Evolution from an anoxic to oxic deep ocean during the Ediacaran–Cambrian transition and implications for bioradiation-Reference-Cited by-同舟云学术

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Evolution from an anoxic to oxic deep ocean during the Ediacaran–Cambrian transition and implications for bioradiation

Published:2012-05 Issue: Volume:306-307 Page:129-138
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Wang Jianguo,Chen Daizhao,Yan Detian,Wei Hengye,Xiang Lei

Funder

National Natural Science Foundation of China

National Key Basic Research Project

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference101 articles.

1. Extinction of Cloudina and Namacalathus at the Precambrian–Cambrian boundary in Oman;Amthor;Geology,2003

2. The Chenjiang Biota: record of the Early Cambrian diversification of life and clues to exceptional preservation of fossils;Babcock;GSA Today,2001

3. Marine carbon reservoir, Corg–Ccarb coupling, and the evolution of the Proterozoic carbon cycle;Bartley;Geology,2004

4. Confirmation of iron limitation of phytoplankton photosynthesis in the equatorial Pacific Ocean;Behrenfeld;Nature,1996

5. Biogeochemical cycles of carbon and sulfur and their effect on atmospheric oxygen over Phanerozoic time;Berner;Global and Planetary Change,1989

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