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Breathless through time: oxygen and animals across Earth’s history

Breathless through time: oxygen and animals across Earth’s history
Breathless through time: oxygen and animals across Earth’s history

Oxygen levels in the atmosphere and ocean have changed dramatically over Earth history, with major impacts on marine life. Because the early part of Earth’s history lacked both atmospheric oxygen and animals, a persistent co-evolutionary narrative has developed linking oxygen change with changes in animal diversity. Although it was long believed that oxygen rose to essentially modern levels around the Cambrian period, a more muted increase is now believed likely. Thus, if oxygen increase facilitated the Cambrian explosion, it did so by crossing critical ecological thresholds at low O2. Atmospheric oxygen likely remained at low or moderate levels through the early Paleozoic era, and this likely contributed to high metazoan extinction rates until oxygen finally rose to modern levels in the later Paleozoic. After this point, ocean de-oxygenation (and marine mass extinctions) is increasingly linked to large igneous province eruptions—massive volcanic carbon inputs to the Earth system that caused global warming, ocean acidification, and oxygen loss. Although the timescales of these ancient events limit their utility as exact analogs for modern anthropogenic global change, the clear message from the geologic record is that large and rapid CO2 injections into the Earth system consistently cause the same deadly trio of stressors that are observed today. The next frontier in understanding the impact of oxygen changes (or, more broadly, temperature-dependent hypoxia) in deep time requires approaches from ecophysiology that will help conservation biologists better calibrate the response of the biosphere at large taxonomic, spatial, and temporal scales.

0006-3185
184-206
Sperling, Erik A.
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Boag, Thomas H.
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Duncan, Murray I.
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Endriga, Cecilia R.
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Marquez, J. Andres
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Mills, Daniel B.
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Monarrez, Pedro M.
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Sclafani, Judith A.
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Stockey, Richard G.
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Payne, Jonathan L.
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Sperling, Erik A.
0c67e5ac-bf08-438f-8bb1-55f8f0522a7f
Boag, Thomas H.
651eb670-969f-4a16-9f27-e7a7197ed851
Duncan, Murray I.
c25892de-330d-4d8c-b187-6c60033f4fc8
Endriga, Cecilia R.
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Marquez, J. Andres
242298a9-a3c0-4005-94da-9a219df967af
Mills, Daniel B.
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Monarrez, Pedro M.
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Sclafani, Judith A.
3cc7ac7f-5440-47fb-95b8-051358a9ed77
Stockey, Richard G.
005ca449-f5c9-4049-835f-0a9c6df3a93d
Payne, Jonathan L.
2c848a08-316c-4caa-a27f-bbce396df660

Sperling, Erik A., Boag, Thomas H., Duncan, Murray I., Endriga, Cecilia R., Marquez, J. Andres, Mills, Daniel B., Monarrez, Pedro M., Sclafani, Judith A., Stockey, Richard G. and Payne, Jonathan L. (2022) Breathless through time: oxygen and animals across Earth’s history. Biological Bulletin, 243 (2), 184-206. (doi:10.1086/721754).

Record type: Article

Abstract

Oxygen levels in the atmosphere and ocean have changed dramatically over Earth history, with major impacts on marine life. Because the early part of Earth’s history lacked both atmospheric oxygen and animals, a persistent co-evolutionary narrative has developed linking oxygen change with changes in animal diversity. Although it was long believed that oxygen rose to essentially modern levels around the Cambrian period, a more muted increase is now believed likely. Thus, if oxygen increase facilitated the Cambrian explosion, it did so by crossing critical ecological thresholds at low O2. Atmospheric oxygen likely remained at low or moderate levels through the early Paleozoic era, and this likely contributed to high metazoan extinction rates until oxygen finally rose to modern levels in the later Paleozoic. After this point, ocean de-oxygenation (and marine mass extinctions) is increasingly linked to large igneous province eruptions—massive volcanic carbon inputs to the Earth system that caused global warming, ocean acidification, and oxygen loss. Although the timescales of these ancient events limit their utility as exact analogs for modern anthropogenic global change, the clear message from the geologic record is that large and rapid CO2 injections into the Earth system consistently cause the same deadly trio of stressors that are observed today. The next frontier in understanding the impact of oxygen changes (or, more broadly, temperature-dependent hypoxia) in deep time requires approaches from ecophysiology that will help conservation biologists better calibrate the response of the biosphere at large taxonomic, spatial, and temporal scales.

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More information

Accepted/In Press date: 30 June 2022
e-pub ahead of print date: 23 September 2022
Published date: 1 October 2022
Additional Information: Funding Information: EAS thanks Lisa Levin for the title suggestion and Lisa Levin and Andrew Knoll for their mentorship during a stimulating postdoctoral research experience studying oxygen and animals. Funding was provided to EAS, RGS, JAS, and JAM by National Science Foundation EAR-1922966 and to EAS and MID by an Environmental Venture Project grant from the Stanford Woods Institute for Environmental Studies. We thank Ben Black for photos of the Siberian Traps, Hunter Olson for help with figure preparation, and the Historical Geobiology Lab for feedback. Publisher Copyright: © 2022 The University of Chicago. All rights reserved. Published by The University of Chicago Press.

Identifiers

Local EPrints ID: 474735
URI: http://eprints.soton.ac.uk/id/eprint/474735
ISSN: 0006-3185
PURE UUID: 685d7b30-7336-4643-ae04-ceeeebd118cf
ORCID for Richard G. Stockey: ORCID iD orcid.org/0000-0001-5541-7987

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Date deposited: 02 Mar 2023 17:37
Last modified: 06 Jun 2024 02:15

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Contributors

Author: Erik A. Sperling
Author: Thomas H. Boag
Author: Murray I. Duncan
Author: Cecilia R. Endriga
Author: J. Andres Marquez
Author: Daniel B. Mills
Author: Pedro M. Monarrez
Author: Judith A. Sclafani
Author: Richard G. Stockey ORCID iD
Author: Jonathan L. Payne

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