Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation

Recent eustatic reconstructions allow for reconsidering the relationships between the fifteen Paleozoic–Mesozoic mass extinctions (mid-Cambrian, end-Ordovician, Llandovery/Wenlock, Late Devonian, Devonian/Carboniferous, mid-Carboniferous, end-Guadalupian, end-Permian, two mid-Triassic, end-Triassic,...

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Main Author: Dmitry A. Ruban
Format: Article
Language:English
Published: MDPI AG 2020-11-01
Series:Life
Subjects:
Online Access:https://www.mdpi.com/2075-1729/10/11/281
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author Dmitry A. Ruban
author_facet Dmitry A. Ruban
author_sort Dmitry A. Ruban
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description Recent eustatic reconstructions allow for reconsidering the relationships between the fifteen Paleozoic–Mesozoic mass extinctions (mid-Cambrian, end-Ordovician, Llandovery/Wenlock, Late Devonian, Devonian/Carboniferous, mid-Carboniferous, end-Guadalupian, end-Permian, two mid-Triassic, end-Triassic, Early Jurassic, Jurassic/Cretaceous, Late Cretaceous, and end-Cretaceous extinctions) and global sea-level changes. The relationships between eustatic rises/falls and period-long eustatic trends are examined. Many eustatic events at the mass extinction intervals were not anomalous. Nonetheless, the majority of the considered mass extinctions coincided with either interruptions or changes in the ongoing eustatic trends. It cannot be excluded that such interruptions and changes could have facilitated or even triggered biodiversity losses in the marine realm.
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spelling doaj.art-caf5cd17368745f192d68f1284cffb472023-11-20T20:59:32ZengMDPI AGLife2075-17292020-11-01101128110.3390/life10110281Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event InterpretationDmitry A. Ruban0K.G. Razumovsky Moscow State University of Technologies and Management (the First Cossack University), Zemlyanoy Val Street 73, 109004 Moscow, RussiaRecent eustatic reconstructions allow for reconsidering the relationships between the fifteen Paleozoic–Mesozoic mass extinctions (mid-Cambrian, end-Ordovician, Llandovery/Wenlock, Late Devonian, Devonian/Carboniferous, mid-Carboniferous, end-Guadalupian, end-Permian, two mid-Triassic, end-Triassic, Early Jurassic, Jurassic/Cretaceous, Late Cretaceous, and end-Cretaceous extinctions) and global sea-level changes. The relationships between eustatic rises/falls and period-long eustatic trends are examined. Many eustatic events at the mass extinction intervals were not anomalous. Nonetheless, the majority of the considered mass extinctions coincided with either interruptions or changes in the ongoing eustatic trends. It cannot be excluded that such interruptions and changes could have facilitated or even triggered biodiversity losses in the marine realm.https://www.mdpi.com/2075-1729/10/11/281biotic crisisglobal sea levellife evolution
spellingShingle Dmitry A. Ruban
Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
Life
biotic crisis
global sea level
life evolution
title Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
title_full Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
title_fullStr Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
title_full_unstemmed Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
title_short Paleozoic–Mesozoic Eustatic Changes and Mass Extinctions: New Insights from Event Interpretation
title_sort paleozoic mesozoic eustatic changes and mass extinctions new insights from event interpretation
topic biotic crisis
global sea level
life evolution
url https://www.mdpi.com/2075-1729/10/11/281
work_keys_str_mv AT dmitryaruban paleozoicmesozoiceustaticchangesandmassextinctionsnewinsightsfromeventinterpretation