Download or read book Carbonate Platform Demise and Recovery at the Toarcian Oceanic Anoxic Event written by Nicholas Patrick Ettinger and published by . This book was released on 2017 with total page 166 pages. Available in PDF, EPUB and Kindle. Book excerpt: The sedimentological, stratigraphic, and geochemical signature of the Toarcian Oceanic Anoxic Event (OAE) on the Bahamian-style, Adriatic Carbonate Platform of Southern Europe is examined here. New stratigraphic sections correlated to previously published data show that a healthy and diverse metazoan carbonate factory characterized the flat-topped platform prior to the onset of the OAE. Carbon isotopes of marine organic matter and bulk carbonate, as well as trace element data (V, Ni, Mo, Mn, Hg) were used to identify the stratigraphic location of the OAE on the outer platform. A negative organic carbon isotope excursion of -2.2‰ coincident with enrichments in Mo and Fe was used to correlate to time equivalent strata in both the inner platform and adjacent basin. The onset of the OAE heralded a carbonate factory collapse on the outer platform that was driven by deoxygenation, eutrophication, and possibly ocean acidification. At the same time, a shallow intrashelf basin developed, while the adjacent deep-water basin accumulated black shales. The cessation of carbonate production throughout the OAE yielded a significant drowning unconformity on the outer platform as sea-level continued to rise, while restricted, organic-rich mudstones accumulated on the inner platform under a euxinic regime. Recovery of carbonate production is characterized mainly by calcitic fauna and ooids. By the Middle Jurassic, ooids generated on the outer margin spilled into the adjacent basin forming a thick deep-water oolitic fan, and they prograded to the inner platform, reestablishing a flat-topped carbonate platform.

Download or read book Carbonate Factory Response and Recovery After Ocean Anoxic Event 1a Pearsall Formation Central Texas written by Esben Skjold Pedersen and published by . This book was released on 2020 with total page 232 pages. Available in PDF, EPUB and Kindle. Book excerpt: Ocean Anoxic Events (OAEs) are major carbon cycle perturbations that occurred several times in the Mesozoic. OAEs are commonly found to have been caused by a combination of climatic warming and increased surface weathering delivering surface nutrients to the oceans. This feedback loop leads to the expansion of the oxygen minimum zone of the waterbody and increased influx of terrigenous material. The resultant dysoxic to euxinic conditions are thought to have played a prominent role in the suppression of the benthic carbonate factory and deposition of organic-rich mudstones. The establishment of these oceanographic conditions are postulated to have imparted a lasting effect on the deposition of stressed-carbonate facies during the recovery phase of OAEs. Major questions regarding OAE events remain, including the degree of variability in the impact that OAEs have on carbonate factories and the drivers for this variability, on both global and regional scales. This study builds upon previous work and further investigates the regional Early Cretaceous (Aptian) OAE-1a signal that is recorded in the Pearsall Formation in Central Texas, with a particular focus on the record of carbonate factory recovery observed in transects from the San Marcos Arch to the Pearsall Arch. Shoreline-proximal data include outcrops and 8 cores with 1530 ft of coverage. Distal cores include 7 subsurface exploration wells (total 1745 ft core) from the San Marcos Arch to the Pearsall Arch, a strike-parallel distance of 210 km. Physical characterization of stratigraphic data was paired with the multivariate statistical analysis of 10 pXRF datasets, involving Principal Component Analysis (PCA) segmentation, which led to the establishment of five end member chemofacies. These chemofacies allow for high-resolution identification of mineralogic variability across OAE-1a, including the documentation of pulses of terrigenous input as well as cycles of dysoxic to euxinic oceanographic conditions at a sub-lithofacies scale. When paired with the development and application of a deep learning neural network trained by a type-pXRF training dataset, this study outlines a new methodology that allows for the direct comparison of pXRF data across core control through a unified chemofacies schema. The oceanographic conditions identified with this workflow are then used to delineate oceanographic variability and pulses of terrigenous enrichment in association with the recovery from OAE-1a. The characterization of these geochemical processes is particularly relevant in the mudrock component of depositional systems, where biologic productivity, bottom-water redox conditions, and any subsequent diagenesis are critical determinants for the ultimate preservation of TOC in organic-rich shales. TOC rich shale intervals then create potential for an economical petroleum source rock and successive charge of either conventional or unconventional reservoirs. The incidence of OAE-1a is found to be a fundamental driver of facies evolution and faunal composition in the three composite sequences studied: the James (Aptian) composite sequence, the Bexar (Aptian-Albian) composite sequence, and the Glen Rose composite sequence (Albian) (cf. Phelps et al., 2014). OAE-1 is coincident with the drowning of the antecedent Sligo reef margin and deposition of the Pine Island Shale. This drowning event was a result of environmental stressors posed by the OAE and the resultant suppression of sedimentation rates on the platform as the carbonate factory was substantially weakened. Partial recovery of the carbonate factory from OAE-1a is expressed in the deposition of the Cow Creek Member before punctuation of deposition due to the subaerial exposure event at the top-James composite sequence boundary. A second phase of recovery is documented in the Bexar and Glen Rose composite sequences, including reef systems in the platform interior that are coeval with transgression and deposition of the Hensel Formation, as well as the progradation of Lower Glen Rose carbonates and the aggradation of microbial-coral-rudist bioherms in highstand depositional sequences of the Glen Rose Formation. Recovery of the carbonate factory was fundamentally different between the San Marcos Arch and Pearsall Arch areas. Earliest recovery fauna in the Cow Creek Member is comprised of monospecific echinoid-mollusk packstones-grainstones in shoreline proximal settings and oyster-oncoid rudstones distally. Combined observations from pXRF data and the heightened prevalence of pyrite in oncoid cortices on the San Marcos Arch compared to the Pearsall area is interpreted to represent a higher degree of dysoxic and/or euxinic conditions on the San Marcos Arch. During later stages of recovery, the Cow Creek in the Pearsall Arch area is shown to have maintained healthier carbonate deposition in comparison to the San Marcos Arch, including the sustained deposition of reefal assemblages, such as the sequence of stromatoporoid boundstone present in the Tenneco Sirianni well. This combined core-outcrop framework demonstrates the superimposed regional variability inherent even in global carbon cycle perturbations such as OAE-1a, driven by the degree of shelf restriction, oceanographic circulation patterns, basin geometry, and the degree of terrigenous influx. The documented differences in oceanographic conditions and carbonate factory recovery on the regional scale of OAE-1a will aid in better understanding the multi-scaled geochemical and environmental evolution associated with these events, and ultimately pushes towards the development of predictive concepts for future studies

Download or read book Carbon Cycle and Ecosystem Response to the Jenkyns Event in the Early Toarcian Jurassic written by M. Reolid and published by Geological Society of London. This book was released on 2021-11-30 with total page 418 pages. Available in PDF, EPUB and Kindle. Book excerpt: The Toarcian Oceanic Anoxic Event, also known as the Jenkyns Event, was a hyperthermal episode which occurred during the early Toarcian (c. 183 Ma; Early Jurassic) and resulted in numerous collateral effects including global warming, enhanced weathering, sea-level change, carbonate crisis, marine anoxia–dysoxia, and a second-order mass extinction. This volume presents the last advances for understanding early Toarcian environmental changes through different disciplines: biostratigraphy, micropalaeontology, palaeontology, ichnology, palaeoecology, sedimentology, integrated stratigraphy, inorganic, organic and isotopic geochemistry, and cyclostratigraphy. The study of this abrupt climate change is critical for predicting future global changes, and for understanding the complex biogeochemical interactions through time between geosphere, atmosphere, hydrosphere and biosphere.

Download or read book The Toarcian Oceanic Anoxic Event in the South Iberian Palaeomargin written by Matías Reolid and published by Springer. This book was released on 2017-09-05 with total page 127 pages. Available in PDF, EPUB and Kindle. Book excerpt: This book presents the first overview of the Toarcian Oceanic Anoxic Event in the southern Iberian paleomargin, in the western Tethys. The study of catastrophic events that affected the ecosystems in the past is of great interest, because it offers the possibility of establishing models that can be applied to current and future environmental changes. The book provides comprehensive information on the changes in marine ecosystems in connection with a global massive extinction, the Early Toarcian, and with the deposition of black shales, global warming and a disruption of the carbon cycle. In addition, the book describes the incidence of this event in this part of the Tethys close to the connection with the Protoatlantic, the Hispanic Corridor. Special attention is paid to sedimentological and ichnological aspects, fossil content (macroscopic and microscopic), and geochemistry. It also presents the facies changes related to fragmentation of the shelf and the evolution to hemipel agic troughs and swells in this paleomargin. Lastly, it characterizes this anoxic event in under-researched outcrops from southern Spain and compares the findings with those in well-known sections from northern and central Europe. This book offers a unique resource for all researchers interested in the Toarcian Oceanic Anoxic Event, but also in oceanic anoxic events that occurred during the Mesozoic in general, because of their similarity to recent climatic changes.

Download or read book 35th IAS Meeting of Sedimentology Book of Abstracts written by Ondřej Bábek and published by Palacký University Olomouc. This book was released on with total page 570 pages. Available in PDF, EPUB and Kindle. Book excerpt: The 35th International Meeting of Sedimentology supported by the International Association of Sedimentologists is an annual conference with global impact among the community of sedimentary geologists. Original scheduled at June 2020, the 35 the IAS Meeting of Sedimentology was postponed to June 21-25, 2021, and will be held virtually. The main convenor, Ondřej Bábek, is an employee of Palacký University Olomouc.

Download or read book The Llanbedr Mochras Farm Borehole written by A. W. Woodland and published by . This book was released on 1971-01-01 with total page 115 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Download or read book Carbon Isotope Stratigraphy written by Michael Montenari and published by Academic Press. This book was released on 2020-10-30 with total page 780 pages. Available in PDF, EPUB and Kindle. Book excerpt: Carbon Isotope Stratigraphy, Volume Five in the Advances in Sequence Stratigraphy series, covers research in stratigraphic disciplines, including the most recent developments in the geosciences. This fully commissioned review publication aims to foster and convey progress in stratigraphy with its inclusion of a variety of topics, including Carbon isotope stratigraphy - principles and applications, Interpreting Phanerozoic d13C patterns as periodic glacio-eustatic sequences, Stable carbon isotopes in archaeological plant remains, Review of the Upper Ediacaran-Lower Cambrian Detrital Series in Central and North Iberia: NE Africa as possible Source Area, Calibrating d13C and d18O chemostratigraphic correlations across Cambrian strata of SW, and much more. Contains contributions from leading authorities in the field Informs and updates on all the latest developments in the field Aims to foster and convey progress in stratigraphy, including geochronology, magnetostratigraphy, lithostratigraphy, event-stratigraphy, and more

Download or read book Mesozoic and Cenozoic Sequence Stratigraphy of European Basins written by Pierre Charles de Graciansky and published by . This book was released on 1998 with total page 818 pages. Available in PDF, EPUB and Kindle. Book excerpt: This project was designed to build a documented chronostratigraphic and outcrop record of depositional sequences calibrated across European basins. Data on standard stages, magnetostratigraphy, and geochronology integrated with high resolution biostratigraphy calibrate the stratigraphic position of depositional sequence boundaries. Higher order eustatic sequences show a significant increase in the number identified. A good portion of the European Mesozoic and Cenozoic succession is set in the sequence stratigraphic context with a stratigraphic record of its bonding surfaces.

Download or read book Chemostratigraphy Across Major Chronological Boundaries written by Alcides N. Sial and published by John Wiley & Sons. This book was released on 2018-12-18 with total page 318 pages. Available in PDF, EPUB and Kindle. Book excerpt: Winner of the 2020 PROSE Award for Earth Science! Exploring environmental changes through Earth’s geological history using chemostratigraphy Chemostratigraphy is the study of the chemical characteristics of different rock layers. Decoding this geochemical record across chronostratigraphic boundaries can provide insights into geological history, past climates, and sedimentary processes. Chemostratigraphy Across Major Chronological Boundaries presents state-of-the-art applications of chemostratigraphic methods and demonstrates how chemical signatures can decipher past environmental conditions. Volume highlights include: Presents a global perspective on chronostratigraphic boundaries Describes how different proxies can reveal distinct elemental and isotopic events in the geologic past Examines the Archaean-Paleoproterozoic, Proterozoic-Paleozoic, Paleozoic-Mesozoic, and Mesozoic-Paleogene boundaries Explores cause-and-effect through major, trace, PGE, and REE elemental, stable, and radiogenic isotopes Offers solutions to persistent chemostratigraphic problems on a micro-global scale Geared toward academic and researchgeoscientists, particularly in the fields of sedimentary petrology, stratigraphy, isotope geology, geochemistry, petroleum geology, atmospheric science, oceanography, climate change and environmental science, Chemostratigraphy Across Major Chronological Boundaries offers invaluable insights into environmental evolution and climatic change. Read the Editors' Vox: https://eos.org/editors-vox/unravelling-the-past-using-elements-and-isotopes

Download or read book Volcanism Impacts and Mass Extinctions Causes and Effects written by Gerta Keller and published by Geological Society of America. This book was released on 2014-09-16 with total page 468 pages. Available in PDF, EPUB and Kindle. Book excerpt: "Comprises articles stemming from the March 2013 international conference at London's Natural History Museum. Researchers across geological, geophysical, and biological disciplines present key results from research concerning the causes of mass extinction events"--

Download or read book 250 Million Years of Earth History in Central Italy written by Christian Koeberl and published by Geological Society of America. This book was released on 2019-11-04 with total page 532 pages. Available in PDF, EPUB and Kindle. Book excerpt: "The Umbria-Marche Apennines are entirely made of marine sedimentary rocks, representing a continuous record of the geotectonic evolution of an epeiric sea from the Early Triassic to the Pleistocene. The book includes reviews and original research works accomplished with the support of the Geological Observatory of Coldigioco"--

Download or read book Petroleum Abstracts Literature and Patents written by and published by . This book was released on 1990 with total page 1416 pages. Available in PDF, EPUB and Kindle. Book excerpt:

Download or read book Biostratigraphic and Geological Significance of Planktonic Foraminifera written by Marcelle K. BouDagher-Fadel and published by UCL Press. This book was released on 2015-10-02 with total page 320 pages. Available in PDF, EPUB and Kindle. Book excerpt: The role of fossil planktonic foraminifera as markers for biostratigraphical zonation and correlation underpins most drilling of marine sedimentary sequences and is key to hydrocarbon exploration. The first - and only - book to synthesise the whole biostratigraphic and geological usefulness of planktonic foraminifera, Biostratigraphic and Geological Significance of Planktonic Foraminifera unifies existing biostratigraphic schemes and provides an improved correlation reflecting regional biogeographies.Renowned micropaleontologist Marcelle K. Boudagher-Fadel presents a comprehensive analysis of existing data on fossil planktonic foraminifera genera and their phylogenetic evolution in time and space. This important text, now in its Second Edition, is in considerable demand and is now being republished by UCL Press.

Download or read book Calcareous Nannofossil Biostratigraphy written by Paul R. Bown and published by Springer. This book was released on 2012-12-16 with total page 315 pages. Available in PDF, EPUB and Kindle. Book excerpt: Calcareous nannofossils are an exceptionally important microfossil group, with their living counterparts, coccolithopores, representing one of the major components of phytoplankton in present day oceans. Their abundant fossil record and world-wide distribution has led to their rapid acceptance as one of the most important index-fossil groups in stratigraphical research. The first two chapters of this book provide general information concerning calcareous nannofossils, including reviews of their biology and palaeobiology, and preparation and observation techniques. Chapters 3-9 are ordered stratigraphically, and present state-of-the-art summaries of calcareous nannofossil biostratigraphy for each time period, with comprehensive illustrations of all taxa within a standardised classification based on the latest research into structure and biomineralization. The practical application of these biostratigraphic schemes is discussed, including comments on zones biogeography, taxonomy and evolution. This information is internationally relevant, and global correlation is discussed. Calcareous Nannofossil Biostratigraphy is the most comprehensive atlas of this fossil group ever produced, containing 65 full page plates with over 2,000 individual photographs, together with comments concerning stratigraphic distribution and identification. Chapters on the Mesozoic contain electron microscope illustrations as well as light micrographs. The inclusion of much recent, previously unpublished, research provides a new level of biostratigraphic resolution for a number of time periods, making the book both a valuable synthesis and a significant step forward in biogeographical research. Calcareous Nannofossil Biostratigraphy is a comprehensive practical handbook for palaeontologists and organizations who use calcareous nannofossils in biostratigraphy, and provides a valuable practical reference work for earth scientists engaged in stratigraphic research, and those interested in palaeontology, palaeoceanography, stratigraphy and geochronology.

Download or read book Cretaceous Resources Events and Rhythms written by Robert N. Ginsburg and published by Springer Science & Business Media. This book was released on 1990-02-28 with total page 390 pages. Available in PDF, EPUB and Kindle. Book excerpt: ' this volume represents perhaps the best available report on state-of-the-science cretaceous research. Some may query the wisdom of grand schemes such as the GSGP, believing that science is best left to the imaginative individual. This useful volume offers a persuasive counter-argument. That it speaks with many voices (if not languages) is to be expected and indeed adds to its strength.' Cretaceous Research 11, 1990

Download or read book Petroleum Formation and Occurrence written by B.P. Tissot and published by Springer Science & Business Media. This book was released on 2013-11-11 with total page 715 pages. Available in PDF, EPUB and Kindle. Book excerpt: Current and authoritative with many advanced concepts for petroleum geologists, geochemists, geophysicists, or engineers engaged in the search for or production of crude oil and natural gas, or interested in their habitats and the factors that control them, this book is an excellent reference. It is recommended without reservation. AAPG Bulletin.

Download or read book Carbonate Sedimentology and Sequence Stratigraphy written by Wolfgang Schlager and published by SEPM Soc for Sed Geology. This book was released on 2005 with total page 210 pages. Available in PDF, EPUB and Kindle. Book excerpt: Sedimentology and stratigraphy are neighbors yet distinctly separate entities within the earth sciences. Sedimentology searches for the common traits of sedimentary rocks regardless of age as it reconstructs environments and processes of deposition and erosion from the sediment record. Stratigraphy, by contrast, concentrates on changes with time, on measuring time and correlating coeval events. Sequence stratigraphy straddles the boundary between the two fields. This book, dedicated to carbonate rocks, approaches sequence stratigraphy from its sedimentologic background. This book attempts to communicate by combining different specialities and different lines of reasoning, and by searching for principles underlying the bewildering diversity of carbonate rocks. It provides enough general background, in introductory chapters and appendices, to be easily digestible for sedimentologists and stratigraphers as well as earth scientists at large.