2012-07-24 15:49:12.0 [mpmorahan] insert Definition (id: null text: Corals are generally members of the order Scleractinia, which have hard calcerous skeletons supporting softer tissues. For paleoclimatic studies, the important coral subgroup is the reef-building, massive corals known as hermatypic corals. Coral growth rates vary and are sensitive to sea surface temperatures (SSTs). Dating coral growth has shown high correspondence between large excursions of oxygen-18 (del18O) and El Nino Southern Oscillation (ENSO) events. Coral growth studies have led to new information about paleo-SSTs, rainfall, river runoff, ocean circulation, and tropical wind systems. language code: en);
2012-07-24 15:34:44.0 [mpmorahan] Move Concepts delete broader relation (null); add broader relation (CORAL DEPOSITS [47d6c670-db83-4975-b684-1be787811ac8,40031] - OCEAN/LAKE RECORDS [5237fae3-c98e-4d4a-9013-d7c824b3862b,40027]);
2012-07-24 15:34:30.0 [mpmorahan] Move Concepts add broader relation (CORAL DEPOSITS [47d6c670-db83-4975-b684-1be787811ac8,40031] - BOREHOLES [8f8c1808-ac5f-43e5-8397-dbb3d171144c,40029]); delete broader relation (null);
CORAL DEPOSITS
Corals are generally members of the order Scleractinia, which have hard calcerous skeletons supporting softer tissues. For paleoclimatic studies, the important coral subgroup is the reef-building, massive corals known as hermatypic corals. Coral growth rates vary and are sensitive to sea surface temperatures (SSTs). Dating coral growth has shown high correspondence between large excursions of oxygen-18 (del18O) and El Nino Southern Oscillation (ENSO) events. Coral growth studies have led to new information about paleo-SSTs, rainfall, river runoff, ocean circulation, and tropical wind systems.
OCEAN/LAKE RECORDS