Low coral cover in a high-CO2 world

Coral reefs generally exist within a relatively narrow band of temperatures, light, and seawater aragonite saturation states. The growth of coral reefs is minimal or nonexistent outside this envelope. Climate change, through its effect on ocean temperature, has already had an impact on the world...

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Published in:Journal of Geophysical Research
Main Author: Hoegh-Guldberg, Ove
Format: Article in Journal/Newspaper
Language:English
Published: American Geophysical Union 2005
Subjects:
Online Access:https://espace.library.uq.edu.au/view/UQ:55716/UQ55716_OA.pdf
https://espace.library.uq.edu.au/view/UQ:55716
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spelling ftunivqespace:oai:espace.library.uq.edu.au:UQ:55716 2023-05-15T16:39:19+02:00 Low coral cover in a high-CO2 world Hoegh-Guldberg, Ove 2005-01-01 https://espace.library.uq.edu.au/view/UQ:55716/UQ55716_OA.pdf https://espace.library.uq.edu.au/view/UQ:55716 eng eng American Geophysical Union doi:10.1029/2004JC002528 issn:0148-0227 orcid:0000-0001-7510-6713 Oceanography Great-barrier-reef Co2 Partial-pressure Calcium-carbonate Saturation Vostok Ice Core Climate-change Ultraviolet-radiation Elevated-temperature Fish Communities Bleaching Event Stylophora-pistillata 069902 Global Change Biology Journal Article 2005 ftunivqespace https://doi.org/10.1029/2004JC002528 2020-12-28T23:22:03Z Coral reefs generally exist within a relatively narrow band of temperatures, light, and seawater aragonite saturation states. The growth of coral reefs is minimal or nonexistent outside this envelope. Climate change, through its effect on ocean temperature, has already had an impact on the world's coral reefs, with almost 30% of corals having disappeared since the beginning of the 1980s. Abnormally warm temperatures cause corals to bleach ( lose their brown dinoflagellate symbionts) and, if elevated for long enough, to die. Increasing atmospheric CO2 is also potentially affecting coral reefs by lowering the aragonite saturation state of seawater, making carbonate ions less available for calcification. The synergistic interaction of elevated temperature and CO2 is likely to produce major changes to coral reefs over the next few decades and centuries. Known tolerances of corals to projected changes to sea temperatures indicate that corals are unlikely to remain abundant on reefs and could be rare by the middle of this century if the atmospheric CO2 concentration doubles or triples. The combination of changes to sea temperature and carbonate ion availability could trigger large- scale changes in the biodiversity and function of coral reefs. The ramifications of these changes for the hundred of millions of coral reef - dependent people and industries living in a high- CO2 world have yet to be properly defined. The weight of evidence suggests, however, that projected changes will cause major shifts in the prospects for industries and societies that depend on having healthy coral reefs along their coastlines. Article in Journal/Newspaper ice core The University of Queensland: UQ eSpace Journal of Geophysical Research 110 C9
institution Open Polar
collection The University of Queensland: UQ eSpace
op_collection_id ftunivqespace
language English
topic Oceanography
Great-barrier-reef
Co2 Partial-pressure
Calcium-carbonate Saturation
Vostok Ice Core
Climate-change
Ultraviolet-radiation
Elevated-temperature
Fish Communities
Bleaching Event
Stylophora-pistillata
069902 Global Change Biology
spellingShingle Oceanography
Great-barrier-reef
Co2 Partial-pressure
Calcium-carbonate Saturation
Vostok Ice Core
Climate-change
Ultraviolet-radiation
Elevated-temperature
Fish Communities
Bleaching Event
Stylophora-pistillata
069902 Global Change Biology
Hoegh-Guldberg, Ove
Low coral cover in a high-CO2 world
topic_facet Oceanography
Great-barrier-reef
Co2 Partial-pressure
Calcium-carbonate Saturation
Vostok Ice Core
Climate-change
Ultraviolet-radiation
Elevated-temperature
Fish Communities
Bleaching Event
Stylophora-pistillata
069902 Global Change Biology
description Coral reefs generally exist within a relatively narrow band of temperatures, light, and seawater aragonite saturation states. The growth of coral reefs is minimal or nonexistent outside this envelope. Climate change, through its effect on ocean temperature, has already had an impact on the world's coral reefs, with almost 30% of corals having disappeared since the beginning of the 1980s. Abnormally warm temperatures cause corals to bleach ( lose their brown dinoflagellate symbionts) and, if elevated for long enough, to die. Increasing atmospheric CO2 is also potentially affecting coral reefs by lowering the aragonite saturation state of seawater, making carbonate ions less available for calcification. The synergistic interaction of elevated temperature and CO2 is likely to produce major changes to coral reefs over the next few decades and centuries. Known tolerances of corals to projected changes to sea temperatures indicate that corals are unlikely to remain abundant on reefs and could be rare by the middle of this century if the atmospheric CO2 concentration doubles or triples. The combination of changes to sea temperature and carbonate ion availability could trigger large- scale changes in the biodiversity and function of coral reefs. The ramifications of these changes for the hundred of millions of coral reef - dependent people and industries living in a high- CO2 world have yet to be properly defined. The weight of evidence suggests, however, that projected changes will cause major shifts in the prospects for industries and societies that depend on having healthy coral reefs along their coastlines.
format Article in Journal/Newspaper
author Hoegh-Guldberg, Ove
author_facet Hoegh-Guldberg, Ove
author_sort Hoegh-Guldberg, Ove
title Low coral cover in a high-CO2 world
title_short Low coral cover in a high-CO2 world
title_full Low coral cover in a high-CO2 world
title_fullStr Low coral cover in a high-CO2 world
title_full_unstemmed Low coral cover in a high-CO2 world
title_sort low coral cover in a high-co2 world
publisher American Geophysical Union
publishDate 2005
url https://espace.library.uq.edu.au/view/UQ:55716/UQ55716_OA.pdf
https://espace.library.uq.edu.au/view/UQ:55716
genre ice core
genre_facet ice core
op_relation doi:10.1029/2004JC002528
issn:0148-0227
orcid:0000-0001-7510-6713
op_doi https://doi.org/10.1029/2004JC002528
container_title Journal of Geophysical Research
container_volume 110
container_issue C9
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