Continental weathering intensity during the termination of the Marinoan Snowball Earth: Mg isotope evidence from the basal Doushantuo cap carbonate in South China-Reference-Cited by-同舟云学术

Continental weathering intensity during the termination of the Marinoan Snowball Earth: Mg isotope evidence from the basal Doushantuo cap carbonate in South China

Published:2020-08 Issue: Volume:552 Page:109774
ISSN:0031-0182
Container-title:Palaeogeography, Palaeoclimatology, Palaeoecology
language:en
Short-container-title:Palaeogeography, Palaeoclimatology, Palaeoecology

Author:

Li Jian,Hao Cuiguo,Wang Zhihong,Dong Lin,Wang Yiwu,Huang Kang-Jun,Lang Xianguo,Huang Tianzheng,Yuan Honglin,Zhou Chuanming,Shen Bing

Funder

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Paleontology,Earth-Surface Processes,Ecology, Evolution, Behavior and Systematics,Oceanography

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