Saturday, February 19, 2011: 2:30 PM
101 (Washington Convention Center )
Coral reefs are sensitive recorders of past sea-level and environmental change. Their histories can be accurately dated by mass spectrometry to identify the chronology of events that accompanied sea-level change during the last several glacial cycles. With only small corrections, records derived from scientific ocean drilling of atolls and reef terraces can achieve meter accuracy of sea-level history over the last 20,000 years, and perhaps longer.
See more of: Where Ocean Meets Land: Dynamic Shorelines in a Warming World
See more of: Climate Change
See more of: Symposia
See more of: Climate Change
See more of: Symposia