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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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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