A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration

In the Earth's history, the timing of oceanic large-scale events of oxygen depletion remains poorly understood. Here, the authors show that palaeogeography was a major preconditioning factor during the Cretaceous, implying that thresholds to shift toward a global anoxia are likely to be much hi...

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Autores principales:	Yannick Donnadieu, Emmanuelle Pucéat, Mathieu Moiroud, François Guillocheau, Jean- François Deconinck
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2016
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/6c39ec6dd14e4c15bc296fc392d7da38
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id	oai:doaj.org-article:6c39ec6dd14e4c15bc296fc392d7da38
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spelling	oai:doaj.org-article:6c39ec6dd14e4c15bc296fc392d7da382021-12-02T17:31:51ZA better-ventilated ocean triggered by Late Cretaceous changes in continental configuration10.1038/ncomms103162041-1723https://doaj.org/article/6c39ec6dd14e4c15bc296fc392d7da382016-01-01T00:00:00Zhttps://doi.org/10.1038/ncomms10316https://doaj.org/toc/2041-1723In the Earth's history, the timing of oceanic large-scale events of oxygen depletion remains poorly understood. Here, the authors show that palaeogeography was a major preconditioning factor during the Cretaceous, implying that thresholds to shift toward a global anoxia are likely to be much higher at present.Yannick DonnadieuEmmanuelle PucéatMathieu MoiroudFrançois GuillocheauJean- François DeconinckNature PortfolioarticleScienceQENNature Communications, Vol 7, Iss 1, Pp 1-12 (2016)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Yannick Donnadieu Emmanuelle Pucéat Mathieu Moiroud François Guillocheau Jean- François Deconinck A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration
description	In the Earth's history, the timing of oceanic large-scale events of oxygen depletion remains poorly understood. Here, the authors show that palaeogeography was a major preconditioning factor during the Cretaceous, implying that thresholds to shift toward a global anoxia are likely to be much higher at present.
format	article
author	Yannick Donnadieu Emmanuelle Pucéat Mathieu Moiroud François Guillocheau Jean- François Deconinck
author_facet	Yannick Donnadieu Emmanuelle Pucéat Mathieu Moiroud François Guillocheau Jean- François Deconinck
author_sort	Yannick Donnadieu
title	A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration
title_short	A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration
title_full	A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration
title_fullStr	A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration
title_full_unstemmed	A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration
title_sort	better-ventilated ocean triggered by late cretaceous changes in continental configuration
publisher	Nature Portfolio
publishDate	2016
url	https://doaj.org/article/6c39ec6dd14e4c15bc296fc392d7da38
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A better-ventilated ocean triggered by Late Cretaceous changes in continental configuration

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