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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Format: | Article |
Language: | English |
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Nature Portfolio
2018-10-01
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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. |
first_indexed | 2024-12-23T02:06:25Z |
format | Article |
id | doaj.art-68afd2e30ba2451c9018c611aebbac65 |
institution | Directory Open Access Journal |
issn | 2041-1723 |
language | English |
last_indexed | 2024-12-23T02:06:25Z |
publishDate | 2018-10-01 |
publisher | Nature Portfolio |
record_format | Article |
series | Nature Communications |
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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