Global marine redox changes drove the rise and fall of the Ediacara biota-Reference-Cited by-同舟云学术

Global marine redox changes drove the rise and fall of the Ediacara biota

Published:2019-07-28 Issue:6 Volume:17 Page:594-610
ISSN:1472-4677
Container-title:Geobiology
language:en
Short-container-title:Geobiology

Author:

Zhang Feifei¹²³⁴^ORCID,Xiao Shuhai⁵^ORCID,Romaniello Stephen J.⁴,Hardisty Dalton⁶,Li Chao⁷^ORCID,Melezhik Victor⁸,Pokrovsky Boris⁹,Cheng Meng⁷,Shi Wei⁷,Lenton Timothy M.¹⁰,Anbar Ariel D.⁴¹¹

Affiliation:

1. School of Earth Sciences and Engineering Nanjing University Nanjing China

2. Department of Geology and Geophysics Yale University New Haven CT USA

3. The Globe Institute University of Copenhagen Copenhagen K Denmark

4. School of Earth and Space Exploration Arizona State University Tempe AZ USA

5. Department of Geosciences Virginia Tech Blacksburg VA USA

6. Department of Earth and Environmental Science Michigan State University East Lansing MI USA

7. State Key Laboratory of Biogeology and Environmental Geology China University of Geosciences Wuhan China

8. Geological Survey of Norway Trondheim Norway

9. Geological Institute Russian Academy of Sciences Moscow Russia

10. Global Systems Institute University of Exeter Exeter UK

11. School of Molecular Science Arizona State University Tempe AZ USA

Funder

Natural Environment Research Council

National Natural Science Foundation of China

Publisher

Wiley

Subject

General Earth and Planetary Sciences,General Environmental Science,Ecology, Evolution, Behavior and Systematics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1111/gbi.12359

Reference91 articles.

1. Stratigraphic position of the Ediacaran Miaohe biota and its constrains on the age of the upper Doushantuo δ 13 C anomaly in the Yangtze Gorges area, South China

2. A modern framework for the interpretation of 238U/235U in studies of ancient ocean redox

3. The stratigraphic expression of a large negative carbon isotope excursion from the Ediacaran Johnnie Formation, Death Valley

4. Rapid expansion of oceanic anoxia immediately before the end-Permian mass extinction

5. Carbon isotope excursions and the oxidant budget of the Ediacaran atmosphere and ocean

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