セッション概要
 
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ID B-PT03
タイトル 和文 Biomineralization and the Geochemistry of Proxies -Field ecology, Laboratory culture and Paleo
英文 Biomineralization and the Geochemistry of Proxies -Field ecology, Laboratory culture and Paleo
タイトル短縮名 和文 Biocalcification and Proxies
英文 Biocalcification and Proxies
代表コンビーナ 氏名 和文 豊福 高志
英文 Takashi Toyofuku
所属 和文 独立行政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 北里 洋
英文 Hiroshi Kitazato
所属 和文 独立行政法人海洋研究開発機構海洋・極限環境生物圏領域
英文 Institute of Biogeosciences (BioGeos),Japan Agency for Marine-Earth Science and Technology (JAMSTEC)
共同コンビーナ 2 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 fur Polar- und Meeresforschung
共同コンビーナ 3 氏名 和文 Simon Redfern
英文 Simon Redfern
所属 和文 University of Cambridge
英文 University of Cambridge
国際セッション開催希望 国際セッションとしての開催を希望する
発表主要言語 英語
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 maybe 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 biocalcification mechanisms and the incorporation of proxy signals.
In this session we failitate contributions related to the biocalcification, 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 maybe 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 biocalcification mechanisms and the incorporation of proxy signals.
In this session we failitate contributions related to the biocalcification, calibration and validation of marine proxies from field study, laboratory culture experiment and paleo environmental reconstruction.
発表方法希望 口頭および(または)ポスターセッション
招待講演