The future of coral reefs in an age of global change

被引:185
作者
Kleypas, JA
Buddemeier, RW
Gattuso, JP
机构
[1] Natl Ctr Atmospher Res, Oceanog Sect, Boulder, CO 80307 USA
[2] Univ Kansas, Kansas Geol Survey, Lawrence, KS 66047 USA
[3] UPMC, ESA 7076, CNRS, Observ Oceanol, F-06234 Villefranche Sur Mer, France
关键词
coral reef; global change; calcium carbonate; saturation state; temperature; CO2;
D O I
10.1007/s005310000125
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
Coral reefs are the only ecosystem that is strongly defined by a geological component - most definitions require that the biological community produces its own build-up of calcium carbonate. In terms of "reef-building," the geological record reveals that coral reefs have flourished over the past few million years, particularly during interglacial periods. Based on our observations of modern-day reefs, which are limited to the past few centuries, we tend to link "coral reef health" to carbonate production; however, reef ecosystems face future global-scale environmental changes that may decrease their reef-building capacity. In contrast to past discussions of the factors which determine reef-building potential by a coral reef community, the essential question that arises from this review is: How important is reef building to a coral reef community?
引用
收藏
页码:426 / 437
页数:12
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