Marine redox stratification during the early Cambrian (ca. 529-509 Ma) and its control on the development of organic-rich shales in Yangtze Platform-Reference-Cited by-同舟云学术

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Marine redox stratification during the early Cambrian (ca. 529-509 Ma) and its control on the development of organic-rich shales in Yangtze Platform

Published:2017-06 Issue:6 Volume:18 Page:2354-2369
ISSN:1525-2027
Container-title:Geochemistry, Geophysics, Geosystems
language:en
Short-container-title:Geochem. Geophys. Geosyst.

Author:

Zhang Yuying¹^ORCID,He Zhiliang²³,Jiang Shu⁴^ORCID,Gao Bo²³,Liu Zhongbao²³,Han Bo¹,Wang Hu¹

Affiliation:

1. School of Energy Resources; China University of Geosciences; Beijing People's Republic of China

2. State Key Laboratory of Shale Oil and Gas Enrichment Mechanisms and Effective Development; Beijing People's Republic of China

3. Petroleum Exploration and Production Research Institute, SINOPEC; Beijing People's Republic of China

4. Energy and Geoscience Institute, University of Utah; Salt Lake City Utah USA

Funder

Science and Technology

SINOPEC

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

http://onlinelibrary.wiley.com/wol1/doi/10.1002/2017GC006864/fullpdf

Reference98 articles.

1. Mo-total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions;Algeo;Paleoceanography,2006

2. Sources and mechanisms for the enrichment of highly reactive iron in euxinic black sea sediments;Anderson;Am. J. Sci.,2004

3. Global climate, sea level cycles, and biotic events in the Cambrian Period;Babcock;Palaeoworld,2015

4. Differential adsorption of molybdate and tetrathio molybdate on pyrite (FeS2);Bostick;Environ. Sci. Technol.,2003

5. Background to the Cambrian explosion;Brasier;J. Geol. Soc. London,1992

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