Coral Reef Ecosystems under Climate Change and Ocean Acidification

Coral reefs are found in a wide range of environments, where they provide food and habitat to a large range of organisms as well as providing many other ecological goods and services. Warm-water coral reefs, for example, occupy shallow sunlit, warm, and alkaline waters in order to grow and calcify a...

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Main Authors: Ove Hoegh-Guldberg, Elvira S. Poloczanska, William Skirving, Sophie Dove
Format: Article
Language:English
Published: Frontiers Media S.A. 2017-05-01
Series:Frontiers in Marine Science
Subjects:
Online Access:http://journal.frontiersin.org/article/10.3389/fmars.2017.00158/full
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spelling doaj-1025404569b244cdafef9c4637a3b6fa2020-11-25T00:21:29ZengFrontiers Media S.A.Frontiers in Marine Science2296-77452017-05-01410.3389/fmars.2017.00158252954Coral Reef Ecosystems under Climate Change and Ocean AcidificationOve Hoegh-Guldberg0Ove Hoegh-Guldberg1Ove Hoegh-Guldberg2Elvira S. Poloczanska3Elvira S. Poloczanska4William Skirving5Sophie Dove6Sophie Dove7The Global Change Institute, The University of QueenslandSt Lucia, QLD, AustraliaARC Centre for Excellence in Coral Reef Studies, The University of QueenslandSt Lucia, QLD, AustraliaSchool of Biological Sciences, The University of QueenslandSt Lucia, QLD, AustraliaThe Global Change Institute, The University of QueenslandSt Lucia, QLD, AustraliaCSIRO Oceans and Atmosphere, Queensland Biosciences PrecinctSt Lucia, QLD, AustraliaCoral Reef Watch, National Oceanic and Atmospheric Administration (NOAA)College Park, MD, United StatesARC Centre for Excellence in Coral Reef Studies, The University of QueenslandSt Lucia, QLD, AustraliaSchool of Biological Sciences, The University of QueenslandSt Lucia, QLD, AustraliaCoral reefs are found in a wide range of environments, where they provide food and habitat to a large range of organisms as well as providing many other ecological goods and services. Warm-water coral reefs, for example, occupy shallow sunlit, warm, and alkaline waters in order to grow and calcify at the high rates necessary to build and maintain their calcium carbonate structures. At deeper locations (40–150 m), “mesophotic” (low light) coral reefs accumulate calcium carbonate at much lower rates (if at all in some cases) yet remain important as habitat for a wide range of organisms, including those important for fisheries. Finally, even deeper, down to 2,000 m or more, the so-called “cold-water” coral reefs are found in the dark depths. Despite their importance, coral reefs are facing significant challenges from human activities including pollution, over-harvesting, physical destruction, and climate change. In the latter case, even lower greenhouse gas emission scenarios (such as Representative Concentration Pathway RCP 4.5) are likely drive the elimination of most warm-water coral reefs by 2040–2050. Cold-water corals are also threatened by warming temperatures and ocean acidification although evidence of the direct effect of climate change is less clear. Evidence that coral reefs can adapt at rates which are sufficient for them to keep up with rapid ocean warming and acidification is minimal, especially given that corals are long-lived and hence have slow rates of evolution. Conclusions that coral reefs will migrate to higher latitudes as they warm are equally unfounded, with the observations of tropical species appearing at high latitudes “necessary but not sufficient” evidence that entire coral reef ecosystems are shifting. On the contrary, coral reefs are likely to degrade rapidly over the next 20 years, presenting fundamental challenges for the 500 million people who derive food, income, coastal protection, and a range of other services from coral reefs. Unless rapid advances to the goals of the Paris Climate Change Agreement occur over the next decade, hundreds of millions of people are likely to face increasing amounts of poverty and social disruption, and, in some cases, regional insecurity.http://journal.frontiersin.org/article/10.3389/fmars.2017.00158/fullcoralsclimate changeecosystems goods and servicesdeclinewarming oceanocean acidification
collection DOAJ
language English
format Article
sources DOAJ
author Ove Hoegh-Guldberg
Ove Hoegh-Guldberg
Ove Hoegh-Guldberg
Elvira S. Poloczanska
Elvira S. Poloczanska
William Skirving
Sophie Dove
Sophie Dove
spellingShingle Ove Hoegh-Guldberg
Ove Hoegh-Guldberg
Ove Hoegh-Guldberg
Elvira S. Poloczanska
Elvira S. Poloczanska
William Skirving
Sophie Dove
Sophie Dove
Coral Reef Ecosystems under Climate Change and Ocean Acidification
Frontiers in Marine Science
corals
climate change
ecosystems goods and services
decline
warming ocean
ocean acidification
author_facet Ove Hoegh-Guldberg
Ove Hoegh-Guldberg
Ove Hoegh-Guldberg
Elvira S. Poloczanska
Elvira S. Poloczanska
William Skirving
Sophie Dove
Sophie Dove
author_sort Ove Hoegh-Guldberg
title Coral Reef Ecosystems under Climate Change and Ocean Acidification
title_short Coral Reef Ecosystems under Climate Change and Ocean Acidification
title_full Coral Reef Ecosystems under Climate Change and Ocean Acidification
title_fullStr Coral Reef Ecosystems under Climate Change and Ocean Acidification
title_full_unstemmed Coral Reef Ecosystems under Climate Change and Ocean Acidification
title_sort coral reef ecosystems under climate change and ocean acidification
publisher Frontiers Media S.A.
series Frontiers in Marine Science
issn 2296-7745
publishDate 2017-05-01
description Coral reefs are found in a wide range of environments, where they provide food and habitat to a large range of organisms as well as providing many other ecological goods and services. Warm-water coral reefs, for example, occupy shallow sunlit, warm, and alkaline waters in order to grow and calcify at the high rates necessary to build and maintain their calcium carbonate structures. At deeper locations (40–150 m), “mesophotic” (low light) coral reefs accumulate calcium carbonate at much lower rates (if at all in some cases) yet remain important as habitat for a wide range of organisms, including those important for fisheries. Finally, even deeper, down to 2,000 m or more, the so-called “cold-water” coral reefs are found in the dark depths. Despite their importance, coral reefs are facing significant challenges from human activities including pollution, over-harvesting, physical destruction, and climate change. In the latter case, even lower greenhouse gas emission scenarios (such as Representative Concentration Pathway RCP 4.5) are likely drive the elimination of most warm-water coral reefs by 2040–2050. Cold-water corals are also threatened by warming temperatures and ocean acidification although evidence of the direct effect of climate change is less clear. Evidence that coral reefs can adapt at rates which are sufficient for them to keep up with rapid ocean warming and acidification is minimal, especially given that corals are long-lived and hence have slow rates of evolution. Conclusions that coral reefs will migrate to higher latitudes as they warm are equally unfounded, with the observations of tropical species appearing at high latitudes “necessary but not sufficient” evidence that entire coral reef ecosystems are shifting. On the contrary, coral reefs are likely to degrade rapidly over the next 20 years, presenting fundamental challenges for the 500 million people who derive food, income, coastal protection, and a range of other services from coral reefs. Unless rapid advances to the goals of the Paris Climate Change Agreement occur over the next decade, hundreds of millions of people are likely to face increasing amounts of poverty and social disruption, and, in some cases, regional insecurity.
topic corals
climate change
ecosystems goods and services
decline
warming ocean
ocean acidification
url http://journal.frontiersin.org/article/10.3389/fmars.2017.00158/full
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