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Open AccessJournal ArticleDOI

Coral Reef Ecosystems under Climate Change and Ocean Acidification

TLDR
In this article, it was shown that even lower greenhouse gas emission scenarios (such as Representative Concentration Pathway RCP 4.5) are likely to drive the elimination of most warm-water coral reefs by 2040-2050.
Abstract
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 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 2000 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.

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Impacts of 1.5°C Global Warming on Natural and Human Systems

Ove Hoegh-Guldberg, +86 more
TL;DR: In this article, the authors present a survey of women's sportswriters in South Africa and Ivory Coast, including: Marco Bindi (Italy), Sally Brown (UK), Ines Camilloni (Argentina), Arona Diedhiou (Ivory Coast/Senegal), Riyanti Djalante (Japan/Indonesia), Kristie L. Ebi (USA), Francois Engelbrecht (South Africa), Joel Guiot (France), Yasuaki Hijioka (Japan), Shagun Mehrotra (USA/India), Ant
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Climate Change, Human Impacts, and Coastal Ecosystems in the Anthropocene

TL;DR: It is underscores that an enhanced understanding of interactions between climate change and local human impacts is of profound importance to improving predictions of climate change impacts, devising climate-smart conservation actions, and helping enhance adaption of coastal societies to climate change in the Anthropocene.
Journal Article

Mixed responses of tropical Pacific fisheries and aquaculture to climate change : supplementary material

TL;DR: In this paper, the authors report how changes to the atmosphere-ocean are likely to affect the food webs, habitats and stocks underpinning fisheries and aquaculture across the region.
Journal ArticleDOI

The Globalization of Cultural Eutrophication in the Coastal Ocean: Causes and Consequences

TL;DR: In this paper, the authors compared six contrasting coastal ecosystems that are subjected to a range of riverine inputs of freshwater (buoyancy) and nutrients to address impacts of anthropogenic nutrient inputs on ecosystem services; how ecosystem traits minimize or amplify these impacts; synergies among pressures (nutrient enrichment, over fishing, coastal development, and climate-driven pressures in particular); and management of nutrient inputs to coastal ecosystems.
References
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Journal ArticleDOI

Global analyses of sea surface temperature, sea ice, and night marine air temperature since the late nineteenth century

TL;DR: HadISST1 as mentioned in this paper replaces the global sea ice and sea surface temperature (GISST) data sets and is a unique combination of monthly globally complete fields of SST and sea ice concentration on a 1° latitude-longitude grid from 1871.

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

TL;DR: The recent completion of drilling at Vostok station in East Antarctica has allowed the extension of the ice record of atmospheric composition and climate to the past four glacial-interglacial cycles.
Journal ArticleDOI

Climate and atmospheric history of the past 420,000 years from the Vostok ice core, Antarctica

TL;DR: The recent completion of drilling at Vostok station in East Antarctica has allowed the extension of the ice record of atmospheric composition and climate to the past four glacial-interglacial cycles as discussed by the authors.
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