Persistent global marine euxinia in the early Silurian

The Late Ordovician mass extinction has been attributed to extended marine anoxia. Here, the authors use a metal isotope mass balance model and find the marine anoxic event lasted over 3 million years, notably longer than the anoxic event associated with the Permian-Triassic extinction and Cretaceou...

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Autores principales: Richard G. Stockey, Devon B. Cole, Noah J. Planavsky, David K. Loydell, Jiří Frýda, Erik A. Sperling
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2020
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Acceso en línea:https://doaj.org/article/cb6814aa30384c9a9eca2d509be1855f
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