A Cenozoic-Style Scenario for the End-Ordovician Glaciation
International audience The end-Ordovician (Hirnantian) was an enigmatic interval in the Phanerozoic, known for massive glaciationpotentially at elevated CO2 levels, biogeochemical cycle disruptions recorded as large isotope anomalies and adevastating extinction event. Such linkage of eustatic, biolo...
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Bibliographic Details
Main Authors: |
Desrochers, André,
Ghienne, Jean-François,
Vandenbroucke, T.R.A.,
Achab, Aïcha,
Dabard, Marie-Pierre,
Al., Et |
Other Authors: |
Department of Earth Sciences Ottawa,
University of Ottawa Ottawa,
Institut de physique du globe de Strasbourg (IPGS),
Université de Strasbourg (UNISTRA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS),
Géosystèmes - UMR 8217 (Géosystèmes),
Université de Picardie Jules Verne (UPJV)-Centre National de la Recherche Scientifique (CNRS)-Université de Lille, Sciences et Technologies,
Géosciences Rennes (GR),
Centre National de la Recherche Scientifique (CNRS)-Observatoire des Sciences de l'Univers de Rennes (OSUR)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rennes 1 (UR1),
Université de Rennes (UNIV-RENNES)-Université de Rennes (UNIV-RENNES),
European Geoscience Union |
Format: | Conference Object
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Language: | English |
Published: |
HAL CCSD
2015
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Subjects: |
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Online Access: | https://hal-insu.archives-ouvertes.fr/insu-01137649
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