[E] Poster
B (Biogeosciences ) » B-PT Paleontology
convener:Takashi Toyofuku(Japan Agency for Marine-Earth Science and Technology (JAMSTEC)), Jelle Bijma(Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung), Hiroshi Kitazato(Tokyo University of Marine Science and Technology (TUMSAT)), Kotaro Hirose(Faculty of Science and Engineering, Waseda University)
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.
Riki Miyai1, Hideki Takami2, Daisuke Muraoka2, Atsushi Suzuki3, Yukihiro Nojiri4, *Mayuri Inoue1 (1.Department of Earth Sciences, Okayama University, 2.Tohoku National Fisheries Research Institute, 3.Geological Survey of Japan, AIST, 4.Faculty of Science and Technology, Hirosaki University)
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*Sumika Yoneto1, Kotaro Hirose1, Hideo Yamazaki2, Kazuo Kamura1 (1.Faculty of creative science and engineering of the department of resources and environmental engineering, Waseda University, 2.Department of Life Science, School of Science and Engineering, Kindai University)
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*Doi Nobuhiro1, Koji Kameo2 (1.Division of Earth and Environmental Sciences, School of Science and Engineering, Chiba University, 2.Department of Earth Sciences, Faculty of Sciences, Chiba University)
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*Yukiko Kozaka1, Katsuyoshi Michibayashi2, Yui Kouketsu2, Yuki Tokuda3, Hiroshi Sato4 (1.Institute for Space-Earth Environmental Research, Nagoya University, 2.Department of Earth & Planetary Sciences, Graduate School of Environmental Studies, Nagoya University, 3.Faculty of Environmental Studies, Tottori University of Environmental Studies, 4.School of Business Administration, Senshu University)
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*Megumi Saito-Kato1, Yukiko Nagai1,2, Hayato Yokoyama3 (1.Department of Geology and Paleontology, National Museum of Nature and Science, 2.Japan Agency for Marine-Earth Science and Technology, 3.RC Gear)
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*Yukiko Nagai1,2, Remi Tsubaki3, Nanami Kishigami2, Takashi Toyofuku2,4 (1.National Museum of Nature and Science of Tokyo, 2.Japan Agency for Marine-earth Science and Technology , 3.The University Museum, The University of Tokyo, 4.Tokyo University of Marine Science and Technology)
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*Hiroshi Kitazato1 (1.Tokyo University of Marine Science and Technology (TUMSAT))
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*Kana Fujimori1, Hirotaka Nishino1, Tasuku Akagi1 (1.Department of Earth and Planetary Sciences, Faculty of Sciences, Kyushu University)
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