Ocean euxinia and climate change “double whammy” drove the Late Ordovician mass extinction

Author:

Zou Caineng12,Qiu Zhen12,Poulton Simon W.3,Dong Dazhong12,Wang Hongyan12,Chen Daizhao4,Lu Bin12,Shi Zhensheng12,Tao Huifei5

Affiliation:

1. China National Petroleum Corporation, Research Institute of Petroleum Exploration & Development, 100083 Beijing, China

2. National Energy Shale Gas Research & Development (Experiment) Center, 065007 Langfang, China

3. School of Earth and Environment, University of Leeds, Leeds LS2 9JT, UK

4. Institute of Geology and Geophysics, Chinese Academy of Sciences (IGG-CAS), 100029 Beijing, China

5. Key Laboratory of Petroleum Resources Research, Institute of Geology and Geophysics, Chinese Academy of Sciences, 730000 Lanzhou, China

Publisher

Geological Society of America

Subject

Geology

Reference25 articles.

1. Disentangling the record of diagenesis, local redox conditions, and global seawater chemistry during the latest Ordovician glaciation;Ahm;Earth and Planetary Science Letters,2017

2. Bathymetric and isotopic evidence for a short-lived Ordovician glaciation in a greenhouse period;Brenchley;Geology,1994

3. Do all mass extinctions represent an ecological crisis? Evidence from the Late Ordovician;Brenchley;Geological Journal,2001

4. A late Ordovician (Hirnantian) karstic surface in a submarine channel, recording glacio-eustatic sea-level changes: Meifod, central Wales;Brenchley;Geological Journal,2006

5. Assessing the utility of Fe/Al and Fe-speciation to record water column redox conditions in carbonate-rich sediments;Clarkson;Chemical Geology,2014

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