Earth’s youngest banded iron formation implies ferruginous conditions in the Early Cambrian ocean

It has been proposed that anoxic and iron-rich (ferruginous) marine conditions were common through most of Earth history. This view represents a major shift in our understanding of the evolution of marine chemistry. However, thus far, evidence for ferruginous conditions comes predominantly from Fe-s...

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Detalles Bibliográficos
Autores principales: Li, Zhi-Quan, Zhang, Lian-Chang, Xue, Chun-Ji, Zheng, Meng-Tian, Zhu, Ming-Tian, Robbins, Leslie J., Slack, John F., Planavsky, Noah J., Konhauser, Kurt O.
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/PMC6028650/
https://www.ncbi.nlm.nih.gov/pubmed/29967405
http://dx.doi.org/10.1038/s41598-018-28187-2

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6028650/
https://www.ncbi.nlm.nih.gov/pubmed/29967405
http://dx.doi.org/10.1038/s41598-018-28187-2

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