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...

Descripción completa

Guardado en:

Detalles Bibliográficos
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
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/cb6814aa30384c9a9eca2d509be1855f
Etiquetas:	Agregar Etiqueta Sin Etiquetas, Sea el primero en etiquetar este registro!

id	oai:doaj.org-article:cb6814aa30384c9a9eca2d509be1855f
record_format	dspace
spelling	oai:doaj.org-article:cb6814aa30384c9a9eca2d509be1855f2021-12-02T16:49:27ZPersistent global marine euxinia in the early Silurian10.1038/s41467-020-15400-y2041-1723https://doaj.org/article/cb6814aa30384c9a9eca2d509be1855f2020-04-01T00:00:00Zhttps://doi.org/10.1038/s41467-020-15400-yhttps://doaj.org/toc/2041-1723The 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 Cretaceous ocean anoxic events.Richard G. StockeyDevon B. ColeNoah J. PlanavskyDavid K. LoydellJiří FrýdaErik A. SperlingNature PortfolioarticleScienceQENNature Communications, Vol 11, Iss 1, Pp 1-10 (2020)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Richard G. Stockey Devon B. Cole Noah J. Planavsky David K. Loydell Jiří Frýda Erik A. Sperling Persistent global marine euxinia in the early Silurian
description	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 Cretaceous ocean anoxic events.
format	article
author	Richard G. Stockey Devon B. Cole Noah J. Planavsky David K. Loydell Jiří Frýda Erik A. Sperling
author_facet	Richard G. Stockey Devon B. Cole Noah J. Planavsky David K. Loydell Jiří Frýda Erik A. Sperling
author_sort	Richard G. Stockey
title	Persistent global marine euxinia in the early Silurian
title_short	Persistent global marine euxinia in the early Silurian
title_full	Persistent global marine euxinia in the early Silurian
title_fullStr	Persistent global marine euxinia in the early Silurian
title_full_unstemmed	Persistent global marine euxinia in the early Silurian
title_sort	persistent global marine euxinia in the early silurian
publisher	Nature Portfolio
publishDate	2020
url	https://doaj.org/article/cb6814aa30384c9a9eca2d509be1855f
work_keys_str_mv	AT richardgstockey persistentglobalmarineeuxiniaintheearlysilurian AT devonbcole persistentglobalmarineeuxiniaintheearlysilurian AT noahjplanavsky persistentglobalmarineeuxiniaintheearlysilurian AT davidkloydell persistentglobalmarineeuxiniaintheearlysilurian AT jirifryda persistentglobalmarineeuxiniaintheearlysilurian AT erikasperling persistentglobalmarineeuxiniaintheearlysilurian
_version_	1718383362526150656

Persistent global marine euxinia in the early Silurian

Ejemplares similares