Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing

The extent to which the onset of bioturbation affected global biogeochemistry during the Palaeozoic remains unclear. Here, the authors integrate bioturbation into the COPSE model, compare output with geochemical proxies, and suggest shallow burrowing contributed to a global low oxygen state during t...

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Autores principales:	Sebastiaan van de Velde, Benjamin J. W. Mills, Filip J. R. Meysman, Timothy M. Lenton, Simon W. Poulton
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/918906cc22d24adbb80c148035aa59d6
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spelling	oai:doaj.org-article:918906cc22d24adbb80c148035aa59d62021-12-02T15:34:49ZEarly Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing10.1038/s41467-018-04973-42041-1723https://doaj.org/article/918906cc22d24adbb80c148035aa59d62018-07-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-04973-4https://doaj.org/toc/2041-1723The extent to which the onset of bioturbation affected global biogeochemistry during the Palaeozoic remains unclear. Here, the authors integrate bioturbation into the COPSE model, compare output with geochemical proxies, and suggest shallow burrowing contributed to a global low oxygen state during the early Cambrian.Sebastiaan van de VeldeBenjamin J. W. MillsFilip J. R. MeysmanTimothy M. LentonSimon W. PoultonNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-10 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Sebastiaan van de Velde Benjamin J. W. Mills Filip J. R. Meysman Timothy M. Lenton Simon W. Poulton Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing
description	The extent to which the onset of bioturbation affected global biogeochemistry during the Palaeozoic remains unclear. Here, the authors integrate bioturbation into the COPSE model, compare output with geochemical proxies, and suggest shallow burrowing contributed to a global low oxygen state during the early Cambrian.
format	article
author	Sebastiaan van de Velde Benjamin J. W. Mills Filip J. R. Meysman Timothy M. Lenton Simon W. Poulton
author_facet	Sebastiaan van de Velde Benjamin J. W. Mills Filip J. R. Meysman Timothy M. Lenton Simon W. Poulton
author_sort	Sebastiaan van de Velde
title	Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing
title_short	Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing
title_full	Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing
title_fullStr	Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing
title_full_unstemmed	Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing
title_sort	early palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/918906cc22d24adbb80c148035aa59d6
work_keys_str_mv	AT sebastiaanvandevelde earlypalaeozoicoceananoxiaandglobalwarmingdrivenbytheevolutionofshallowburrowing AT benjaminjwmills earlypalaeozoicoceananoxiaandglobalwarmingdrivenbytheevolutionofshallowburrowing AT filipjrmeysman earlypalaeozoicoceananoxiaandglobalwarmingdrivenbytheevolutionofshallowburrowing AT timothymlenton earlypalaeozoicoceananoxiaandglobalwarmingdrivenbytheevolutionofshallowburrowing AT simonwpoulton earlypalaeozoicoceananoxiaandglobalwarmingdrivenbytheevolutionofshallowburrowing
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Early Palaeozoic ocean anoxia and global warming driven by the evolution of shallow burrowing

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