Absolute dating available from the study área.
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More than half of the publishers listed alongside IntechOpen (18 out of 30) are Social Science and Humanities publishers. IntechOpen is an exception to this as a leader in not only Open Access content but Open Access content across all scientific disciplines, including Physical Sciences, Engineering and Technology, Health Sciences, Life Science, and Social Sciences and Humanities.
\\n\\nOur breakdown of titles published demonstrates this with 47% PET, 31% HS, 18% LS, and 4% SSH books published.
\\n\\n“Even though ItechOpen has shown the potential of sci-tech books using an OA approach,” other publishers “have shown little interest in OA books.”
\\n\\nAdditionally, each book published by IntechOpen contains original content and research findings.
\\n\\nWe are honored to be among such prestigious publishers and we hope to continue to spearhead that growth in our quest to promote Open Access as a true pioneer in OA book publishing.
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Simba Information has released its Open Access Book Publishing 2020 - 2024 report and has again identified IntechOpen as the world’s largest Open Access book publisher by title count.
\n\nSimba Information is a leading provider for market intelligence and forecasts in the media and publishing industry. The report, published every year, provides an overview and financial outlook for the global professional e-book publishing market.
\n\nIntechOpen, De Gruyter, and Frontiers are the largest OA book publishers by title count, with IntechOpen coming in at first place with 5,101 OA books published, a good 1,782 titles ahead of the nearest competitor.
\n\nSince the first Open Access Book Publishing report published in 2016, IntechOpen has held the top stop each year.
\n\n\n\nMore than half of the publishers listed alongside IntechOpen (18 out of 30) are Social Science and Humanities publishers. IntechOpen is an exception to this as a leader in not only Open Access content but Open Access content across all scientific disciplines, including Physical Sciences, Engineering and Technology, Health Sciences, Life Science, and Social Sciences and Humanities.
\n\nOur breakdown of titles published demonstrates this with 47% PET, 31% HS, 18% LS, and 4% SSH books published.
\n\n“Even though ItechOpen has shown the potential of sci-tech books using an OA approach,” other publishers “have shown little interest in OA books.”
\n\nAdditionally, each book published by IntechOpen contains original content and research findings.
\n\nWe are honored to be among such prestigious publishers and we hope to continue to spearhead that growth in our quest to promote Open Access as a true pioneer in OA book publishing.
\n\n\n\n
\n'}],latestNews:[{slug:"webinar-introduction-to-open-science-wednesday-18-may-1-pm-cest-20220518",title:"Webinar: Introduction to Open Science | Wednesday 18 May, 1 PM CEST"},{slug:"step-in-the-right-direction-intechopen-launches-a-portfolio-of-open-science-journals-20220414",title:"Step in the Right Direction: IntechOpen Launches a Portfolio of Open Science Journals"},{slug:"let-s-meet-at-london-book-fair-5-7-april-2022-olympia-london-20220321",title:"Let’s meet at London Book Fair, 5-7 April 2022, Olympia London"},{slug:"50-books-published-as-part-of-intechopen-and-knowledge-unlatched-ku-collaboration-20220316",title:"50 Books published as part of IntechOpen and Knowledge Unlatched (KU) Collaboration"},{slug:"intechopen-joins-the-united-nations-sustainable-development-goals-publishers-compact-20221702",title:"IntechOpen joins the United Nations Sustainable Development Goals Publishers Compact"},{slug:"intechopen-signs-exclusive-representation-agreement-with-lsr-libros-servicios-y-representaciones-s-a-de-c-v-20211123",title:"IntechOpen Signs Exclusive Representation Agreement with LSR Libros Servicios y Representaciones S.A. de C.V"},{slug:"intechopen-expands-partnership-with-research4life-20211110",title:"IntechOpen Expands Partnership with Research4Life"},{slug:"introducing-intechopen-book-series-a-new-publishing-format-for-oa-books-20210915",title:"Introducing IntechOpen Book Series - A New Publishing Format for OA Books"}]},book:{item:{type:"book",id:"1346",leadTitle:null,fullTitle:"Coronary Angiography - Advances in Noninvasive Imaging Approach for Evaluation of Coronary Artery Disease",title:"Coronary Angiography",subtitle:"Advances in Noninvasive Imaging Approach for Evaluation of Coronary Artery Disease",reviewType:"peer-reviewed",abstract:"In the intervening 10 years tremendous advances in the field of cardiac computed tomography have occurred. We now can legitimately claim that computed tomography angiography (CTA) of the coronary arteries is available. In the evaluation of patients with suspected coronary artery disease (CAD), many guidelines today consider CTA an alternative to stress testing. The use of CTA in primary prevention patients is more controversial in considering diagnostic test interpretation in populations with a low prevalence to disease. However the nuclear technique most frequently used by cardiologists is myocardial perfusion imaging (MPI). The combination of a nuclear camera with CTA allows for the attainment of coronary anatomic, cardiac function and MPI from one piece of equipment. PET/SPECT cameras can now assess perfusion, function, and metabolism. Assessing cardiac viability is now fairly routine with these enhancements to cardiac imaging. This issue is full of important information that every cardiologist needs to now.",isbn:null,printIsbn:"978-953-307-675-1",pdfIsbn:"978-953-51-6485-2",doi:"10.5772/1812",price:139,priceEur:155,priceUsd:179,slug:"coronary-angiography-advances-in-noninvasive-imaging-approach-for-evaluation-of-coronary-artery-disease",numberOfPages:428,isOpenForSubmission:!1,isInWos:1,isInBkci:!1,hash:"a12df3d9245e8428ede66b6ae0c7836c",bookSignature:"Branislav Baskot",publishedDate:"September 15th 2011",coverURL:"https://cdn.intechopen.com/books/images_new/1346.jpg",numberOfDownloads:51050,numberOfWosCitations:14,numberOfCrossrefCitations:9,numberOfCrossrefCitationsByBook:0,numberOfDimensionsCitations:23,numberOfDimensionsCitationsByBook:0,hasAltmetrics:1,numberOfTotalCitations:46,isAvailableForWebshopOrdering:!0,dateEndFirstStepPublish:"October 27th 2010",dateEndSecondStepPublish:"November 24th 2010",dateEndThirdStepPublish:"March 31st 2011",dateEndFourthStepPublish:"April 30th 2011",dateEndFifthStepPublish:"June 29th 2011",currentStepOfPublishingProcess:5,indexedIn:"1,2,3,4,5,6",editedByType:"Edited by",kuFlag:!1,featuredMarkup:null,editors:[{id:"33401",title:"Prof.",name:"Baskot",middleName:null,surname:"Branislav",slug:"baskot-branislav",fullName:"Baskot Branislav",profilePictureURL:"https://mts.intechopen.com/storage/users/33401/images/1794_n.jpg",biography:"Branislav Baskot MD PhD Ass Prof; was born 1958. in Ruma, Serbia. He finished Medicine Faculty in Sarajevo, Bosnia and Hercegovina, and specialization of Nuclear Medicine on Military Medical Academy in Belgrade, Serbia in 1994. The main occupation in the field of Nuclear medicine was nuclear cardiology. He obtained his Doctoral degree in 2005.; “Determination of culprit lesion before and after percutaneous coronary intervention by myocardial perfusion imaging” and Master’s Degree; “Myocardial perfusion imaging with 99mTc-Tetrofosmin in the diagnosis ischemic heart disease” in 2003. 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This has led to the precise management of gynecological problems in the field of infertility, recurrent miscarriages, postmenopausal bleeding, uterine cancer, and menstrual disorders. Although transvaginal ultrasound scanning in 2D and 3D mode are considered useful tools for first line screening, the gap between precise diagnosis before treatment was covered by the introduction of a fine hysteroscope, which provides more accurate information. Nevertheless in most cases operative hysteroscopy substituted the blind technique of dilation and curettage, solely used over the past years.
Office hysteroscopy is a very useful technique for diagnosis and treatment of uterine pathology in an office-based environment (Figure 1). It is directly related to the technological explosion, which during the last years has further evolved and given us the opportunity to perform hysteroscopy without providing general anesthesia or sedation to the patients, due to the narrow width of the latest generation hysteroscopes. This means that after adequate and thorough experience and toward the reduction of the cost and satisfaction of the patients, hysteroscopy in an outpatient environment, called office hysteroscopy, has started to attract the majority of gynecologists.
The aim of this chapter is to familiarize the clinicians in the field of gynecology with the instrumentation and setup, the technique itself, indications, and contraindications for performing office hysteroscopy and finally the advantages for the patient and the clinician who perform this endoscopic approach.
Typical setup for office hysteroscopy in a private office-based practice
There are two different types of hysteroscopes available. The rigid hysteroscopes are composed of two parts, the scope and the outer sheath with a total diameter of 2.9–4 mm (Figure 2, Figure 3). The outer sheath comes with suction and irrigation valves, which allows the inflow and outflow of the distension medium of the uterine cavity and can be mounted on an irrigation-suction device. Further, there is an operating channel from which specifically designed instruments can go through for operative purposes or retrieval of endometrial tissue for biopsy. The advantages are that they are exactly the same as the non-office hysteroscopes, so for a clinician who is experienced in hysteroscopy there is no learning curve, and they can be used without inserting a vaginal speculum (no-touch technique or vaginoscopic approach). Furthermore, they can be used with suction device, while a great variety of instruments are specifically designed for these and the scopes are available in 12, 25, or 30 degrees angular vision. In the disadvantages we need to mention that they come in many parts and also the optics are very thin, from 2 mm in diameter, which makes them very fragile during cleaning and disinfection, while there is an existing risk of uterine perforation due to the rigidity. Finally, they have greater width compared with the flexible hysteroscopes.
Operative hysteroscope for office hysteroscopy
The flexible hysteroscopes (Figure 4) are compact without any additional part, even the light source cable is permanently fixed on these. They do not come with an outer sheath, which means that they lack suction mechanism but there is a working channel, through which flexible instruments can be inserted and used for biopsy and minor surgical procedures. The visual angle is up to 120 degrees due to the flexibility, so there is no external manipulation of the hysteroscope, which can minimize the discomfort of the patient. Cleaning, disinfection, and storage are simpler than the rigid ones. The possible perforation of the uterus is quite non-existing, but on the contrary during insertion the scope might be obstructed by even loose adhesions or endometrial structures such as large polyps or fibroids. In practice, and from our experience, it means that it is preferable to dilate the cervical canal before insertion with a thin dilator. The vaginoscopic approach is more difficult to be performed with a flexible hysteroscope compared to the rigid ones and therefore in all cases the use of a vaginal speculum is needed but on the other hand the use of a tenaculum for straightening the cervical canal is almost never needed, as long as due to the flexibility the scope can easily go through all types of uterus (anteverted, retroverted, etc.). Finally, there is clear evidence that in procedures where flexible hysteroscopes are used patients experience less pain and discomfort [1].
Distal part of an office operative hysteroscope
Flexible hysteroscope of 3.1 mm total diameter
The basic setup in order to perform an office hysteroscopy consists of a camera, a camera control unit connected to a -DVD recording device, a light source, and a monitor, connected exactly the same way as in the operating theater, all of them placed on an equipment cart, or there are also compact devices where all the above mentioned come as a single appliance. An irrigation-suction unit for the distension medium can be used, but for diagnostic purposes a handcuff with a manual air pump can be used for irrigation, around the bottle of the distension medium, as long as for experienced clinicians the whole procedure will last less than 5 minutes and the amount of the distension medium to be used will be less than 200 ml. Additional equipment ready for use can be a dental syringe fitted with a sealed cartridge containing anesthetic solution for cervical local anesthesia and a plastic cervical dilator, a vaginal speculum, sterile gauges, and a forceps in order to control spotting bleeding from the cervix, after injection of local anesthetic, all placed on a secondary equipment cart. The patient is placed on a gynecological chair, in lithotomy position that will allow the clinician to perform manipulations with the hysteroscope without restrictions. It is advised that a flat examination bed is also present in the same room, in case of vasovagal reaction after the end of the procedure. A typical setup is shown in Figure 1. Finally it is advised that a chaperon is present during the procedure, but in terms of assistance the setup described is ideal for a single person to perform.
There is no clear evidence that local anesthesia should be used prior to office hysteroscopy, while results from several studies cannot reach a definite conclusion. Nevertheless in cases of non-vaginoscopic procedures from our experience, we strongly recommend the proposal of cervical local anesthetic, which can possibly lead to less pain experienced by the patients, especially if cervical dilatation is needed, but also gives a feeling of confidence to the patients before getting through the procedure. Moreover, in cases where the use of tenaculum is needed, local cervical anesthesia should be applied [2]. It should be mentioned that use of intracervical or paracervical local anesthesia for preventing vasovagal reactions is not an indication.
Conscious sedation should not be used as it does not contribute to pain control more than local anesthesia and also dangerous complications that may occur cannot be controlled in an office-cased environment [3].
As far as analgesia is concerned, it is recommended that NSAIDS (non-steroidal anti-inflammatory drugs) should be used an hour prior to the procedure for pain relief but the use of opioids should be avoided as they may have adverse effects like nausea, vomiting, and drowsiness [2].
In general the choice for analgesia prior or during the procedure should be decided by the clinician according to the patient’s history, possible vasovagal reaction in the past, the condition of the uterine cervix (nulliparous or multiparous), and the reluctancy of the patient regarding the possible pain that she may experience during the procedure. All the choices should be offered to the patients during the consent procedure.
Office hysteroscopy can be performed with the use of normal saline solution or CO2. It is advisable that the choice of the medium is at the discretion of the clinician. Nevertheless, there seem to be advantages from the use of normal saline as long as it can provide better visibility and clearing out of blood clots and debris, less possible vasovagal reactions (sickness, bradycardia, and hypotension) from the patients, and also the setup is more simple and more practical compared to CO2. Furthermore, the use of normal saline does not offer reduction of pain but can lead to quicker procedures [4,5], but the latter is clearly affected also by the clinician’s experience with the medium and the procedure itself.
Office hysteroscopy is the most accurate diagnostic tool for endometrial pathologies and a second line tool after primary diagnosis deriving from 2D or 3D transvaginal ultrasound scan. Compared to the hysteroscopy performed in the operating theater under general anesthesia or sedation, there are clear benefits for the patients, such as the avoidance of taking general anesthesia, especially for patients who are at high-risk for anesthetic complications. The reduced time of the whole procedure and also the location, especially when performed in an out-of hospital environment, are crucial for the patients in order to decide. Also, the reduced cost of around 40–60%, as long as hospital and anesthetic costs are excluded, attracts more patients and also more clinicians to propose, especially in current years of financial recession. Finally the provision of this diagnostic tool in an office-based environment gives an added value to the private practice and its services, but also assists the clinicians to provide more than one choice to their patients.
Indications for diagnostic office hysteroscopy can be categorized for premenopausal and postmenopausal women.
Abnormal uterine bleeding is an indication for office hysteroscopy, if there is clear evidence of pathology at the ultrasound scan. The authors recommend that before proposing the technique, if there are no obvious ultrasonographic findings, it is wise to exclude any other endocrine, ovarian, or cervical pathology.
In terms of infertility investigation, office hysteroscopy is very useful in the investigation of the endometrial cavity in women who underwent two complete cycles of in vitro fertilization (IVF) – two failed implantations, even if there is no ultrasonographic evidence. The same indication stands for women with recurrent miscarriages – more than three consecutive miscarriages. Small endometrial polyps, uterine septae, endometrial adhesions, and cervical adhesions are common findings, which can be revealed with hysteroscopy. This approach is, also, very useful for the evaluation of the quality of the endometrium during the luteal phase.
Women who take tamoxifen as a regime for breast cancer are in need of endometrial assessment by biopsy and thus hysteroscopy is not an absolute indication, but in cases where endometrial thickness is ≥ 8 mm it is highly recommended in order to exclude an endometrial polyp or ongoing endometrial cancer [6].
Postmenopausal women with uterine bleeding should be investigated with office hysteroscopy regardless of the ultrasonographic findings, which apart from benign pathologies can lead to the diagnosis of uterine or cervical cancer. In cases of cancer the benefit of accurate diagnosis outweighs the risk of spreading neoplastic cells into the abdominal cavity and thus dilatation and curettage is advised not to be preferred over hysteroscopy [7]. A finding of an endometrial polyp in postmenopausal women is not a rare finding.
Operative procedures performed in an office-based environment are quite limited. There is no specific guideline regarding operative procedures but usually minor procedures such as endometrial biopsies, removal of endometrial polyps, dissection of loose intrauterine adhesions, removal of intrauterine devices with a missing thread or foreign objects and also for permanent tubal sterilization with the insertion of tubal coils (Essure®) are performed in the everyday clinical practice and are well tolerated by the patients. Operative office hysteroscopy can be an extension of diagnostic office hysteroscopy, as long as there are no special setup requirements and cervical preparation is not needed.
Contraindications for both diagnostic and operative hysteroscopy are heavy uterine bleeding or menstruation, vaginal infection, active pelvic inflammatory disease, and history of adverse reactions during a previous office hysteroscopy. As mentioned earlier, suspicion of cancer is not a contraindication for performing diagnostic hysteroscopy and biopsy.
Office hysteroscopy is mainly designed for the patient’s advantage. The use of hysteroscopy in an office-based environment, especially in the “one-stop” clinic, in a hospital or in a private practice, can give fast and accurate diagnosis and treatment without waiting lists and at a substantially lower cost, as hospital and anesthetic costs are excluded. Without the use of sedation or anesthesia, patients can go back to their everyday activities just after the end of the procedure. The disadvantage of the possible discomfort during the procedure or the cramp-like lower abdominal pain after are outweighed by the benefits that the patients can have.
For the clinicians in the fields of gynecology, infertility, and gynecological oncology, office hysteroscopy is the ultimate tool for accurate diagnosis of endometrial pathologies. A future management plan can be easily scheduled after the end of the procedure, unless a further pathology report from biopsies is expected.
Regarding the diagnosis, from our experience, miniature hysteroscopes with a low width inflow channel for the distention medium provide low pressure distention of the uterine cavity and so in cases of soft tissue structures like polyps, adenomyomas, and fundal adhesions we get a first more realistic depiction of the uterine cavity.
Of course the setup in a private practice is not time-consuming, as long as the time needed for the setup arrangements before and after the procedure is many times more than the procedure itself and so it is suggested that a special separate room or appointment on a specific day should be used, if the same room is to be used after for other examination purposes. In general though, in a private gynecological practice, application of office hysteroscopy extends the list of the provisional services and gives the clinician an added value, though even in our days the technique is not very widespread.
Office hysteroscopy is the undoubtful gold-standard tool for the investigation of the uterine cavity. It is a technology-based technique that has greatly evolved during the last decade, and there is still place for further improvements. Ideas for change come from the gynecologists, through the everyday practice, and should be addressed to the manufacturing companies in the field.
For the clinicians who want to apply hysteroscopy in an office-based environment, the training is much shorter and easier if they had previous training and experience in hysteroscopy under general anesthesia. This, on the other hand may restrict many clinicians from getting involved for the first time with diagnostic office hysteroscopy, which is a simple and low-risk technique. This reluctance may also derive from up-to-date guidelines, which are unclear in specific details as the type of hysteroscope to choose, provision of local anesthesia or not.
Practically, from the patient’s point of view and against all the benefits that office hysteroscopy provides, the only fear is the experience of pain and discomfort during the procedure. On the contrary pain intensity is a subjective evidence described in relative research, thus local anesthetic should always be discussed with the patients when consenting and provided according to the possible length of the procedure.
The use of flexible hysteroscopes result in less painful diagnostic procedures compared to the rigid one, so for a clinician who will only perform diagnostic hysteroscopy in the office seems like a better choice, though taking into consideration that the learning curve is longer, compared to the rigid hysteroscope.
Clinicians in the field of gynecology who are reluctant against the technique should get more familiar with office hysteroscopy where training is available, courses or any type of medical literature. Further research will probably clarify some details and assist the clinicians to take the right decisions for providing the best possible care according to the patients’ needs. We assume that in the near future almost all diagnostic and minor operative hysteroscopic procedures will be solely performed in an office-based environment either inside a hospital or in a private practice.
It is evident that office hysteroscopy enables the clinician to perform not only diagnostic but also minor operative procedures in an office setting with less risk, low cost, and better results. The near future comprises improvements in the hysteroscopic instrumentation, new energy supplies, and new systems for controlling intrauterine pressure, which will yield further benefits for the patients and the clinicians.
The Quaternary is characterized worldwide by important climate oscillations, with extremes represented by glacial and interglacial periods resulting from temperature variations that caused marked changes in sea level (e.g., [1]). In coastal areas, transgressive-regressive events have generated a sequence of erosion forms (coastal terraces and paleocliffs) and beach deposits that, for different reasons, have been protected from degradation processes and are therefore an important testimony of climate changes that have occurred in most recent geologic time [2].
In 1941, Milankovitch developed a planetary theory that attributes Quaternary glacial and interglacial cycles to modifications of orbital parameters such as eccentricity (100 Ka), obliquity (41Ka), and precession of the equinoxes (19 Ka).
Since the beginning of the Pleistocene, climatic oscillations would have followed periodic cycles of about 40 Ky that seem to conform the variation cycle of the earth axis. The amplitude of the cycles tended to increase 1.5 My ago, and from 600 Ka the glacial cycles have occurred at intervals of between 80 and 120 Ky (e.g., [3, 4]). This duration of the recent cycles is similar to the period of variation of the eccentricity of the earth orbit, of 100 Ky.
The different glacial and interglacial events occurred during the Quaternary were differentiated through the marine isotope stages (MIS). These MIS represent alternate cold and warm periods established on the basis of δ180 of benthic foraminifers, obtained from cores of the sea bottom [5]. Emialiani [6] divided the last million years in successive isotopic stages on the basis of the δ180/δ160 relationship. Each isotopic stage represents a glacial period (designated with an odd number) or interglacial (designated with an even number), and reveal the advance and retreat of the ice during the last glaciations.
Globally, the MIS 11 encompasses from 424 to 374 ka. It was a long warm period that reached a global mean sea level of 6 to 13 m above the present one between 410 and 400 ka [2]. Some authors (e.g., [7, 8, 9]) consider the MIS 11 as an analogous of the Holocene both in climatic conditions and orbital forcing. According to Ashton et al. [10] the climatic conditions in marine isotopic and ice sheet records include at least two large warm episodes with an intermediate cooling phase. The warm conditions of this interglacial were reflected in different marine and terrestrial communities (e.g., [9, 11, 12]).
MIS 9 encompasses from ca. 330 up to 310 ka and sea level was 3 ± 3 m below the present one [13]. In the Northern Hemisphere, at Henderson Island (24°22’S/128°20’W), the highest sea level recorded in MIS 9 is between 334 ± 4 and 324 ± 3 ka in agreement with the maximum sun insulation of 333 ka [14]. In the western Mediterranean (Spain) the sea surface temperature (SST) and the salinity recorded in this interglacial were similar to those of MIS 7 and MIS 5e [15], whereas other authors (e.g., [16]) suggested that according to paleontological evidence, this interglacial was warmer than MIS 7 and the Holocene, and similar to MIS 5e.
MIS 7 encompasses from ca. 245 up to 190 ka [17] with three temperature maximums [18]. Isotopic data of some deep sea cores suggest that the sea level would not have reached the level of the present cero [19, 20], although other authors suggest values around −18 m [17]. SST of this interglacial was higher than the present one [21, 22, 23]. In the European coasts, the marine deposits of MIS 7 record the appearance of the “Senegalese” marine fauna from the African coast, confirming this stage as warm in the Northern Hemisphere (e.g., [24, 25, 26]). Similar conditions are observed in the Southern Hemisphere: the SST of the southern Argentine Patagonia (42°–43°S) is proposed to be similar or slightly warmer than today on the basis of the record of warm water mollusks (e.g., [27, 28]).
MIS 5 in the substage e, is one of the most studied episodes, and best represented worldwide. It encompasses from ca. 130 ± 2 to 119 ± 2 ka [29] and the SST was approximately 2°C higher than the present one (e.g., [30, 31]). Comparing with other interglacials, MIS 5e has the best records of SST [18]. Evidence of warm water benthic mollusks, and changes in their geographic distribution was found in MIS 5e (e.g., [5, 26, 27, 32, 33, 34, 35, 36, 37, 38, 39, 40, 41, 42, 43, 44, 45, 46, 47, 48]).
MIS 1 encompasses the last 11.7 ka [49], when the last glaciation is considered to be ended [50]. There is an increase of the SST and humidity worldwide (e.g., [4, 51, 52, 53, 54, 55, 56]) with some records in the Southern Hemisphere (e.g., [37, 49, 50, 57, 58, 59]). This phenomenon is reflected worldwide in the biotic communities with changes in composition, abundance, diversity and distribution (e.g., [60, 61, 62]).
In the Argentine Patagonian region, the stages MIS 11 to MIS 1 are represented, as well as ingressions older then MIS 11, but with poor records and fossil content [32].
Along the Argentine coast, broad extensions of the littoral of the Buenos Aires Province (BAP) and north Patagonia were affected by accumulation and erosion processes produced by sea level oscillations during Quaternary transgressions (e.g., [63, 64]).
Northern Patagonia has been divided into two regions according to their province. The first groups three areas of the south of the BAP (A-C) and record the presence of the interglacials ≥ MIS 9, MIS 5e and MIS 1 [5, 65, 66], and the other one belongs to region D, and records the presence of the interglacials ≥ MIS 9, MIS 7, MIS 5e, and MIS 1 (Figure 1).
(A) Map of study, and (B) four areas in the northern Patagonia in Argentina.
In region A, from Peninsula Verde to Otero Island, the transgressive deposits have been assigned to the Sangamon (? Late Pleistocene), which are represented in the area of the Colorado River delta by paleocliffs associated with coast lines up to 10 m height [67]. These marine deposits are assigned to the oldest interglacials because of their geomorphological, altimetric and cementation similarity [68]. Among them, there are scarce, thin, and isolated deposits on the continent which are assigned to ≥ MIS 9 [68, 69]. The terminal area of the delta is formed by the marine deposits of the MIS 1 ingression, which are beach ridges or intertidal environments [68].
In region B, which extends from the Otero Island to near the Jabalí Island, Weiler [70] correlated the Pleistocene and Holocene marine deposits of the central area with three transgressive events of the Late Pleistocene and Holocene, and related them to environments of barriers and coastal lagoons of the transgression of the Sangamon interglacial (with a minimum age of 43 Ka), the interstadial transgression of the middle Wisconsin (38.5 to 25 Ka), and the postglacial transgression of the MIS 1 (middle Holocene, between 5 and 5.2 Ka). More recently, Schnack et al. [71] related the oldest deposits of the area described by Weiler [43] with the Interglacial MIS 5e, considering the radiocarbon datings as minimum ages.
In region C, from the Jabalí Island up to Villa 7 de Marzo, Fucks et al. [68] reinterpreted the stratigraphic sequences, assigning a minimum of four transgressive cycles. Beach ridges, as well as beach strand plains and tidal plains, with maximum altitudes of 6 m a.s.l. and very clear morphologies are present from the coast to the present day continent, particularly in Isla Jabalí. Above them, at altitudes of 8 to 10 m a.s.l. that increase gradually to over 30 m a.s.l., clear ridges could be probably related to MIS 5e. These could have been originated in two ≥ 9 transgressive events.
In region D, north of San Matías Gulf from near the El Cóndor beach up to Las Grutas beach, there are records of the interglacials MIS 7, MIS 5e and MIS 1 plus a fourth one, 60 m height, that probably corresponds to an interglacial ≥ MIS 9. According to Fucks et al. [72] the deposits of interglacials MIS 7 and MIS 5e correspond to Baliza San Matias and San Antonio formations, respectively, and those of Holocene age have no designation.
The main geomorphological features are littoral ridges formed by high energy conditions, although, deposits corresponding to intertidal environments, coastal lagoons, spit sand cliffs forms have been described mainly for the Holocene transgressive event as well (e.g.,[5, 68, 72, 73, 74, 75]).
All these deposits contain marine mollusks, particularly gastropods and bivalves (Figure 2) (Table 1) [5, 35, 36, 37, 65, 82].
(A) Profile of Holocene deposit with
Province | Área | Coordinates (Lat-long) | Sites | Ages (14C and ESR) | Altitude (m.a.m.s.l) | Cites |
---|---|---|---|---|---|---|
South of Buenos Aires | Delta del río Colorado | 39°20′S;62°04′W–39°55′S;62°08′W | P. Verde (39°21′S;62°5.9′W) | 2170 ± 86 ka | 5–2.5 | [76] |
Pta Laberinto – rio Colorado Viejo (39°30′S–39°50′S) | 6.63 ± 0.12 ka–0.409 ± 0.10 ka | 10–7.5 7.5 and 2 | [74] | |||
Sur del río Colorado viejo (39°53′S; 62°10′W) | 9.46 ± 0.12 ka–0.407 ± 0.10 ka | 5–2.5 | [74] | |||
Bahía Anegada | 39°55′S;62°08′W–40°28′S;62°11′W | Pleistocene deposits (40°03′S–40°26′S) | 43 ka, 38.55 ka, 25 ka | 40–25 | [70, 77] | |
43 ka, 38.8 ka, 31 ka | 10–7 | [75] | ||||
Canal Villalonga (40°1’S; 62°19’W) | 5.98 ± 0.10 ka–3.69 ± 0.10 ka | 4–2.5 | ||||
Los Pocitos (42°25′S; 62°25′W) | 4.4 ± 0.08 and 4.5 ± 0.09 ka | 3 | [72, 74, 78] | |||
Isla Jabalí – Villa 7 de marzo | 40°36′S;62°11′W–41°1′S;62°45′W | Oeste de isla Jabalí (40°40′S;62°30′W) | 30.78 ± 1.65 ka–28.4 ± 0.80 ka | 3–9.5 | [75, 79] | |
Isla Jabalí (40°34′S;62°13′W) | 5. 37 ± 0.11 ka-2.17 ± 0.11 | 4–5 | [37] | |||
Faro Segunda Barranca (40°46′S;62°16′W) | 102–108 ka 94.5, 79 and 72.7 ka 28 a 40 ka | 8–10 | [80, 81] | |||
Northern of Rio Negro | Norte del golfo San Matías | 40°51′S;65°7′W–41°02′S; 62°49′W | Caleta Falsa correlation with localities: south of Piedras Coloradas | ≥230 and ≥169 ka | 8–12 | [80, 81] |
Baliza San Matias (40°42′S; 64°51′W) | 97.3–83 ka | 8 | [73] | |||
La Rinconada (40°41′S;65°9′W) | 107–91 ka | 10 | ||||
Las Grutas (40°48′S;65°4′W) | 70.3–66.8 ka | 10 | ||||
La Conchilla (40°49’S/64°52’O) | 2.43 ± 0.60 ka | 1.50 | [5] |
Absolute dating available from the study área.
A total of 84 localities were studied in two areas, 31 Pleistocene, 29 Holocene, and 24 modern ones. In these localities 7385 valves and shells of mollusks were collected. Each coastal deposit to be studied is identified on topographic maps. At each level of the site, a volumetric sample of 1 dm3. In contrast, at modern beach sites the sample is taken in a quadrant 1 m x 1 m along transects perpendicular to the coast line.
Each fraction of biogenic content recovered from the sieves (2.80, 1.40 and 0.080 mm) was identified, measured with digital caliper, and labeled. Species were identified through catalogs and specific literature.
Valves and shells found in the marine deposits are considered as assemblages representing the accumulation of non-contemporary individuals in a single set, and occurs because the time of generation of these individuals is faster than the burial rates. In this context, it has to be taken into account the changes produced during the transition of the animal remains from the biosphere to the lithospere, which is studied through a discipline called taphonomy (etymologically derived from the Greek taphos, tomb, and nom, law). Taphonomy was defined by Efremov [83] as the science that studies the laws of burial, and accepted that taphonomic processes lead to the loss of information and are the cause of gaps in the fossil record. Currently this concept has been reversed since numerous studies (e.g., [84, 85, 86, 87]) support the idea that the faunal associations of both current and fossil valves provide relevant information on living communities, or paleocommunities, being able in both cases to reconstruct the environments or paleoenvironments from the analysis of the faunal associations and thus interpret environmental and climatic changes.
The studied mollusks form transported faunal associations, which, according to different authors, preserve compositional fidelity concerning taxonomy and relative abundance of the communities that inhabited each environment within the considered period, and represent the accumulations of non-contemporary individuals as a whole.
The four areas identified in northern Patagonian according to their geomorphology (A-D), in which 84 sites were studied, yielded 78 species (42 bivalves and 36 gastropods). Eleven of them are micromollusks:
Bivalves | Salinity | Life habit | Depth (m) | Substrate | Trophic type | Distribution area |
---|---|---|---|---|---|---|
E | I | 0–200 | S | D | 23°S–53.5°S | |
E | I | 5–1850 | S | D | 22.93°S–55.5°S | |
E | I | 20–75 | S | D | 22.93°S–39°S* | |
E | I | 10–75 | S | Sf | 10°S–42°S | |
P–E | Ep | 0–50 | H | Sf | 68°N–55.5°S | |
P–E | Ep | 0–25 | H | Sf | 34°S–42°S | |
E | Ep | 0–30 | H | Sf | 34°S–55.5°S | |
E | Ep | 10–120 | M | Sf | 21°S–42.58°S | |
P–E | Ce | 0–3 | H | Sf | 35°N–35°S* | |
E | Ce | 0–120 | H | Sf | 35.3°N–34°S* | |
P–E | Ce | 0–80 | H | C | 37°N–42°S | |
P–E | Ce | 0–70 | H | C | 22°S–42°S | |
P–E | Ce | 0–50 | H | C | 21.4°S–35°S | |
E | Ce | 0–40 | H | Sf | Cosmopolitan | |
E | I | 36–102 | S | Sf | 21°S–42.58°S | |
E | I | 25–77 | S | Sf | 21°S–42°S | |
E | I | 17–70 | S | Sf | 23°S–39°S* | |
E | I | 0–11 | S | Sf | 35°N–42°S | |
P–E | I | 0–25 | S | Sf | 34°S–42°S | |
P–E | I | 0–25 | S | Sf | 23°S–42°S | |
P–E | I | 0–11 | S | Sf | 39°N–41°S | |
E | I | 0–20 | S | Sf | 23°S–41°S | |
E | I | 10–18 | S | Sf | 23°S–39°S* | |
E | I | 18–70 | S | D | 29°S–39°S* | |
E | I | 13–55 | S | D | 23°S–43°S | |
E | I | 0–50 | S | D | 35°N–23°S* | |
P | I | 0–10 | S | Sf | 42°N–54°S | |
E | I | 0–55 | S | Sf | 21°S–42°S | |
P–E | I | 0.3–5 | S | Sf | 18°N–39°S* | |
E | I | 10–100 | S | Sf | 22°S–38.7°S* | |
E | I | 0–20 | S | Sf | 19°S–43°S | |
E | I | 50–70 | S | Sf | 34°S–55.5°S | |
E | I | 5–50 | S | Sf | 34°S–54°S | |
E | I | 25–75 | S | Sf | 23°S–48°S | |
E | I | 15–90 | S | Sf | 23°S–43°S | |
E | I | 11–67 | S | Sf | 19°S–43°S | |
E | I | 10–27 | S | Sf | 6°S–42°S | |
E | I | 15–150 | R | Sf | 34°S–43°S | |
E | I | 50–86 | S | Sf | 38.3°S–41°S | |
E | I | ? | S | Sf | 35°S–40.5°S | |
E | I | 50–86 | S | Sf | 22°S–42.58°S |
Ecological requeriments and distribution of bivalves.
Taxa found in the studied area.
The references of species are found on MolluscanBase eds(2021).
Ep, epifaunal; I, infaunal; Ce, cemented; H, hard; S, soft; C, carnivorous; D, detritivorous; He, herbivore; Sf, suspension feeder; O, oligohaline (3–8‰); M, mesohaline (8–18‰); P, polyhaline (18–30‰); E, euhaline (>30–35‰).
Gastropods | Salinity | Life habit | Depth (m) | Substrate | Trophic type | Distribution area |
---|---|---|---|---|---|---|
E | Ep | 0–200 | H | He | 38.5°S–55.5°S | |
E | Ep | 0–15 | H | He | 11°N–45°S | |
E | Ep | 0 | H | He | 48°S–55°S | |
E | Ep | 0–55 | H | He | 23°S– | |
E | Ep | 0–60 | S | He | 40.37°S–41.67°S | |
E | Ep | 13–86 | S | He | 30°S–44.21°S | |
E | Ep | 0–57 | H | He | 23°S–54°S | |
E | Ep | 0–9 | H | He | 38°S–55°S | |
E | Ep | 0–46 | H | Sf | 25°S–45.8°S | |
E | Ep | 30–50 | H | Sf | 38°S–41.03°S | |
E | Ep | 0–66 | H | Sf | 35°S–55.8°S | |
E | I | 0–113 | S | C | 22.4°S–42.58°S | |
O, P, M | Ep | 0–60 | M | He | 24°S–41°S | |
E | Ep | 0–101 | M | He | 23.37°S–44.27°S | |
E | Ep | 30 | M | He | 23°S–41°S | |
E | Ep | 0–50 | H | C | 32°S–40°S | |
E | Ep | 0–58 | H | C | 36.42°S–54.98°S | |
E | Ep | 28–28 | H | C | 32°S–41°S | |
E | Ep | 10–90 | S | C | 23°S–42°S | |
E | Ep | 0–250 | S | C | 23°S–52°S | |
E | Ep | 40–75 | S | C | 20° S–52°S | |
E | Ep | 10–200 | M | C | 35°S–55.2°S | |
E | Ep | 10–80 | S | C | 22.93°S–42°S | |
E | Ep | 15–57 | S | C | 23.69°S–43°S | |
E | Ep | 5–50 | S | C | 19°S–42°S | |
E | Ep | 0–22 | S | C | 23°S–42.5°S | |
E | Ep | 0–30 | S | C | 23°S–40.6°S | |
E | Ep | 0–50 | S | C | 35°N–42°S | |
E | Ep | 5–66 | S | C | 23°S–42.58°S | |
E | Ep | 0–6 | S | C | 35°S–46°S | |
E | Ep | 15–45 | S | C | 24°S–42°S | |
E | Ep | 10–65 | S | C | 30°S–54°S | |
E | Ec | 0–20 | S | C | 35°N–54°S | |
E | Ec | 18–57 | S | C | 35°S–41°S | |
E | Ec | 30–65 | S | C | 39°S–41°S | |
E | Ec | 30–65 | S | C | 40°S–46°S | |
E | Ep | 0 | H | He | 32°S–55.22°S |
Ecological requeriments and distribution of gastropods.
The references of species are found on MolluscanBase eds(2021).
Ep, epifaunal; I, infaunal; Ce, cemented; Ec, ectoparasite; H, hard; S, soft; M, mixed; C, carnivorous; D, detritivorous; He, herbivore; Sf, suspension feeder; O, oligohaline (3–8‰); M, mesohaline (8–18‰); P, polyhaline (18–30‰); E, euhaline (>30–35‰).
Seventy species were identified in areas A-C (37 bivalves and 33 gastropods), and 45 species in region D (19 bivalves and 24 gastropods), with a similarity of 51.3% in bivalve species and 48.5% in gastropods.
In areas A-C, all the studied sites assigned to the interglacial ≥ MIS 9, are paleobeaches and littoral ridges; i.e., high energy environments in which the marine fauna is euryhaline (salinity > 30–35 gr/l) and of sandy substrate. Warm water species prevailed in bivalve associations (50–67%) compared to the other interglacials recorded in the area. However, no bivalve or gastropod of warm lineage that constitutes itself a paleoindicator was found.
Interglacial MIS 5e is represented in all the studied sites mostly by littoral ridges in which most associations are euryhaline, of sandy substrate and subordinate rocky substrate. Most species are epifaunal except in region A, prevailing filter feeders and carnivores. The proportion of warm water species in this interglacial is lower than in the previous one (44–50%) being outstanding the record of the warm lineage bivalve
Interglacial MIS 1 was recorded in the whole study area, with two types of deposits in areas A-C: littoral ridges (high energy environments) and tidal plains (low energy environments). In the first ones, the malacofaunal associations are mostly euryhaline, of sandy substrates. In the second ones instead, the associations vary in salinity from oligohaline to mesohaline-polyhaline (salinity between 3 and 30 gr/l), of fine sand substrate, mostly epifaunal and filter feeders prevailing infaunal and carnivores in region A. This latter would be related to the modern geomorphological features of low energy environments (wide tidal plains, tidal channels and non-functional fluvial courses), that resulted in the formation of islands which can be seen in all the southern coast of the Buenos Aires Province. This interglacial MIS 1 is recognized in area D in littoral ridges, being the malacofaunal associations mostly euryhaline, of sandy substrate with rocky subordinate. In the associations of MIS 1 there is 45 to 50% of warm water species in areas A-C, unlike areas D in which this proportion is only 18% of the total bivalves.
In modern beaches of the south of BAP, but not in the northern sector of Bahía Anegada there are sandy beaches together with mud-sandy ones, and malacofaunal associations correspond to marine parameters of high energy, euryhaline of sandy substrate with scattered rocky substrate, mainly in area C. Instead, the modern beaches of area D are larger often exceeding hundreds of meters wide. There are two types of beaches regarding the granulometry: a low intertidal sector of fine to medium sand with high distal sectors of gravels, organogenic in composition, and a low intertidal sector and high distal one of fine-medium sand. Both are associated with high energy environments where the malacological associations are mostly euryhaline, of sandy substrate, with less proportion of fauna of scattered rocky substrate. There is one exception, the modern beach of Villa 7 de Marzo which has a particular feature, fine sand substrate with abundance of two bivalves
In area D, all the analyzed sites of MIS 7 correspond to paleobeaches. They are currently represented by coastal platforms, of high energy, with mostly euryhaline malacofaunal associations of sandy substrate and subordinated rocky substrate. Respect to the indicators of sea water temperature, these associations are formed only by 20% of warm water bivalves, although it is recorded the gastropod
In MIS 5e there is a slightly higher proportion of associations of warm waters (27%) with respect to the previous interglacial, being conspicuous the presence of
In MIS 1 the associations of warm water are in lesser proportion than those of MIS 5e (18%), being outstanding the record of
Paleoecological features of all regions (A–D) in interglacial MIS 5e.
Paleoecological features of all regions (A–D) in interglacial MIS 1.
Paleoecological features of all regions (A–D) in modern beaches.
Paleoecological features of region D in interglacial MIS 7.
These two interglacials recorded in area D were not recorded in the northeast of BAP. In areas A-C, a total of nine species of mollusks were recorded in the Interglacial ≥ MIS 9, and among them, there is 50–67% of warm water species of bivalves, being this the oldest record of marine mollusks for the BAP. In MIS 7 analyzed in area D, a total of 11 species was recorded with 20% of warm water bivalves. Most recorded species in both interglacials still inhabit the modern coasts of Argentina, except for the gastropod
Both interglacials (≥MIS 9 and MIS 7) revealed the presence of warm water mollusks which are not recorded in the marine deposits of the northeast of BAP where these deposits have not been preserved [124]. The record of these interglacials in the BAP is a novelty in the analysis of gastropods and bivalves. Whereas Aguirre et al. [27, 28] reported that in the coasts of southern Patagonia, in areas such as Bahía Vera-Camarones (44.2° to 45°S) and Bahía Bustamente-Caleta Olivia (44.9°–45.3°S, Chubut Province, Argentina), the environmental conditions (substrate, depth, and energy conditions) during the late Pleistocene (MIS 7 and MIS 5e) suggest SST similar to those of the modern littoral and even slightly higher than present, recording faunas of warm to temperate waters.
In the marine deposits of this interglacial in area D, 44 molluskan species (25 bivalves and 19 gastropods) were recorded. These deposits are represented by littoral ridges and tidal plains along the south of the BAP coast, and by littoral ridges along area D, with scarce content of calcium carbonate, favoring the record of mollusks. In area C the associations of MIS 5e and MIS 1 have respectively 34 and 33 species. This similarity was also found in area D, in which 22 species were recognized for MIS 5e and 23 for MIS 1. Unlike area D, the mollusks of MIS 5e of the northeast of the BAP are characterized by less abundance and diversity of species related to those of the Holocene MIS 1 [32]. This could be due to a less representation of the Interglacial MIS 5e, and because most valves and shells of Pleistocene deposits are dissolved and/or crystallized, preventing the species identification.
Between 50 and 44% of warm water species of bivalves recorded in the Interglacial MIS 5e of area D, are represented in areas A-C, whereas this relationship is only 27% of the species from area D. Warm water mollusks were recognized in the study area, among the most prominent species of this interglacial, in areas A-C, is the bivalve
The warm species of Pleistocene. (A)
Another warm lineage species found in area D, is the bivalve
A total of 58 species (31 bivalves and 27 gastropods) was recorded in the marine malacofauna of the Interglacial MIS 1 of northern Patagonia (areas A-D), which differs from the northeast of BAP where Aguirre [89] reported a total of 62 species (25 bivalves and 37 gastropods). Concerning the molluscan composition, in the northeast of BAP, gastropods are more abundant than bivalves both in number of species and of individuals. As a comparison, among the regions studied, area A recorded 51 species (29 bivalves and 22 gastropods), and area B 49 species (25 bivalves and 24 gastropods), being in both regions, bivalves more numerous than gastropods. Whereas in area C, 34 species (17 bivalves and 17 gastropods) were recorded, unlike area D where 42 species (20 bivalves and 22 gastropods) were recorded, being in this latter the number of gastropods slightly higher than bivalves.
The marine deposits of MIS 1 in areas A-C are formed by tidal plains and littoral ridges. Tidal plains yielded mainly
The marine deposits and their malacofauna in the northeast and south (areas A-C) of the BAP are similar in the two types of deposits of the Interglacial MIS 1. The tidal plains are represented in regions A-C and are related to the development of the Colorado River and Bahía Anegada. The most common species are
Warm water vs. cold water during the quaternary in all regions (A–D).
In the last 400.000 years there were variations in the molluskan paleocommunities of north Patagonia (southern BAP and north of Río Negro Province). The marine malacofauna of this area is composed by two associations, the first one is formed by Holocene sites with abundance of
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