Abstract
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 "reefs-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.
| Original language | English |
|---|---|
| Pages (from-to) | 426-437 |
| Number of pages | 12 |
| Journal | International Journal of Earth Sciences |
| Volume | 90 |
| Issue number | 2 |
| DOIs | |
| State | Published - 2001 |
Keywords
- Calcium carbonate
- CO
- Coral reef
- Global change
- Saturation state
- Temperature