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Journal ArticleDOI

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

Wolfgang Kiessling, +1 more
- 01 Jan 2011 - 
- Vol. 17, Iss: 1, pp 56-67
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TLDR
In this article, the authors 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.
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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Citations
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Journal ArticleDOI

Projecting Coral Reef Futures Under Global Warming and Ocean Acidification

TL;DR: Emerging evidence for variability in the coral calcification response to acidification, geographical variation in bleaching susceptibility and recovery, responses to past climate change, and potential rates of adaptation to rapid warming supports an alternative scenario in which reef degradation occurs with greater temporal and spatial heterogeneity than current projections suggest.
Book ChapterDOI

Impact of ocean warming and ocean acidication on marine invertebrate life history stages: Vulnerabilities and potential for persistence in a changing ocean

TL;DR: To address questions of future vulnerabilities, data on the thermo- and pH/ pco2 tolerance of fertilization and development in marine invertebrates are reviewed in the context of the change in the oceans that are forecast to occur over the next 100-200 years.
Journal ArticleDOI

Sensitivities of extant animal taxa to ocean acidification

TL;DR: Analysis of the sensitivities of five animal groups to a wide range of CO2 concentrations finds a variety of responses within and between taxa, indicating that acidification will drive substantial changes in ocean ecosystems this century.
Journal ArticleDOI

Predicting evolutionary responses to climate change in the sea

TL;DR: Why an evolutionary perspective is crucial to understanding climate change impacts in the sea is emphasised and the various experimental approaches that can be used to estimate evolutionary potential are outlined, focusing on molecular tools, quantitative genetics, and experimental evolution.
References
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Book

Climate change 2007 : the physical science basis : contribution of Working Group I to the Fourth Assessment Report of the Intergovernmental Panel on Climate Change

Susan Solomon
TL;DR: In this article, the authors present a historical overview of climate change science, including changes in atmospheric constituents and radiative forcing, as well as changes in snow, ice, and frozen ground.
Journal ArticleDOI

Coral Reefs Under Rapid Climate Change and Ocean Acidification

TL;DR: As the International Year of the Reef 2008 begins, scaled-up management intervention and decisive action on global emissions are required if the loss of coral-dominated ecosystems is to be avoided.
Journal ArticleDOI

Extraterrestrial Cause for the Cretaceous-Tertiary Extinction

TL;DR: A hypothesis is suggested which accounts for the extinctions and the iridium observations, and the chemical composition of the boundary clay, which is thought to come from the stratospheric dust, is markedly different from that of clay mixed with the Cretaceous and Tertiary limestones, which are chemically similar to each other.
Journal ArticleDOI

Oceanography: anthropogenic carbon and ocean pH.

TL;DR: It is found that oceanic absorption of CO2 from fossil fuels may result in larger pH changes over the next several centuries than any inferred from the geological record of the past 300 million years.
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