Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?

Ocean acidification in modern oceans is linked to rapid increase in atmospheric CO2, raising concern about marine diversity, food security and ecosystem services. Proxy evidence for acidification during past crises may help predict future change, but three issues limit confidence of comparisons betw...

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Main Authors: Marie-Béatrice Forel, Pierre-Yves Collin, Yue Li, Stephen Kershaw, Sylvie Crasquin
Format: Article
Language:English
Published: MDPI AG 2012-09-01
Series:Geosciences
Subjects:
Online Access:http://www.mdpi.com/2076-3263/2/4/221
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author Marie-Béatrice Forel
Pierre-Yves Collin
Yue Li
Stephen Kershaw
Sylvie Crasquin
author_facet Marie-Béatrice Forel
Pierre-Yves Collin
Yue Li
Stephen Kershaw
Sylvie Crasquin
author_sort Marie-Béatrice Forel
collection DOAJ
description Ocean acidification in modern oceans is linked to rapid increase in atmospheric CO2, raising concern about marine diversity, food security and ecosystem services. Proxy evidence for acidification during past crises may help predict future change, but three issues limit confidence of comparisons between modern and ancient ocean acidification, illustrated from the end-Permian extinction, 252 million years ago: (1) problems with evidence for ocean acidification preserved in sedimentary rocks, where proposed marine dissolution surfaces may be subaerial. Sedimentary evidence that the extinction was partly due to ocean acidification is therefore inconclusive; (2) Fossils of marine animals potentially affected by ocean acidification are imperfect records of past conditions; selective extinction of hypercalcifying organisms is uncertain evidence for acidification; (3) The current high rates of acidification may not reflect past rates, which cannot be measured directly, and whose temporal resolution decreases in older rocks. Thus large increases in CO2 in the past may have occurred over a long enough time to have allowed assimilation into the oceans, and acidification may not have stressed ocean biota to the present extent. Although we acknowledge the very likely occurrence of past ocean acidification, obtaining support presents a continuing challenge for the Earth science community.
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spelling doaj.art-264f435306314a609c30bb906e7f1fd62022-12-21T18:12:11ZengMDPI AGGeosciences2076-32632012-09-012422123410.3390/geosciences2040221Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?Marie-Béatrice ForelPierre-Yves CollinYue LiStephen KershawSylvie CrasquinOcean acidification in modern oceans is linked to rapid increase in atmospheric CO2, raising concern about marine diversity, food security and ecosystem services. Proxy evidence for acidification during past crises may help predict future change, but three issues limit confidence of comparisons between modern and ancient ocean acidification, illustrated from the end-Permian extinction, 252 million years ago: (1) problems with evidence for ocean acidification preserved in sedimentary rocks, where proposed marine dissolution surfaces may be subaerial. Sedimentary evidence that the extinction was partly due to ocean acidification is therefore inconclusive; (2) Fossils of marine animals potentially affected by ocean acidification are imperfect records of past conditions; selective extinction of hypercalcifying organisms is uncertain evidence for acidification; (3) The current high rates of acidification may not reflect past rates, which cannot be measured directly, and whose temporal resolution decreases in older rocks. Thus large increases in CO2 in the past may have occurred over a long enough time to have allowed assimilation into the oceans, and acidification may not have stressed ocean biota to the present extent. Although we acknowledge the very likely occurrence of past ocean acidification, obtaining support presents a continuing challenge for the Earth science community.http://www.mdpi.com/2076-3263/2/4/221ocean acidificationend-Permian extinctionmicrobialiteocean bufferstylolite
spellingShingle Marie-Béatrice Forel
Pierre-Yves Collin
Yue Li
Stephen Kershaw
Sylvie Crasquin
Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?
Geosciences
ocean acidification
end-Permian extinction
microbialite
ocean buffer
stylolite
title Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?
title_full Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?
title_fullStr Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?
title_full_unstemmed Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?
title_short Ocean Acidification and the End-Permian Mass Extinction: To What Extent does Evidence Support Hypothesis?
title_sort ocean acidification and the end permian mass extinction to what extent does evidence support hypothesis
topic ocean acidification
end-Permian extinction
microbialite
ocean buffer
stylolite
url http://www.mdpi.com/2076-3263/2/4/221
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