Active methanogenesis during the melting of Marinoan snowball Earth

Geological evidence indicates that the deglaciation of Marinoan snowball Earth ice age (~635 Myr ago) was associated with intense continental weathering, recovery of primary productivity, transient marine euxinia, and potentially extensive CH(4) emission. It is proposed that the deglacial CH(4) emis...

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Detalles Bibliográficos
Autores principales: Zhao, Zhouqiao, Shen, Bing, Zhu, Jian-Ming, Lang, Xianguo, Wu, Guangliang, Tan, Decan, Pei, Haoxiang, Huang, Tianzheng, Ning, Meng, Ma, Haoran
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7878791/
https://www.ncbi.nlm.nih.gov/pubmed/33574253
http://dx.doi.org/10.1038/s41467-021-21114-6

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7878791/
https://www.ncbi.nlm.nih.gov/pubmed/33574253
http://dx.doi.org/10.1038/s41467-021-21114-6

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