UCL Discovery
UCL home » Library Services » Electronic resources » UCL Discovery

Changes in continental weathering regimes inhibited global marine deoxygenation during the Paleocene-Eocene thermal maximum

Wei, Guang-Yi; Pohl, Alexandre; Jiang, Shijun; Zhang, Hua; Wang, Wenqian; A E Pogge von Strandmann, Philip; Maffre, Pierre; ... Zhang, Feifei; + view all (2025) Changes in continental weathering regimes inhibited global marine deoxygenation during the Paleocene-Eocene thermal maximum. Nature Communications , 16 , Article 9163. 10.1038/s41467-025-64217-0. Green open access

[thumbnail of Wei 2025 Li isotopes PETM.pdf]
Preview
Text
Wei 2025 Li isotopes PETM.pdf - Published Version

Download (1MB) | Preview

Abstract

The moderate impact of rapid global warming on oceanic redox and biodiversity during the Paleocene-Eocene thermal maximum (PETM; ~55.9 Ma) contrasts with other hyperthermal events in Earth's history, and remains mostly unexplained. Here, we use lithium isotope (δ7Li) proxy and Earth system model simulations to reconstruct continental weathering regimes during the PETM. Negative δ7Li excursions of 3-4‰ in shallow-marine carbonates suggests globally increased erosion rates and decreased weathering intensities. Further, large negative δ7Li excursions of 4-5‰ in siliciclastic successions reflect enhanced accumulation of detrital clays exhumed from previous clay-rich sedimentary rocks, rather than those from weathering of igneous rocks. Changes in continental weathering regimes and associated flux of nutrients to oceans provide an explanation to the muted increase in oceanic anoxia and overall biodiversity loss during the PETM. The concomitant increases in physical erosion and clay delivery also enhanced organic carbon burial efficiency, permitting rapid return of global climate to pre-perturbation state.

Type: Article
Title: Changes in continental weathering regimes inhibited global marine deoxygenation during the Paleocene-Eocene thermal maximum
Location: England
Open access status: An open access version is available from UCL Discovery
DOI: 10.1038/s41467-025-64217-0
Publisher version: https://doi.org/10.1038/s41467-025-64217-0
Language: English
Additional information: This article is licensed under a Creative Commons Attribution-NonCommercial-NoDerivatives 4.0 International License, which permits any non-commercial use, sharing, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons licence, and indicate if you modified the licensed material. You do not have permission under this licence to share adapted material derived from this article or parts of it. The images or other third party material in this article are included in the article’s Creative Commons licence, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons licence and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this licence, visit http://creativecommons.org/licenses/by-nc-nd/4.0/.
UCL classification: UCL
UCL > Provost and Vice Provost Offices > UCL BEAMS
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences
UCL > Provost and Vice Provost Offices > UCL BEAMS > Faculty of Maths and Physical Sciences > Dept of Earth Sciences
URI: https://discovery.ucl.ac.uk/id/eprint/10215919
Downloads since deposit
9Downloads
Download activity - last month
Download activity - last 12 months
Downloads by country - last 12 months

Archive Staff Only

View Item View Item