地球生命科学(B)
セッション小記号古生物学・古生態学(PT)
セッションIDB-PT04
タイトル和文Biomineralization and Geochemistry of Proxies
英文Biomineralization and Geochemistry of Proxies
タイトル短縮名和文Biomineralization and Geochemistry
英文Biomineralization and Geochemistry
代表コンビーナ氏名和文豊福 高志
英文Takashi Toyofuku
所属和文国立研究開発法人海洋研究開発機構
英文Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
共同コンビーナ 1氏名和文Bijma Jelle
英文Jelle Bijma
所属和文アルフレッドウェゲナー極域海洋研究所
英文Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
共同コンビーナ 2氏名和文北里 洋
英文Hiroshi Kitazato
所属和文国立大学法人東京海洋大学
英文Tokyo University of Marine Science and Technology (TUMSAT)
共同コンビーナ 3氏名和文廣瀬 孝太郎
英文Kotaro Hirose
所属和文早稲田大学  大学院創造理工学研究科 地球・環境資源理工学専攻
英文Faculty of Science & Engineering, Waseda University
発表言語E
スコープ和文In order to reconstruct the Earth climate system, marine paleoclimatologists resort to transfer functions or geochemical proxies, which are produced or affected by organisms. The relationships used for reconstructions are generally based on field calibrations or derived from laboratory experiments. The danger of these so-called empirical relationships is that they may be valid only within the restricted parameter space of their calibration. Application of proxy relationships to very different environmental settings (e.g. high vs. low latitude or glacial vs. interglacial) requires a mechanistic understanding of these relationships. Much progress can be expected by a better understanding of the biomineralization mechanisms and the incorporation of proxy signals.
In this session we facilitate contributions related to the biomineralization, calibration and validation of marine proxies from field study, laboratory culture experiment and paleo-environmental reconstruction.
英文In order to reconstruct the Earth climate system, marine paleoclimatologists resort to transfer functions or geochemical proxies, which are produced or affected by organisms. The relationships used for reconstructions are generally based on field calibrations or derived from laboratory experiments. The danger of these so-called empirical relationships is that they may be valid only within the restricted parameter space of their calibration. Application of proxy relationships to very different environmental settings (e.g. high vs. low latitude or glacial vs. interglacial) requires a mechanistic understanding of these relationships. Much progress can be expected by a better understanding of the biomineralization mechanisms and the incorporation of proxy signals.
In this session we facilitate contributions related to the biomineralization, calibration and validation of marine proxies from field study, laboratory culture experiment and paleo-environmental reconstruction.
発表方法口頭および(または)ポスターセッション
ジョイントセッションEGU