Hidden impacts of ocean acidification to live and dead coral framework

被引:103
|
作者
Hennige, S. J. [1 ]
Wicks, L. C. [1 ]
Kamenos, N. A. [2 ]
Perna, G. [2 ]
Findlay, H. S. [3 ]
Roberts, J. M. [1 ,4 ,5 ]
机构
[1] Heriot Watt Univ, Ctr Marine Biodivers & Biotechnol, Edinburgh EH14 4AS, Midlothian, Scotland
[2] Univ Glasgow, Sch Geog & Earth Sci, Glasgow G12 8QQ, Lanark, Scotland
[3] Plymouth Marine Lab, Plymouth PL1 3DH, Devon, England
[4] Univ N Carolina, Dept Biol Sci, Wilmington, NC 28403 USA
[5] Scottish Assoc Marine Sci, Oban PA37 1QA, Argyll, Scotland
基金
英国自然环境研究理事会;
关键词
ocean acidification; cold-water corals; climate change; biomineralization; calcification; Lophelia pertusa; COLD-WATER CORALS; LOPHELIA-PERTUSA; CARBON-DIOXIDE; CALCIFICATION; SEAWATER; DEEP; REEFS; SCLERACTINIA; DISSOCIATION; DISSOLUTION;
D O I
10.1098/rspb.2015.0990
中图分类号
Q [生物科学];
学科分类号
07 ; 0710 ; 09 ;
摘要
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 CO2, 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 CO2 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.
引用
收藏
页数:10
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