A Review of Paleoenvironmental Reconstructions Based on Mg/Ca and Sr/Ca Thermometry in Goral Skeletons

  • Asami Ryuji
    Institute of Geology and Paleontology, Graduate School of Science, Tohoku University
  • Yamada Tsutomu
    Institute of Geology and Paleontology, Graduate School of Science, Tohoku University
  • Iryu Yasufumi
    Institute of Geology and Paleontology, Graduate School of Science, Tohoku University

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  • サンゴ骨格のMg/Ca比,Sr/Ca比を用いた古水温復元法の現状と問題点
  • サンゴ コッカク ノ Mg Caヒ Sr Caヒ オ モチイタ コ スイオン フクゲンホウ ノ ゲンジョウ ト モンダイテン

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Abstract

Reconstruction of changes in the tropical ocean-atmosphere system in the period prior to the use of instrumental records requires the use of climatic and oceanographic proxies such as corals and tree rings. The elemental ratios (Mg/Ca and Sr/Ca) in massive coral skeletons have been used to calculate high-resolution (weekly to monthly) SST (sea surface temperature) in tropical and subtropical oceans during the Quaternary period because there exist significant relationships between the ratios and SST. However, some investigations indicate that skeletal Mg/Ca and Sr/Ca may be influenced by seawater Mg2+/Ca2+ and Sr2+/Ca2+ variations, vital effects, heterogeneity effects, submarine and meteoric diagenesis, and various chemical treatments. If these influences are evaluated quantitatively, the Mg/Ca and Sr/Ca thermometers will provide more accurate past SST than at present.

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