Ocean acidification accelerates dissolution of experimental coral reef communities

Ocean acidification (OA) poses a severe threat to tropical coral reefs, yet much of what is know about these effects comes from individual corals and algae incubated in isolation under high p CO 2 . Studies of similar effects on coral reef communities are scarce. To investigate the response of coral...

Full description

Bibliographic Details
Published in:Biogeosciences
Main Authors: S. Comeau, R. C. Carpenter, C. A. Lantz, P. J. Edmunds
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2015
Subjects:
Online Access:https://doi.org/10.5194/bg-12-365-2015
https://doaj.org/article/425e1c0236b34c7d95249971746c7df1
Description
Summary:Ocean acidification (OA) poses a severe threat to tropical coral reefs, yet much of what is know about these effects comes from individual corals and algae incubated in isolation under high p CO 2 . Studies of similar effects on coral reef communities are scarce. To investigate the response of coral reef communities to OA, we used large outdoor flumes in which communities composed of calcified algae, corals, and sediment were combined to match the percentage cover of benthic communities in the shallow back reef of Moorea, French Polynesia. Reef communities in the flumes were exposed to ambient (~ 400 μatm) and high p CO 2 (~ 1300 μatm) for 8 weeks, and calcification rates measured for the constructed communities including the sediments. Community calcification was reduced by 59% under high p CO 2 , with sediment dissolution explaining ~ 50% of this decrease; net calcification of corals and calcified algae remained positive but was reduced by 29% under elevated p CO 2 . These results show that, despite the capacity of coral reef calcifiers to maintain positive net accretion of calcium carbonate under OA conditions, reef communities might transition to net dissolution as p CO 2 increases, particularly at night, due to enhanced sediment dissolution.