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Hidden impacts of ocean acidification to live and dead coral framework
Author(s) -
Sebastian Hennige,
Laura C. Wicks,
Nicholas A. Kamenos,
Gabriela Perna,
Helen S. Findlay,
J. Murray Roberts
Publication year - 2015
Publication title -
proceedings of the royal society b biological sciences
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.342
H-Index - 253
eISSN - 1471-2954
pISSN - 0962-8452
DOI - 10.1098/rspb.2015.0990
Subject(s) - bioerosion , ocean acidification , coral reef , reef , biodiversity , ecology , marine biodiversity , ecosystem , coral , acclimatization , key (lock) , habitat , climate change , marine ecosystem , biology , oceanography , geology
Cold-water corals, such as Lophelia pertusa , are key habitat-forming organisms found throughout the world's oceans to 3000 m deep. The complex three-dimensional framework made by these vulnerable marine ecosystems support high biodiversity and commercially important species. Given their importance, a key question is how both the living and the dead framework will fare under projected climate change. Here, we demonstrate that over 12 months L. pertusa can physiologically acclimate to increased CO 2 , showing sustained net calcification. However, their new skeletal structure changes and exhibits decreased crystallographic and molecular-scale bonding organization. Although physiological acclimatization was evident, we also demonstrate that there is a negative correlation between increasing CO 2 levels and breaking strength of exposed framework (approx. 20–30% weaker after 12 months), meaning the exposed bases of reefs will be less effective ‘load-bearers’, and will become more susceptible to bioerosion and mechanical damage by 2100.

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