Constraining Morphologic Change Across the Great Ordovician Biodiversification Event PDF Download
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Author: Sarah A. Hennessey
Publisher:
ISBN:
Category : Biodiversity
Languages : en
Pages : 0
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Author: Sarah A. Hennessey
Publisher:
ISBN:
Category : Biodiversity
Languages : en
Pages : 0
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Author: Barry D. Webby
Publisher: Columbia University Press
ISBN: 0231501633
Category : Science
Languages : en
Pages : 497
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Book Description
Two of the greatest evolutionary events in the history of life on Earth occurred during Early Paleozoic time. The first was the Cambrian explosion of skeletonized marine animals about 540 million years ago. The second was the "Great Ordovician Biodiversification Event," which is the focus of this book. During the 46-million-year Ordovician Period (489–443 m.y.), a bewildering array of adaptive radiations of "Paleozoic- and Modern-type" biotas appeared in marine habitats, the first animals (arthropods) walked on land, and the first non-vascular bryophyte-like plants (based on their cryptospore record) colonized terrestrial areas with damp environments. This book represents a compilation by a large team of Ordovician specialists from around the world, who have enthusiastically cooperated to produce this first globally orientated, internationally sponsored IGCP (International Geological Correlation Program) project on Ordovician biotas. The major part is an assembly of genus- and species-level diversity data for the many Ordovician fossil groups. The book also presents an evaluation of how each group diversified through Ordovician time, with assessments of patterns of change and rates of origination and extinction. As such, it will become the standard work and data source for biotic studies on the Ordovician Period.
Author: A.W. Hunter
Publisher: Geological Society of London
ISBN: 178620407X
Category : Science
Languages : en
Pages : 615
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Book Description
Special Publication 485 About 40 million years after the Cambrian Explosion, the Great Ordovician Biodiversification Event (GOBE) represents a second and dramatic burst in marine biodiversity, with major changes in the structure of ecosystems and the progressive replacement of the distinctive Cambrian Evolutionary Fauna by the Paleozoic Evolutionary Fauna. However, the GOBE is not a single, worldwide, short-term event, but rather the complex sum of successive diversifications occurring in distinct taxonomic groups, trophic guilds and regions. This book focuses on the Late Ordovician Tafilalt Biota, Anti-Atlas Morocco, which provides a snapshot of the GOBE in high-latitude regions of the Southern Hemisphere. A series of contributions explore different aspects of the Tafilalt Biota, including its geological setting, the international fossil trade in this area and a series of detailed systematic contributions describing many new taxa of marine invertebrates. This volume represents a significant contribution to the understanding of the Tafilalt Biota and its significance to the GOBE.
Author: Nevin Paul Kozik
Publisher:
ISBN:
Category : Biogeochemistry
Languages : en
Pages : 0
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After decades of research biogeochemists have identified several intervals of variable marine oxygenation throughout Earth's history. These fluctuations in oxygenation have been proposed to directly correlate to changes in ancient biodiversity, and potentially be primary drivers for these observed changes in faunal richness. The Ordovician was a dynamic time in terms of marine biodiversity, as it hosts the largest increase in biodiversity events in the Phanerozoic, which occurs in the Early to Middle Ordovician commonly referred to as the Great Ordovician Biodiversification Event (GOBE). This major marine radiation is subsequently terminated by the second largest mass extinction in Earth's history that occurs in the Late Ordovician, commonly referred to as the Late Ordovician Mass Extinction (LOME). While the primary causal mechanisms for both events remain under debate, an emerging field of study has associated an increase in marine oxygenation with the GOBE, while a decrease in marine oxygenation has been proposed for the LOME. Using a suite of paleoredox proxies, we present new geochemical datasets surrounding key intervals of the GOBE and LOME to elucidate the paleoredox landscape surrounding these events and link the known changes in biodiversity with fluctuations in marine oxygenation. These paleoredox proxies include local proxies that have previously been shown to constrain basinal changes in redox, which allows the use of global proxies to identify global changes in redox which might influence global biodiversity. These local redox proxies include manganese concentrations, iodine-to-calcium ratios, iron speciation, and pyrite sulfur isotopic compositions, while the global redox proxies include thallium isotopic compositions, vanadium, uranium and molybdenum concentrations, and carbonate-associated sulfate isotopic compositions. The major increase in faunal richness associated with the GOBE is thought to begin after the Cambrian-Ordovician boundary, however paleoredox conditions surrounding this interval of time is largely under constrained. Currently a singular paleoredox dataset has been published to constrain paleoredox conditions across this boundary, however this dataset is limited in stratigraphic range, and is not tied to changes in biodiversity. New geochemical datasets from the Baltic Basin presented here from modern day southern Sweden (Scania) provide additional context for paleoredox conditions during the initiation of the GOBE. A progressive increase in oxygenation succeeding the Cambrian-Ordovician boundary is interpreted based on trace metal dynamics and thallium isotopic compositions, which may be providing enhanced metabolic efficiency and new niche space due to newly oxygenated shelf areas leading into the later Ordovician. The Middle-Late Ordovician is associated with peak faunal diversity which has been attributed to enhanced marine oxygenation. Similarly with the Cambrian-Ordovician boundary, very few studies have provided direct paleoredox evidence for a progressive increase in marine oxygenation, and thus redox conditions surrounding this integral period of diversification. New geochemical datasets from the Baltic Basin show a long-term increase in marine oxygenation throughout this interval though novel thallium isotopic compositions. The primary causal mechanisms for the LOME remains unclear, however there is growing evidence that anoxia is playing a larger role than initially thought. Classically, the LOME occurs between two extinction pulses, the first being attributed to climatic cooling and subsequent expansion of Gondwanan glaciation which resulted in widespread habitat loss, while the second pulse is associated with climatic warming, deglaciation, and an expansion of globally reducing conditions. New geochemical evidence from three carbonate successions derived from hydrographically dispersed basins show evidence of persistent reducing conditions throughout the Late Ordovician though low iodine-to-calcium ratios, while carbonate-associated sulfate isotopic suggest an overall reduction of global pyrite burial. Lastly, new thallium isotopic compositions from two Upper Ordovician basins of predominantly organic-rich shales identify highly variable global burial of manganese oxides which is intimately linked to marine (de)oxygenation and the two extinction pulses of the LOME. These thallium isotopic trends show that there were two major fluctuations between oxygenated and reducing conditions, which suggests that dynamic changes in oxygenation levels is a primary control on marine biodiversity, rather than the magnitude of reducing conditions.
Author: University of Paleontolgy. Museum of Paleontology
Publisher:
ISBN:
Category :
Languages : en
Pages : 14
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Author: International Geological Correlation Programme. Project 410
Publisher:
ISBN:
Category : Biodiversity
Languages : en
Pages : 20
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Author:
Publisher:
ISBN:
Category :
Languages : en
Pages : 0
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Author: Shaolin Meliora Censullo
Publisher:
ISBN:
Category : Animals
Languages : en
Pages : 129
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The evolution and biogeographic changes of three Ordovician brachiopod genera were examined using species-level phylogenetic analyses and phylogenetic biogeographic analyses in order to examine geological drivers of biogeographic evolution during the Great Ordovician Biodiversification Event (GOBE). Species-level phylogenetic hypotheses are reconstructed for Laurentian species of Hesperorthis Schuchert and Cooper 1931, Mimella Cooper, 1931, and Oepikina Salmon, 1942 using Bayesian inference. The reconstructed phylogenetic relationships were then used to investigate biogeographic patterns within the speciation of each lineage in order to evaluate how speciation occurred during the GOBE. Results indicate that alternating dispersal and vicariance events throughout the lineages of Hesperorthis, Mimella and Oepikina contributed to their increase in diversification during the Middle Ordovician which conforms to the BIME model of diversification. The oscillations of dispersal and vicariance events were related to fluctuating sea-level changes observed during the Middle to Late Ordovician
Author: Felix M. Gradstein
Publisher: Elsevier
ISBN: 0128243619
Category : Science
Languages : en
Pages : 1393
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Book Description
Geologic Time Scale 2020 (2 volume set) contains contributions from 80+ leading scientists who present syntheses in an easy-to-understand format that includes numerous color charts, maps and photographs. In addition to detailed overviews of chronostratigraphy, evolution, geochemistry, sequence stratigraphy and planetary geology, the GTS2020 volumes have separate chapters on each geologic period with compilations of the history of divisions, the current GSSPs (global boundary stratotypes), detailed bio-geochem-sequence correlation charts, and derivation of the age models. The authors are on the forefront of chronostratigraphic research and initiatives surrounding the creation of an international geologic time scale. The included charts display the most up-to-date, international standard as ratified by the International Commission on Stratigraphy and the International Union of Geological Sciences. As the framework for deciphering the history of our planet Earth, this book is essential for practicing Earth Scientists and academics. • Completely updated geologic time scale • Provides the most detailed integrated geologic time scale available that compiles and synthesize information in one reference • Gives insights on the construction, strengths and limitations of the geological time scale that greatly enhances its function and its utility
Author: Rituparna Bose
Publisher: Springer Science & Business Media
ISBN: 3642317219
Category : Science
Languages : en
Pages : 112
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Book Description
Increasing rate of species extinction in the present day will lead to a huge biodiversity crisis; eventually, this will lead to the paucity of non-renewable resources of energy making our Earth unsustainable in future. To save our mother planet from this crisis, studies need to be performed to discover abundant new fossil sites on Earth for continued access to oil-rich locations. Most importantly, a holistic approach is necessary in solving the present problem of biodiversity loss. This book presents newly developed quantitative models in understanding the biodiversity, evolution and ecology of extinct organisms. This will assist future earth scientists in understanding the natural and anthropogenic causes behind biodiversity crisis and ecosystem collapse. In addition, this study would be of great interest to exploration geologists and geophysicists in potentially unraveling natural resources from our sustainable Earth.
