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Cited by 264

The DOI matches its Crossref record; 108 of the 108 references it cites were found in a registry or an index.

On the potential for ocean acidification to be a general cause of ancient reef crises

KIESSLING, WOLFGANG, SIMPSON, CARL·2011·Global Change Biology

Abstract

Anthropogenic rise in the carbon dioxide concentration in the atmosphere leads to global warming and acidification of the oceans. Ocean acidification (OA) is harmful to many organisms but especially to those that build massive skeletons of calcium carbonate, such as reef corals. Here, we test the recent suggestion that OA leads not only to declining calcification of reef corals and reduced growth rates of reefs but may also have been a trigger of ancient reef crises and mass extinctions in the sea. We analyse the fossil record of biogenic reefs and marine organisms to (1) assess the timing and intensity of ancient reef crises, (2) check which reef crises were concurrent with inferred pulses of carbon dioxide concentrations and (3) evaluate the correlation between reef crises and mass extinctions and their selectivity in terms of inferred physiological buffering. We conclude that four of five global metazoan reef crises in the last 500 Myr were probably at least partially governed by OA and rapid global warming. However, only two of the big five mass extinctions show geological evidence of OA.

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Crossref · 10.1111/j.1365-2486.2010.02204.x

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Metadata

Authors
KIESSLING, W., & SIMPSON, C.
Venue
Global Change Biology
Publisher
Wiley
Published
2010-12-01
Volume
17
Issue
1
Pages
56-67
ISSN
1354-1013 (ISSN-L)
OpenAlex
W2100073969
Cited by
264
References
108
FWCI
12.67
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: On the potential for ocean acidification to be a general cause of ancient reef crises. https://app.cochat.ai/papers/10.1111/j.1365-2486.2010.02204.x
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KIESSLING, W., & SIMPSON, C. (2011). On the potential for ocean acidification to be a general cause of ancient reef crises. Global Change Biology. https://doi.org/10.1111/j.1365-2486.2010.02204.x

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