Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum

Understanding the response of marine productivity and CO2 drawdown to past warming events can provide important insights into the future. Here, the authors use bacterial magnetite nanoparticle fossils to reconstruct nutrient supply and marine deoxygenation during the Palaeocene–Eocene Thermal Maximu...

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Autores principales:	Liao Chang, Richard J. Harrison, Fan Zeng, Thomas A. Berndt, Andrew P. Roberts, David Heslop, Xiang Zhao
Formato:	article
Lenguaje:	EN
Publicado:	Nature Portfolio 2018
Materias:	Science Q
Acceso en línea:	https://doaj.org/article/68afd2e30ba2451c9018c611aebbac65
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spelling	oai:doaj.org-article:68afd2e30ba2451c9018c611aebbac652021-12-02T16:50:05ZCoupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum10.1038/s41467-018-06472-y2041-1723https://doaj.org/article/68afd2e30ba2451c9018c611aebbac652018-10-01T00:00:00Zhttps://doi.org/10.1038/s41467-018-06472-yhttps://doaj.org/toc/2041-1723Understanding the response of marine productivity and CO2 drawdown to past warming events can provide important insights into the future. Here, the authors use bacterial magnetite nanoparticle fossils to reconstruct nutrient supply and marine deoxygenation during the Palaeocene–Eocene Thermal Maximum.Liao ChangRichard J. HarrisonFan ZengThomas A. BerndtAndrew P. RobertsDavid HeslopXiang ZhaoNature PortfolioarticleScienceQENNature Communications, Vol 9, Iss 1, Pp 1-9 (2018)
institution	DOAJ
collection	DOAJ
language	EN
topic	Science Q
spellingShingle	Science Q Liao Chang Richard J. Harrison Fan Zeng Thomas A. Berndt Andrew P. Roberts David Heslop Xiang Zhao Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum
description	Understanding the response of marine productivity and CO2 drawdown to past warming events can provide important insights into the future. Here, the authors use bacterial magnetite nanoparticle fossils to reconstruct nutrient supply and marine deoxygenation during the Palaeocene–Eocene Thermal Maximum.
format	article
author	Liao Chang Richard J. Harrison Fan Zeng Thomas A. Berndt Andrew P. Roberts David Heslop Xiang Zhao
author_facet	Liao Chang Richard J. Harrison Fan Zeng Thomas A. Berndt Andrew P. Roberts David Heslop Xiang Zhao
author_sort	Liao Chang
title	Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum
title_short	Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum
title_full	Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum
title_fullStr	Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum
title_full_unstemmed	Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum
title_sort	coupled microbial bloom and oxygenation decline recorded by magnetofossils during the palaeocene–eocene thermal maximum
publisher	Nature Portfolio
publishDate	2018
url	https://doaj.org/article/68afd2e30ba2451c9018c611aebbac65
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Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum

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