Transient marine euxinia at the end of the terminal Cryogenian glaciation

Termination of the terminal Cryogenian Marinoan snowball Earth glaciation (~650–635 Ma) is associated with the worldwide deposition of a cap carbonate. Modeling studies suggest that, during and immediately following deglaciation, the ocean may have experienced a rapid rise in pH and physical stratif...

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Detalles Bibliográficos
Autores principales: Lang, Xianguo, Shen, Bing, Peng, Yongbo, Xiao, Shuhai, Zhou, Chuanming, Bao, Huiming, Kaufman, Alan Jay, Huang, Kangjun, Crockford, Peter W., Liu, Yonggang, Tang, Wenbo, Ma, Haoran
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6070556/
https://www.ncbi.nlm.nih.gov/pubmed/30068999
http://dx.doi.org/10.1038/s41467-018-05423-x

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6070556/
https://www.ncbi.nlm.nih.gov/pubmed/30068999
http://dx.doi.org/10.1038/s41467-018-05423-x

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