sections Krnes, and Smrekovec G34 (Figure 2). Lithofacies was determined by field observation, and chemical, mineralogical and petrographic analysis. Over 900 thin sections have been inspected in detail.
Alteration minerals were analysed by X-ray diffraction (XRD) techniques in altogether 260 samples. Zeolites and related calcium aluminosilicate minerals were determined in whole-rock powdered samples. Clay minerals were analysed in oriented samples using slurries (<2 μm) dispersed on glass slides and undergoing standard procedures including air-drying and solvation in ethylene glycol. The XRD analysis was performed using a Philips diffractometer PW 3719 and a goniometer PW 1820, owned by the Department of Geology, Faculty of Natural Sciences and Technology, University of Ljubljana. Machine settings for all analysed samples were as follows: generator operated at 40 kV and 30 mA using CuKα radiation (wavelengths Kα1 = 1.54056 Å and Kα2 = 1.54439 Å), Ni filter, with automatic divergence slit and monochromator on. Scanning rate was 2°2
Detailed mineral studies were performed on 9 polished thin sections using a scanning electron microscope (SEM) Jeol JSM-6490 equipped with an energy dispersive spectrometer (EDS) INCA Oxford 250, and located at Geological Survey of Slovenia. Elemental analyses were performed in thin sections having a thickness of 40 μm and uncovered polished upper surface, at accelerating voltage of 15 kV using a defocused electron beam of 20 μm in diameter, with a current of 10 nA and a counting time of 20 s. Synthetic and natural standards were used for calibration.
Chemical analysis of 150 bulk-rock samples of lavas and shallow intrusive bodies was performed in AcmeLabs, Vancouver, Canada, and Actlabs Activation Laboratories Ltd. Ontario, Canada. Major and trace elements were determined by a combination of X-ray fluorescence (XRF), inductively coupled plasma source (ICP) and mass spectroscopy (MS) analytical techniques.
In northern Slovenia, there are four large tectonic units: the Eastern Alps, the Southern Alps, the Outer Dinarides and the south-westernmost extending of the Tertiary system of Pannonian basins [28, 29] with the Smrekovec Volcanic Complex (Figure 1). The most outstanding geological structure is the Periadriatic Line (PAL), a complex regional fault system which represents in palinspastic reconstructions a shear zone developed by Late Cretaceous to Paleogene subduction of the European plate below the African plate [39, 40]. In the Eocene (~45 Ma) the subduction transformed into collision although the convergence continued during the Oligocene and resulted in break off of the southeast-dipping European slab beneath the Alps that generated magmatism along the PAL [41, 42].
The related Oligocene (28-22 Ma) volcanic activity occurred in the Smrekovec Basin (Figure 3) that had been subsided within the Permian and Triassic clastic and carbonate successions [43]. Tertiary sedimentation began in Late Eocene in fluviatile, limnic and shallow-marine depositional environment and changed to outer neritic and bathyal during the Oligocene time [29, 43]. In a middle bathyal environment characterised by sedimentation of organic-rich clayey silts [43], simultaneous volcanic activity created a composite stratovolcano. Magmas had calc-alkaline and medium-K affinity and formed a suite ranging in composition from basaltic andesite to dacite [44, 45, 46]. Volcanic activity had entirely submarine character and after its cessation, the Upper Oligocene to Early Miocene (Egerian) sedimentation continued with fossiliferous marine clayey silt [29]. The stratovolcano hosted hydrothermal system with a deep igneous source and convective-advective flow of hydrothermal fluids (Figure 3).
A conceptual model of the Smrekovec Basin with the stratovolcano and volcanic-hydrothermal system with a deep igneous source of heat and convective-advective flow regime. Hydrothermal fluids originating from heated and chemically modified surface and marine waters ascended through fracture systems and when reached the stratovolcano edifice they outflowed laterally and downward, preferentially through high-permeability layers. High-permeability layers underwent more extensive alteration and the authigenic minerals (e.g., laumontite, prehnite) have higher temperature stability ranges than those in the adjacent underlying or overlying low-permeability layers (e.g., clinoptilolite, heulandite, analcime).
Late Miocene tectonic activity along the Periadriatic Line dissected the stratovolcano edifice and displaced its northern sector in the south-eastern direction on a 100 km scale [29]. The remaining Smrekovec Volcanic Complex probably encompasses about one quarter of the original stratovolcano edifice [36], and scarce outcroppings of volcanic rocks occurring north of the Šoštanj fault (Figure 1) are the assumed displaced remnants [47]. South of the Šoštanj fault Tertiary volcanic deposits occur in the Celje Basin, and together with the Smrekovec Volcanic Complex they are united in a lithostratigraphic unit termed the Smrekovec Series [29].
The succession of lavas, shallow intrusive bodies, and autoclastic, pyroclastic, syn-eruptive resedimented volcaniclastic and mixed siliciclastic-volcaniclastic rocks is over 2500 m thick, and at least 1000 m of the overlying deposits have been eroded already. In the northwest of the complex, the oldest proximal zone lithofacies associations overlie basal fossiliferous siltstone, limestone and calcarenite. As the strata, in general, verge toward the southeast, the oldest lavas can be traced over a distance of about 2 km to the east and south although their thickness changes (Figure 4). Younger, medial-zone lithofacies associations occur in the east and south and their development is typically complex (Figures 5 and 6). The Kramarica Sill is the largest shallow intrusive body in the Smrekovec Volcanic Complex. Its emplacement was related to the formation of a new vent along the Periadriatic Line, some 6 km east of the older one located northwest of Travnik (Figure 2).
The sections Presečnik (left) and Javorec (right) situated in the proximal zone show the change in thickness of lithofacies within a distance of 1.5-2 km toward the southeast.
Lithofacies and the principal alteration minerals in the medial-zone section Krnes.
Lithofacies and the principal alteration minerals in the medial-zone section Smrekovec G34.
A detailed study of lithofacies and alteration has been carried out in two sections composed of medial-zone lithofacies associations, namely Krnes and Smrekovec G34, attaining 400 m and 470 m, respectively (Figures 5 and 6). The section Krnes consists of complexly alternating pyroclastic, autoclastic and syn-eruptive resedimented volcaniclastic deposits with only two thicker lava flows attaining some 25 m and 70 m. Pyroclastic deposits are dominated by fine-grained cross-bedded and horizontally bedded tuffs related to pyroclastic density currents [36], similar to the occurrences described by [48, 49, 50, 51]. Pyroclastic flow deposits [36] are less abundant and commonly consist of basal massive lapilli tuff and the overlaying stratified coarse- and fine-grained tuff. Syn-eruptive resedimented deposits are abundant and comprise volcaniclastic debris-flow deposits and volcaniclastic turbidity flow deposits. Hyaloclastites and resedimented hyaloclastites are subordinate in occurrence but still relatively abundant. Siliciclastic silts are very rare and occur in thin, up to some dm thick stratified units. There are nine peperite deposits occurring at the base and along terminal parts of smaller lava flows.
The section Smrekovec G34 begins in the Kramarica Sill (Figure 6) and comprises three thicker lava flows attaining some 35 m, 90 m and over 50 m, respectively. Based on the occurrence of yugawaralite [37, 52] and with respect to the middle bathyal water depths, the Kramarica Sill was emplaced about 600-800 m below the then surface of stratovolcano. Pyroclastic density current deposits are far less abundant than in the section Krnes and pyroclastic flow deposits are relatively abundant only in the upper half of the section. Syn-eruptive resedimented volcaniclastic deposits are dominated by volcaniclastic debris-flow deposits. Hyaloclastites and resedimented hyaloclastites are less abundant than in the section Krnes. Altogether fifteen peperites have been recognised and most of them are related to terminal parts of lava flows.
In the study area peperites often occur as sheet-like bodies along basal contacts of lava flows and the underlying wet sediments (Figure 7A,B). Sometimes they are encountered on the top of thin lava flows burrowing into a several m thick sequence of fine-grained sediments or along terminal parts of lava flows where they form irregularly shaped or lobate bodies. Peperite domains range in volume from less than a few m3 to several 10s m3 and sometimes they can only be some cm thick. The mingling wet sediment was commonly fine-grained volcanic ash or siliciclastic and carbonaceous silt. More rarely peperites have been recognised in association with coarser-grained volcaniclastic deposits, and most often they occur at the base of lava flows.
The most widespread type is blocky peperite whilst globular peperite and peperitic hyaloclastite are rarer in occurrence. Along the pathway of a single lava flow overriding the same layer of wet sediment the volume and texture of peperite have commonly changed. On a macroscopic scale, an initiation of peperite development along the contact of lava and fine-grained wet sediment was deformation of the underlying strata and laminae, their disintegration into clasts (Figure 7A) and subsequent incorporation into the lava flow where the clasts have undergone further deformation (Figure 7B). Terminal parts of lava flows commonly consist of blocky peperite. A clear zonation of closely packed blocky peperite next to lava and dispersed blocky peperite closer the host sediment has not been identified. Most often irregularly distributed domains of the mentioned textural types have been encountered. Some juvenile clasts may be jigsaw-fit and in some peperite domains, a part of the mingling sediment may occur in the form of clasts (Figure 8A,B).
A, disrupted stratified fine-grained tuff underlying hyaloclastite breccia and peperite. The dotted and dashed lines mark a peperite domain (P) and a separated clast composed of disrupted and convoluted stratified tuff (SC), respectively. Hammer (33 cm) is for scale; B, peperite (P) with abundant clasts of dark-grey fine-grained tuff. The dotted lines mark two larger deformed clasts originating from the underlying deposit (T).
Blocky peperite. A, larger angular juvenile clasts (jc) and fluidised sediment (S, dotted area) in matrix (m) composed of smaller juvenile clasts and fine-grained siliciclastic sediment. Coin (2.5 cm) is for scale; B, juvenile clasts (jc) and the clasts of fine-grained tuff (Sc) in matrix composed of an intimate mixture of the host sediment and juvenile clasts. The matrix is locally extensively altered (A) to laumontite. Coin (2.5 cm) is for scale.
On a macroscopic scale, blocky, sharply angular juvenile clasts are the most common (Figure 9A) although other forms of juvenile clasts have been recognised as well (Figure 9B-F). Globular juvenile clasts can be irregularly shaped or amoeboid (Figure 9B,C), elongated, tapered, and a single clast can have partially fluidal and sub-planar margins. Mixed morphologies of juvenile clasts, particularly sharply angular and elongate globular have been encountered in some rhyodacitic glassy lava flows (Figure 9E). Glassy lavas sometimes undergo ductile fragmentation into irregularly shaped elongated and convoluted globular clasts that resemble welded glass-shards (Figure 9F). Intergranular space is relatively limited and poorly interconnected, and can be infilled with very fine-grained, possibly suspended sediment. Further disintegration and mingling with wet sediment produced peperites developed as intimate mixtures of both components.
(A) angular juvenile clast with perlitic cracks in siliciclastic host sediment. Volcanic glass in perlitic domains is altered to laumontite (white) and Fe-oxides (black); (B) various shapes of juvenile clasts (jc) with indentations (i) of the host sediment (s); (C) amoeboid juvenile clasts (gc) in the host sediment (s); (D) an intimate mixture of juvenile clasts (jc) with the sediment (s) indentations (i), (E) globular(gc) and angular (h) juvenile clasts; (F) a glassy lava fragmented into globular (g), elongated (e) and convoluted (w) juvenile clasts with altered sediment (s) filling interstitial space.
The host sediment can penetrate magma in the form of curviplanar and vermicular indentations or enter lava flow through laminar boundary layers. The indentations (Figure 10A) reaching deeper into the juvenile clasts are commonly disconnected (Figure 10B,C) and initially, irregularly shaped droplets formed (Figure 10D). The droplets commonly advanced deeper into juvenile clasts changing their shapes into spherical and oval (Figure 10E,F). They may be very abundant, and the rock can be termed microglobular peperite, similar to that described by [5]. In an advanced stage peperites of this type may evolve into intimate mixtures of extremely irregularly shaped elongated clasts and tongues of sediment and tapered juvenile clasts having tendril and wispy forms (Figure 11A). The host sediment that penetrates lava through laminar boundary layers at least initially follows the laminae adopting their shape (Figure 11B), but then the flow with the admixed sediment seems to have changed into turbulent (Figure 11C). Sometimes the amount of sediment that mingled with magma in that manner is very low and only isolated patches of the entrained sediment can be encountered in the predominant magma, but there are cases where peperites locally developed as intimate mixtures of nearly equal proportions of tapered juvenile clasts and deformed, elongated clasts of sediment (Figure 11D).
(A) curviplanar indentations (i) of sediment (s) into juvenile clasts (jc); (B) interpenetrating sediment (s) and magma (m). The arrows i and p indicate the penetration directions of sediment and magma, respectively; (C) sediment (s) penetrating juvenile clast (jc). The arrows show the sediment penetration directions. Sediment (brownish) is partially unaltered and partially replaced by laumontite (Lmt). Larger detached droplets of sediment have irregular shapes whilst smaller ones tend to develop more oval or spherical shapes; (D) irregularly shaped droplets of sediment (s) penetrating a juvenile clast (m). The arrows (i) show the sediment penetration directions; (E) larger clast of sediment (s) penetrating a juvenile clast (m) is still unaltered, and smaller ones have already undergone alteration into chlorite (Chl). Some droplets of sediment show the tendency of splitting into several smaller droplets (d) and some smaller droplets already attained oval shapes (o); (F) droplets of siliciclastic sediment (s) in a juvenile clast (jc). Some droplets have oval shape (o) and some droplets indicate their shapes evolved by splitting of larger clasts (d).
(A) an intimate mixture of elongate altered clasts of sediment (S) and juvenile clasts (L); (B) sediment (S) entrained into lava flow (L) through a laminar boundary layer. The arrow shows the entrainment direction. The elongated sediment clast soon becomes thinner (t). Along the first obstacle it becomes thicker (T) by enclosing the phenocryst, and then becomes thinner by avoiding the second phenocryst; (C) microstructure of peperite indicating turbulent flow (t) by disrupted and convoluted sediment layers (S) in lava (L); (D) an intimate mixture of elongated clasts of sediment (S) and juvenile clasts (L); (E) platy juvenile clasts (L) formed by penetration of magma into fine-grained volcanic ash (T); (F) juvenile clasts (jc) and fluidised sediment (S) developed owing to the intrusion of the Kramarica Sill. The sediment is altered to iron oxides and the larger juvenile clast to laumontite (Lmt).
Magma can penetrate the adjacent sediments forming platy or tapered juvenile clasts (Figure 11E). Magma can also penetrate the host sediment along the strata boundaries or other disconformities related to syn-sedimentary tectonic activity or erosion. The emplacement of the Kramarica Sill also disrupted partially consolidated and unconsolidated sediments and made pathways for magma penetration (Figure 11F).
When the unconsolidated mingling sediment is composed of coarse-grained volcaniclastic deposit such as volcaniclastic turbidite or debris flow deposit, peperites can form by erosion and incorporation of sediment into the lava flow. A small-scale penetration of magma into interstitial space has been observed along the basal contacts of lava flows and the underlying sediments (Figure 12A). Sometimes magma penetrated deeper into the sediment while pushing aside and redistributing its constituents such as mineral grains and volcanic rock fragments (Figure 12B), although the advance seems very limited as the penetrating tongues soon became thinner (Figure 12C) or have been stopped by an impenetrable obstacle. Magma itself possibly underwent a sort of separation of its constituents during the process of penetration. Phenocrysts are often stacked close to the magma-sediment boundary while glassy groundmass could have penetrated deeper into the sediment (Figure 12D).
(A) the arrows (i) and (r) show the directions of magma penetration in intergranular space of volcaniclastic turbidite deposit. The arrow (o) indicates the cessation of penetration along a volcanic rock fragment (VRF); (B) penetration of magma (arrows) into volcaniclastic turbidite deposit by pushing aside crystal grains (cg). The cessation of penetration resulted in the formation of a juvenile clast (jc); (C) penetration of magma (m) stopped by crystal grains, the direction is marked by arrows, VRF – volcanic rock fragments; (D) stacked phenocrysts (Ph) of augite and a glassy constituent of magma (g) that penetrated somewhat further into volcaniclastic turbidite deposit, the arrows mark the directions of magma penetration.
Microfacies of peperites has been an essential tool in recognition of alteration of peperites as it encompasses the change in mineral and chemical composition of juvenile clasts and the mingling sediment, and more rarely, the formation of interstitial cement. Juvenile blocky clasts dispersed in abundant siliciclastic silt commonly underwent only devitrification, the alteration of glassy juvenile clasts with perlitic cracks may involve the formation of laumontite and Fe-oxides (Figure 9A). The mingling sediment is, in general, unaltered except for locally developed iron oxides.
Peperites with denser population of juvenile clasts, and particularly juvenile clasts having irregular fluidal or amoeboid shape, that mingled with siliciclastic silt are commonly altered to laumontite or laumontite and iron oxides. The host sediment commonly remained unaltered (Figure 13A).
(A) juvenile clasts (white) altered to laumontite (Lmt), iron oxides (o) and chlorite (Chl). The composition of the mingling siliciclastic sediment (S) remained largely unaltered; (B) a juvenile clast altered to laumontite (Lmt), epidote (Ep) and actinolite (Ac); (C) a clast of fine-grained pyroclastic deposit incorporated in a lava flow has been altered to albite (Ab), quartz (Qtz), chlorite (Chl) and Fe-oxides (o). Some clasts underwent magma assimilation (ma); (D) the mingling fine-grained pyroclastic deposit (S) formed a large oval inclusion in a juvenile clast that has been partially altered into laumontite (Lmt). Smaller inclusions are altered to pumpellyite (Pmp) and quartz, some small spherical inclusions are unaltered (o) and the other replaced by chlorite (Chl). juvenile clasts (jc); (E) an inclusion of fine-grained pyroclastic deposit (s) in a juvenile clast altered to prehnite (Prh) and laumontite (Lmt); (F) inclusions of fine-grained pyroclastic deposit in a juvenile fragment (brownish) altered to pumpellyite (Pmp), epidote (Ep), quartz (Qtz) and albite (Ab). Volcanic glass in the juvenile clast is locally replaced by chlorite (Chl).
Some juvenile clasts are replaced by the assemblage of laumontite, albite, quartz, actinolite and epidote (Figure 13B), or laumontite, albite, quartz, pumpellyite, incipient epidote and chlorite, or laumontite, prehnite, quartz, chlorite and incipient epidote, or laumontite, analcime and interlayered chlorite-smectite. Incipient epidote [53] refers to some μm to a few 10 μm sized, oval and highly birefringent grains. If the mingling sediment was siliciclastic silt it is often altered to microcrystalline quartz, incipient epidote and iron oxides.
If the mingling sediment was fine-grained pyroclastic deposit the alteration minerals commonly resemble those in the juvenile clasts. The most extensive alteration underwent the clasts composed of fine-grained pyroclastic deposit that were incorporated into lava flow, or fine-grained pyroclastic sediment that was entrained into lava flow through lamination boundary layers (Figure 13C). A common alteration assemblage is albite, prehnite, quartz, iron oxides and chlorite or interlayered chlorite-smectite with more than 80% of chlorite layers [54]. In the advanced stage of mingling (Figure 11A) the alteration of sediment commonly remained the same while the juvenile clasts can be altered to iron oxides and chlorite.
Penetration of the host sediment into juvenile clasts had immediate impact to its alteration. Before the sediment penetrated juvenile clasts and also in the initial stage of formation of droplets it commonly remained unaltered (Figure 10B,C), but with advanced penetration and subsequent dispersion into the juvenile clasts, and the transformation of shape from irregular to spherical and oval, the alteration advanced as well (Figure 10E,13D). Such inclusions of the host sediment closely resemble vesicle fillings and could be easily misinterpreted. Common alteration minerals are laumontite (Figure 13D), and the assemblages of or prehnite, laumontite and quartz (Figure 13E), or pumpellyite, albite, quartz and chlorite (Figure 13F), or laumontite, prehnite, quartz, epidote and chlorite.
Platy juvenile clasts related to penetration of magma into the host sediment are commonly extensively altered into laumontite and iron oxides (Figure 11E). The same assemblage typically replaces irregularly shaped juvenile clasts in peperites formed during the emplacement of the Krmarica Sill (Figure 11F).
The alteration of peperites related to coarse-grained host sediment is characterised by chlorite, interlayered chlorite-smectite with more than 90% of chlorite layers, quartz, and sometimes incipient epidote. Laumontite and other zeolites, and pumpellyite, prehnite and epidote are uncommon (Figure 12A-D).
The stratovolcano-hosted hydrothermal system with convective-advective flow regime of hydrothermal fluids (Figure 3), and another important event in the evolution of hydrothermal alteration of volcanic deposits was the emplacement of the Kramarica Sill. Consequently, volcanic deposits underwent alteration related to diverse processes and different superimposed stages of hydrothermal activity [37].
The largest source of geothermal energy and hydrothermal fluids in the time span of volcanic activity some 28-23 mya [43] was a deep igneous body. The alteration resulting from an elevated geothermal gradient is characterised by clinoptilolite, heulandite, analcime, smectite and interstratified smectite-chlorite. The convective flow of hydrothermal fluids occurred primarily through fracture systems and the most typical mineral formed owing to hydrothermal activity is laumontite. Where the fractures were densely distributed, the adjacent rock was altered as well. Laumontite occurs as interstitial cement and replaces volcanic glass and intermediate plagioclases in assemblage with albite, and the principal phyllosilicate mineral is chlorite or interstratified chlorite-smectite with over 80% of chlorite layers. Advective outflow of hydrothermal fluids preferentially occurred through high-permeability layers of the stratovolcano edifice, and laumontite, chlorite, albite and more rarely prehnite are typical minerals encountered in coarse-grained rocks such as volcaniclastic breccias. The adjacent, lower-permeability layers contain authigenic minerals with lower temperature stability ranges, namely clinoptilolite, heulandite, analcime and interlayered chlorite-smectite (Figures 5 and 6) [37, 38]. Stilbite locally occurs as vein mineral and was developed during late-stage of hydrothermal activity.
The emplacement of the Kramarica Sill (Figure 2) was related to the formation of new vent along the Periadriatic Line. Thermal effects of the emplacement promoted a number of progressive alteration reactions such as from laumontite to prehnite, laumontite to yugawaralite, or interlayered chlorite-smectite to chlorite. During the cooling of the sill, local hydrothermal conditions persisted and controlled retrograde reactions such as from prehnite to yugawaralite, from prehnite to laumontite, from laumontite to heulandite or analcime and from chlorite to interlayered corrensite-chlorite [37, 38, 54].
The formation of alteration minerals in volcanic-hydrothermal systems is a complex process affected by temperature, pressure, composition of reacting fluids, porosity, permeability and initial composition of the host-rock, duration of hydrothermal activity and superimposed thermal (or hydrothermal) regimes [55, 56]. Nevertheless, there is a general relationship between temperature and the formation of alteration minerals, and some mineral assemblages can be used to interpret temperatures within a geothermal system (Figure 14). For heulandite and stilbite, laumontite, yugawaralite, pumpellyite and actinolite widely accepted temperature stability ranges are 100-120°C, 120-220°C, 172-234°C, 200-310°C, 220-310°C and 280-460°C [52, 55, 56, 57, 58, 59, 60, 61, 62, 63, 64, 65]. Incipient, fine-grained and poorly crystallised epidote has been encountered in hydrothermal systems of the Philippines [53, 55] and the Nisyros Island [63], respectively, in the temperature range of 180-220°C although epidote generally forms at temperatures higher than 240°C [64, 65]. The temperature stability range of 245-265°C has been reported for mixed-layer R0 and R1 chlorite-smectite from Nesjavellir geothermal field, Iceland [66].
Authigenic calcium-aluminosilicate minerals that commonly serve as geothermometers in volcanic-hydrothermal systems, their chemical formulae and temperature stability ranges, compiled from [
The alteration of peperites from the Smrekovec Volcanic Complex indicates close relationship to the rock composition and texture, and therefore, the style of peperite formation. Porosity and permeability of peperites is, in general, lower than that of the host sediment. The types involving fine-grained host sediments have low permeability and low porosity, and in the stratovolcano-hosted hydrothermal system with convective-advective flow regime (Figure 3) they must have functioned as aquicludes unable to drain effectively the advective flow of hydrothermal fluids that largely controlled hydrothermal alteration of volcanic deposits [37]. In such hydrothermal system, peperites involving coarse-grained host sediments should be more extensively altered and contained authigenic minerals with higher temperature stability ranges than the types involving fine-grained host-sediments, but that is not the case. On contrary, in this type of peperites significant authigenic calcium-aluminosilicate minerals are often lacking and the most common alteration mineral is chlorite or interlayered chlorite-smectite.
In dispersed blocky peperite, matrix composed of siliciclastic host sediment is usually unaltered. The alteration of juvenile clasts often indicates only the reactions of devitrification of volcanic glass, and only juvenile clasts with perlitic cracks can be altered to laumontite and Fe-oxides (Figure 9A). The activity of hot fluids originating from heated pore waters can be assumed, but chemical gradients favourable for the formation of laumontite were attained only inside the juvenile clasts with perlitic cracks. Perlitic cracks apparently served as conduits for hot fluids that leached volcanic glass during the flow, and in this manner underwent the changes in chemical composition (e.g. [67]) that finally resulted in crystallisation of laumontite. Far more extensive alteration of blocky peperites involving fine-grained pyroclastic host sediment supports the forementioned explanation. The interaction of heated pore fluids and highly reactive host sediment apparently controlled geochemical evolution of so-formed hydrothermal solutions and the related extensive alteration of all constituents of peperite. Laumontite or mineral assemblages of laumontite, albite, quartz, pumpellyite, incipient epidote and chlorite, or laumontite, prehnite, quartz, chlorite and incipient epidote, or laumontite, analcime and interlayered chlorite-smectite indicate that temperature gradients were prerequisite but not sufficient for alteration to occur and that the main controlling factor were geochemical gradients.
Microglobular peperite has been interpreted as a frozen example of a fuel-coolant interaction (FCI) between magma and fluidised host sediment [5], and the temperatures of alteration reactions in direct contact with magma must have been higher than in blocky peperite. Microglobules of fine-grained pyroclastic sediment underwent alteration, and typically, smaller microglobules are commonly completely altered to authigenic mineral assemblages with higher temperature stability ranges (e.g. pumpellyite, epidote) than the larger ones that remained incompletely altered or altered to authigenic minerals with lower temperature stability ranges (e.g. laumontite) (Figure 13D). The relationship indicates that high-temperature conditions could not persist for a long period of time.
Despite of the complexity of alteration of volcanic deposits in lithofacies associations of the sections Krnes and Smrekovec G34 the assemblages of authigenic minerals in peperites are different than those in the adjacent underlying and overlying autoclastic, pyroclastic or resedimented volcaniclastic deposits irrespectively of their texture and grain-size (Figures 4 and 5). Particularly outstanding is the occurrence of pumpellyite, actinolite and epidote. In lavas pumpellyite and actinolite very rarely occur as the replacement of volcanic glass and other primary constituents although the temperatures in cooling lavas could be favourable for their formation.
If compared to the section Krnes, the alteration of volcanic deposits in the section Smrekovec G34 has been far more complex owing to the emplacement of the Kramarica Sill. Progressive reactions related to an elevated temperature regime are characterised by the occurrence of prehnite and indicate, at least in the lower half of the section, that the temperatures could have reached over 300°C. Yet, even in such elevated temperature regime the exclusive occurrence of pumpellyite and particularly actinolite in peperites indicates that higher temperatures and specific geochemical conditions related to the formation of peperites must have controlled the crystallisation of pumpellyite and actinolite. The occurrence of the same assemblage in peperites in the section Krnes is particularly important. Here, hydrothermal activity and temperature regime were mainly related to a deep igneous source and the associated convective-advective flow of hydrothermal fluids and elevated geothermal gradients in the area of stratovolcano, and they were not affected, at least significantly, by the emplacement and cooling of the Kramarica Sill. Maximum temperatures have been determined by the temperature stability of laumontite, namely, 234°C which is insufficient for the crystallisation of pumpellyite or actinolite. The alteration of juvenile clasts to laumontite in peperites indicates the presence of hydrothermal conditions although they cannot be conclusively ascribed to specific hydrothermal conditions and geochemical gradients related to the formation of peperites.
The alteration of peperites can be regarded as syn-formational hydrothermal, although it is local, specific and ephemeral lasting until thermal gradients persisted. Authigenic mineral assemblages developed in peperites from the Smrekovec Volcanic Complex are rare on a worldwide scale and have not been identified in such context yet. Geochemical evolution of heated pore fluids circulating in the vicinity of the source of heat controlled the formation of authigenic mineral assemblages and the presence of unstable, reactive volcanic material was crucial for their formation and diversity.
Peperites are commonly developed in submarine environments with contemporaneous volcanic activity and sedimentation. And although the occurrence and complex processes of formation have been studied and explained in many modern and ancient geological settings worldwide [4, 10, 11, 12, 13, 14], and particularly in the Carpathian-Pannonian region [9, 15, 16, 17] where the Smrekovec Volcanic Complex belongs to [29], the studies related to their alteration have been relatively scarce [15, 16, 17, 18, 19, 20]. The present study gives evidence of the existence of localised and ephemeral hydrothermal conditions related to and persisting during the formation of peperites and resulting in their distinct alteration.
The Smrekovec Volcanic Complex is a remnant of an Oligocene submarine stratovolcano characterised by a complex development of an over 2500 m thick succession of volcanic rocks. Submarine environment, the style of eruptions, morphology and the abundance of pyroclastic and syn-eruptively resedimented volcaniclastic deposits were favourable for the formation of peperites that are particularly abundant in medial-zone lithofacies associations. In a succession of volcanic deposits studied in detail in two sections Krnes and Smrekovec G34 attaining 400 m and 470 m, respectively, the alteration of peperites indicates that authigenic minerals have higher temperature stability ranges than those in the adjacent underlying and overlying deposits irrespectively of their lithofacies.
The alteration of peperites indicates close relationship to the rock composition and texture, and therefore, the style of peperite formation. Dispersed blocky peperite involving siliciclastic host sediment is commonly poorly altered. Volcanic glass in juvenile clasts is usually devitrified or hydrated, and only some clasts with perlitic texture can be altered to laumontite. In the textural types with fine-grained pyroclastic host sediment laumontite, or the assemblages of laumontite, albite, quartz, pumpellyite, incipient epidote and chlorite, or laumontite, prehnite, quartz, chlorite and incipient epidote, or laumontite, analcime and interlayered chlorite-smectite may occur. The alteration minerals indicate that thermal gradients were prerequisite but not sufficient for alteration to occur and that the main controlling factor were geochemical gradients in reacting fluids.
Microglobular peperite developed by interaction between magma and fluidised sediment [5], and the temperatures of alteration must have been higher than in blocky peperite. Smaller microglobules are often completely altered to authigenic mineral assemblages with higher temperature stability ranges (e.g. pumpellyite, epidote) while the larger microglobules remained incompletely altered or altered to authigenic minerals with lower temperature stability ranges (e.g. laumontite). The relationship indicates that high-temperature conditions could not persist for a long period of time and had ephemeral character.
Authigenic mineral assemblages developed in peperites indicate that their formation is specific and related to the formation of parent rock itself. Thermal stability ranges of actinolite and pumpellyite indicate the highest temperatures possibly exceeded 280°C and decreased when the parent lava flow and the associated peperite underwent cooling. Hydrothermal fluids mainly originated from heated pore fluids although deuteric fluids could have been locally admixed. The evolution of fluids circulating in peperite was essential for extensive alteration to occur and that was possibly attained by interaction with unstable and highly reactive host sediment. Many peperites have been developed as low-porosity and low-permeability layers, and therefore contemporaneous and later hydrothermal activity related to the stratovolcano-hosted hydrothermal system with convective-advective flow could not have exerted any critical thermal or geochemical impact.
The alteration of peperites in the Smrekovec Volcanic Complex can be regarded as syn-formational, hydrothermal, ephemeral, localised and depending on many factors such as the extent and time span of thermal regime, the process of formation of parent rock and thermal and geochemical evolution of circulating hydrothermal fluids. And although peperite deposits are not rare in similar volcanic-sedimentary settings worldwide, the alteration as recognised in the present study has not been reported yet and indicates the formation and alteration of peperites are complex and distinctive and interrelated processes.
Slovenian Research Agency (ARRS) is acknowledged for granting the research (Programme Mineral Resources P-0025). The editorial work of Academic Editor Dr. Károly Németh and helpful comments of anonymous reviewers are greatly appreciated. Many thanks to Mrs. Mia Vulovic, Author Service Manager for her kind assistance. I thank Ms. Staška Čertalič and Mr. Mladen Štumergar from Geological Survey of Slovenia for technical support.
As this section deals with legal issues pertaining to the rights of individual Authors and IntechOpen, for the avoidance of doubt, each category of publication is dealt with separately. Consequently, much of the information, for example definition of terms used, is repeated to ensure that there can be no misunderstanding of the policies that apply to each category.
",metaTitle:"Copyright Policy",metaDescription:"Copyright is the term used to describe the rights related to the publication and distribution of original works. Most importantly from a publisher's perspective, copyright governs how authors, publishers and the general public can use, publish and distribute publications.",metaKeywords:null,canonicalURL:"/page/copyright-policy",contentRaw:'[{"type":"htmlEditorComponent","content":"Copyright is the term used to describe the rights related to the publication and distribution of original Works. Most importantly from a publisher's perspective, copyright governs how Authors, publishers and the general public can use, publish, and distribute publications.
\\n\\nIntechOpen only publishes manuscripts for which it has publishing rights. This is governed by a publication agreement between the Author and IntechOpen. This agreement is accepted by the Author when the manuscript is submitted and deals with both the rights of the publisher and Author, as well as any obligations concerning a particular manuscript. However, in accepting this agreement, Authors continue to retain significant rights to use and share their publications.
\\n\\nHOW COPYRIGHT WORKS WITH OPEN ACCESS LICENSES?
\\n\\nAgreement samples are listed here for the convenience of prospective Authors:
\\n\\nDEFINITIONS
\\n\\nThe following definitions apply in this Copyright Policy:
\\n\\nAuthor - in order to be identified as an Author, three criteria must be met: (i) Substantial contribution to the conception or design of the Work, or the acquisition, analysis, or interpretation of data for the Work; (ii) Participation in drafting or revising the Work; (iii) Approval of the final version of the Work to be published.
\\n\\nWork - a Chapter, including Conference Papers, a Scientific Article and any and all text, graphics, images and/or other materials forming part of or accompanying the Chapter/Conference Paper.
\\n\\nMonograph/Compacts - a full manuscript usually written by a single Author, including any and all text, graphics, images and/or other materials.
\\n\\nCompilation - a collection of Works distributed in a Book that IntechOpen has selected, and for which the coordination of the preparation, arrangement and publication has been the responsibility of IntechOpen. Any Work included is accepted in its entirety in unmodified form and is published with one or more other contributions, each constituting a separate and independent Work, but which together are assembled into a collective whole.
\\n\\nScientific Journal – Periodical publication intended to further the progress of science.
\\n\\nJournal Article/Scientific Article – Publication based on empirical evidence. It can support a hypothesis with original research, describe existing research or comment on current trends in a specific field.
\\n\\nIntechOpen - Registered publisher with office at 5 Princes Gate Court, London, SW7 2QJ - UNITED KINGDOM
\\n\\nIntechOpen platform - IntechOpen website www.intechopen.com whose main purpose is to host Monographs in the format of Book Chapters, Long Form Monographs, Compacts, Conference Proceedings, Scientific Journals and Videos.
\\n\\nVideo Lecture – an audiovisual recording of a lecture or a speech given by a Lecturer, recorded, edited, owned and published by IntechOpen.
\\n\\nTERMS
\\n\\nAll Works published on the IntechOpen platform and in print are licensed under a Creative Commons Attribution 3.0 Unported and Creative Commons 4.0 International License, a license which allows for the broadest possible reuse of published material.
\\n\\nCopyright on the individual Works belongs to the specific Author, subject to an agreement with IntechOpen. The Creative Common license is granted to all others to:
\\n\\nAnd for any purpose, provided the following conditions are met:
\\n\\nAll Works are published under the CC BY 3.0 and CC BY 4.0 license. However, please note that book Chapters may fall under a different CC license, depending on their publication date as indicated in the table below:
\\n\\n\\n\\n
LICENSE | \\n\\t\\t\\tUSED FROM - | \\n\\t\\t\\tUP TO - | \\n\\t\\t
\\n\\t\\t\\t Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0) \\n\\t\\t\\t | \\n\\t\\t\\t1 July 2005 (2005-07-01) | \\n\\t\\t\\t3 October 2011 (2011-10-03) | \\n\\t\\t
\\n\\t\\t\\t Creative Commons Attribution 3.0 Unported (CC BY 3.0) \\n\\t\\t\\t | \\n\\t\\t\\t5 October 2011 (2011-10-05) | \\n\\t\\t\\tCurrently | \\n\\t\\t
\\n\\t\\t\\t Creative Commons 4.0 International (CC BY 4.0) – for Journal Articles \\n\\t\\t\\t | \\n\\t\\t\\t15 March 2022 | \\n\\t\\t\\tCurrently | \\n\\t\\t
The CC BY 3.0 and CC BY 4.0 license permits Works to be freely shared in any medium or format, as well as the reuse and adaptation of the original contents of Works (e.g. figures and tables created by the Authors), as long as the source Work is cited and its Authors are acknowledged in the following manner:
\\n\\nContent reuse:
\\n\\n© {year} {authors' full names}. Originally published in {short citation} under {license version} license. Available from: {DOI}
\\n\\nContent adaptation & reuse:
\\n\\n© {year} {authors' full names}. Adapted from {short citation}; originally published under {license version} license. Available from: {DOI}
\\n\\nReposting & sharing:
\\n\\nOriginally published in {full citation}. Available from: {DOI}
\\n\\nRepublishing – More about Attribution Policy can be found here.
\\n\\nThe same principles apply to Works published under the CC BY-NC-SA 3.0 license, with the caveats that (1) the content may not be used for commercial purposes, and (2) derivative works building on this content must be distributed under the same license. The restrictions contained in these license terms may, however, be waived by the copyright holder(s). Users wishing to circumvent any of the license terms are required to obtain explicit permission to do so from the copyright holder(s).
\\n\\nDISCLAIMER: Neither the CC BY 3.0 license, CC BY 4.0, nor any other license IntechOpen currently uses or has used before, applies to figures and tables reproduced from other works, as they may be subject to different terms of reuse. In such cases, if the copyright holder is not noted in the source of a figure or table, it is the responsibility of the User to investigate and determine the exact copyright status of any information utilised. Users requiring assistance in that regard are welcome to send an inquiry to permissions@intechopen.com.
\\n\\nAll rights to Books and Journals and all other compilations published on the IntechOpen platform and in print are reserved by IntechOpen.
\\n\\nThe copyright to Books, Journals and other compilations is subject to separate copyright from those that exist in the included Works.
\\n\\nAll Long Form Monographs/Compacts are licensed under the Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) license granted to all others.
\\n\\nCopyright to the individual Works (Chapters) belongs to their specific Authors, subject to an agreement with IntechOpen and the Creative Common license granted to all others to:
\\n\\nUnder the following terms:
\\n\\nThere must be an Attribution, giving appropriate credit, provision of a link to the license, and indication if any changes were made.
\\n\\nNonCommercial - The use of the material for commercial purposes is prohibited. Commercial rights are reserved to IntechOpen or its licensees.
\\n\\nNo additional restrictions that apply legal terms or technological measures that restrict others from doing anything the license permits are allowed.
\\n\\nThe CC BY-NC 4.0 license permits Works to be freely shared in any medium or format, as well as reuse and adaptation of the original contents of Works (e.g. figures and tables created by the Authors), as long as it is not used for commercial purposes. The source Work must be cited and its Authors acknowledged in the following manner:
\\n\\nContent reuse:
\\n\\n© {year} {authors' full names}. Originally published in {short citation} under {license version} license. Available from: {DOI}
\\n\\nContent adaptation & reuse:
\\n\\n© {year} {authors' full names}. Adapted from {short citation}; originally published under {license version} license. Available from: {DOI}
\\n\\nReposting & sharing:
\\n\\nOriginally published in {full citation}. Available from: {DOI}
\\n\\nAll Book cover design elements, as well as Video image graphics are subject to copyright by IntechOpen.
\\n\\nEvery reproduction of a front cover image must be accompanied by an appropriate Copyright Notice displayed adjacent to the image. The exact Copyright Notice depends on who the Author of a particular cover image is. Users wishing to reproduce cover images should contact permissions@intechopen.com.
\\n\\nAll Video Lectures under IntechOpen's production are subject to copyright and are property of IntechOpen, unless defined otherwise, and are licensed under the Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) license. This grants all others the right to:
\\n\\nShare — copy and redistribute the material in any medium or format
\\n\\nUnder the following terms:
\\n\\nUsers wishing to repost and share the Video Lectures are welcome to do so as long as they acknowledge the source in the following manner:
\\n\\n© {year} IntechOpen. Published under CC BY-NC-ND 4.0 license. Available from: {DOI}
\\n\\nUsers wishing to reuse, modify, or adapt the Video Lectures in a way not permitted by the license are welcome to contact us at permissions@intechopen.com to discuss waiving particular license terms.
\\n\\nAll software used on the IntechOpen platform, any used during the publishing process, and the copyright in the code constituting such software, is the property of IntechOpen or its software suppliers. As such, it may not be downloaded or copied without permission.
\\n\\nUnless otherwise indicated, all IntechOpen websites are the property of IntechOpen.
\\n\\nAll content included on IntechOpen Websites not forming part of contributed materials (such as text, images, logos, graphics, design elements, videos, sounds, pictures, trademarks, etc.), are subject to copyright and are property of, or licensed to, IntechOpen. Any other use, including the reproduction, modification, distribution, transmission, republication, display, or performance of the content on this site is strictly prohibited.
\\n\\nPolicy last updated: 2016-06-08
\\n"}]'},components:[{type:"htmlEditorComponent",content:'Copyright is the term used to describe the rights related to the publication and distribution of original Works. Most importantly from a publisher's perspective, copyright governs how Authors, publishers and the general public can use, publish, and distribute publications.
\n\nIntechOpen only publishes manuscripts for which it has publishing rights. This is governed by a publication agreement between the Author and IntechOpen. This agreement is accepted by the Author when the manuscript is submitted and deals with both the rights of the publisher and Author, as well as any obligations concerning a particular manuscript. However, in accepting this agreement, Authors continue to retain significant rights to use and share their publications.
\n\nHOW COPYRIGHT WORKS WITH OPEN ACCESS LICENSES?
\n\nAgreement samples are listed here for the convenience of prospective Authors:
\n\nDEFINITIONS
\n\nThe following definitions apply in this Copyright Policy:
\n\nAuthor - in order to be identified as an Author, three criteria must be met: (i) Substantial contribution to the conception or design of the Work, or the acquisition, analysis, or interpretation of data for the Work; (ii) Participation in drafting or revising the Work; (iii) Approval of the final version of the Work to be published.
\n\nWork - a Chapter, including Conference Papers, a Scientific Article and any and all text, graphics, images and/or other materials forming part of or accompanying the Chapter/Conference Paper.
\n\nMonograph/Compacts - a full manuscript usually written by a single Author, including any and all text, graphics, images and/or other materials.
\n\nCompilation - a collection of Works distributed in a Book that IntechOpen has selected, and for which the coordination of the preparation, arrangement and publication has been the responsibility of IntechOpen. Any Work included is accepted in its entirety in unmodified form and is published with one or more other contributions, each constituting a separate and independent Work, but which together are assembled into a collective whole.
\n\nScientific Journal – Periodical publication intended to further the progress of science.
\n\nJournal Article/Scientific Article – Publication based on empirical evidence. It can support a hypothesis with original research, describe existing research or comment on current trends in a specific field.
\n\nIntechOpen - Registered publisher with office at 5 Princes Gate Court, London, SW7 2QJ - UNITED KINGDOM
\n\nIntechOpen platform - IntechOpen website www.intechopen.com whose main purpose is to host Monographs in the format of Book Chapters, Long Form Monographs, Compacts, Conference Proceedings, Scientific Journals and Videos.
\n\nVideo Lecture – an audiovisual recording of a lecture or a speech given by a Lecturer, recorded, edited, owned and published by IntechOpen.
\n\nTERMS
\n\nAll Works published on the IntechOpen platform and in print are licensed under a Creative Commons Attribution 3.0 Unported and Creative Commons 4.0 International License, a license which allows for the broadest possible reuse of published material.
\n\nCopyright on the individual Works belongs to the specific Author, subject to an agreement with IntechOpen. The Creative Common license is granted to all others to:
\n\nAnd for any purpose, provided the following conditions are met:
\n\nAll Works are published under the CC BY 3.0 and CC BY 4.0 license. However, please note that book Chapters may fall under a different CC license, depending on their publication date as indicated in the table below:
\n\n\n\n
LICENSE | \n\t\t\tUSED FROM - | \n\t\t\tUP TO - | \n\t\t
\n\t\t\t Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0) \n\t\t\t | \n\t\t\t1 July 2005 (2005-07-01) | \n\t\t\t3 October 2011 (2011-10-03) | \n\t\t
\n\t\t\t Creative Commons Attribution 3.0 Unported (CC BY 3.0) \n\t\t\t | \n\t\t\t5 October 2011 (2011-10-05) | \n\t\t\tCurrently | \n\t\t
\n\t\t\t Creative Commons 4.0 International (CC BY 4.0) – for Journal Articles \n\t\t\t | \n\t\t\t15 March 2022 | \n\t\t\tCurrently | \n\t\t
The CC BY 3.0 and CC BY 4.0 license permits Works to be freely shared in any medium or format, as well as the reuse and adaptation of the original contents of Works (e.g. figures and tables created by the Authors), as long as the source Work is cited and its Authors are acknowledged in the following manner:
\n\nContent reuse:
\n\n© {year} {authors' full names}. Originally published in {short citation} under {license version} license. Available from: {DOI}
\n\nContent adaptation & reuse:
\n\n© {year} {authors' full names}. Adapted from {short citation}; originally published under {license version} license. Available from: {DOI}
\n\nReposting & sharing:
\n\nOriginally published in {full citation}. Available from: {DOI}
\n\nRepublishing – More about Attribution Policy can be found here.
\n\nThe same principles apply to Works published under the CC BY-NC-SA 3.0 license, with the caveats that (1) the content may not be used for commercial purposes, and (2) derivative works building on this content must be distributed under the same license. The restrictions contained in these license terms may, however, be waived by the copyright holder(s). Users wishing to circumvent any of the license terms are required to obtain explicit permission to do so from the copyright holder(s).
\n\nDISCLAIMER: Neither the CC BY 3.0 license, CC BY 4.0, nor any other license IntechOpen currently uses or has used before, applies to figures and tables reproduced from other works, as they may be subject to different terms of reuse. In such cases, if the copyright holder is not noted in the source of a figure or table, it is the responsibility of the User to investigate and determine the exact copyright status of any information utilised. Users requiring assistance in that regard are welcome to send an inquiry to permissions@intechopen.com.
\n\nAll rights to Books and Journals and all other compilations published on the IntechOpen platform and in print are reserved by IntechOpen.
\n\nThe copyright to Books, Journals and other compilations is subject to separate copyright from those that exist in the included Works.
\n\nAll Long Form Monographs/Compacts are licensed under the Creative Commons Attribution-NonCommercial 4.0 International (CC BY-NC 4.0) license granted to all others.
\n\nCopyright to the individual Works (Chapters) belongs to their specific Authors, subject to an agreement with IntechOpen and the Creative Common license granted to all others to:
\n\nUnder the following terms:
\n\nThere must be an Attribution, giving appropriate credit, provision of a link to the license, and indication if any changes were made.
\n\nNonCommercial - The use of the material for commercial purposes is prohibited. Commercial rights are reserved to IntechOpen or its licensees.
\n\nNo additional restrictions that apply legal terms or technological measures that restrict others from doing anything the license permits are allowed.
\n\nThe CC BY-NC 4.0 license permits Works to be freely shared in any medium or format, as well as reuse and adaptation of the original contents of Works (e.g. figures and tables created by the Authors), as long as it is not used for commercial purposes. The source Work must be cited and its Authors acknowledged in the following manner:
\n\nContent reuse:
\n\n© {year} {authors' full names}. Originally published in {short citation} under {license version} license. Available from: {DOI}
\n\nContent adaptation & reuse:
\n\n© {year} {authors' full names}. Adapted from {short citation}; originally published under {license version} license. Available from: {DOI}
\n\nReposting & sharing:
\n\nOriginally published in {full citation}. Available from: {DOI}
\n\nAll Book cover design elements, as well as Video image graphics are subject to copyright by IntechOpen.
\n\nEvery reproduction of a front cover image must be accompanied by an appropriate Copyright Notice displayed adjacent to the image. The exact Copyright Notice depends on who the Author of a particular cover image is. Users wishing to reproduce cover images should contact permissions@intechopen.com.
\n\nAll Video Lectures under IntechOpen's production are subject to copyright and are property of IntechOpen, unless defined otherwise, and are licensed under the Attribution-NonCommercial-NoDerivatives 4.0 International (CC BY-NC-ND 4.0) license. This grants all others the right to:
\n\nShare — copy and redistribute the material in any medium or format
\n\nUnder the following terms:
\n\nUsers wishing to repost and share the Video Lectures are welcome to do so as long as they acknowledge the source in the following manner:
\n\n© {year} IntechOpen. Published under CC BY-NC-ND 4.0 license. Available from: {DOI}
\n\nUsers wishing to reuse, modify, or adapt the Video Lectures in a way not permitted by the license are welcome to contact us at permissions@intechopen.com to discuss waiving particular license terms.
\n\nAll software used on the IntechOpen platform, any used during the publishing process, and the copyright in the code constituting such software, is the property of IntechOpen or its software suppliers. As such, it may not be downloaded or copied without permission.
\n\nUnless otherwise indicated, all IntechOpen websites are the property of IntechOpen.
\n\nAll content included on IntechOpen Websites not forming part of contributed materials (such as text, images, logos, graphics, design elements, videos, sounds, pictures, trademarks, etc.), are subject to copyright and are property of, or licensed to, IntechOpen. Any other use, including the reproduction, modification, distribution, transmission, republication, display, or performance of the content on this site is strictly prohibited.
\n\nPolicy last updated: 2016-06-08
\n'}]},successStories:{items:[]},authorsAndEditors:{filterParams:{id:"965887@"},profiles:[],filtersByRegion:[{group:"region",caption:"North America",value:1,count:6601},{group:"region",caption:"Middle and South America",value:2,count:5906},{group:"region",caption:"Africa",value:3,count:2400},{group:"region",caption:"Asia",value:4,count:12541},{group:"region",caption:"Australia and Oceania",value:5,count:1008},{group:"region",caption:"Europe",value:6,count:17561}],offset:0,limit:12,total:null},chapterEmbeded:{data:{}},editorApplication:{success:null,errors:{}},ofsBooks:{filterParams:{hasNoEditors:"0",sort:"-dateEndThirdStepPublish",topicId:"23,21"},books:[{type:"book",id:"11433",title:"Human Migration in the Last Three Centuries",subtitle:null,isOpenForSubmission:!0,hash:"9836df9e82aa9f82e3852a60204909a8",slug:null,bookSignature:"Dr. Ingrid Muenstermann",coverURL:"https://cdn.intechopen.com/books/images_new/11433.jpg",editedByType:null,editors:[{id:"77112",title:"Dr.",name:"Ingrid",surname:"Muenstermann",slug:"ingrid-muenstermann",fullName:"Ingrid Muenstermann"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11443",title:"Empathy - Advanced Research and Applications",subtitle:null,isOpenForSubmission:!0,hash:"4c1042dfe15aa9cea6019524c4cbff38",slug:null,bookSignature:"Ph.D. Sara Ventura",coverURL:"https://cdn.intechopen.com/books/images_new/11443.jpg",editedByType:null,editors:[{id:"227763",title:"Ph.D.",name:"Sara",surname:"Ventura",slug:"sara-ventura",fullName:"Sara Ventura"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11437",title:"Social Media - Risks and Opportunities",subtitle:null,isOpenForSubmission:!0,hash:"000e31f2e2f7295805e9a3864158ad63",slug:null,bookSignature:"Dr. Shafizan Mohamed and Dr. Shazleen Mohamed",coverURL:"https://cdn.intechopen.com/books/images_new/11437.jpg",editedByType:null,editors:[{id:"302450",title:"Dr.",name:"Shafizan",surname:"Mohamed",slug:"shafizan-mohamed",fullName:"Shafizan Mohamed"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11780",title:"Volunteering",subtitle:null,isOpenForSubmission:!0,hash:"008a5fc8005ea6b9228cfe39f9521abe",slug:null,bookSignature:"Ph.D. Diann Kelly",coverURL:"https://cdn.intechopen.com/books/images_new/11780.jpg",editedByType:null,editors:[{id:"325207",title:"Ph.D.",name:"Diann",surname:"Kelly",slug:"diann-kelly",fullName:"Diann Kelly"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11783",title:"Motivation and Success",subtitle:null,isOpenForSubmission:!0,hash:"f660b7cd35b9af94bdfc3564df138161",slug:null,bookSignature:"Dr. Simon George Taukeni",coverURL:"https://cdn.intechopen.com/books/images_new/11783.jpg",editedByType:null,editors:[{id:"202046",title:"Dr.",name:"Simon George",surname:"Taukeni",slug:"simon-george-taukeni",fullName:"Simon George Taukeni"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11781",title:"Family Therapy - Recent Advances in Clinical and Crisis Settings",subtitle:null,isOpenForSubmission:!0,hash:"8c5b7d5e4233594de70d2f830209b757",slug:null,bookSignature:"Dr. Oluwatoyin Olatundun Ilesanmi",coverURL:"https://cdn.intechopen.com/books/images_new/11781.jpg",editedByType:null,editors:[{id:"440049",title:"Dr.",name:"Oluwatoyin Olatundun",surname:"Ilesanmi",slug:"oluwatoyin-olatundun-ilesanmi",fullName:"Oluwatoyin Olatundun Ilesanmi"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11474",title:"Quality of Life Interventions - Magnitude of Effect and Transferability",subtitle:null,isOpenForSubmission:!0,hash:"5a6bcdaf5ee144d043bcdab893ff9e1c",slug:null,bookSignature:"Ph.D. Sage Arbor",coverURL:"https://cdn.intechopen.com/books/images_new/11474.jpg",editedByType:null,editors:[{id:"245319",title:"Ph.D.",name:"Sage",surname:"Arbor",slug:"sage-arbor",fullName:"Sage Arbor"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11777",title:"LGBT Communities",subtitle:null,isOpenForSubmission:!0,hash:"e08bb222c250dcebf093b7ab595a14a7",slug:null,bookSignature:"Dr. Deborah Woodman",coverURL:"https://cdn.intechopen.com/books/images_new/11777.jpg",editedByType:null,editors:[{id:"463750",title:"Dr.",name:"Deborah",surname:"Woodman",slug:"deborah-woodman",fullName:"Deborah Woodman"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11478",title:"Recent Advances in the Study of Dyslexia",subtitle:null,isOpenForSubmission:!0,hash:"26764a18c6b776698823e0e1c3022d2f",slug:null,bookSignature:"Prof. Jonathan Glazzard",coverURL:"https://cdn.intechopen.com/books/images_new/11478.jpg",editedByType:null,editors:[{id:"294281",title:"Prof.",name:"Jonathan",surname:"Glazzard",slug:"jonathan-glazzard",fullName:"Jonathan Glazzard"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11779",title:"Non-government Organizations - New Perspectives",subtitle:null,isOpenForSubmission:!0,hash:"c109a472a9e0ea8398ae95e2d21be039",slug:null,bookSignature:"Prof. Vito Bobek and Dr. Tatjana Horvat",coverURL:"https://cdn.intechopen.com/books/images_new/11779.jpg",editedByType:null,editors:[{id:"128342",title:"Prof.",name:"Vito",surname:"Bobek",slug:"vito-bobek",fullName:"Vito Bobek"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11444",title:"Happiness - Biopsychosocial and Anthropological Perspectives",subtitle:null,isOpenForSubmission:!0,hash:"fa84e7fc3611e5428e070239dcf5a93f",slug:null,bookSignature:"Dr. Floriana Irtelli and Prof. Fabio Gabrielli",coverURL:"https://cdn.intechopen.com/books/images_new/11444.jpg",editedByType:null,editors:[{id:"174641",title:"Dr.",name:"Floriana",surname:"Irtelli",slug:"floriana-irtelli",fullName:"Floriana Irtelli"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11782",title:"Personality Traits - The Role in Psychopathology",subtitle:null,isOpenForSubmission:!0,hash:"d3a491e5194cad4c59b900dd57a11842",slug:null,bookSignature:" Vladimir V. Kalinin",coverURL:"https://cdn.intechopen.com/books/images_new/11782.jpg",editedByType:null,editors:[{id:"31572",title:null,name:"Vladimir V.",surname:"Kalinin",slug:"vladimir-v.-kalinin",fullName:"Vladimir V. Kalinin"}],productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}}],filtersByTopic:[{group:"topic",caption:"Agricultural and Biological Sciences",value:5,count:43},{group:"topic",caption:"Biochemistry, Genetics and Molecular Biology",value:6,count:11},{group:"topic",caption:"Business, Management and Economics",value:7,count:5},{group:"topic",caption:"Chemistry",value:8,count:23},{group:"topic",caption:"Computer and Information Science",value:9,count:21},{group:"topic",caption:"Earth and Planetary Sciences",value:10,count:17},{group:"topic",caption:"Engineering",value:11,count:62},{group:"topic",caption:"Environmental Sciences",value:12,count:9},{group:"topic",caption:"Immunology and Microbiology",value:13,count:10},{group:"topic",caption:"Materials Science",value:14,count:29},{group:"topic",caption:"Mathematics",value:15,count:10},{group:"topic",caption:"Medicine",value:16,count:122},{group:"topic",caption:"Nanotechnology and Nanomaterials",value:17,count:9},{group:"topic",caption:"Neuroscience",value:18,count:3},{group:"topic",caption:"Pharmacology, Toxicology and Pharmaceutical Science",value:19,count:6},{group:"topic",caption:"Physics",value:20,count:12},{group:"topic",caption:"Psychology",value:21,count:9},{group:"topic",caption:"Robotics",value:22,count:4},{group:"topic",caption:"Social Sciences",value:23,count:8},{group:"topic",caption:"Veterinary Medicine and Science",value:25,count:4}],offset:12,limit:12,total:17},popularBooks:{featuredBooks:[{type:"book",id:"10584",title:"Engineered Wood Products for Construction",subtitle:null,isOpenForSubmission:!1,hash:"421757c56a3735986055250821275a51",slug:"engineered-wood-products-for-construction",bookSignature:"Meng Gong",coverURL:"https://cdn.intechopen.com/books/images_new/10584.jpg",editors:[{id:"274242",title:"Dr.",name:"Meng",middleName:null,surname:"Gong",slug:"meng-gong",fullName:"Meng Gong"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10222",title:"Demyelination Disorders",subtitle:null,isOpenForSubmission:!1,hash:"b6c26ceccacdde70c41c587361bd5558",slug:"demyelination-disorders",bookSignature:"Stavros J. Baloyannis, Fabian H. Rossi and Welwin Liu",coverURL:"https://cdn.intechopen.com/books/images_new/10222.jpg",editors:[{id:"156098",title:"Emeritus Prof.",name:"Stavros J.",middleName:"J.",surname:"Baloyannis",slug:"stavros-j.-baloyannis",fullName:"Stavros J. Baloyannis"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"9544",title:"Global Trade in the Emerging Business Environment",subtitle:null,isOpenForSubmission:!1,hash:"fb8cb09b9599246add78d508a98273d5",slug:"global-trade-in-the-emerging-business-environment",bookSignature:"Muhammad Mohiuddin, Jingbin Wang , Md. Samim Al Azad and Selim Ahmed",coverURL:"https://cdn.intechopen.com/books/images_new/9544.jpg",editors:[{id:"418514",title:"Dr.",name:"Muhammad",middleName:null,surname:"Mohiuddin",slug:"muhammad-mohiuddin",fullName:"Muhammad Mohiuddin"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10979",title:"Parenting",subtitle:"Challenges of Child Rearing in a Changing Society",isOpenForSubmission:!1,hash:"6f345ebcf4fd61e73643c69063a12c7b",slug:"parenting-challenges-of-child-rearing-in-a-changing-society",bookSignature:"Sayyed Ali Samadi",coverURL:"https://cdn.intechopen.com/books/images_new/10979.jpg",editors:[{id:"52145",title:"Dr.",name:"Sayyed Ali",middleName:null,surname:"Samadi",slug:"sayyed-ali-samadi",fullName:"Sayyed Ali Samadi"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"9808",title:"Contemporary Topics in Patient Safety",subtitle:"Volume 1",isOpenForSubmission:!1,hash:"fb6371607c2c6c02c6a2af8892765aba",slug:"contemporary-topics-in-patient-safety-volume-1",bookSignature:"Stanislaw P. Stawicki and Michael S. Firstenberg",coverURL:"https://cdn.intechopen.com/books/images_new/9808.jpg",editors:[{id:"181694",title:"Dr.",name:"Stanislaw P.",middleName:null,surname:"Stawicki",slug:"stanislaw-p.-stawicki",fullName:"Stanislaw P. Stawicki"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10681",title:"Biodegradation Technology of Organic and Inorganic Pollutants",subtitle:null,isOpenForSubmission:!1,hash:"9a6e10e02788092872fd249436898e97",slug:"biodegradation-technology-of-organic-and-inorganic-pollutants",bookSignature:"Kassio Ferreira Mendes, Rodrigo Nogueira de Sousa and Kamila Cabral Mielke",coverURL:"https://cdn.intechopen.com/books/images_new/10681.jpg",editors:[{id:"197720",title:"Ph.D.",name:"Kassio",middleName:null,surname:"Ferreira Mendes",slug:"kassio-ferreira-mendes",fullName:"Kassio Ferreira Mendes"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10764",title:"Antenna Systems",subtitle:null,isOpenForSubmission:!1,hash:"2fbf1c7a5d92723f08198fc9b526a8ad",slug:"antenna-systems",bookSignature:"Hussain Al-Rizzo and Said Abushamleh",coverURL:"https://cdn.intechopen.com/books/images_new/10764.jpg",editors:[{id:"153384",title:"Prof.",name:"Hussain",middleName:null,surname:"Al-Rizzo",slug:"hussain-al-rizzo",fullName:"Hussain Al-Rizzo"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10668",title:"Sustainability of Concrete With Synthetic and Recycled Aggregates",subtitle:null,isOpenForSubmission:!1,hash:"55856c6a8bc3a5b21dae5a1af09a56b6",slug:"sustainability-of-concrete-with-synthetic-and-recycled-aggregates",bookSignature:"Hosam M. Saleh",coverURL:"https://cdn.intechopen.com/books/images_new/10668.jpg",editors:[{id:"144691",title:"Prof.",name:"Hosam",middleName:null,surname:"Saleh",slug:"hosam-saleh",fullName:"Hosam Saleh"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10803",title:"Reactive Oxygen Species",subtitle:null,isOpenForSubmission:!1,hash:"176adcf090fdd1f93cb8ce3146e79ca1",slug:"reactive-oxygen-species",bookSignature:"Rizwan Ahmad",coverURL:"https://cdn.intechopen.com/books/images_new/10803.jpg",editors:[{id:"40482",title:null,name:"Rizwan",middleName:null,surname:"Ahmad",slug:"rizwan-ahmad",fullName:"Rizwan Ahmad"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"9032",title:"Corporate Social Responsibility",subtitle:null,isOpenForSubmission:!1,hash:"f609bf3251d7cc7bae0099a4374adfc3",slug:"corporate-social-responsibility",bookSignature:"Beatrice Orlando",coverURL:"https://cdn.intechopen.com/books/images_new/9032.jpg",editors:[{id:"232969",title:"Prof.",name:"Beatrice",middleName:null,surname:"Orlando",slug:"beatrice-orlando",fullName:"Beatrice Orlando"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10351",title:"Enhanced Liposuction",subtitle:"New Perspectives and Techniques",isOpenForSubmission:!1,hash:"f08ed6de16da357614586c5b58ed4dfa",slug:"enhanced-liposuction-new-perspectives-and-techniques",bookSignature:"Diane Irvine Duncan",coverURL:"https://cdn.intechopen.com/books/images_new/10351.jpg",editors:[{id:"279869",title:"Dr.",name:"Diane Irvine",middleName:null,surname:"Duncan",slug:"diane-irvine-duncan",fullName:"Diane Irvine Duncan"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10779",title:"21st Century Nanostructured Materials",subtitle:"Physics, Chemistry, Classification, and Emerging Applications in Industry, Biomedicine, and Agriculture",isOpenForSubmission:!1,hash:"72c67f97f9bef68200df115b5fd79884",slug:"21st-century-nanostructured-materials-physics-chemistry-classification-and-emerging-applications-in-industry-biomedicine-and-agriculture",bookSignature:"Phuong V. Pham",coverURL:"https://cdn.intechopen.com/books/images_new/10779.jpg",editors:[{id:"236073",title:"Dr.",name:"Phuong",middleName:"Viet",surname:"Pham",slug:"phuong-pham",fullName:"Phuong Pham"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}}],offset:12,limit:12,total:4389},hotBookTopics:{hotBooks:[],offset:0,limit:12,total:null},publish:{},publishingProposal:{success:null,errors:{}},books:{featuredBooks:[{type:"book",id:"9974",title:"E-Learning and Digital Education in the Twenty-First Century",subtitle:null,isOpenForSubmission:!1,hash:"88b58d66e975df20425fc1dfd22d53aa",slug:"e-learning-and-digital-education-in-the-twenty-first-century",bookSignature:"M. Mahruf C. Shohel",coverURL:"https://cdn.intechopen.com/books/images_new/9974.jpg",publishedDate:"May 18th 2022",numberOfDownloads:3340,editors:[{id:"94099",title:"Dr.",name:"M. Mahruf C.",middleName:null,surname:"Shohel",slug:"m.-mahruf-c.-shohel",fullName:"M. Mahruf C. Shohel"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"11001",title:"Density Functional Theory",subtitle:"Recent Advances, New Perspectives and Applications",isOpenForSubmission:!1,hash:"82d53383af78ab41eb982086c02fb2bb",slug:"density-functional-theory-recent-advances-new-perspectives-and-applications",bookSignature:"Daniel Glossman-Mitnik",coverURL:"https://cdn.intechopen.com/books/images_new/11001.jpg",publishedDate:"May 18th 2022",numberOfDownloads:1845,editors:[{id:"198499",title:"Dr.",name:"Daniel",middleName:null,surname:"Glossman-Mitnik",slug:"daniel-glossman-mitnik",fullName:"Daniel Glossman-Mitnik"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10251",title:"Plankton Communities",subtitle:null,isOpenForSubmission:!1,hash:"e11e441ca2d2d5f631b1b4704505cfb6",slug:"plankton-communities",bookSignature:"Leonel Pereira and Ana Marta Gonçalves",coverURL:"https://cdn.intechopen.com/books/images_new/10251.jpg",publishedDate:"May 18th 2022",numberOfDownloads:1096,editors:[{id:"279788",title:"Dr.",name:"Leonel",middleName:null,surname:"Pereira",slug:"leonel-pereira",fullName:"Leonel Pereira"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10830",title:"Animal Feed Science and Nutrition",subtitle:"Production, Health and Environment",isOpenForSubmission:!1,hash:"79944fc8fbbaa329aed6fde388154832",slug:"animal-feed-science-and-nutrition-production-health-and-environment",bookSignature:"Amlan Kumar Patra",coverURL:"https://cdn.intechopen.com/books/images_new/10830.jpg",publishedDate:"May 18th 2022",numberOfDownloads:995,editors:[{id:"310962",title:"Dr.",name:"Amlan",middleName:"Kumar",surname:"Patra",slug:"amlan-patra",fullName:"Amlan Patra"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10356",title:"Natural Medicinal Plants",subtitle:null,isOpenForSubmission:!1,hash:"943e56ccaaf19ff696d25aa638ae37d6",slug:"natural-medicinal-plants",bookSignature:"Hany A. El-Shemy",coverURL:"https://cdn.intechopen.com/books/images_new/10356.jpg",publishedDate:"May 11th 2022",numberOfDownloads:3791,editors:[{id:"54719",title:"Prof.",name:"Hany",middleName:null,surname:"El-Shemy",slug:"hany-el-shemy",fullName:"Hany El-Shemy"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"11752",title:"Natural Drugs from Plants",subtitle:null,isOpenForSubmission:!1,hash:"a0a83c0822608ef7592bf16a5ed0ada4",slug:"natural-drugs-from-plants",bookSignature:"Hany A. El-Shemy",coverURL:"https://cdn.intechopen.com/books/images_new/11752.jpg",publishedDate:"May 11th 2022",numberOfDownloads:2982,editors:[{id:"54719",title:"Prof.",name:"Hany",middleName:null,surname:"El-Shemy",slug:"hany-el-shemy",fullName:"Hany El-Shemy"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10853",title:"Recent Advances in Polynomials",subtitle:null,isOpenForSubmission:!1,hash:"9e8671bae09ccaa8b8e276c639a737fc",slug:"recent-advances-in-polynomials",bookSignature:"Kamal Shah",coverURL:"https://cdn.intechopen.com/books/images_new/10853.jpg",publishedDate:"May 18th 2022",numberOfDownloads:559,editors:[{id:"231748",title:"Dr.",name:"Kamal",middleName:null,surname:"Shah",slug:"kamal-shah",fullName:"Kamal Shah"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10676",title:"Recent Applications in Graph Theory",subtitle:null,isOpenForSubmission:!1,hash:"900c60742d224080732bd16bd25ccba8",slug:"recent-applications-in-graph-theory",bookSignature:"Harun Pirim",coverURL:"https://cdn.intechopen.com/books/images_new/10676.jpg",publishedDate:"May 18th 2022",numberOfDownloads:546,editors:[{id:"146092",title:"Dr.",name:"Harun",middleName:null,surname:"Pirim",slug:"harun-pirim",fullName:"Harun Pirim"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10903",title:"Genetically Modified Plants and Beyond",subtitle:null,isOpenForSubmission:!1,hash:"4d7ed4faab99c92cd4d676dc86501df9",slug:"genetically-modified-plants-and-beyond",bookSignature:"Idah Sithole Niang",coverURL:"https://cdn.intechopen.com/books/images_new/10903.jpg",publishedDate:"May 18th 2022",numberOfDownloads:539,editors:[{id:"90172",title:"Prof.",name:"Idah",middleName:null,surname:"Sithole-Niang",slug:"idah-sithole-niang",fullName:"Idah Sithole-Niang"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}},{type:"book",id:"10904",title:"Fusarium",subtitle:"An Overview of the Genus",isOpenForSubmission:!1,hash:"49d9063e43f94bd1517d65fbc58b93c3",slug:"fusarium-an-overview-of-the-genus",bookSignature:"Seyed Mahyar Mirmajlessi",coverURL:"https://cdn.intechopen.com/books/images_new/10904.jpg",publishedDate:"May 18th 2022",numberOfDownloads:535,editors:[{id:"100573",title:"Dr.",name:"Seyed Mahyar",middleName:null,surname:"Mirmajlessi",slug:"seyed-mahyar-mirmajlessi",fullName:"Seyed Mahyar Mirmajlessi"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter"}}],latestBooks:[{type:"book",id:"10251",title:"Plankton Communities",subtitle:null,isOpenForSubmission:!1,hash:"e11e441ca2d2d5f631b1b4704505cfb6",slug:"plankton-communities",bookSignature:"Leonel Pereira and Ana Marta Gonçalves",coverURL:"https://cdn.intechopen.com/books/images_new/10251.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"279788",title:"Dr.",name:"Leonel",middleName:null,surname:"Pereira",slug:"leonel-pereira",fullName:"Leonel Pereira"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"10830",title:"Animal Feed Science and Nutrition",subtitle:"Production, Health and Environment",isOpenForSubmission:!1,hash:"79944fc8fbbaa329aed6fde388154832",slug:"animal-feed-science-and-nutrition-production-health-and-environment",bookSignature:"Amlan Kumar Patra",coverURL:"https://cdn.intechopen.com/books/images_new/10830.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"310962",title:"Dr.",name:"Amlan",middleName:"Kumar",surname:"Patra",slug:"amlan-patra",fullName:"Amlan Patra"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"10853",title:"Recent Advances in Polynomials",subtitle:null,isOpenForSubmission:!1,hash:"9e8671bae09ccaa8b8e276c639a737fc",slug:"recent-advances-in-polynomials",bookSignature:"Kamal Shah",coverURL:"https://cdn.intechopen.com/books/images_new/10853.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"231748",title:"Dr.",name:"Kamal",middleName:null,surname:"Shah",slug:"kamal-shah",fullName:"Kamal Shah"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"10871",title:"Computed-Tomography (CT) Scan",subtitle:null,isOpenForSubmission:!1,hash:"966d8cf74fa27eea1b9cbc9a6ee94993",slug:"computed-tomography-ct-scan",bookSignature:"Reda R. Gharieb",coverURL:"https://cdn.intechopen.com/books/images_new/10871.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"225387",title:"Prof.",name:"Reda R.",middleName:"R.",surname:"Gharieb",slug:"reda-r.-gharieb",fullName:"Reda R. Gharieb"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"10903",title:"Genetically Modified Plants and Beyond",subtitle:null,isOpenForSubmission:!1,hash:"4d7ed4faab99c92cd4d676dc86501df9",slug:"genetically-modified-plants-and-beyond",bookSignature:"Idah Sithole Niang",coverURL:"https://cdn.intechopen.com/books/images_new/10903.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"90172",title:"Prof.",name:"Idah",middleName:null,surname:"Sithole-Niang",slug:"idah-sithole-niang",fullName:"Idah Sithole-Niang"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"10904",title:"Fusarium",subtitle:"An Overview of the Genus",isOpenForSubmission:!1,hash:"49d9063e43f94bd1517d65fbc58b93c3",slug:"fusarium-an-overview-of-the-genus",bookSignature:"Seyed Mahyar Mirmajlessi",coverURL:"https://cdn.intechopen.com/books/images_new/10904.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"100573",title:"Dr.",name:"Seyed Mahyar",middleName:null,surname:"Mirmajlessi",slug:"seyed-mahyar-mirmajlessi",fullName:"Seyed Mahyar Mirmajlessi"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"10654",title:"Brain-Computer Interface",subtitle:null,isOpenForSubmission:!1,hash:"a5308884068cc53ed31c6baba756857f",slug:"brain-computer-interface",bookSignature:"Vahid Asadpour",coverURL:"https://cdn.intechopen.com/books/images_new/10654.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"165328",title:"Dr.",name:"Vahid",middleName:null,surname:"Asadpour",slug:"vahid-asadpour",fullName:"Vahid Asadpour"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"10676",title:"Recent Applications in Graph Theory",subtitle:null,isOpenForSubmission:!1,hash:"900c60742d224080732bd16bd25ccba8",slug:"recent-applications-in-graph-theory",bookSignature:"Harun Pirim",coverURL:"https://cdn.intechopen.com/books/images_new/10676.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"146092",title:"Dr.",name:"Harun",middleName:null,surname:"Pirim",slug:"harun-pirim",fullName:"Harun Pirim"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"11196",title:"New Updates in E-Learning",subtitle:null,isOpenForSubmission:!1,hash:"6afaadf68e2a0a4b370ac5ceb5ca89c6",slug:"new-updates-in-e-learning",bookSignature:"Eduard Babulak",coverURL:"https://cdn.intechopen.com/books/images_new/11196.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"10086",title:"Prof.",name:"Eduard",middleName:null,surname:"Babulak",slug:"eduard-babulak",fullName:"Eduard Babulak"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"9974",title:"E-Learning and Digital Education in the Twenty-First Century",subtitle:null,isOpenForSubmission:!1,hash:"88b58d66e975df20425fc1dfd22d53aa",slug:"e-learning-and-digital-education-in-the-twenty-first-century",bookSignature:"M. Mahruf C. Shohel",coverURL:"https://cdn.intechopen.com/books/images_new/9974.jpg",editedByType:"Edited by",publishedDate:"May 18th 2022",editors:[{id:"94099",title:"Dr.",name:"M. Mahruf C.",middleName:null,surname:"Shohel",slug:"m.-mahruf-c.-shohel",fullName:"M. Mahruf C. Shohel"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}}]},subject:{topic:{id:"105",title:"Marine Biology",slug:"earth-and-planetary-sciences-marine-biology",parent:{id:"10",title:"Earth and Planetary Sciences",slug:"earth-and-planetary-sciences"},numberOfBooks:15,numberOfSeries:0,numberOfAuthorsAndEditors:375,numberOfWosCitations:325,numberOfCrossrefCitations:236,numberOfDimensionsCitations:488,videoUrl:null,fallbackUrl:null,description:null},booksByTopicFilter:{topicId:"105",sort:"-publishedDate",limit:12,offset:0},booksByTopicCollection:[{type:"book",id:"9243",title:"Coastal Environments",subtitle:null,isOpenForSubmission:!1,hash:"8e05e5f631e935eef366980f2e28295d",slug:"coastal-environments",bookSignature:"Yuanzhi Zhang and X. San Liang",coverURL:"https://cdn.intechopen.com/books/images_new/9243.jpg",editedByType:"Edited by",editors:[{id:"77597",title:"Prof.",name:"Yuanzhi",middleName:null,surname:"Zhang",slug:"yuanzhi-zhang",fullName:"Yuanzhi Zhang"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"8882",title:"Advances in the Studies of the Benthic Zone",subtitle:null,isOpenForSubmission:!1,hash:"79f77db18a383e92371a06aa07937f90",slug:"advances-in-the-studies-of-the-benthic-zone",bookSignature:"Luis A. Soto",coverURL:"https://cdn.intechopen.com/books/images_new/8882.jpg",editedByType:"Edited by",editors:[{id:"256002",title:"Ph.D.",name:"Luis",middleName:null,surname:"Soto",slug:"luis-soto",fullName:"Luis Soto"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"7746",title:"Lagoon Environments Around the World",subtitle:"A Scientific Perspective",isOpenForSubmission:!1,hash:"372053f50e624aa8f1e2269abb0a246d",slug:"lagoon-environments-around-the-world-a-scientific-perspective",bookSignature:"Andrew J. Manning",coverURL:"https://cdn.intechopen.com/books/images_new/7746.jpg",editedByType:"Edited by",editors:[{id:"23008",title:"Prof.",name:"Andrew James",middleName:null,surname:"Manning",slug:"andrew-james-manning",fullName:"Andrew James Manning"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"8159",title:"Crustacea",subtitle:null,isOpenForSubmission:!1,hash:"a1d529af4d4f995de30137efc9a7b02e",slug:"crustacea",bookSignature:"Genaro Diarte-Plata and Ruth Escamilla-Montes",coverURL:"https://cdn.intechopen.com/books/images_new/8159.jpg",editedByType:"Edited by",editors:[{id:"198991",title:"Dr.",name:"Genaro",middleName:null,surname:"Diarte-Plata",slug:"genaro-diarte-plata",fullName:"Genaro Diarte-Plata"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"8421",title:"Invertebrates",subtitle:"Ecophysiology and Management",isOpenForSubmission:!1,hash:"524faf733c0ebf32b356f89b2148e6de",slug:"invertebrates-ecophysiology-and-management",bookSignature:"Sajal Ray, Genaro Diarte-Plata and Ruth Escamilla-Montes",coverURL:"https://cdn.intechopen.com/books/images_new/8421.jpg",editedByType:"Edited by",editors:[{id:"173697",title:"Prof.",name:"Sajal",middleName:null,surname:"Ray",slug:"sajal-ray",fullName:"Sajal Ray"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"7912",title:"Biological Research in Aquatic Science",subtitle:null,isOpenForSubmission:!1,hash:"8f86a91e9a5c76a2d11a861d879bc96a",slug:"biological-research-in-aquatic-science",bookSignature:"Yusuf Bozkurt",coverURL:"https://cdn.intechopen.com/books/images_new/7912.jpg",editedByType:"Edited by",editors:[{id:"90846",title:"Prof.",name:"Yusuf",middleName:null,surname:"Bozkurt",slug:"yusuf-bozkurt",fullName:"Yusuf Bozkurt"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"6411",title:"Mangrove Ecosystem Ecology and Function",subtitle:null,isOpenForSubmission:!1,hash:"5425ea4e90ed12b902f30186f807f8f5",slug:"mangrove-ecosystem-ecology-and-function",bookSignature:"Sahadev Sharma",coverURL:"https://cdn.intechopen.com/books/images_new/6411.jpg",editedByType:"Edited by",editors:[{id:"227169",title:"Ph.D.",name:"Sahadev",middleName:null,surname:"Sharma",slug:"sahadev-sharma",fullName:"Sahadev Sharma"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"6645",title:"Seabirds",subtitle:null,isOpenForSubmission:!1,hash:"6ce1372af411b6ada3b53e881f7b85fc",slug:"seabirds",bookSignature:"Heimo Mikkola",coverURL:"https://cdn.intechopen.com/books/images_new/6645.jpg",editedByType:"Edited by",editors:[{id:"144330",title:"Dr.",name:"Heimo",middleName:"Juhani",surname:"Mikkola",slug:"heimo-mikkola",fullName:"Heimo Mikkola"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"6266",title:"Marine Ecology",subtitle:"Biotic and Abiotic Interactions",isOpenForSubmission:!1,hash:"9d821ed950a497c8f50de67abf419259",slug:"marine-ecology-biotic-and-abiotic-interactions",bookSignature:"Muhammet Türkoğlu, Umur Önal and Ali Ismen",coverURL:"https://cdn.intechopen.com/books/images_new/6266.jpg",editedByType:"Edited by",editors:[{id:"99483",title:"Prof.",name:"Muhammet",middleName:null,surname:"Turkoglu",slug:"muhammet-turkoglu",fullName:"Muhammet Turkoglu"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"6344",title:"Biological Resources of Water",subtitle:null,isOpenForSubmission:!1,hash:"ca4f407275697c7cf547debc6b1e85a9",slug:"biological-resources-of-water",bookSignature:"Sajal Ray",coverURL:"https://cdn.intechopen.com/books/images_new/6344.jpg",editedByType:"Edited by",editors:[{id:"173697",title:"Prof.",name:"Sajal",middleName:null,surname:"Ray",slug:"sajal-ray",fullName:"Sajal Ray"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"5765",title:"Corals in a Changing World",subtitle:null,isOpenForSubmission:!1,hash:"eed323f414d06a6bd994cc9d37ad24c4",slug:"corals-in-a-changing-world",bookSignature:"Carmenza Duque Beltran and Edisson Tello Camacho",coverURL:"https://cdn.intechopen.com/books/images_new/5765.jpg",editedByType:"Edited by",editors:[{id:"155319",title:"Emeritus Prof.",name:"Carmenza",middleName:null,surname:"Duque",slug:"carmenza-duque",fullName:"Carmenza Duque"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}},{type:"book",id:"3517",title:"Topics in Oceanography",subtitle:null,isOpenForSubmission:!1,hash:"cbe56ad1fcc5e5d113b608b6596a928a",slug:"topics-in-oceanography",bookSignature:"Enrico Zambianchi",coverURL:"https://cdn.intechopen.com/books/images_new/3517.jpg",editedByType:"Edited by",editors:[{id:"150979",title:"Prof.",name:"Enrico",middleName:null,surname:"Zambianchi",slug:"enrico-zambianchi",fullName:"Enrico Zambianchi"}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null,productType:{id:"1",chapterContentType:"chapter",authoredCaption:"Edited by"}}],booksByTopicTotal:15,seriesByTopicCollection:[],seriesByTopicTotal:0,mostCitedChapters:[{id:"45249",doi:"10.5772/56414",title:"Challenges and New Advances in Ocean Color Remote Sensing of Coastal Waters",slug:"challenges-and-new-advances-in-ocean-color-remote-sensing-of-coastal-waters",totalDownloads:3255,totalCrossrefCites:11,totalDimensionsCites:26,abstract:null,book:{id:"3517",slug:"topics-in-oceanography",title:"Topics in Oceanography",fullTitle:"Topics in Oceanography"},signatures:"Hubert Loisel, Vincent Vantrepotte, Cédric Jamet and Dinh Ngoc\nDat",authors:[{id:"66224",title:"Prof.",name:"Hubert",middleName:null,surname:"Loisel",slug:"hubert-loisel",fullName:"Hubert Loisel"},{id:"99752",title:"Dr.",name:"Cédric",middleName:null,surname:"Jamet",slug:"cedric-jamet",fullName:"Cédric Jamet"},{id:"163462",title:"Dr.",name:"Vincent",middleName:null,surname:"Vantrepotte",slug:"vincent-vantrepotte",fullName:"Vincent Vantrepotte"},{id:"167707",title:"MSc.",name:"Dat",middleName:null,surname:"Dinh Ngoc",slug:"dat-dinh-ngoc",fullName:"Dat Dinh Ngoc"}]},{id:"20922",doi:"10.5772/21416",title:"Sediment Transport and River Channel Dynamics in Romania – Variability and Control Factors",slug:"sediment-transport-and-river-channel-dynamics-in-romania-variability-and-control-factors",totalDownloads:3051,totalCrossrefCites:10,totalDimensionsCites:25,abstract:null,book:{id:"304",slug:"sediment-transport-in-aquatic-environments",title:"Sediment Transport in Aquatic Environments",fullTitle:"Sediment Transport in Aquatic Environments"},signatures:"Liliana Zaharia, Florina Grecu, Gabriela Ioana-Toroimac and Gianina Neculau",authors:[{id:"43010",title:"Prof.",name:"Liliana",middleName:null,surname:"Zaharia",slug:"liliana-zaharia",fullName:"Liliana Zaharia"},{id:"55977",title:"Dr.",name:"Gabriela",middleName:null,surname:"Ioana-Toroimac",slug:"gabriela-ioana-toroimac",fullName:"Gabriela Ioana-Toroimac"},{id:"91185",title:"Prof.",name:"Grecu",middleName:null,surname:"Florina",slug:"grecu-florina",fullName:"Grecu Florina"},{id:"91186",title:"Dr.",name:"Gianina",middleName:null,surname:"Neculau",slug:"gianina-neculau",fullName:"Gianina Neculau"}]},{id:"66461",doi:"10.5772/intechopen.85139",title:"Fish Sperm Physiology: Structure, Factors Regulating Motility, and Motility Evaluation",slug:"fish-sperm-physiology-structure-factors-regulating-motility-and-motility-evaluation",totalDownloads:1840,totalCrossrefCites:10,totalDimensionsCites:25,abstract:"For reproduction, most fish species adopt external fertilization: their spermatozoa are delivered in the external milieu (marine- or freshwater) that represents both a drastic environment and a source of signals that control the motility function. This chapter is an updated overview of the signaling pathways going from external signals such as osmolarity and ionic concentration and their membrane reception to their transduction through the membrane and their final reception at the flagellar axoneme level. Additional factors such as energy management will be addressed as they constitute a limiting factor of the motility period of fish spermatozoa. Modern technologies used nowadays for quantitative description of fish sperm flagella in movement will be briefly described as they are more and more needed for prediction of the quality of sperm used for artificial propagation of many fish species used in aquaculture. The chapter will present some applications of these technologies and the information to which they allow access in some aquaculture species.",book:{id:"7912",slug:"biological-research-in-aquatic-science",title:"Biological Research in Aquatic Science",fullTitle:"Biological Research in Aquatic Science"},signatures:"Jacky Cosson",authors:[{id:"188281",title:"Dr.",name:"Jacky",middleName:null,surname:"Cosson",slug:"jacky-cosson",fullName:"Jacky Cosson"}]},{id:"20911",doi:"10.5772/19948",title:"The Significance of Suspended Sediment Transport Determination on the Amazonian Hydrological Scenario",slug:"the-significance-of-suspended-sediment-transport-determination-on-the-amazonian-hydrological-scenari",totalDownloads:4130,totalCrossrefCites:13,totalDimensionsCites:24,abstract:null,book:{id:"304",slug:"sediment-transport-in-aquatic-environments",title:"Sediment Transport in Aquatic Environments",fullTitle:"Sediment Transport in Aquatic Environments"},signatures:"Naziano Filizola, Jean-Loup Guyot, Hella Wittmann, Jean-Michel Martinez and Eurides de Oliveira",authors:[{id:"36890",title:"Dr.",name:"Naziano",middleName:null,surname:"Filizola",slug:"naziano-filizola",fullName:"Naziano Filizola"},{id:"60004",title:"Dr.",name:"Jean-Michel",middleName:null,surname:"Martinez",slug:"jean-michel-martinez",fullName:"Jean-Michel Martinez"},{id:"60005",title:"Dr.",name:"Jean-Loup",middleName:null,surname:"Guyot",slug:"jean-loup-guyot",fullName:"Jean-Loup Guyot"},{id:"102592",title:"Dr.",name:"Hella",middleName:null,surname:"Wittmann",slug:"hella-wittmann",fullName:"Hella Wittmann"},{id:"102593",title:"Mr.",name:"Eurides",middleName:null,surname:"De Oliveira",slug:"eurides-de-oliveira",fullName:"Eurides De Oliveira"}]},{id:"45198",doi:"10.5772/56105",title:"Stable Isotope Methods for the Study of the Nitrogen Cycle",slug:"stable-isotope-methods-for-the-study-of-the-nitrogen-cycle",totalDownloads:4680,totalCrossrefCites:11,totalDimensionsCites:18,abstract:null,book:{id:"3517",slug:"topics-in-oceanography",title:"Topics in Oceanography",fullTitle:"Topics in Oceanography"},signatures:"Evgenia Ryabenko",authors:[{id:"163463",title:"Dr.",name:"Evgenia",middleName:null,surname:"Ryabenko",slug:"evgenia-ryabenko",fullName:"Evgenia Ryabenko"}]}],mostDownloadedChaptersLast30Days:[{id:"60368",title:"Biological and Medicinal Importance of Sponge",slug:"biological-and-medicinal-importance-of-sponge",totalDownloads:2505,totalCrossrefCites:1,totalDimensionsCites:3,abstract:"Sponges are multicellular, heterotrophic parazoan organisms, characterized by the possession of unique feeding system among the animals. They are the most primitive types of animals in existence, featuring a cell-based organization where different cells have different tasks, but do not form tissues. Sponges (Porifera) are a predominantly marine phylum living from the intertidal to the abyssal (deepest ocean) zone. There are approximately 8500 described species of sponges worldwide with a prominent role in many reef coral communities. Several ecological studies reported have shown that secondary metabolites isolated from sponges often serve defensive purposes to protect them from threats such as predator attacks, biofouling, microbial infections, and overgrowth by other sessile organisms. In the recent years, interest in marine sponges has risen considerably due to presence of high number of interesting biologically active natural products. More than 5300 different natural products are known from sponges and their associated microorganisms, and every year hundreds of new substances are discovered. In addition to the unusual nucleosides, other classes of substances such as bioactive terpenes, sterols, fatty acids, alkaloids, cyclic peptides, peroxides, and amino acid derivatives (which are frequently halogenated) have been described from sponges or from their associated microorganisms. Many of these natural products from sponges have shown a wide range of pharmacological activities such as anticancer, antifungal, antiviral, anthelmintic, antiprotozoal, anti-inflammatory, immunosuppressive, neurosuppressive, and antifouling activities. This chapter covers extensive work published regarding new compounds isolated from marine sponges and biological activities associated with them.",book:{id:"6344",slug:"biological-resources-of-water",title:"Biological Resources of Water",fullTitle:"Biological Resources of Water"},signatures:"Musarat Amina and Nawal M. Al Musayeib",authors:[{id:"213049",title:"Dr.",name:"Musarat",middleName:null,surname:"Amina",slug:"musarat-amina",fullName:"Musarat Amina"},{id:"213050",title:"Dr.",name:"Nawal",middleName:null,surname:"M. Al Musayeib",slug:"nawal-m.-al-musayeib",fullName:"Nawal M. Al Musayeib"}]},{id:"59865",title:"Marine Fisheries in Nigeria: A Review",slug:"marine-fisheries-in-nigeria-a-review",totalDownloads:3853,totalCrossrefCites:8,totalDimensionsCites:10,abstract:"Fisheries production especially from marine is important for the socio-economic development of Nigerians and its contribution to the nation’s economic growth through the Gross Domestic Product (GDP). Nigeria is blessed with enough marine fisheries resources that could enhance increased fish production. Yet, fish supply from domestic production is far below the fish demand of her citizens. This chapter is therefore focused on marine fisheries in Nigeria. We adopted a desk review approach. This chapter is divided into different sections such as the Nigerian fisheries sector, marine fisheries resources in Nigeria, status of marine fisheries production in Nigeria, marine fisheries regulations, and constraints to optimal marine fisheries production in Nigeria. We concluded that the contribution of aquaculture to marine fisheries production has been low, compared to the marine capture fisheries production. Also, we noted that despite the availability of regulations, noncompliance by fisher folks has not helped to optimize marine fisheries production. We therefore recommended that the culture of marine fishes should be intensified. Marine waters should also be protected against destruction and pollution as a result of human activities. Available marine fisheries regulations should be enforced and violators of the regulations should be punished as stipulated in the regulations.",book:{id:"6266",slug:"marine-ecology-biotic-and-abiotic-interactions",title:"Marine Ecology",fullTitle:"Marine Ecology - Biotic and Abiotic Interactions"},signatures:"Olalekan Jacob Olaoye and Wahab Gbenga Ojebiyi",authors:null},{id:"57327",title:"Closed Aquaculture System: Zero Water Discharge for Shrimp and Prawn Farming in Indonesia",slug:"closed-aquaculture-system-zero-water-discharge-for-shrimp-and-prawn-farming-in-indonesia",totalDownloads:2465,totalCrossrefCites:2,totalDimensionsCites:3,abstract:"This chapter focuses on the development and application of zero water discharge (ZWD) system, which has become an alternative solution to conventional methods of aquaculture production. With this system, it is expected to answer many issues in aquaculture cultivation, such as environmental damage, disease outbreak, and land-use change, and to create a sustainable aquaculture cultivation system. ZWD system is an improved batch system with an emphasis on microbial manipulation in rearing tank. The principle of microbial selection is based on the role of each microbial component in nutrient cycle in the rearing tank. This chapter contains in detail how methods and stages are performed in order to conduct this system, including design of construction system, cultivation of microbial components, initial conditioning of this system, and microbial manipulation. The performance of the system was tested in crustacean culture such as white shrimp and giant freshwater prawns, and it showed that the system can increase the average survival rate of 10–20%. In addition, the technical and economic feasibility of this system was evaluated to illustrate the production efficiency upon the application of this system in the industry.",book:{id:"6344",slug:"biological-resources-of-water",title:"Biological Resources of Water",fullTitle:"Biological Resources of Water"},signatures:"Gede Suantika, Magdalena Lenny Situmorang, Pingkan Aditiawati,\nDea Indriani Astuti, Fahma Fiqhiyyah Nur Azizah and Harish\nMuhammad",authors:[{id:"216920",title:"Dr.",name:"Gede",middleName:null,surname:"Suantika",slug:"gede-suantika",fullName:"Gede Suantika"},{id:"220079",title:"Dr.",name:"Magdalena Lenny",middleName:null,surname:"Situmorang",slug:"magdalena-lenny-situmorang",fullName:"Magdalena Lenny Situmorang"},{id:"220081",title:"Dr.",name:"Pingkan",middleName:null,surname:"Aditiawati",slug:"pingkan-aditiawati",fullName:"Pingkan Aditiawati"},{id:"220082",title:"Dr.",name:"Dea Indriani",middleName:null,surname:"Astuti",slug:"dea-indriani-astuti",fullName:"Dea Indriani Astuti"},{id:"220083",title:"MSc.",name:"Fahma Fiqhiyyah Nur",middleName:null,surname:"Azizah",slug:"fahma-fiqhiyyah-nur-azizah",fullName:"Fahma Fiqhiyyah Nur Azizah"}]},{id:"59973",title:"Genetic Applications in the Conservation of Neotropical Freshwater Fish",slug:"genetic-applications-in-the-conservation-of-neotropical-freshwater-fish",totalDownloads:1627,totalCrossrefCites:3,totalDimensionsCites:8,abstract:"Neotropical fish correspond to approximately 30% of all fish species worldwide. The diversity of fish species found in Neotropical basins reflects variations in life-history strategies and exhibition of particular morphological, physiological and ecological attributes. These attributes are mainly related to different forms of feeding, life maintenance and reproduction. Today, fish populations are being threatened by anthropogenic actions that are having a visible impact on the natural state of continental aquatic ecosystems. The main causes are overfishing, non-native species introduction, reservoir-dam systems, mining, pollution and deforestation. The biology and population dynamics of the species are still unclear due to lack of research. Genetic tools can be useful resources for the conservation of Neotropical fish species in several ways. Molecular genetic markers are considered powerful tools to identify cryptic and hybrid fish and also allow the evaluation of the genetic variability and structure of populations of Neotropical ichthyofauna. Several analyses of molecular markers have been performed on Neotropical fish, including allozyme analysis, restriction fragment length polymorphisms in regions of DNA (RFLP), randomly amplified polymorphic DNA (AFLP), randomly amplified polymorphic DNA (RAPD), microsatellites, single nucleotide polymorphisms (SNPs) and mitochondrial DNA (mtDNA) markers. In order to analyse a high number of markers, next generation sequencing has allowed researchers to generate a large amount of genomic information that can be applied to the conservation of Neotropical fish.",book:{id:"6344",slug:"biological-resources-of-water",title:"Biological Resources of Water",fullTitle:"Biological Resources of Water"},signatures:"Vito Antonio Mastrochirico Filho, Milena V. Freitas, Raquel B.\nAriede, Lieschen V.G. Lira, Natália J. Mendes and Diogo T.\nHashimoto",authors:[{id:"215385",title:"Dr.",name:"Diogo",middleName:null,surname:"Hashimoto",slug:"diogo-hashimoto",fullName:"Diogo Hashimoto"},{id:"226741",title:"MSc.",name:"Vito",middleName:null,surname:"Matrochirico-Filho",slug:"vito-matrochirico-filho",fullName:"Vito Matrochirico-Filho"},{id:"226743",title:"MSc.",name:"Milena",middleName:null,surname:"Freitas",slug:"milena-freitas",fullName:"Milena Freitas"},{id:"226744",title:"MSc.",name:"Raquel",middleName:null,surname:"Ariede",slug:"raquel-ariede",fullName:"Raquel Ariede"},{id:"226745",title:"MSc.",name:"Natália",middleName:null,surname:"Mendes",slug:"natalia-mendes",fullName:"Natália Mendes"},{id:"226746",title:"MSc.",name:"Lieschen",middleName:null,surname:"Lira",slug:"lieschen-lira",fullName:"Lieschen Lira"}]},{id:"62582",title:"Mangrove Species Distribution and Composition, Adaptive Strategies and Ecosystem Services in the Niger River Delta, Nigeria",slug:"mangrove-species-distribution-and-composition-adaptive-strategies-and-ecosystem-services-in-the-nige",totalDownloads:2139,totalCrossrefCites:5,totalDimensionsCites:11,abstract:"Mangroves of the Niger River Delta grade into several plant communities from land to sea. This mangrove is a biodiversity hot spot, and one of the richest in ecosystem services in the world, but due to lack of data it is often not mentioned in many global mangrove studies. Inland areas are sandy and mostly inhabited by button wood mangroves (Conocarpus erectus) and grass species while seaward areas are mostly inhabited by red (Rhizophora racemosa), black (Laguncularia racemosa) and white (Avicennia germinans) mangroves species. Anthropogenic activities such as oil and gas exploration, deforestation, dredging, urbanization and invasive nypa palms had changed the soil type from swampy to sandy mud soil. Muddy soil supports nypa palms while sandy soil supports different grass species, core mangrove soil supports red mangroves (R. racemosa), which are the most dominant of all species, with importance value (Iv) of 52.02. The red mangroves are adapted to the swampy soils. They possess long root system (i.e. 10 m) that originates from the tree stem to the ground, to provide extra support. The red mangrove trees are economically most viable as the main source of fire wood for cooking, medicinal herbs and dyes for clothes.",book:{id:"6411",slug:"mangrove-ecosystem-ecology-and-function",title:"Mangrove Ecosystem Ecology and Function",fullTitle:"Mangrove Ecosystem Ecology and Function"},signatures:"Aroloye O. Numbere",authors:[{id:"215285",title:"Dr.",name:"Aroloye O.",middleName:null,surname:"Numbere",slug:"aroloye-o.-numbere",fullName:"Aroloye O. Numbere"}]}],onlineFirstChaptersFilter:{topicId:"105",limit:6,offset:0},onlineFirstChaptersCollection:[],onlineFirstChaptersTotal:0},preDownload:{success:null,errors:{}},subscriptionForm:{success:null,errors:{}},aboutIntechopen:{},privacyPolicy:{},peerReviewing:{},howOpenAccessPublishingWithIntechopenWorks:{},sponsorshipBooks:{sponsorshipBooks:[],offset:8,limit:8,total:0},allSeries:{pteSeriesList:[{id:"14",title:"Artificial Intelligence",numberOfPublishedBooks:9,numberOfPublishedChapters:87,numberOfOpenTopics:6,numberOfUpcomingTopics:0,issn:"2633-1403",doi:"10.5772/intechopen.79920",isOpenForSubmission:!0},{id:"7",title:"Biomedical Engineering",numberOfPublishedBooks:12,numberOfPublishedChapters:98,numberOfOpenTopics:3,numberOfUpcomingTopics:0,issn:"2631-5343",doi:"10.5772/intechopen.71985",isOpenForSubmission:!0}],lsSeriesList:[{id:"11",title:"Biochemistry",numberOfPublishedBooks:27,numberOfPublishedChapters:287,numberOfOpenTopics:4,numberOfUpcomingTopics:0,issn:"2632-0983",doi:"10.5772/intechopen.72877",isOpenForSubmission:!0},{id:"25",title:"Environmental Sciences",numberOfPublishedBooks:1,numberOfPublishedChapters:9,numberOfOpenTopics:4,numberOfUpcomingTopics:0,issn:"2754-6713",doi:"10.5772/intechopen.100362",isOpenForSubmission:!0},{id:"10",title:"Physiology",numberOfPublishedBooks:11,numberOfPublishedChapters:139,numberOfOpenTopics:4,numberOfUpcomingTopics:0,issn:"2631-8261",doi:"10.5772/intechopen.72796",isOpenForSubmission:!0}],hsSeriesList:[{id:"3",title:"Dentistry",numberOfPublishedBooks:8,numberOfPublishedChapters:129,numberOfOpenTopics:0,numberOfUpcomingTopics:2,issn:"2631-6218",doi:"10.5772/intechopen.71199",isOpenForSubmission:!1},{id:"6",title:"Infectious Diseases",numberOfPublishedBooks:13,numberOfPublishedChapters:107,numberOfOpenTopics:3,numberOfUpcomingTopics:1,issn:"2631-6188",doi:"10.5772/intechopen.71852",isOpenForSubmission:!0},{id:"13",title:"Veterinary Medicine and Science",numberOfPublishedBooks:10,numberOfPublishedChapters:103,numberOfOpenTopics:3,numberOfUpcomingTopics:0,issn:"2632-0517",doi:"10.5772/intechopen.73681",isOpenForSubmission:!0}],sshSeriesList:[{id:"22",title:"Business, Management and Economics",numberOfPublishedBooks:1,numberOfPublishedChapters:12,numberOfOpenTopics:2,numberOfUpcomingTopics:1,issn:null,doi:"10.5772/intechopen.100359",isOpenForSubmission:!0},{id:"23",title:"Education and Human Development",numberOfPublishedBooks:0,numberOfPublishedChapters:0,numberOfOpenTopics:2,numberOfUpcomingTopics:0,issn:null,doi:"10.5772/intechopen.100360",isOpenForSubmission:!1},{id:"24",title:"Sustainable Development",numberOfPublishedBooks:0,numberOfPublishedChapters:10,numberOfOpenTopics:4,numberOfUpcomingTopics:1,issn:null,doi:"10.5772/intechopen.100361",isOpenForSubmission:!0}],testimonialsList:[{id:"13",text:"The collaboration with and support of the technical staff of IntechOpen is fantastic. The whole process of submitting an article and editing of the submitted article goes extremely smooth and fast, the number of reads and downloads of chapters is high, and the contributions are also frequently cited.",author:{id:"55578",name:"Antonio",surname:"Jurado-Navas",institutionString:null,profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRisIQAS/Profile_Picture_1626166543950",slug:"antonio-jurado-navas",institution:{id:"720",name:"University of Malaga",country:{id:null,name:"Spain"}}}},{id:"6",text:"It is great to work with the IntechOpen to produce a worthwhile collection of research that also becomes a great educational resource and guide for future research endeavors.",author:{id:"259298",name:"Edward",surname:"Narayan",institutionString:null,profilePictureURL:"https://mts.intechopen.com/storage/users/259298/images/system/259298.jpeg",slug:"edward-narayan",institution:{id:"3",name:"University of Queensland",country:{id:null,name:"Australia"}}}}]},series:{item:{id:"24",title:"Sustainable Development",doi:"10.5772/intechopen.100361",issn:null,scope:"