Chemical–to–reverse weathering triggered a pronounced positive carbon isotope excursion in a forced regressive to transgressive dolostone succession during the terminal Ediacaran glaciation-Reference-Cited by-同舟云学术

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Chemical–to–reverse weathering triggered a pronounced positive carbon isotope excursion in a forced regressive to transgressive dolostone succession during the terminal Ediacaran glaciation

Published:2024-09 Issue: Volume:240 Page:104521
ISSN:0921-8181
Container-title:Global and Planetary Change
language:en
Short-container-title:Global and Planetary Change

Author:

Zhang Yan,Zhu Guangyou,Li Xi,Ai Yifei,Duan Pengzhen,Li Mengqi,Liu Jincheng

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Reference157 articles.

1. A multilayered water column in the Ediacaran Yangtze platform? Insights from carbonate and organic matter paired δ13C;Ader;Earth Planet. Sci. Lett.,2009

2. Interpreting Phanerozoic δ13C patterns as periodic glacio-eustatic sequences;Al-Husseini,2020

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

4. Continental igneous rock composition: A major control of past global chemical weathering;Bataille;Sci. Adv.,2017

5. The long-term carbon cycle, fossil fuels and atmospheric composition;Berner;Nature,2003

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