\r\n\tOver the years, the concept of maintenance became more comprehensive, reducing fault occurrence and increasing industrial system availability. Besides, reliability, safety, and criticality requirements were associated with the system or equipment under analysis. Maintenance strategies or schemes can be classified as corrective (run-to-break), preventive (time-based), and predictive (condition-based maintenance). Corrective maintenance is only performed after an occurrence of a fault. Therefore, it involves unexpected breakdowns, high costs, changes in the production chain, and it could lead to catastrophic events. Preventive maintenance and interventions occur based on a scheduled maintenance plan or the equipment's mean time between failures. Although it is more effective than corrective maintenance, unexpected failure may still occur by preventing most failures. Additionally, the process cost is still high, especially the costs associated with labor, inventory, and unnecessary replacement of equipment or components.
\r\n\tOn the other hand, predictive maintenance analyses the equipment condition so that a possible fault can still be identified at an early stage. Predictive maintenance aims to identify a machine anomaly so that it does not result in a fault. Such maintenance involves advanced monitoring, processing, and signal analysis techniques, which are generally performed non-invasively and, in many cases, in real-time. In the case of machines or processes, these techniques can be developed based on vibration, temperature, acoustic emission, or electrical current signal monitoring. It should be noted that monitoring such signals or parameters to verify the operating condition is called condition monitoring. Condition monitoring aims to observe the machine's current operational condition and predict its future condition, keeping it under a systematic analysis during its remaining life. In this sense, a fault condition can be detected and identified from systematic machine condition monitoring. A diagnosis procedure can be established, whereby properly investigating the fault symptoms and prognosis.
\r\n\t
\r\n\tThis book will aim to merge all these ideas in a single volume, aggregate new maintenance experiences, apply new techniques and approaches, and report field experiences to establish new maintenance processes and management paradigms.
\r\n\t
Improvements in medical care have significantly extended life expectancies, upwardly shifting demographic indicators of the elderly worldwide. Coupled with falling birth rates, however, the number of patients suffering cognitive deficits has also increased. World Health Organization projections, for example, indicate that by 2050, more than 20% will fall in this sector, with considerably higher percentages in developed nations, placing large numbers of individuals at risk [1]. Among the elderly the most prevalent neurodegenerative disease is Alzheimer’s disease (AD) with a lifetime risk above 60 of 33% for males and 45% for females. Its growth rate is anticipated to exceed nearly 100% that of current levels in developed nations and more than 300% in Southeast Asian countries [2]. These increases in age-related diseases, moreover, add to an already significant burden from such prevalent mental health diseases as schizophrenia and bipolar disorder.
\nSymptomatically, prevalent diseases like AD and Korsakoff’s syndrome, exhibit profound memory losses. In AD a broad consensus posits that its early symptoms include memory lapses that involve episodic memory, semantic recall, and visual orienting [3]. Among its earliest is an impaired sense of smell, a feature that may relate to evolutionary survival value. With the progression of AD, recent memories fade, and there is a proportionately greater retention of older ones, a characteristic observation termed Ribot’s law.
\nDefined as a process of encoding, storing, and retrieving sensorial or mental information, memory dysfunctions induced by AD may be functionally interpreted as to the manner by which one or more of these phases are affected. Accordingly, the loss of formed memories, or retrograde amnesia, observed in AD patients, can be explained either by a loss of stored memories or an inability to retrieve them. In fact, existing evidence suggests that both phases are affected. Anatomical studies, for example, show a deterioration of thinly myelinated regions like the hippocampus relatively early in the disease progression compared to other regions [4]. Since the hippocampus is a critical center for recently formed memories, this evidence is consistent with loss of memories, particularly those that have formed first.
\nOn the other hand, the disease is known to also specifically affect DMN operation [5], a domain thought to be critical to forming the self-construct. First identified by nuclear imaging studies that showed consistently higher levels of activity during passive task conditions, the DMN was hypothesized to monitor the external environment, body, and even emotions [6]. Task-related increases in activity in regional brain zones coincided with its decreased activity, indicating a reciprocal relation between the two zones related to the performance state of the task. Functional MRI shows that these relative activity levels are substantially and progressively altered by Alzheimer’s disease [7]. For example, in AD patients the posterior cingulate and right inferior temporal cortical activities decline, whereas the activity of the bilateral inferior parietal cortex increases. Because the zones form central connectivity hubs within the DMN, the activity changes appear to reflect a weakening of causally influential relations among its principal nuclei. Metastability indices for AD patients, for example, are reduced in decoupled, desynchronized states, revealing that the disease progression significantly reduces the brain’s ability to entrain regional dynamical activity [8].
\nUnlike AD, on the other hand, Korsakoff’s syndrome manifests as a persistent memory impairment that associates chiefly with the acquisition of new information [9, 10, 11, 12]. Accordingly, it has been frequently classified as a disease yielding an anterograde form of amnesia. Like AD, on the other hand, its influence is multipronged, with studies showing that it also affects memory retrieval. Moreover, other studies show a preponderance of perifunctional influences rather than direct influences on episodic and semantic memory per se. For example, context memory, which makes an important contribution to memory recollection, has been shown to be significantly impaired in Korsakoff’s patient. In memory tests, additionally, differential impairments are seen between AD and Korsakoff’s disease and also Huntingdon’s disease. For example, KS and HD patients performed considerably better than AD patients in recall memory [13].
\nThe complexity of the influences of the two diseases on memory, notwithstanding, the distinctions in their manifestation suggest that these could be exploited both to resolve the likely etiological differences between the two and also to gain insight into underlying processes of memory and its relation to the self-construct. Differences in phenotypic manifestation, notably, have motivated much research, on the presupposition that they reflect the presence of different processes contributing to a single, albeit complex, function. Moreover, differences in manifestation also have bearing on therapeutic interventions and managed patient care, illustrated in the chapters of this edited volume.
\nResearch into diseases like hemophilia has traditionally sought to resolve underlying etiopathological features by exploring genetic and biochemical differences that traced their manifestations to single, albeit critical, constituents of biochemical mechanisms, like the coagulation defects of Factor VIII in hemophiliac patients [14]. Cognitive diseases, on the other hand, are likely to differ greatly from those with such ‘metabolite-like features due to the nervous systems’s global role in integrating organismal function. Thus numerous aspects affected by these diseases are likely to differ, including their manner of functioning, composition, and hierarchy [15, 16]. Hence, there is the question of whether traditional strategies based on reductive approaches that attempt to determine etiology from genetic or molecular origins are an adequate beginning for investigating normal or disease-affected cognition. Indeed, the present volume illustrates both the challenge and the enigmatic character of such diseases. Accordingly, it is the intention of this introductory chapter to consider the limitations to study emerging from the adoption of such reductive strategies and the prospects of exploiting “higher-order differences” of the sort seen in AD and Korsakoff’s disease, to infer etiopathological origins.
\nClinically, the identification of risk alleles has significantly benefitted medical diagnosis and therapy. For example, diagnosis of the risk allele for hemophilia A, Factor VIII has high predictive power of, for example, likely hematoma when the hemophilia patient is injured. Its utility, however, extends beyond risk prediction. Because mutant alleles usually constitute sources of malfunctioning protein products, genetic identification of the product can afford access to an otherwise enigmatic etiology. Studies of the Factor VIII allele have facilitated, for example, the determination of the disease’s genetic basis, the role of the Factor VIII protein in clotting, and moleular therapeutic options [17].
\nThe strategy of investigating etiology via risk alleles is a legacy of experimental designs that were successfully pursued for the elucidation of biochemical pathways. The presupposition behind these early, now classical approaches conceived of such pathways as linear sequences of progressively altered metabolite products, where each succeeding step entailed a molecular modification and the succession of steps yielded a unique biochemical product. Biochemical pathways fit this decidedly causal and prototypical model. The successive conversion of glucose to pyruvate in the glycolytic pathway, for example, evidenced the stepwise deconstruction by which the larger glucose molecule was gradually disassembled to the smaller pyruvate metabolite. Alleles controlled individual steps through their enzymatic products, which regulated each biochemical change. By rendering the protein products nonfunctional through techniques like mutagenesis given steps of the pathway could be arrested.
\nSuch mutagenesis strategies achieved remarkable success in elucidating pathway steps due to the high specificity and mono-functionality of the enzymes regulating metabolite conversion. Mutation of the gene loci notably yielded focal and highly targeted effects that enabled the reconstruction of the entire pathway, when occurring within a linear sequence and involving a sufficient number of interruptions. By building on naturally occurring lesions, the development of reagents capable of modifying DNA rapidly expanded available tools for DNA dissection. With the advent of molecular biological procedures gene products could be altered at virtually any locus, allowing both pathway reconstruction and characterization of whole clusters of supramolecular assemblies [18].
\nThe success of pathway reconstruction in metabolism led to the implementation of mutagenesis to dissect neural function in simple organisms amenable to genetic manipulation, like
The success of the mutagenesis strategy for elucidating biochemical pathways, which had motivated its use for exploring neural function, however, was due to a fortuitous confluence that juxtaposed the compositional nature of metabolism - with its linear and precise factory like assembly - with a causal conception involving successive influences effected via steplike sequences. Applied to neural function this conception analogized photopotential generation to a metabolite and the neural events of transduction to successive changes in a single molecular substance. Rather than metering the presence of a physical product, assessments were thus made in terms of the physiological feature, which was viewed as its conceptual equivalent.
\nLarge-scale mutagenesis of fruit flies generated numerous “risk alleles” affecting various components of the photopotential, including its onset, maintenance, termination, and facilitation [19, 20, 21, 22]. The strategy usefully characterized highly penetrant alleles with Mendelian-like features, such as those affecting the photopigment protein, and physical components directly mediating the photopotential, like temperature-sensitive channel variants. However, while the strategy yielded numerous novel observations about photoreceptor function—including insight into mechanisms of prolonged potential activation, habituation-like responses, and degenerative cascades—the resolution of transduction per se was less easily and less well resolved. With hindsight and drawing from ongoing parallel studies of phototransduction that did not resort to genetic studies, the lack of resolution may now be partially traced to the conceptual equating of a physical component with a physiological function. Differences in the physical instantiation of a function - as opposed to a metabolite - became notably apparent with the discovery of features such as gated switching, nonlinear dynamical gain and the use of multicomponent protein complexes [23]. For example, generation of the photopotential is critically dependent on the asymmetric distribution of Na and K ions across the photoreceptor cell membrane. Yet, the ionic distribution is not itself generated by the transduction event but is an a priori condition that is required to successfully elicit the photopotential, one that must be maintained continuously against a concentration gradient by energy-consuming ionic pumps. A mutation rendering the pumps ineffective—for example, through a temperature-sensitive, cell mosaic line—would result in the absence of the photopotential and so be interpreted as affecting a step in the transduction pathway. Likewise, the photopotential amplitude displays gain adjustments that enable the detection of intensity variation under widely variant background illumination conditions affecting but not directly constituting the phototransduction events. These observations reveal that unlike the succession of steps occurring in metabolite processing the generation of the photopotential entails a coordinated operation of multiple independent functionalities that are each necessary but not sufficient for the potential to occur. Because each of these functionalities is potentially influenced by multiple alleles, the number of alleles affecting the transduction mechanism is likely to be much larger than that needed in a simple sequence of molecular alterations involving a single substance. In other words, the number of risk alleles that could affect the function is likely to be considerably more than the number of processional events needed to yield the function and indeed is likely to multiply that number. The magnitude of this multiplicative effect becomes especially significant when scaled for complex neural events. Accordingly, differences between the physical mechanisms of metabolism and those of photopotential generation require that the equating of neural function with metabolite processing be reconceived, a conceptual adjustment revealed through the findings of the mutagenesis approach.
\nPhototransduction clearly constitutes a moderately complex but nonetheless basic function that has evolved to capture light information, in which multiple functionalities work together to yield the photopotential. As a neural mechanism, however, its level of complexity is arguably much less than many behavioral mechanisms operating at systemic and global scales. Motor execution and action identification, for example, require the involvement of visual pathways, task positive frontoparietal networks, premotor and motor cortices, and cerebellar circuits [24]. These are further complicated by the need to evoke egocentric frameworks in goal-directed actions. Consistent with these broad operational requirements, key risk alleles for major cognitive etiopathologies like schizophrenia—with a prevalence of 0.5–1%—are now known to include more than 120 significant loci, that is, alleles that introduce statistically significant changes in manifest clinical symptoms [25]. Moreover, the rate of increase in their discovery has accelerated in recent years, not slowed. Classically, traits governed by large numbers of alleles yield only marginal and quantitative trait variation, with significant changes observed only in cases of rare alleles with high penetrance. Accordingly, many more difficult to detect alleles are likely to also contribute to the manifestation of the disease. In like manner, genetic studies of AD have also identified numerous risk alleles contributing to its etiopathology [26].
\nTogether, the genetic studies show that cognitive diseases, as a group, are polygenic, often influencing hundreds of known alleles with perhaps a much greater unidentified number also influencing disease severity. Variation in behavioral effects due to any single allele, moreover, is small, with observed changes likely to be of a quantitative rather than a qualitative nature. Alone, the use of risk alleles as a strategical undertaking is therefore unlikely to offer significant insight into a causal etiology. The studies, rather, implicate large numbers of affected neurons and circuits, that is, effects likely to be mediated at systemic and even organismal levels of neural function. The range of investigations that have been undertaken over decades of exploration, in fact, from single allele variation to genome-wide investigations reveal that while genetic influences are clearly at work in cognition—such diseases typically display statistically significant familial effects—such influences are apparently mediated through a complex overarching matrix of constraints, one that bears little resemblance to a stepwise biochemical sequence, for which allele study and mutational analyses were first and successfully used.
\nThe massive number of affected alleles and the generally enigmatic character of cognitive diseases—more than 13 different, major hypotheses have been advanced to date to explain AD etiopathology—pose significant quandaries in the selection of research strategies, which clearly have as their ultimate objective whole rather than partial and ineffective therapeutic intervention. In light of these realities that seem linked to the extraordinarily complex scales of cognitive operation, the observations from mutagenesis strategies of intermediate-level phenomena like the photopotential offer a strong stimulus for moving beyond purely reductive options in the strategic analysis of cognitive disease etiology.
\nThe recognition that functions often require supramolecular structures, for instance, has motivated the use of proteomics to characterize large-scale protein aggregates. This move would dispense with the lower-level allele studies and focus on how function emerges from clusters of interacting units. Such an approach also holds a promise for its access to the technical virtuosity acquired over decades in the use of translational technologies and analytical protein and peptide biochemistries. In principal virtually any protein segment can now be modified and analyzed to ascertain how such changes causally interact with other protein components to yield specific functions.
\nFor example, the flagellar motor that propels bacterial motion is a well-characterized example of a large supramolecular aggregate consisting of more than seven distinct proteins activated during chemotaxis. Ligand-based stimuli, internal-based phosphorylation modifications, and enhanced protein-binding interactions are now all known events discerned through proteomic studies. These mechanical features are an important aspect of explaining the causal succession for the motor’s function, identified in philosophy of science accounts as the “how” question in functional explanation [27]. The motor’s performance, however, must also conform to an organizational, that is, design, principle to be functional, which is to say that the explanation for the motor’s function must include a dimension beyond that of the succession of internal events leading to functional output. This latter explanation, termed the “why” question, is significant for revealing that efficient causal interactions require the design principle as an a priori condition for their realization, hence, answers to the ‘how’ question represent only causal outcomes of organizational form.
\nThis invocaton of design principle is significant for identifying the primary causal origin of a function. Rather than determined from below, the mechanistic steps emerge from a predetermined order that is critical for defining material composition and operation. Moreover, the elicited function—the motor’s operation, for example—is framed within the context of global organismal need. Accordingly, the emergence of the function is fundamentally related to non-reductive, top-down effects that reflect two aspects of organismal operation; first, an organizational order that governs associations of larger-order complexes (e.g., evident in motifs and network analysis) and, second, a global requirement to satisfy organismal need, seen, for instance, in goal directed activity.
\nConceiving of neural function from this higher-order perspective—i.e, dynamically oriented and not static as in the conception of metabolites—has implications for considering the primacy of causes eliciting neural organization—not chiefly through the structuring of its anatomical features, where it is built from the bottom up, but as a dynamic and functional order that has a purposeful orientation, which is determined from the top down.
\nViewed from the dynamic aspect of function, the order of causal priority is reversed where the chief influences underlying organization and performance are systemic and teleological. Lesions of higher-order neural functions, like memory, appear thereby as dysfunctional properties of global representations. Risk alleles, in this reading, and similar reductive approaches can be expected to offer little insight into cognitive operation at the level of neural constructs likely to be impaired in cognitive diseases. Investigations into cognition, instead, seem better directed when exploring the operation of extended networks that function as components of larger systemic or even global operations. By extension, lesions that may fruitfully reveal aspects of large-scale operation are more likely to involve systemic effects that are more closely apposed to global processes mediating organismal tasking.
\nModels that define the source of this tasking, accordingly, are likely to be helpful for identifying the sorts of lesions that can be usefully exploited for cognitive study. Key features underwriting global cognition notably include those preserving existential independence and the integration of the organism as a whole, that is, those providing for autonomous existence [28]. Understood as a capacity, autonomy implicates dispositional qualities of self-recognition and self-directedness; that is, it invokes self-constructs that elicit higher order operations, which, accordingly, can be disrupted by cognitive disease. As one such higher order operation, for instance, memory is directly elicited by such self constructs in order to facilitate autonomy. Lesions of higher-order capacities like memory, which are evoked by global constructs, may thus be usefully exploited for their properties and manner of elicitation [29, 30].
\nEmerging from the global operation of the brain, constructs like the self are clearly extraordinarily complex and in many respects seem less tangible than material constituents of reductive and low-level functions. Nonetheless, their organismal reality is clearly evident in manifestations of behavioral activity. For example, the association between a representation of the whole individual by his body and its physical realization in the neural activity of the brain, that is, as a global brain state, is consistently observed in varied perceptual realizations of the self. And in another example the failure of infants in the A not B task to move toward a goal where last seen is interpreted as a failure in motor planning due to maturational insufficiency in mechanisms needed to situate the motor plan that are associated with representing the self as the whole body [31]. These examples suggest that top down aproaches can offer strategic alternatives that more readily yield insight into global brain operations that are manifested at organismal scales.
\nIndeed, the modern concept of the neural representation of the self, for example, evoked in circumstances where the body is dynamically engaged in intentional actions, is an increasingly well-understood global operation that has emerged from several experimental legacies traced to the notion of the motor image [24]. The image is now known to involve a covert action undertaken only mentally and as a simulation of a non-executed action, with current evidence suggesting that there is a close correspondence between goal-directed information and self-representation [32]. Mechanisms that are likely to shape self-content can therefore be expected to include, for example, cells, circuits, or processes that bear desires and intentions of the author, which are likely to be contained in egocentric networks [33], and which encode agent specific content about an experience. These have been sited to specific domains of the hippocampus, such as the lateral entorhinal cortex where they appear to be influenced by memory recall [34] such as the lateral entorhinal cortex, and to the angular gyrus of the parietal cortex, a region that has been previously identified with self- and bodily representation. Indeed, goal-directed information contained in these networks can be expected to uniquely modify the self-representation by relating the individual to an intended terminus via information that is goal specific.
\nThe promise of top-down analysis predicts that global organization is selectively impaired at intermediate and even higher levels of brain function, such as those now being investigated through the motor plan. Indeed, disturbances in the sense of self that mark schizophrenia, for example, in prodromal and acute stages, have led to the recognition of the loss of self as a core symptom [35] where both body ownershipa nd sense of agency are impacted [36]. Current evidence on how representational content of the self may be affected and how this may be linked to the body suggest, in fact, that it is mediated through the motor plan, which thereby offers a strategic investigative tool. Insight into the neural features that these results may implicate, for example, can be inferred from misattribution errors that are experimentally evoked in normal individuals and that appear to be pathologically exacerbated in schizophrenic individuals [37].
\nBy extension, memory losses in AD and KS are in their broad features consistent with functional losses that have organismal bearing and that can be revealed through such top-down analysis. Accordingly, this volume represents an effort to forward an argument for global strategies that can be pursued in cognitive etiopathologies. It is a proposal that emerges from the intractability of reductive study faced with the incredible complexity of operation that is intrinsic to cognition. While lacking in the tangible manifestations that have come to mark genetic and molecular study, the reality of global operation is nonetheless manifestly evident. Moreover, it is a reality for which new investigative tools are emerging from research studies, such as the motor plan. Revelation of distinct functional differences in memory loss in diseases like AD and KS, therefore, can be expected to further options for global, top-down study.
\nThe Yangtze block is located in South China, with the Qinling-Dabie-Sulu orogenic belt in the north and the Songpan-Ganzi fold belt in the west [1].
The Sichuan cratonic basin located in the western region of the Yangtze block has experienced multiple tectonic movements during its evolution. During the Permian, the structural differentiation caused by the Dongwu movement and the Emei rifting activity controlled the sedimentary system [2].
Moreover, the depositional systems controlled the distribution of the Permian carbonate gas reservoirs in the area, where several new gas fields have been discovered in recent years. The platform margin reef-shoal facies of the Upper Permian Changxing Formation is one of the favorable sedimentary facies belts for the formation of favorable reservoirs in the Puguang and Yuanba gas fields [3, 4]. Besides, the high-energy granular beach sedimentary facies belt of the Middle Permian is also considered as a reasonable basis for the development of natural gas reservoirs with the discovery of several high-yield gas fields in the northwestern and central part of the Sichuan Basin [5, 6]. On the other hand, shales with high organic matter content widely developed in the Wujiaping period of Upper Permian in the Sichuan Basin are the suitable hydrocarbon-generating beds [7]. Therefore, it is of considerable significance for natural gas exploration to analyze and study the structural differentiation and sedimentary system of the Permian Sichuan cratonic basin.
Although many different opinions have been put forward on the genetic mechanisms of the structural differentiation pattern of the Sichuan Basin [2, 5, 8, 9], these opinions lack a complete analysis on the basin sedimentary filling processes. The previous study lack a detailed discussion on the relationships between the structural differentiation and the depositional processes in the basin, which is precisely the basis and key of structural sedimentary evolution in the Sichuan Basin.
In this study, we focus on the structural differentiation, on the sedimentary systems, and on the tectono-sedimentary evolution of the Sichuan cratonic basin during the Permian.
The Sichuan Basin is a superimposed basin developed on the upper Yangtze craton [8] (Figure 1). However, the craton block has long been in the transitional position between Gondwana and Laurasia [10, 11], showing a vigorous tectonic activity. During the later stage there are many regional unconformities in the craton. The cratonic margin was involved in orogenic deformation and was strongly re-shaped. The processes of basin formation and evolution were quite complicated.
(a) Location of the Yangtze block and its relationships with other tectonic units in Permian; (b) the restoration of Permian global paleogeography (modified from Huang et al. [
At the end of Mesoproterozoic (1000 Ma), the island arc and accreted continental crust in the margin of the Yangtze Paleocontinent were spliced onto the Yangtze block. The Yangtze, Cathaysia, and North China blocks were combined to form a part of Rodinia ancient land [11, 12]. Since 850 Ma, it has experienced (1) the early cracking, the formation of rifted sag, passive continental margin basin, and composite basin of intra-cratonic depression in 850–460.9 Ma (Nh-O2), and (2) the late convergence, the establishment of intra-continental foreland basin and large-scale tectonic uplift in 460.9–416 Ma (O3-S) [12]. In the Tethys Ocean evolutionary stage from Sinian to Silurian, the inner plate tension between the Yangtze block and the Cathaysia block resulted in the formation of the Xianggui continental rift basin and in the internal and marginal rifting of the middle and upper Yangtze craton. Then the compression orogeny in the Caledonian stage resulted in the formation of the South China continent. In the Late Paleozoic, it turned into the Paleo-Tethys Ocean evolution stage.
From the Late Paleozoic to the Middle Triassic, the formation and evolution of the Sichuan Basin was genetically related to the geological process of South China block splitting and drifting from the northern margin of the Gondwana continent. The southwestern and northern margin of the Yangtze block became passive continental margins facing on different branches of the Paleo-Tethys Ocean. The middle and upper Yangtze block experienced a relatively short convergence and compression process from Devonian to Permian, forming the inner depression, the marginal depression, the passive continental margin, and the foreland basin of the middle and upper Yangtze craton [12, 13, 14, 15].
After the development of the foreland basin in the Late Triassic, the middle and upper Yangtze were involved in an extensional and convergent cycle, closely related to the development of the Neo-Tethys Ocean, which included (1) the short-term extension from the Early Jurassic to the Early-Middle Jurassic (199.6–167.7 Ma) and (2) the long-term compression and transformation from the Late-Middle Jurassic to the Quaternary (167.7–0 Ma) [12, 16].
Above all, the basin prototypes of the Sichuan Basin were controlled by the activities of the surrounding plates in different phases. The basement of the basin was formed in the Pre-Nanhua Period; the rift basin was established in the Nanhua Period; the cratonic margin rift and the cratonic inner depression were created in the Sinian-Ordovician; the cratonic inner depression and the peripheral foreland basin were developed in the Silurian; the cratonic margin rift and the cratonic inner depression were developed from the Devonian to the depositional period of the third member of the Xujiahe Formation in the Late Triassic (D-T3x3); the foreland basin was established in the depositional period of the upper Xujiahe Formation (T3x4–6); the large-scale cratonic depression was developed in the Early to the Middle Jurassic; the compressional basin was developed in the Late Jurassic-Early Cretaceous; the depression basin was established from the Late Jurassic to the Early Cretaceous; and from the Late Cretaceous to the Quaternary, a transitional compressional foreland basin was formed. As a whole, the Sichuan Basin shows the characteristics of an alternating development of extensional basin (Z-O, D-P-T3x3, J1–2) and compressional basin (S, T3x4–6, J3-K1) [12].
In the Early Permian the striped continents composed of the Cimmerian block, Qiangtang block, and Sibumasu block were separated from the northern margin of Gondwana. Then the back part was extended to form the new Tethys Ocean. In the Middle Permian the transgression reached its maximum in South China, leading to the development of a wide southward-dipping carbonate platform. At that time, the Jiangnan-Xuefeng area was a submerged structural high and was separated by the southern and northern sedimentary regions. On the north side of the Yangtze block, the sedimentary environments were the shallow slope and deepwater basin southward of the Qinling Ocean, where deepwater dark limestones with nodular cherts and bedded cherts were deposited. The southern Qinling Ocean crust was subducted northward under the Qinling micro-block at the end of the Early Permian and developed corresponding island arc volcanic rocks, while the passive continental margin on its southern side was still growing (Figure 1).
In the Sichuan Basin, the Middle Permian strata include the Liangshan Formation (P2l), the Qixia Formation (P2q), and the Maokou Formation (P2m), with a thickness of 400–500 m. In the early transgression stage of the Middle Permian sandstones, mudstones, marls, and marshes were deposited. In the middle period, the deposits evolved to shallow platform limestones and shaly limestones interlayered with sandy limestones. Massive limestones, dolomites, and black shales developed in the late Middle Permian, during which Leshan-Luzhou biological shoals grew.
At the end of the Middle Permian characterized by the Emei rift movement, the region was uplifted, and the Maokou strata were denuded in different degrees. The event of the Emei rift may be related to the subduction of the Jinshajiang-Mojiang ocean basin from the south to the north, and a large-scale extension occurred in the back of the arc (Figure 1). Longmenshan, Kaijiang-Liangping, and Chengkou-Exi rifts developed in the Yangtze craton block [12, 17].
During the Permian, the Yangtze block was generally located in the low-latitude area near the equator [18, 19], in the transitional position between the Gondwana and the Laurasia supercontinents. From the Early Permian to the Late Permian, the Yangtze platform was surrounded by the Paleo-Tethys Ocean and the Paleo-Pacific Ocean [20]. It rotated mainly anticlockwisely and formed the South China block, together with the Cathaysia block in the southeast (Figure 2). In the Late Permian the North China block was located northward of the South China block.
Structural differentiation profile of the middle and upper Yangtze plate in the Permian (A-A’, NW-SE direction; B-B′, NE–SW direction, location in
The paleomagnetic data showed that both the North China block and the South China block had the trend of northward movement and their latitudinal changes showed a certain degree of synchronicity, which may be related to the first collision of the two blocks in the east [21]. The South Qinling Ocean was located between the two blocks, opening toward the west in the form of scissors, with an angle of 70–80° [21]. Because of the continuous northward subduction, the North Qinling orogenic belt was formed at the southern margin of the North China block, while a passive continental margin emplaced at the north margin of the Yangtze block [22].
The southwest margin of the South China block was Simao-Indosinian block, which was located in the low-latitude area near the equator [23]. Between the two blocks was Jinshajiang Ocean, a branch of the Paleo-Tethys Ocean. The ocean basin rapidly expanded from the Early Permian to the Late Permian [24]. The subduction of the Jinshajiang Ocean to the Simao-Indosinian block in the southwest reflected a strong tectonic compression, while the South China block was a passive continental margin in the overall extensional setting [25]. The South China block was connected with the Songpan-Ganzi Ocean in the west, while the Jiangnan-Xuefeng intra-continental rifting zone was connected with Youjiang rifting zone, mainly in deepwater shelf environment, with isolated carbonate platform sporadically developed [26]. During the Permian, the tectonic setting of South China block was mainly of regional extension, showing the characteristics of a strong tension at the margins of the block.
In the Permian period, the tectonic setting of the South China block was mainly of regional extension, showing the characteristics of strong extension at the margin of the block and of a weak tension within the block and developing a set of marginal rift basins, intra-continental depression basins, and rift basins. In the Kangtien ancient land area, located on the southwestern margin of the block, a basalt eruption was considered to be a stratigraphic marker of the extensional process. The exposed area of basalt could reach 250,000 square kilometers, with a wide range of influence [9, 27]. During the Permian, the upper Yangtze block had the characteristics of a structural high to the south and of a depression to the north. The Kangtien ancient land was the main source area supplying terrigenous clastic in the upper Yangtze craton [28, 29]. To the north, it was dominated by the shallow sea carbonate environment and graded into the passive continental margin basinal environment.
The Sichuan Basin is a typical cratonic basin located in the western margin of the Yangtze block, which has recorded many geological events during the Permian. Several geological events occurred in the Permian, including the Emeishan Large Igneous Province [30, 31, 32], the Paleo-Tethys Ocean expansion and evolution [19, 33, 34, 35], and the end of the Permian biological extinction, have been widely of concern by scholars [36, 37, 38, 39]. During recent years, according to the field outcrop data and to the stratigraphic records of drilling data, it was found that from the southwest to the northeast of the basin, the Sichuan Basin has deposited a wide range of marine carbonate rocks during the Permian. However, in the central and northern sectors of the basin, there were many deepwater sedimentary areas toward the carbonate platform margins. This unique sedimentary filling pattern reflects that the Sichuan Basin had the unique structural differentiation characteristics during the Permian [40].
Permian strata widely developed in the eastern sectors of the Sichuan Basin during the early depositional stages, when carbonate rocks are dominant. During late stages, the difference between the eastern and the western sectors increased. In the Panxi area, the continental basic volcanic rocks were dominant, while the eastward transition was represented by continental clastic rocks. On the contrary, in the eastern Sichuan Basin, thick marine carbonate rocks were dominant [41]. In the Sichuan Basin, the Permian strata can be divided into the Middle Permian Liangshan Formation, Qixia Formation, Maokou Formation, and Upper Permian Wujiaping Formation and Changxing Formation (Figure 3).
Generalized Permian stratigraphy and division of fusulinid zones in SW China (after He et al. [
In the late Early Permian, the tectonic movement uplifted the northwestern region of the upper Yangtze to land, controlling variable degrees of denudation of the Paleozoic strata [42]. Until the Middle Permian, transgression occurred from south to north, and the Liangshan Formation was the product of the land-sea transformation at the beginning of this transgression [41, 43, 44]. The Liangshan Formation, widely developed in the Sichuan Basin and its adjacent areas, which is a coal-bearing deposit dominated by clastic rocks, and the contact between Liangshan Formation and underlying strata (e.g., Carboniferous or older layers) are disconformable [41, 43, 44, 45].
In the Sichuan Basin and Panxi areas, the lithology and the thickness of the Liangshan Formation considerably vary [41, 44]: (1) The sandstone content of the Liangshan Formation deposited in the western region is relatively large, with a thickness generally ranging from 10 to 42 m and finally reaching 88 m (e.g., Gan Luo). (2) The sedimentary thickness of the Liangshan Formation rapidly decreases eastward to 5–15 m in the area of Emeishan and Leshan, which is often dominated by carbonaceous shales. (3) The Liangshan Formation in the south of Sichuan is 4–17 m thick and is mainly composed of carbonaceous shale and clay rock, containing bauxite and hematite. (4) The Liangshan Formation in eastern Sichuan is dominated by coal-bearing claystone and sandstone and occasionally contains oolitic and bean-shaped hematite, with a thickness of 4–8 m, reaching 21 m. (5) The Liangshan Formation in the north of Sichuan and Longmenshan is 3–30 m thick, thinning eastward, and is mainly composed of aluminum clay rocks, bauxite, and weak coal seams. The Liangshan Formation contains plant fossils (e.g.,
During the deposition period of the Qixia Formation, the crustal subsidence was stable and seawater intruded on a large scale. As a result, the early sedimentary environment dominated by clastic rocks was transformed into carbonate platform sedimentary environment [41, 45].
Qixia Formation is widely distributed in the middle and eastern sectors of the Sichuan Basin. It is mainly composed of dark gray-black limestone, with a massive and micrite structure, locally mixed with bioclastic limestone, siliceous limestone, siliceous bands, and siliceous concretion [41, 44]. The limestones of the Qixia Formation generally contain high asphaltene and siliceous components and show dolomitization, and abundant eyeball-shaped structures (e.g., Huayingshan area) occur locally [46]. The Qixia Formation is interlayered above the Liangshan Formation, and its stratigraphic thickness ranges from tens of meters to more than 300 meters, gradually thickening from west to east [41].
According to the observation results of the outcrop in the wild, the Qixia Formation can be divided into two types [44]. One is called “White Qixia,” which is distributed in the northern section of Micangshan and Longmenshan. It is mainly composed of light gray-black limestone with dolomitic limestone and dolomite and with shale at the bottom. The other is called “Black Qixia,” which is distributed in other areas of the Sichuan Basin, with shale and siliceous layer at the bottom, dark gray thick layer of biological limestone, micritic shell limestone in the lower part, and light gray biological limestone in the upper part.
The Qixia Formation contains many types of fossils, mainly including fusulinids (e.g.,
In the Sichuan Basin, the lithology of the Maokou Formation is relatively uniform with shallow marine, light gray, thick micritic fossiliferous limestone, including siliceous concretions and thin siliceous layers, ranging in thickness from 50 m to 600 m. Due to the influence of the Dongwu tectonic movement, the Maokou Formation was involved by various degrees of erosion, and the integrity of the strata gradually improved from west to east. In the southern part of the Sichuan Basin, basalts erupted in the middle sedimentary period of the Maokou Formation. The Maokou Formation can be divided into two members in the northeastern Sichuan Basin and into three members in the central Sichuan Basin.
The lower member of the Maokou Formation is composed of dark gray muddy micritic limestones, bioclastic limestones with black calcareous shales, and a thin siliceous layer at the top. Microbial rocks and storm rocks can be seen in southern Sichuan, eastern Sichuan, and Longmenshan areas. The Maokou Formation contains brachiopods (e.g.,
The middle member of Maokou Formation consists of light gray and dark gray thick layer massive micritic bioclastic limestone and micritic limestones with siliceous concretions. In the northwest and south of Sichuan, tempestite is relatively developed. There are abundant organisms, including fusulinids (e.g.,
The upper member of the Maokou Formation consists of gray-white micritic limestone with siliceous concretion, gray-black micritic limestone, and bioclastic limestone, including fusulinids (e.g.,
The Maokou Formation in Dabashan, Wushan, and southeastern Sichuan only remains lower and middle members. Parts of the lower, middle, and upper members of the Maokou Formation are preserved in Micangshan, Longmenshan, and Huayingshan. The Maokou Formation is well preserved in southern Sichuan (such as Gongxian).
The Wujiaping Formation is mainly distributed in the northeastern Sichuan Basin and can be subdivided into two members according to lithology differences. The lower member (formerly known as Wangpo shale) is a coal-bearing stratum at the intersection of land and sea. Its lithology is an aluminous clay rock, carbonaceous shales with coal seam or coal lines, oolitic hematite, and monohydrallite.
The upper member of the Wujiaping Formation (limestone section) has little change in lithology, which is micritic limestone, limestone with calcareous, siliceous, carbonaceous shale, and coal lines, with a siliceous layer at the top. From west to east, the dolomite content of deposits increased. In Mianzhu and Youyang, there are thin micritic limestone, limestone with shale, and multilayer coals. To the west of the line of Mianzhu-Daxian-Nanchuan-Gulin, Wujiaping Formation gradually changed into Longtan Formation.
In the Sichuan Basin, Wujiaping Formation consists of fusulinids (e.g.,
As a lithostratigraphic unit at the top of the Permian, the Changxing Formation usually refers to the carbonate formation of platform facies sedimentary under the Lower Triassic in the Sichuan Basin, which is roughly equivalent to the sedimentary period of the Dalong Formation, and the difference between them is the sedimentary environment [47].
The Changxing Formation is mainly composed of shallow water carbonate, while the Dalong Formation primarily consists of deepwater siliceous rock and shale. Therefore, the sedimentary area of the Dalong Formation is also called “siliciclastic rock basin” [48].
The Dalong Formation is defined as the layer dominated by black and gray-black thin-layer siliceous rocks and siliceous shales in Sichuan and Chongqing area, with relatively stable sedimentary thickness, generally 15–42 m. The Dalong Formation is interlayered with the underlying Wujiaping Formation and the overlying Feixianguan Formation, and there is no apparent stratigraphic division between them [41]. In the Sichuan Basin, the distribution of the Dalong Formation is strictly controlled by the paleogeographic pattern, which is distributed in the north deepwater trough or basin facies area, roughly along the line of Guangyuan- Wangcang-Chengkou-Wushan. The lithology of the Dalong Formation is dominated by siliceous rock, siliceous shales, and siliceous limestones with tuff, mudstone, shales, and siltstones, and the siliceous composition is gradually reduced from the bottom to the top. There are abundant fossils, mainly including fusulinids (e.g.,
The lithology of the Changxing Formation is mainly composed of medium-thick bioclastic limestones, micritic limestones, reef limestone, and dolomites, containing siliceous bands and concretions. The sedimentary thickness of the Changxing Formation varies from tens of meters to more than 100 m, and in some places, it can be as thick as 200–300 m. The fossils of the Changxing Formation are extremely rich, including algae (e.g.,
Coral reefs and sponge reefs in the Changxing Formation is very well developed. Due to the tectonic control of faults within the platform, the shallow water area around the trough is deposited to form a platform margin reef. The most developed reef is located eastward of Sichuan, such as Wujiti, Huanglongchang, Damaoping, Gaofeng, and Laolongdong. The high-quality reservoir formed by the Changxing reef also provides favorable conditions for the formation of a reef gas reservoir [4].
After the small-scale transgression in Late Carboniferous, the Sichuan Basin experienced tectonic uplift in the Early Permian, controlling a wide stratigraphic gap, as shown by the lacking of Lower Permian strata in the basin filling. At the beginning of the Middle Permian, a new transgression occurred in the Sichuan Basin, which extended to the west of Hunan. As a result, the pre-existing ancient land around the basin was submerged by seawater. Only the Kangtien ancient land in the southwest of the basin and the Xuefeng ancient land in the east of the basin remained, which controlled the source supply in the basin and around the basin [41].
During the Middle Permian, the Liangshan Formation, the Sichuan Basin, and its surrounding areas were generally characterized by clastic shore deposits, as controlled by the relatively shallow water body and by the high siliciclastic supply [45]. In the area around the paleo-uplift, the sediments were mainly medium-grained or fine-grained quartz sandstone, which represented the near-source coastal sedimentary environment. In the central Sichuan area, due to its high structural position, the lithology was mainly composed of sandy carbonate sediments, which showed a sedimentary environment of sand flat. In other areas of the basin, due to the relatively deepwater and lower water energy, the sedimentary environment was mainly muddy flat (Figure 4).
Tectono-sedimentary system of the Liangshan period in the Sichuan Basin and its adjacent areas (modified from Huang et al. [
During the deposition of the Qixia Formation, the sea level gradually decreased. At this time, the overall topography of the basin was high in the west and low in the east. With the relative shallowness of the water depth, as well as the subsidence of the depression in the basin and the extensional rifting of the basin margin, the sedimentary environment changed accordingly [45].
In the periphery of the Kangtien ancient land, it was still shoring facies. In the southwest of the basin, the lithology was mainly characterized by dolomites, dolomitic limestones, sandy limestones, and marls, with a low biological content, showing a typically restricted platform facies deposition. To the east of the restricted platform was an open platform facies area with good circulation of seawater, dominated by micrites and locally developed bioclastic limestones. The platform margin was established in the northwestern Sichuan Basin, roughly along the line of Mianzhu-Guangyuan. The sediments of the platform margin facies were mainly composed of thick bioclastic limestones, which were rich in species and high in abundance, and dolomitization locally occurred. In the northern part of the Sichuan Basin, influenced by Longmenshan ancient fault in the west, the terrain was sharply reduced, and the sediments were mainly mudstone, limestones, and shales, representing slope deposits (Figure 5).
Tectono-sedimentary system of the Qixia period in the Sichuan Basin and its adjacent areas.
During the deposition of the Maokou Formation, the southwestern margin of the upper Yangtze block was the Kangtien ancient land, and the northeastern margin was the passive continental margin environment, which was connected with the South Qinling continental margin basin. The northern part of the basin was mainly extensional. In contrast, the southern part of the Kangtien ancient land was continuously uplifting, and the basin was distributed in the pattern of uplift and depression [49]. From the southwest to the northeast, the seawater gradually deepened, and the sedimentary environment slowly changed from the continental environment to the marine one. The terrigenous shore facies, the restricted platform facies, the open platform facies, the platform margin facies, and the slope deepwater shelf facies then developed.
The restricted platform facies is distributed in Leshan-Emeishan-Zigong and other places in the southwest of the basin, and bioclastic beach facies is locally developed. The open platform facies area is located in the vast area to the east of the restricted platform facies area, where bioclastic banks are widely deposited in the higher ground, and micrite representing a low-energy environment was widely deposited in other places. The platform margin shoals were developed in the northwest of the basin, generally along the line of Qionglai-Anxian-Jiangyou-Guangyuan. In the area west of the platform margin, the seawater was steeply deepened, and the sedimentary environment also changed into slope deep shelf (Figure 6).
Tectono-sedimentary system of the Maokou period in the Sichuan Basin and its adjacent areas.
In the Late Permian the Sichuan Basin was located eastward of the Paleo-Tethys Ocean, with a high relief in the southwest and a low relief in the northeast. During the deposition of the Wujiaping Formation, the seawater transgressed from the northeast of the basin, and the provenance was mainly from the Kangtien ancient land [41, 50]. From the southwest to the northeast, due to the deepening of the ocean, the Sichuan Basin and its surrounding areas successively developed terrigenous shore facies, restricted platform facies, open platform facies, platform margin facies, and slope facies.
Shoreline facies extended from the southwest to the southeast of the basin, being composed mainly of coal-bearing terrigenous clastic deposits. In the area of Chengdu, Suining, Guangan, Chongqing, Nanchuan, and Zunyi, the poor circulation of seawater controlled the deposition of restricted platform facies. The area located eastward of the restricted platform was an open platform facies, where micrite and bioclastic limestones deposited. In the north and east Sichuan, a series of bioclastic shoals were developed along the line of Guangyuan-Dazhou-Wanyuan-Shizhu, which together form the platform margin. On the west side of the range of Guangyuan-Dazhou-Wanyuan-Shizhu, there were slope and deepwater shelf sedimentary environments, and the sediments are mainly mudstone and siliceous rock (Figure 7).
Tectono-sedimentary system of the Wujiaping period in the Sichuan Basin and its adjacent areas.
During the deposition of the Upper Permian Changxing Formation, the paleogeographic pattern of the Sichuan Basin and its surrounding areas was controlled by the Longmenshan-Kangdian ancient land in the west [51]. Its structural lithofacies paleogeographic pattern features can be summarized as strong tectonic activity (e.g., “Emei ground fissure movement” [27]), obvious lithofacies differentiation (e.g., siliceous clastic lithofacies and shallow marine carbonate lithofacies), and relatively rich and complex paleogeomorphic types (e.g., trough and uplift) [50].
During the Late Permian, the eruption of Emei basalts reached its peak due to the strong ground fissure movement, which was called the “Emei ground fissure movement” [27]. This volcano-tectonic activity had a profound impact on the paleogeographic pattern of the Late Permian and Early Triassic in the upper Yangtze region. Wang et al. believed that a series of the northwest and southeast deepwater troughs developed in the Late Permian in the upper Yangtze region, such as “Guangyuan-Wangcang trough,” “Kaijiang-Liangping trough” in the west, and “Chengkou-Exi trough” in the east. The formation of these troughs was controlled by the extensional movement of the southern Qinling Ocean in the north and the “Emei rift movement” in the west [27, 52]. In the Late Permian, the sedimentary facies belts in the upper Yangtze area were obviously different. The dark thin siliceous rocks, siliceous mudstones, and siliceous limestones were mainly deposited in the deepwater trough facies area, and the bioclastic limestones and reef limestones were mainly deposited in the shallow water platform facies area [53].
The sedimentary characteristics of the Late Permian can be summarized as follows: the sedimentary facies belt was generally distributed in the east–west direction and was controlled by the north–south direction structure and differentiated; reef and beach deposits are generally distributed in a belt along the trough to form the platform margin. On the west side of the platform margin, open platform, restricted platform, and terrigenous shore facies were developed, respectively, and on the east side, slope facies and deepwater shelf facies are developed (Figure 8).
Tectono-sedimentary system of the Changxing period in the Sichuan Basin and its adjacent areas.
The northern and western margins of the Yangtze block were passive continental marginal environments, while the southern and southeastern margins were continental marginal rift basins with deepwater settings.
During the deposition of the Liangshan and Qixia formations, the northern and western margins of Sichuan cratonic basin were discrete passive continental margin environments, while the south and southeast margins were continental margin rift basins with deepwater sedimentary characteristics. The sedimentary environment in this period gradually changed from the early shore tidal flat to the stable carbonate platform, which was generally characterized by east–west differentiation and north–south gradual change.
The tectonic setting of the basin was relatively stable in the Maokou period. The Kangtien ancient land in the south of the basin showed a trend of continuous uplift. The basin presented a pattern of alternating structural highs and depressions. The development of sedimentary facies belts in each sedimentary stage had obvious inheritance and migration. From southwest to northeast, the sedimentary facies included shore facies, limited platform facies, open platform facies, continental shelf facies, platform margin facies, and slope facies. These are the characteristics of a carbonate platform system.
Being influenced by the regional extension controlled by the Emei rifting, the tectonic subsidence of the basin in the Late Permian gradually increased from southwest to northeast. In the early stage, the basin was controlled by the thermal effect of deep materials, and then the northern part of the basin was mainly affected by the superimposition of regional extensional phases and finally formed the sedimentary pattern of platform shelf structural differentiation. At the same time, the sea level changes and the development of reefs and beaches at the platform edge had an important impact on the filling sequence. In the study area transgression gradually occurred from NE to SW, forming a sequence of shelf, slope, platform margin, carbonate platform, mixed platform, tidal flat, and volcanic facies.
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Singh",profilePictureURL:"https://mts.intechopen.com/storage/users/329385/images/system/329385.png",institutionString:"Punjab Technical University",institution:{name:"Punjab Technical University",institutionURL:null,country:{name:"India"}}}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null},{type:"book",id:"8018",title:"Extracellular Matrix",subtitle:"Developments and Therapeutics",coverURL:"https://cdn.intechopen.com/books/images_new/8018.jpg",slug:"extracellular-matrix-developments-and-therapeutics",publishedDate:"October 27th 2021",editedByType:"Edited by",bookSignature:"Rama Sashank Madhurapantula, Joseph Orgel P.R.O. and Zvi Loewy",hash:"c85e82851e80b40282ff9be99ddf2046",volumeInSeries:23,fullTitle:"Extracellular Matrix - Developments and Therapeutics",editors:[{id:"212416",title:"Dr.",name:"Rama Sashank",middleName:null,surname:"Madhurapantula",slug:"rama-sashank-madhurapantula",fullName:"Rama Sashank Madhurapantula",profilePictureURL:"https://mts.intechopen.com/storage/users/212416/images/system/212416.jpg",institutionString:"Illinois Institute of Technology",institution:{name:"Illinois Institute of Technology",institutionURL:null,country:{name:"United States of America"}}}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null},{type:"book",id:"9759",title:"Vitamin E in Health and Disease",subtitle:"Interactions, Diseases and Health Aspects",coverURL:"https://cdn.intechopen.com/books/images_new/9759.jpg",slug:"vitamin-e-in-health-and-disease-interactions-diseases-and-health-aspects",publishedDate:"October 6th 2021",editedByType:"Edited by",bookSignature:"Pınar Erkekoglu and Júlia Scherer Santos",hash:"6c3ddcc13626110de289b57f2516ac8f",volumeInSeries:22,fullTitle:"Vitamin E in Health and Disease - Interactions, Diseases and Health Aspects",editors:[{id:"109978",title:"Prof.",name:"Pınar",middleName:null,surname:"Erkekoğlu",slug:"pinar-erkekoglu",fullName:"Pınar Erkekoğlu",profilePictureURL:"https://mts.intechopen.com/storage/users/109978/images/system/109978.jpg",institutionString:"Hacettepe University",institution:{name:"Hacettepe University",institutionURL:null,country:{name:"Turkey"}}}],equalEditorOne:null,equalEditorTwo:null,equalEditorThree:null}]},subseriesFiltersForPublishedBooks:[{group:"subseries",caption:"Proteomics",value:18,count:4},{group:"subseries",caption:"Metabolism",value:17,count:6},{group:"subseries",caption:"Cell and Molecular Biology",value:14,count:9},{group:"subseries",caption:"Chemical Biology",value:15,count:13}],publicationYearFilters:[{group:"publicationYear",caption:"2022",value:2022,count:8},{group:"publicationYear",caption:"2021",value:2021,count:7},{group:"publicationYear",caption:"2020",value:2020,count:12},{group:"publicationYear",caption:"2019",value:2019,count:3},{group:"publicationYear",caption:"2018",value:2018,count:2}],authors:{paginationCount:229,paginationItems:[{id:"318170",title:"Dr.",name:"Aneesa",middleName:null,surname:"Moolla",slug:"aneesa-moolla",fullName:"Aneesa Moolla",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/318170/images/system/318170.png",biography:"Dr. Aneesa Moolla has extensive experience in the diverse fields of health care having previously worked in dental private practice, at the Red Cross Flying Doctors association, and in healthcare corporate settings. She is now a lecturer at the University of Witwatersrand, South Africa, and a principal researcher at the Health Economics and Epidemiology Research Office (HE2RO), South Africa. Dr. Moolla holds a Ph.D. in Psychology with her research being focused on mental health and resilience. In her professional work capacity, her research has further expanded into the fields of early childhood development, mental health, the HIV and TB care cascades, as well as COVID. She is also a UNESCO-trained International Bioethics Facilitator.",institutionString:"University of the Witwatersrand",institution:{name:"University of the Witwatersrand",country:{name:"South Africa"}}},{id:"419588",title:"Ph.D.",name:"Sergio",middleName:"Alexandre",surname:"Gehrke",slug:"sergio-gehrke",fullName:"Sergio Gehrke",position:null,profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0033Y000038WgMKQA0/Profile_Picture_2022-06-02T11:44:20.jpg",biography:"Dr. Sergio Alexandre Gehrke is a doctorate holder in two fields. The first is a Ph.D. in Cellular and Molecular Biology from the Pontificia Catholic University, Porto Alegre, Brazil, in 2010 and the other is an International Ph.D. in Bioengineering from the Universidad Miguel Hernandez, Elche/Alicante, Spain, obtained in 2020. In 2018, he completed a postdoctoral fellowship in Materials Engineering in the NUCLEMAT of the Pontificia Catholic University, Porto Alegre, Brazil. He is currently the Director of the Postgraduate Program in Implantology of the Bioface/UCAM/PgO (Montevideo, Uruguay), Director of the Cathedra of Biotechnology of the Catholic University of Murcia (Murcia, Spain), an Extraordinary Full Professor of the Catholic University of Murcia (Murcia, Spain) as well as the Director of the private center of research Biotecnos – Technology and Science (Montevideo, Uruguay). Applied biomaterials, cellular and molecular biology, and dental implants are among his research interests. He has published several original papers in renowned journals. In addition, he is also a Collaborating Professor in several Postgraduate programs at different universities all over the world.",institutionString:null,institution:{name:"Universidad Católica San Antonio de Murcia",country:{name:"Spain"}}},{id:"342152",title:"Dr.",name:"Santo",middleName:null,surname:"Grace Umesh",slug:"santo-grace-umesh",fullName:"Santo Grace Umesh",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/342152/images/16311_n.jpg",biography:null,institutionString:null,institution:{name:"SRM Dental College",country:{name:"India"}}},{id:"333647",title:"Dr.",name:"Shreya",middleName:null,surname:"Kishore",slug:"shreya-kishore",fullName:"Shreya Kishore",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/333647/images/14701_n.jpg",biography:"Dr. Shreya Kishore completed her Bachelor in Dental Surgery in Chettinad Dental College and Research Institute, Chennai, and her Master of Dental Surgery (Orthodontics) in Saveetha Dental College, Chennai. She is also Invisalign certified. She’s working as a Senior Lecturer in the Department of Orthodontics, SRM Dental College since November 2019. She is actively involved in teaching orthodontics to the undergraduates and the postgraduates. Her clinical research topics include new orthodontic brackets, fixed appliances and TADs. She’s published 4 articles in well renowned indexed journals and has a published patency of her own. Her private practice is currently limited to orthodontics and works as a consultant in various clinics.",institutionString:null,institution:{name:"SRM Dental College",country:{name:"India"}}},{id:"323731",title:"Prof.",name:"Deepak M.",middleName:"Macchindra",surname:"Vikhe",slug:"deepak-m.-vikhe",fullName:"Deepak M. Vikhe",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/323731/images/13613_n.jpg",biography:"Dr Deepak M.Vikhe .\n\n\t\n\tDr Deepak M.Vikhe , completed his Masters & PhD in Prosthodontics from Rural Dental College, Loni securing third rank in the Pravara Institute of Medical Sciences Deemed University. He was awarded Dr.G.C.DAS Memorial Award for Research on Implants at 39th IPS conference Dubai (U A E).He has two patents under his name. He has received Dr.Saraswati medal award for best research for implant study in 2017.He has received Fully funded scholarship to Spain ,university of Santiago de Compostela. He has completed fellowship in Implantlogy from Noble Biocare. \nHe has attended various conferences and CDE programmes and has national publications to his credit. His field of interest is in Implant supported prosthesis. Presently he is working as a associate professor in the Dept of Prosthodontics, Rural Dental College, Loni and maintains a successful private practice specialising in Implantology at Rahata.\n\nEmail: drdeepak_mvikhe@yahoo.com..................",institutionString:null,institution:{name:"Pravara Institute of Medical Sciences",country:{name:"India"}}},{id:"204110",title:"Dr.",name:"Ahmed A.",middleName:null,surname:"Madfa",slug:"ahmed-a.-madfa",fullName:"Ahmed A. Madfa",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/204110/images/system/204110.jpg",biography:"Dr. Madfa is currently Associate Professor of Endodontics at Thamar University and a visiting lecturer at Sana'a University and University of Sciences and Technology. He has more than 6 years of experience in teaching. His research interests include root canal morphology, functionally graded concept, dental biomaterials, epidemiology and dental education, biomimetic restoration, finite element analysis and endodontic regeneration. Dr. Madfa has numerous international publications, full articles, two patents, a book and a book chapter. Furthermore, he won 14 international scientific awards. Furthermore, he is involved in many academic activities ranging from editorial board member, reviewer for many international journals and postgraduate students' supervisor. Besides, I deliver many courses and training workshops at various scientific events. Dr. Madfa also regularly attends international conferences and holds administrative positions (Deputy Dean of the Faculty for Students’ & Academic Affairs and Deputy Head of Research Unit).",institutionString:"Thamar University",institution:null},{id:"210472",title:"Dr.",name:"Nermin",middleName:"Mohammed Ahmed",surname:"Yussif",slug:"nermin-yussif",fullName:"Nermin Yussif",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/210472/images/system/210472.jpg",biography:"Dr. Nermin Mohammed Ahmed Yussif is working at the Faculty of dentistry, University for October university for modern sciences and arts (MSA). Her areas of expertise include: periodontology, dental laserology, oral implantology, periodontal plastic surgeries, oral mesotherapy, nutrition, dental pharmacology. She is an editor and reviewer in numerous international journals.",institutionString:"MSA University",institution:null},{id:"204606",title:"Dr.",name:"Serdar",middleName:null,surname:"Gözler",slug:"serdar-gozler",fullName:"Serdar Gözler",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/204606/images/system/204606.jpeg",biography:"Dr. Serdar Gözler has completed his undergraduate studies at the Marmara University Faculty of Dentistry in 1978, followed by an assistantship in the Prosthesis Department of Dicle University Faculty of Dentistry. Starting his PhD work on non-resilient overdentures with Assoc. Prof. Hüsnü Yavuzyılmaz, he continued his studies with Prof. Dr. Gürbüz Öztürk of Istanbul University Faculty of Dentistry Department of Prosthodontics, this time on Gnatology. He attended training programs on occlusion, neurology, neurophysiology, EMG, radiology and biostatistics. In 1982, he presented his PhD thesis \\Gerber and Lauritzen Occlusion Analysis Techniques: Diagnosis Values,\\ at Istanbul University School of Dentistry, Department of Prosthodontics. As he was also working with Prof. Senih Çalıkkocaoğlu on The Physiology of Chewing at the same time, Gözler has written a chapter in Çalıkkocaoğlu\\'s book \\Complete Prostheses\\ entitled \\The Place of Neuromuscular Mechanism in Prosthetic Dentistry.\\ The book was published five times since by the Istanbul University Publications. Having presented in various conferences about occlusion analysis until 1998, Dr. Gözler has also decided to use the T-Scan II occlusion analysis method. Having been personally trained by Dr. Robert Kerstein on this method, Dr. Gözler has been lecturing on the T-Scan Occlusion Analysis Method in conferences both in Turkey and abroad. Dr. Gözler has various articles and presentations on Digital Occlusion Analysis methods. He is now Head of the TMD Clinic at Prosthodontic Department of Faculty of Dentistry , Istanbul Aydın University , Turkey.",institutionString:"Istanbul Aydin University",institution:{name:"Istanbul Aydın University",country:{name:"Turkey"}}},{id:"240870",title:"Ph.D.",name:"Alaa Eddin Omar",middleName:null,surname:"Al Ostwani",slug:"alaa-eddin-omar-al-ostwani",fullName:"Alaa Eddin Omar Al Ostwani",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/240870/images/system/240870.jpeg",biography:"Dr. Al Ostwani Alaa Eddin Omar received his Master in dentistry from Damascus University in 2010, and his Ph.D. in Pediatric Dentistry from Damascus University in 2014. Dr. Al Ostwani is an assistant professor and faculty member at IUST University since 2014. \nDuring his academic experience, he has received several awards including the scientific research award from the Union of Arab Universities, the Syrian gold medal and the international gold medal for invention and creativity. Dr. Al Ostwani is a Member of the International Association of Dental Traumatology and the Syrian Society for Research and Preventive Dentistry since 2017. He is also a Member of the Reviewer Board of International Journal of Dental Medicine (IJDM), and the Indian Journal of Conservative and Endodontics since 2016.",institutionString:"International University for Science and Technology.",institution:{name:"Islamic University of Science and Technology",country:{name:"India"}}},{id:"42847",title:"Dr.",name:"Belma",middleName:null,surname:"Işik Aslan",slug:"belma-isik-aslan",fullName:"Belma Işik Aslan",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/42847/images/system/42847.jpg",biography:"Dr. Belma IşIk Aslan was born in 1976 in Ankara-TURKEY. After graduating from TED Ankara College in 1994, she attended to Gazi University, Faculty of Dentistry in Ankara. She completed her PhD in orthodontic education at Gazi University between 1999-2005. Dr. Işık Aslan stayed at the Providence Hospital Craniofacial Institude and Reconstructive Surgery in Michigan, USA for three months as an observer. She worked as a specialist doctor at Gazi University, Dentistry Faculty, Department of Orthodontics between 2005-2014. She was appointed as associate professor in January, 2014 and as professor in 2021. Dr. Işık Aslan still works as an instructor at the same faculty. She has published a total of 35 articles, 10 book chapters, 39 conference proceedings both internationally and nationally. Also she was the academic editor of the international book 'Current Advances in Orthodontics'. She is a member of the Turkish Orthodontic Society and Turkish Cleft Lip and Palate Society. She is married and has 2 children. Her knowledge of English is at an advanced level.",institutionString:"Gazi University Dentistry Faculty Department of Orthodontics",institution:null},{id:"178412",title:"Associate Prof.",name:"Guhan",middleName:null,surname:"Dergin",slug:"guhan-dergin",fullName:"Guhan Dergin",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/178412/images/6954_n.jpg",biography:"Assoc. Prof. Dr. Gühan Dergin was born in 1973 in Izmit. He graduated from Marmara University Faculty of Dentistry in 1999. He completed his specialty of OMFS surgery in Marmara University Faculty of Dentistry and obtained his PhD degree in 2006. In 2005, he was invited as a visiting doctor in the Oral and Maxillofacial Surgery Department of the University of North Carolina, USA, where he went on a scholarship. Dr. Dergin still continues his academic career as an associate professor in Marmara University Faculty of Dentistry. He has many articles in international and national scientific journals and chapters in books.",institutionString:null,institution:{name:"Marmara University",country:{name:"Turkey"}}},{id:"178414",title:"Prof.",name:"Yusuf",middleName:null,surname:"Emes",slug:"yusuf-emes",fullName:"Yusuf Emes",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/178414/images/6953_n.jpg",biography:"Born in Istanbul in 1974, Dr. Emes graduated from Istanbul University Faculty of Dentistry in 1997 and completed his PhD degree in Istanbul University faculty of Dentistry Department of Oral and Maxillofacial Surgery in 2005. He has papers published in international and national scientific journals, including research articles on implantology, oroantral fistulas, odontogenic cysts, and temporomandibular disorders. Dr. Emes is currently working as a full-time academic staff in Istanbul University faculty of Dentistry Department of Oral and Maxillofacial Surgery.",institutionString:null,institution:{name:"Istanbul University",country:{name:"Turkey"}}},{id:"192229",title:"Ph.D.",name:"Ana Luiza",middleName:null,surname:"De Carvalho Felippini",slug:"ana-luiza-de-carvalho-felippini",fullName:"Ana Luiza De Carvalho Felippini",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/192229/images/system/192229.jpg",biography:null,institutionString:"University of São Paulo",institution:{name:"University of Sao Paulo",country:{name:"Brazil"}}},{id:"256851",title:"Prof.",name:"Ayşe",middleName:null,surname:"Gülşen",slug:"ayse-gulsen",fullName:"Ayşe Gülşen",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/256851/images/9696_n.jpg",biography:"Dr. Ayşe Gülşen graduated in 1990 from Faculty of Dentistry, University of Ankara and did a postgraduate program at University of Gazi. \nShe worked as an observer and research assistant in Craniofacial Surgery Departments in New York, Providence Hospital in Michigan and Chang Gung Memorial Hospital in Taiwan. \nShe works as Craniofacial Orthodontist in Department of Aesthetic, Plastic and Reconstructive Surgery, Faculty of Medicine, University of Gazi, Ankara Turkey since 2004.",institutionString:"Univeristy of Gazi",institution:null},{id:"255366",title:"Prof.",name:"Tosun",middleName:null,surname:"Tosun",slug:"tosun-tosun",fullName:"Tosun Tosun",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/255366/images/7347_n.jpg",biography:"Graduated at the Faculty of Dentistry, University of Istanbul, Turkey in 1989;\nVisitor Assistant at the University of Padua, Italy and Branemark Osseointegration Center of Treviso, Italy between 1993-94;\nPhD thesis on oral implantology in University of Istanbul and was awarded the academic title “Dr.med.dent.”, 1997;\nHe was awarded the academic title “Doç.Dr.” (Associated Professor) in 2003;\nProficiency in Botulinum Toxin Applications, Reading-UK in 2009;\nMastership, RWTH Certificate in Laser Therapy in Dentistry, AALZ-Aachen University, Germany 2009-11;\nMaster of Science (MSc) in Laser Dentistry, University of Genoa, Italy 2013-14.\n\nDr.Tosun worked as Research Assistant in the Department of Oral Implantology, Faculty of Dentistry, University of Istanbul between 1990-2002. \nHe worked part-time as Consultant surgeon in Harvard Medical International Hospitals and John Hopkins Medicine, Istanbul between years 2007-09.\u2028He was contract Professor in the Department of Surgical and Diagnostic Sciences (DI.S.C.), Medical School, University of Genova, Italy between years 2011-16. \nSince 2015 he is visiting Professor at Medical School, University of Plovdiv, Bulgaria. \nCurrently he is Associated Prof.Dr. at the Dental School, Oral Surgery Dept., Istanbul Aydin University and since 2003 he works in his own private clinic in Istanbul, Turkey.\u2028\nDr.Tosun is reviewer in journal ‘Laser in Medical Sciences’, reviewer in journal ‘Folia Medica\\', a Fellow of the International Team for Implantology, Clinical Lecturer of DGZI German Association of Oral Implantology, Expert Lecturer of Laser&Health Academy, Country Representative of World Federation for Laser Dentistry, member of European Federation of Periodontology, member of Academy of Laser Dentistry. Dr.Tosun presents papers in international and national congresses and has scientific publications in international and national journals. He speaks english, spanish, italian and french.",institutionString:null,institution:{name:"Istanbul Aydın University",country:{name:"Turkey"}}},{id:"171887",title:"Prof.",name:"Zühre",middleName:null,surname:"Akarslan",slug:"zuhre-akarslan",fullName:"Zühre Akarslan",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/171887/images/system/171887.jpg",biography:"Zühre Akarslan was born in 1977 in Cyprus. She graduated from Gazi University Faculty of Dentistry, Ankara, Turkey in 2000. \r\nLater she received her Ph.D. degree from the Oral Diagnosis and Radiology Department; which was recently renamed as Oral and Dentomaxillofacial Radiology, from the same university. \r\nShe is working as a full-time Associate Professor and is a lecturer and an academic researcher. \r\nHer expertise areas are dental caries, cancer, dental fear and anxiety, gag reflex in dentistry, oral medicine, and dentomaxillofacial radiology.",institutionString:"Gazi University",institution:{name:"Gazi University",country:{name:"Turkey"}}},{id:"256417",title:"Associate Prof.",name:"Sanaz",middleName:null,surname:"Sadry",slug:"sanaz-sadry",fullName:"Sanaz Sadry",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/256417/images/8106_n.jpg",biography:null,institutionString:null,institution:null},{id:"272237",title:"Dr.",name:"Pinar",middleName:"Kiymet",surname:"Karataban",slug:"pinar-karataban",fullName:"Pinar Karataban",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/272237/images/8911_n.png",biography:"Assist.Prof.Dr.Pınar Kıymet Karataban, DDS PhD \n\nDr.Pınar Kıymet Karataban was born in Istanbul in 1975. After her graduation from Marmara University Faculty of Dentistry in 1998 she started her PhD in Paediatric Dentistry focused on children with special needs; mainly children with Cerebral Palsy. She finished her pHD thesis entitled \\'Investigation of occlusion via cast analysis and evaluation of dental caries prevalance, periodontal status and muscle dysfunctions in children with cerebral palsy” in 2008. She got her Assist. Proffessor degree in Istanbul Aydın University Paediatric Dentistry Department in 2015-2018. ın 2019 she started her new career in Bahcesehir University, Istanbul as Head of Department of Pediatric Dentistry. In 2020 she was accepted to BAU International University, Batumi as Professor of Pediatric Dentistry. She’s a lecturer in the same university meanwhile working part-time in private practice in Ege Dental Studio (https://www.egedisklinigi.com/) a multidisciplinary dental clinic in Istanbul. Her main interests are paleodontology, ancient and contemporary dentistry, oral microbiology, cerebral palsy and special care dentistry. She has national and international publications, scientific reports and is a member of IAPO (International Association for Paleodontology), IADH (International Association of Disability and Oral Health) and EAPD (European Association of Pediatric Dentistry).",institutionString:null,institution:null},{id:"202198",title:"Dr.",name:"Buket",middleName:null,surname:"Aybar",slug:"buket-aybar",fullName:"Buket Aybar",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/202198/images/6955_n.jpg",biography:"Buket Aybar, DDS, PhD, was born in 1971. She graduated from Istanbul University, Faculty of Dentistry, in 1992 and completed her PhD degree on Oral and Maxillofacial Surgery in Istanbul University in 1997.\nDr. Aybar is currently a full-time professor in Istanbul University, Faculty of Dentistry Department of Oral and Maxillofacial Surgery. She has teaching responsibilities in graduate and postgraduate programs. Her clinical practice includes mainly dentoalveolar surgery.\nHer topics of interest are biomaterials science and cell culture studies. She has many articles in international and national scientific journals and chapters in books; she also has participated in several scientific projects supported by Istanbul University Research fund.",institutionString:null,institution:null},{id:"260116",title:"Dr.",name:"Mehmet",middleName:null,surname:"Yaltirik",slug:"mehmet-yaltirik",fullName:"Mehmet Yaltirik",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/260116/images/7413_n.jpg",biography:"Birth Date 25.09.1965\r\nBirth Place Adana- Turkey\r\nSex Male\r\nMarrial Status Bachelor\r\nDriving License Acquired\r\nMother Tongue Turkish\r\n\r\nAddress:\r\nWork:University of Istanbul,Faculty of Dentistry, Department of Oral Surgery and Oral Medicine 34093 Capa,Istanbul- TURKIYE",institutionString:null,institution:null},{id:"172009",title:"Dr.",name:"Fatma Deniz",middleName:null,surname:"Uzuner",slug:"fatma-deniz-uzuner",fullName:"Fatma Deniz Uzuner",position:null,profilePictureURL:"https://mts.intechopen.com/storage/users/172009/images/7122_n.jpg",biography:"Dr. Deniz Uzuner was born in 1969 in Kocaeli-TURKEY. After graduating from TED Ankara College in 1986, she attended the Hacettepe University, Faculty of Dentistry in Ankara. \nIn 1993 she attended the Gazi University, Faculty of Dentistry, Department of Orthodontics for her PhD education. After finishing the PhD education, she worked as orthodontist in Ankara Dental Hospital under the Turkish Government, Ministry of Health and in a special Orthodontic Clinic till 2011. Between 2011 and 2016, Dr. Deniz Uzuner worked as a specialist in the Department of Orthodontics, Faculty of Dentistry, Gazi University in Ankara/Turkey. In 2016, she was appointed associate professor. Dr. Deniz Uzuner has authored 23 Journal Papers, 3 Book Chapters and has had 39 oral/poster presentations. She is a member of the Turkish Orthodontic Society. 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Biochemistry examines macromolecules - proteins, nucleic acids, carbohydrates, and lipids – and their building blocks, structures, functions, and interactions. Much of biochemistry is devoted to enzymes, proteins that catalyze chemical reactions, enzyme structures, mechanisms of action and their roles within cells. Biochemistry also studies small signaling molecules, coenzymes, inhibitors, vitamins, and hormones, which play roles in life processes. Biochemical experimentation, besides coopting classical chemistry methods, e.g., chromatography, adopted new techniques, e.g., X-ray diffraction, electron microscopy, NMR, radioisotopes, and developed sophisticated microbial genetic tools, e.g., auxotroph mutants and their revertants, fermentation, etc. More recently, biochemistry embraced the ‘big data’ omics systems. Initial biochemical studies have been exclusively analytic: dissecting, purifying, and examining individual components of a biological system; in the apt words of Efraim Racker (1913 –1991), “Don’t waste clean thinking on dirty enzymes.” Today, however, biochemistry is becoming more agglomerative and comprehensive, setting out to integrate and describe entirely particular biological systems. The ‘big data’ metabolomics can define the complement of small molecules, e.g., in a soil or biofilm sample; proteomics can distinguish all the comprising proteins, e.g., serum; metagenomics can identify all the genes in a complex environment, e.g., the bovine rumen. This Biochemistry Series will address the current research on biomolecules and the emerging trends with great promise.",coverUrl:"https://cdn.intechopen.com/series/covers/11.jpg",latestPublicationDate:"July 5th, 2022",hasOnlineFirst:!0,numberOfOpenTopics:4,numberOfPublishedChapters:320,numberOfPublishedBooks:32,editor:{id:"31610",title:"Dr.",name:"Miroslav",middleName:null,surname:"Blumenberg",fullName:"Miroslav Blumenberg",profilePictureURL:"https://mts.intechopen.com/storage/users/31610/images/system/31610.jpg",biography:"Miroslav Blumenberg, Ph.D., was born in Subotica and received his BSc in Belgrade, Yugoslavia. He completed his Ph.D. at MIT in Organic Chemistry; he followed up his Ph.D. with two postdoctoral study periods at Stanford University. Since 1983, he has been a faculty member of the RO Perelman Department of Dermatology, NYU School of Medicine, where he is codirector of a training grant in cutaneous biology. Dr. Blumenberg’s research is focused on the epidermis, expression of keratin genes, transcription profiling, keratinocyte differentiation, inflammatory diseases and cancers, and most recently the effects of the microbiome on the skin. He has published more than 100 peer-reviewed research articles and graduated numerous Ph.D. and postdoctoral students.",institutionString:null,institution:{name:"New York University Langone Medical Center",institutionURL:null,country:{name:"United States of America"}}},subseries:[{id:"14",title:"Cell and Molecular Biology",keywords:"Omics (Transcriptomics; Proteomics; Metabolomics), Molecular Biology, Cell Biology, Signal Transduction and Regulation, Cell Growth and Differentiation, Apoptosis, Necroptosis, Ferroptosis, Autophagy, Cell Cycle, Macromolecules and Complexes, Gene Expression",scope:"The Cell and Molecular Biology topic within the IntechOpen Biochemistry Series aims to rapidly publish contributions on all aspects of cell and molecular biology, including aspects related to biochemical and genetic research (not only in humans but all living beings). We encourage the submission of manuscripts that provide novel and mechanistic insights that report significant advances in the fields. Topics include, but are not limited to: Advanced techniques of cellular and molecular biology (Molecular methodologies, imaging techniques, and bioinformatics); Biological activities at the molecular level; Biological processes of cell functions, cell division, senescence, maintenance, and cell death; Biomolecules interactions; Cancer; Cell biology; Chemical biology; Computational biology; Cytochemistry; Developmental biology; Disease mechanisms and therapeutics; DNA, and RNA metabolism; Gene functions, genetics, and genomics; Genetics; Immunology; Medical microbiology; Molecular biology; Molecular genetics; Molecular processes of cell and organelle dynamics; Neuroscience; Protein biosynthesis, degradation, and functions; Regulation of molecular interactions in a cell; Signalling networks and system biology; Structural biology; Virology and microbiology.",annualVolume:11410,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/14.jpg",editor:{id:"165627",title:"Dr.",name:"Rosa María",middleName:null,surname:"Martínez-Espinosa",fullName:"Rosa María Martínez-Espinosa",profilePictureURL:"https://mts.intechopen.com/storage/users/165627/images/system/165627.jpeg",institutionString:null,institution:{name:"University of Alicante",institutionURL:null,country:{name:"Spain"}}},editorTwo:null,editorThree:null,editorialBoard:[{id:"79367",title:"Dr.",name:"Ana Isabel",middleName:null,surname:"Flores",fullName:"Ana Isabel Flores",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRpIOQA0/Profile_Picture_1632418099564",institutionString:null,institution:{name:"Hospital Universitario 12 De Octubre",institutionURL:null,country:{name:"Spain"}}},{id:"328234",title:"Ph.D.",name:"Christian",middleName:null,surname:"Palavecino",fullName:"Christian Palavecino",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0033Y000030DhEhQAK/Profile_Picture_1628835318625",institutionString:null,institution:{name:"Central University of Chile",institutionURL:null,country:{name:"Chile"}}},{id:"186585",title:"Dr.",name:"Francisco Javier",middleName:null,surname:"Martin-Romero",fullName:"Francisco Javier Martin-Romero",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bSB3HQAW/Profile_Picture_1631258137641",institutionString:null,institution:{name:"University of Extremadura",institutionURL:null,country:{name:"Spain"}}}]},{id:"15",title:"Chemical Biology",keywords:"Phenolic Compounds, Essential Oils, Modification of Biomolecules, Glycobiology, Combinatorial Chemistry, Therapeutic peptides, Enzyme Inhibitors",scope:"Chemical biology spans the fields of chemistry and biology involving the application of biological and chemical molecules and techniques. In recent years, the application of chemistry to biological molecules has gained significant interest in medicinal and pharmacological studies. This topic will be devoted to understanding the interplay between biomolecules and chemical compounds, their structure and function, and their potential applications in related fields. Being a part of the biochemistry discipline, the ideas and concepts that have emerged from Chemical Biology have affected other related areas. This topic will closely deal with all emerging trends in this discipline.",annualVolume:11411,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/15.jpg",editor:{id:"441442",title:"Dr.",name:"Şükrü",middleName:null,surname:"Beydemir",fullName:"Şükrü Beydemir",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0033Y00003GsUoIQAV/Profile_Picture_1634557147521",institutionString:null,institution:{name:"Anadolu University",institutionURL:null,country:{name:"Turkey"}}},editorTwo:{id:"13652",title:"Prof.",name:"Deniz",middleName:null,surname:"Ekinci",fullName:"Deniz Ekinci",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002aYLT1QAO/Profile_Picture_1634557223079",institutionString:null,institution:{name:"Ondokuz Mayıs University",institutionURL:null,country:{name:"Turkey"}}},editorThree:null,editorialBoard:[{id:"219081",title:"Dr.",name:"Abdulsamed",middleName:null,surname:"Kükürt",fullName:"Abdulsamed Kükürt",profilePictureURL:"https://mts.intechopen.com/storage/users/219081/images/system/219081.png",institutionString:null,institution:{name:"Kafkas University",institutionURL:null,country:{name:"Turkey"}}},{id:"241413",title:"Dr.",name:"Azhar",middleName:null,surname:"Rasul",fullName:"Azhar Rasul",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRT1oQAG/Profile_Picture_1635251978933",institutionString:null,institution:{name:"Government College University, Faisalabad",institutionURL:null,country:{name:"Pakistan"}}},{id:"178316",title:"Ph.D.",name:"Sergey",middleName:null,surname:"Sedykh",fullName:"Sergey Sedykh",profilePictureURL:"https://mts.intechopen.com/storage/users/178316/images/system/178316.jfif",institutionString:null,institution:{name:"Novosibirsk State University",institutionURL:null,country:{name:"Russia"}}}]},{id:"17",title:"Metabolism",keywords:"Biomolecules Metabolism, Energy Metabolism, Metabolic Pathways, Key Metabolic Enzymes, Metabolic Adaptation",scope:"Metabolism is frequently defined in biochemistry textbooks as the overall process that allows living systems to acquire and use the free energy they need for their vital functions or the chemical processes that occur within a living organism to maintain life. Behind these definitions are hidden all the aspects of normal and pathological functioning of all processes that the topic ‘Metabolism’ will cover within the Biochemistry Series. Thus all studies on metabolism will be considered for publication.",annualVolume:11413,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/17.jpg",editor:{id:"138626",title:"Dr.",name:"Yannis",middleName:null,surname:"Karamanos",fullName:"Yannis Karamanos",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002g6Jv2QAE/Profile_Picture_1629356660984",institutionString:null,institution:{name:"Artois University",institutionURL:null,country:{name:"France"}}},editorTwo:null,editorThree:null,editorialBoard:[{id:"243049",title:"Dr.",name:"Anca",middleName:null,surname:"Pantea Stoian",fullName:"Anca Pantea Stoian",profilePictureURL:"https://mts.intechopen.com/storage/users/243049/images/system/243049.jpg",institutionString:null,institution:{name:"Carol Davila University of Medicine and Pharmacy",institutionURL:null,country:{name:"Romania"}}},{id:"203824",title:"Dr.",name:"Attilio",middleName:null,surname:"Rigotti",fullName:"Attilio Rigotti",profilePictureURL:"//cdnintech.com/web/frontend/www/assets/author.svg",institutionString:null,institution:{name:"Pontifical Catholic University of Chile",institutionURL:null,country:{name:"Chile"}}},{id:"300470",title:"Dr.",name:"Yanfei (Jacob)",middleName:null,surname:"Qi",fullName:"Yanfei (Jacob) Qi",profilePictureURL:"https://mts.intechopen.com/storage/users/300470/images/system/300470.jpg",institutionString:null,institution:{name:"Centenary Institute of Cancer Medicine and Cell Biology",institutionURL:null,country:{name:"Australia"}}}]},{id:"18",title:"Proteomics",keywords:"Mono- and Two-Dimensional Gel Electrophoresis (1-and 2-DE), Liquid Chromatography (LC), Mass Spectrometry/Tandem Mass Spectrometry (MS; MS/MS), Proteins",scope:"With the recognition that the human genome cannot provide answers to the etiology of a disorder, changes in the proteins expressed by a genome became a focus in research. Thus proteomics, an area of research that detects all protein forms expressed in an organism, including splice isoforms and post-translational modifications, is more suitable than genomics for a comprehensive understanding of the biochemical processes that govern life. The most common proteomics applications are currently in the clinical field for the identification, in a variety of biological matrices, of biomarkers for diagnosis and therapeutic intervention of disorders. From the comparison of proteomic profiles of control and disease or different physiological states, which may emerge, changes in protein expression can provide new insights into the roles played by some proteins in human pathologies. Understanding how proteins function and interact with each other is another goal of proteomics that makes this approach even more intriguing. Specialized technology and expertise are required to assess the proteome of any biological sample. Currently, proteomics relies mainly on mass spectrometry (MS) combined with electrophoretic (1 or 2-DE-MS) and/or chromatographic techniques (LC-MS/MS). MS is an excellent tool that has gained popularity in proteomics because of its ability to gather a complex body of information such as cataloging protein expression, identifying protein modification sites, and defining protein interactions. The Proteomics topic aims to attract contributions on all aspects of MS-based proteomics that, by pushing the boundaries of MS capabilities, may address biological problems that have not been resolved yet.",annualVolume:11414,isOpenForSubmission:!0,coverUrl:"https://cdn.intechopen.com/series_topics/covers/18.jpg",editor:{id:"200689",title:"Prof.",name:"Paolo",middleName:null,surname:"Iadarola",fullName:"Paolo Iadarola",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bSCl8QAG/Profile_Picture_1623568118342",institutionString:null,institution:{name:"University of Pavia",institutionURL:null,country:{name:"Italy"}}},editorTwo:{id:"201414",title:"Dr.",name:"Simona",middleName:null,surname:"Viglio",fullName:"Simona Viglio",profilePictureURL:"https://s3.us-east-1.amazonaws.com/intech-files/0030O00002bRKDHQA4/Profile_Picture_1630402531487",institutionString:null,institution:{name:"University of Pavia",institutionURL:null,country:{name:"Italy"}}},editorThree:null,editorialBoard:[{id:"72288",title:"Dr.",name:"Arli Aditya",middleName:null,surname:"Parikesit",fullName:"Arli Aditya Parikesit",profilePictureURL:"https://mts.intechopen.com/storage/users/72288/images/system/72288.jpg",institutionString:null,institution:{name:"Indonesia International Institute for Life Sciences",institutionURL:null,country:{name:"Indonesia"}}},{id:"40928",title:"Dr.",name:"Cesar",middleName:null,surname:"Lopez-Camarillo",fullName:"Cesar Lopez-Camarillo",profilePictureURL:"https://mts.intechopen.com/storage/users/40928/images/3884_n.png",institutionString:null,institution:{name:"Universidad Autónoma de la Ciudad de México",institutionURL:null,country:{name:"Mexico"}}},{id:"81926",title:"Dr.",name:"Shymaa",middleName:null,surname:"Enany",fullName:"Shymaa Enany",profilePictureURL:"https://mts.intechopen.com/storage/users/81926/images/system/81926.png",institutionString:"Suez Canal University",institution:{name:"Suez Canal University",institutionURL:null,country:{name:"Egypt"}}}]}]}},libraryRecommendation:{success:null,errors:{},institutions:[]},route:{name:"chapter.detail",path:"/chapters/66476",hash:"",query:{},params:{id:"66476"},fullPath:"/chapters/66476",meta:{},from:{name:null,path:"/",hash:"",query:{},params:{},fullPath:"/",meta:{}}}},function(){var e;(e=document.currentScript||document.scripts[document.scripts.length-1]).parentNode.removeChild(e)}()