Molar tooth carbonates and benthic methane fluxes in Proterozoic oceans

Molar tooth structures are ptygmatically folded and microspar-filled structures common in early- and mid-Proterozoic (∼2,500–750 million years ago, Ma) subtidal successions, but extremely rare in rocks <750 Ma. Here, on the basis of Mg and S isotopes, we show that molar tooth structures may have...

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Detalles Bibliográficos
Autores principales: Shen, Bing, Dong, Lin, Xiao, Shuhai, Lang, Xianguo, Huang, Kangjun, Peng, Yongbo, Zhou, Chuanming, Ke, Shan, Liu, Pengju
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4729840/
https://www.ncbi.nlm.nih.gov/pubmed/26739600
http://dx.doi.org/10.1038/ncomms10317

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4729840/
https://www.ncbi.nlm.nih.gov/pubmed/26739600
http://dx.doi.org/10.1038/ncomms10317

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