Rchr
J-GLOBAL ID:200901088947994029   Update date: May. 23, 2014

SUTO, Itsuki

ストウ イツキ | SUTO, Itsuki
Affiliation and department:
Homepage URL  (2): http://www.geocities.jp/restingspace2/http://www.geocities.jp/restingspace2/
Research field  (2): Stratigraphy/Paleontology ,  Geology
MISC (43):
Books (10):
  • Diatoms, The Database of Japanese Fossil Type Specimens Described During the 20th Century (Part 3).
    Special Publication of the Palaeontological Society of Japan 2003
  • The Database on Geological Museum Samples (DGEMS)
    http://www.aist.go.jp/RIODB/dform/ 2004
  • Paleoceanographic and tectonic evolution of the central Arctic Ocean. Integrated Ocean Drilling Program Expedition 302 Scientific Prospectus, ACEX Arctic Coring Expedition
    http://www.ecord.org/exp/acex/302SP.pdf 2004
  • Paleoceanographic and tectonic evolution of the central Arctic Ocean 7 August-13 September 2004. Integrated Ocean Drilling Program Expedition 302 Preliminary Report, Arctic Coring Expedition (ACEX)
    http://www.ecord.org/exp/acex/302PR.pdf 2004
  • Proceedings of the Integrated Ocean Drilling Program, 302.
    2006
more...
Lectures and oral presentations  (18):
  • 微化石古生物学が描く藻類進化のダイナミクス
    (日本地球惑星科学連合2011年大会セッション (B-BG21:代表 柏山祐一郎)「光エネルギーを巡る生命システムの進化ダイナミクス」 2011)
  • 珪藻微化石群集解析からみたカンタベリー海盆 (IODP Ex. 317)の鮮新世-更新世の古環境
    (日本地球惑星科学連合2011年大会セッション (M-IS22:代表 沖野 郷子)「地球掘削科学」 2011)
  • Paleoceanography based on Pliocene and Pleistocene diatom floras from the Canterbury Basin (IODP Exp. 317 Hole U1352B)
    (IODP Leg 317, Post Cruise Workshop 2011)
  • Changes in upwelling mechanisms drove the evolution of marine organisms, estimated by three events of genus Chaetoceros
    (3rd Polar Marine Diatom Taxonomy and Ecology Workshop 2011)
  • Middle Eocene diatom resting spores from the central Arctic Basin
    (The 4th Joint Meeting of the Silicofossil and Palynology groups of The Micropalaeontological Society (TMS) 2011)
more...
※ Researcher’s information displayed in J-GLOBAL is based on the information registered in researchmap. For details, see here.

Return to Previous Page