過去数百年間の古気候・古海洋変動を記録する現生サンゴ : 数年〜数十年スケールの変動と長期変動の復元(<特集>炭酸塩の地球化学)

概要

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Massive hermatypic corals are one of the most excellent archives for reconstructing paleoclimatic and paleoceanographic changes because they commonly live in shallow tropical and subtropical oceans, grow at a rapid rate, and contain a remarkable array of geochemical tracers within their skeletons. In particular, oxygen isotopic composition and Sr/Ca ratio of coral skeletons have been used as proxies for past thermal and hydrological variations in sea surface conditions. Recent investigations on geochemical records of modern long coral cores provide continuous time series of sea surface temperature and salinity in many tropical regions, which document climatic variability on interannual and decadal to multidecadal timescales (El Nino/ Southern Oscillation, Indian Ocean Dipole mode, and Inter-decadal Pacific Oscillation), volcanic eruptions, and global warming. However, high-resolution paleoclimatic records of coral skeletons over the last several centuries are spatially limited and the mechanisms causing the climatic variability remain unclear at present. High-fidelity paleoclimatology should be progressed in order to expand our knowledge on the nature and causes of global climatic changes.
日本地球化学会の論文
2006-08-25