Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum-Reference-Cited by-同舟云学术

Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum

Published:2021-10-15 Issue:42 Volume:7 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Pogge von Strandmann Philip A. E.¹²^ORCID,Jones Morgan T.³^ORCID,West A. Joshua⁴^ORCID,Murphy Melissa J.²⁵,Stokke Ella W.³^ORCID,Tarbuck Gary²^ORCID,Wilson David J.²^ORCID,Pearce Christopher R.⁶^ORCID,Schmidt Daniela N.⁷^ORCID

Affiliation:

1. Institute of Geosciences, Johannes Gutenberg University, 55122 Mainz, Germany.

2. London Geochemistry and Isotope Centre (LOGIC), Institute of Earth and Planetary Sciences, University College London and Birkbeck, University of London, Gower Place, London WC1E 6BS, UK.

3. Centre for Earth Evolution and Dynamics (CEED), University of Oslo, Pb. 1028 Blindern, 0315 Oslo, Norway.

4. Department of Earth Sciences, University of Southern California, 3651 Trousdale Parkway—ZHS 117, Los Angeles, CA 90089, USA.

5. Centre for Permafrost, University of Copenhagen, Copenhagen, Denmark.

6. National Oceanography Centre Southampton, University of Southampton Waterfront Campus, European Way, Southampton SO14 3ZH, UK.

7. School of Earth Sciences, University of Bristol, Wills Memorial Building, Queens Road, Bristol BS8 1RJ, UK.

Abstract

Silicate weathering and physical erosion markedly increased during the rapid warming of the PETM, allowing climatic recovery.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference135 articles.

1. Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum

2. Climate model and proxy data constraints on ocean warming across the Paleocene–Eocene Thermal Maximum

3. Very large release of mostly volcanic carbon during the Palaeocene–Eocene Thermal Maximum

4. Rapid carbon sequestration at the termination of the Palaeocene–Eocene Thermal Maximum

5. Redox-controlled carbon and phosphorus burial: A mechanism for enhanced organic carbon sequestration during the PETM

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