Persistent global marine euxinia in the early Silurian

The second pulse of the Late Ordovician mass extinction occurred around the Hirnantian-Rhuddanian boundary (~444 Ma) and has been correlated with expanded marine anoxia lasting into the earliest Silurian. Characterization of the Hirnantian ocean anoxic event has focused on the onset of anoxia, with...

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Detalles Bibliográficos
Autores principales: Stockey, Richard G., Cole, Devon B., Planavsky, Noah J., Loydell, David K., Frýda, Jiří, Sperling, Erik A.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7156380/
https://www.ncbi.nlm.nih.gov/pubmed/32286253
http://dx.doi.org/10.1038/s41467-020-15400-y

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7156380/
https://www.ncbi.nlm.nih.gov/pubmed/32286253
http://dx.doi.org/10.1038/s41467-020-15400-y

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