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...
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 |
Similar Items
-
Mercury anomalies across the Palaeocene–Eocene thermal maximum
by: Jones, M, et al.
Published: (2019) -
Mercury anomalies across the Palaeocene–Eocene Thermal Maximum
by: M. T. Jones, et al.
Published: (2019-02-01) -
Deciphering the Palaeocene-Eocene thermal maximum by Granger causality test
by: Zeyang Liu, et al.
Published: (2023-02-01) -
Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum
by: Berndt, C, et al.
Published: (2023) -
Reduced carbon cycle resilience across the Palaeocene–Eocene Thermal Maximum
by: D. I. Armstrong McKay, et al.
Published: (2018-10-01)