Coral reefs will transition to net dissolving before end of century-Reference-Cited by-同舟云学术

Coral reefs will transition to net dissolving before end of century

Published:2018-02-23 Issue:6378 Volume:359 Page:908-911
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Eyre Bradley D.¹^ORCID,Cyronak Tyler²^ORCID,Drupp Patrick³^ORCID,De Carlo Eric Heinen³,Sachs Julian P.⁴,Andersson Andreas J.²^ORCID

Affiliation:

1. Centre for Coastal Biogeochemistry, School of Environment, Science and Engineering, Southern Cross University, Lismore, NSW 2480, Australia.

2. Scripps Institution of Oceanography, University of California, San Diego, La Jolla, CA 92093-0244, USA.

3. Department of Oceanography, University of Hawaii at Manoa, Honolulu, HI 96822, USA.

4. School of Oceanography, University of Washington, Seattle, WA 98195, USA.

Abstract

Acid reef-flux The uptake of anthropogenic carbon dioxide from the atmosphere is reducing the pH of the oceans. Ocean acidification means that calcium carbonate—the material with which coral reefs are built—will be more difficult for organisms to generate and will dissolve more quickly. Eyre et al. report that some reefs are already experiencing net sediment dissolution. Worryingly, the rates of loss will increase as ocean acidification intensifies. Science , this issue p. 908

Funder

Australian Research Council

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

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