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Atmospheric CO2 over the past 66 million years from marine archives

Atmospheric CO2 over the past 66 million years from marine archives
Atmospheric CO2 over the past 66 million years from marine archives
Throughout Earth's history, CO2 is thought to have exerted a fundamental control on environmental change. Here we review and revise CO2 reconstructions from boron isotopes in carbonates and carbon isotopes in organic matter over the Cenozoic—the past 66 million years. We find close coupling between CO2 and climate throughout the Cenozoic, with peak CO2 levels of ∼1,500 ppm in the Eocene greenhouse, decreasing to ∼500 ppm in the Miocene, and falling further into the ice age world of the Plio–Pleistocene. Around two-thirds of Cenozoic CO2 drawdown is explained by an increase in the ratio of ocean alkalinity to dissolved inorganic carbon, likely linked to a change in the balance of weathering to outgassing, with the remaining one-third due to changing ocean temperature and major ion composition. Earth system climate sensitivity is explored and may vary between different time intervals. The Cenozoic CO2 record highlights the truly geological scale of anthropogenic CO2 change: Current CO2 levels were last seen around 3 million years ago, and major cuts in emissions are required to prevent a return to the CO2 levels of the Miocene or Eocene in the coming century.▪  CO2 reconstructions over the past 66 Myr from boron isotopes and alkenones are reviewed and re-evaluated.▪  CO2 estimates from the different proxies show close agreement, yielding a consistent picture of the evolution of the ocean-atmosphere CO2 system over the Cenozoic.▪  CO2 and climate are coupled throughout the past 66 Myr, providing broad constraints on Earth system climate sensitivity.▪  Twenty-first-century carbon emissions have the potential to return CO2 to levels not seen since the much warmer climates of Earth's distant past.
alkenones, boron isotopes, Cenozoic, climate, CO2
0084-6597
609-641
Rae, James W.B.
e22c24a8-9049-43a8-997a-c6dc10a3a26e
Zhang, Yi Ge
57eb90b7-b182-4203-93a1-0a0be4227c34
Liu, Xiaoqing
39f7a3a4-8d30-4b27-9350-277cd0946c05
Foster, Gavin L.
fbaa7255-7267-4443-a55e-e2a791213022
Stoll, Heather M.
fcb9ed2d-744d-4815-b1ea-e67029e8538c
Whiteford, Ross D.M.
a2420c32-3c9c-4c13-87d9-8020e649b73f
Rae, James W.B.
e22c24a8-9049-43a8-997a-c6dc10a3a26e
Zhang, Yi Ge
57eb90b7-b182-4203-93a1-0a0be4227c34
Liu, Xiaoqing
39f7a3a4-8d30-4b27-9350-277cd0946c05
Foster, Gavin L.
fbaa7255-7267-4443-a55e-e2a791213022
Stoll, Heather M.
fcb9ed2d-744d-4815-b1ea-e67029e8538c
Whiteford, Ross D.M.
a2420c32-3c9c-4c13-87d9-8020e649b73f

Rae, James W.B., Zhang, Yi Ge, Liu, Xiaoqing, Foster, Gavin L., Stoll, Heather M. and Whiteford, Ross D.M. (2021) Atmospheric CO2 over the past 66 million years from marine archives. Annual Review of Earth and Planetary Sciences, 49, 609-641. (doi:10.1146/annurev-earth-082420-063026).

Record type: Review

Abstract

Throughout Earth's history, CO2 is thought to have exerted a fundamental control on environmental change. Here we review and revise CO2 reconstructions from boron isotopes in carbonates and carbon isotopes in organic matter over the Cenozoic—the past 66 million years. We find close coupling between CO2 and climate throughout the Cenozoic, with peak CO2 levels of ∼1,500 ppm in the Eocene greenhouse, decreasing to ∼500 ppm in the Miocene, and falling further into the ice age world of the Plio–Pleistocene. Around two-thirds of Cenozoic CO2 drawdown is explained by an increase in the ratio of ocean alkalinity to dissolved inorganic carbon, likely linked to a change in the balance of weathering to outgassing, with the remaining one-third due to changing ocean temperature and major ion composition. Earth system climate sensitivity is explored and may vary between different time intervals. The Cenozoic CO2 record highlights the truly geological scale of anthropogenic CO2 change: Current CO2 levels were last seen around 3 million years ago, and major cuts in emissions are required to prevent a return to the CO2 levels of the Miocene or Eocene in the coming century.▪  CO2 reconstructions over the past 66 Myr from boron isotopes and alkenones are reviewed and re-evaluated.▪  CO2 estimates from the different proxies show close agreement, yielding a consistent picture of the evolution of the ocean-atmosphere CO2 system over the Cenozoic.▪  CO2 and climate are coupled throughout the past 66 Myr, providing broad constraints on Earth system climate sensitivity.▪  Twenty-first-century carbon emissions have the potential to return CO2 to levels not seen since the much warmer climates of Earth's distant past.

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More information

e-pub ahead of print date: 23 March 2021
Published date: 30 May 2021
Additional Information: Publisher Copyright: © 2021 Annual Reviews Inc.. All rights reserved.
Keywords: alkenones, boron isotopes, Cenozoic, climate, CO2

Identifiers

Local EPrints ID: 490645
URI: http://eprints.soton.ac.uk/id/eprint/490645
ISSN: 0084-6597
PURE UUID: 1a849c6a-99a1-42b2-bf3a-4dde68d82f8b
ORCID for Gavin L. Foster: ORCID iD orcid.org/0000-0003-3688-9668

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Date deposited: 31 May 2024 16:55
Last modified: 01 Jun 2024 01:42

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Contributors

Author: James W.B. Rae
Author: Yi Ge Zhang
Author: Xiaoqing Liu
Author: Gavin L. Foster ORCID iD
Author: Heather M. Stoll
Author: Ross D.M. Whiteford

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