The origin of cap carbonate after the Ediacaran glaciations

Author:

Wang Ruimin,Xing Chaochao,Wen Bin,Wang Xubin,Liu Kunwei,Huang Tianzheng,Zhou Chuanming,Shen Bing

Publisher

Elsevier BV

Subject

Oceanography,Global and Planetary Change

Reference113 articles.

1. Triple oxygen isotope evidence for elevated CO2 levels after a Neoproterozoic glaciation;Bao;Nature,2008

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

3. Mineralogical constraints on the paleoenvironments of the Ediacaran Doushantuo Formation;Bristow;Proc. Natl. Acad. Sci.,2009

4. Late proterozoic to early palaeozoic diamictites/tillites and associated glaciogenic sediments in the Serie Pourpree of Western Hoggar, Algeria;Caby,1981

5. U-Pb zircon age constraints on late Neoproterozoic glaciation in Tasmania;Calver;Geology,2004

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