The future of coral reefs in an age of global change

被引:0
|
作者
Joan A. Kleypas
Robert W. Buddemeier
Jean-Pierre Gattuso
机构
[1] Oceanography Section,
[2] National Center for Atmospheric Research,undefined
[3] P.O. Box 3000,undefined
[4] Boulder,undefined
[5] CO 80307,undefined
[6] Kansas Geological Survey,undefined
[7] University of Kansas,undefined
[8] Lawrence,undefined
[9] KS 66047,undefined
[10] Observatoire Océanologique,undefined
[11] ESA 7076 CNRS-UPMC,undefined
[12] B.P. 28,undefined
[13] 06234 Villefranche-sur-mer Cedex,undefined
关键词
Coral reef Global change Calcium carbonate Saturation state Temperature CO2;
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中图分类号
学科分类号
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?
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页码:426 / 437
页数:11
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