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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...
| Autores principales: | , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2021
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| Materias: | |
| 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 |