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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Main Authors: Liao Chang, Richard J. Harrison, Fan Zeng, Thomas A. Berndt, Andrew P. Roberts, David Heslop, Xiang Zhao
Format: Article
Language:English
Published: Nature Portfolio 2018-10-01
Series:Nature Communications
Online Access:https://doi.org/10.1038/s41467-018-06472-y
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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
collection DOAJ
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.
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spelling doaj.art-68afd2e30ba2451c9018c611aebbac652022-12-21T18:03:52ZengNature PortfolioNature Communications2041-17232018-10-01911910.1038/s41467-018-06472-yCoupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal MaximumLiao Chang0Richard J. Harrison1Fan Zeng2Thomas A. Berndt3Andrew P. Roberts4David Heslop5Xiang Zhao6Laboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking UniversityDepartment of Earth Sciences, University of CambridgeLaboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking UniversityLaboratory of Orogenic Belts and Crustal Evolution, School of Earth and Space Sciences, Peking UniversityResearch School of Earth Sciences, Australian National UniversityResearch School of Earth Sciences, Australian National UniversityResearch School of Earth Sciences, Australian National UniversityUnderstanding 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.https://doi.org/10.1038/s41467-018-06472-y
spellingShingle 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
Nature Communications
title 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_short 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
url https://doi.org/10.1038/s41467-018-06472-y
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