PP011
Development and Application of Coral Proxies for Ocean Change
Development and Application of Coral Proxies for Ocean Change
Session ID#: 77637
Session Description:
Corals open an exceptional window into ocean climate and biogeochemical change, from its deepest interior to its sunlit surface, on timescales ranging from the Paleozoic to the present. Coral skeletons grow in rhythmic structural patterns and can be accurately dated using radiometric methods, providing unmatched temporal resolution and chronometric constraint. Traditional isotope and element:calcium coral-based proxies have been widely applied to reconstruct ocean temperature, salinity and circulation. Now, creative new approaches are mining the organic and inorganic components of corals and gorgonians for novel information about the inner workings of the global oceans. In parallel, an improved understanding of the processes governing biomineralization, as well as the application of proxy system models, are bringing new perspectives to coral proxies. This session welcomes submissions from field, laboratory, theoretical and modeling studies that develop and apply both traditional and novel coral-based proxies to enhance understanding of ocean change on all timescales.
Co-Organized:
- OS - Ocean Sciences
Index Terms:
1635 Oceans [GLOBAL CHANGE]
4220 Coral reef systems [OCEANOGRAPHY: GENERAL]
4825 Geochemistry [OCEANOGRAPHY: CHEMICAL]
4916 Corals [PALEOCEANOGRAPHY]
Primary Convener: Xingchen Tony Wang, California Institute of Technology, Pasadena, CA, United States
Conveners: Anne L Cohen, Woods Hole Oceanographic Inst, Woods Hole, MA, United States and Anne M Gothmann, St. Olaf College, Environmental Studies and Physics, Northfield, MN, United States
Primary Liaison: Xingchen Tony Wang, California Institute of Technology, Pasadena, CA, United States
See more of: Paleoceanography and Paleoclimatology
