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Environmental changes from greenhouse earth to icehouse earth through a study of chalk/black shale sequence

Research Project

Project/Area Number 10304039
Research Category

Grant-in-Aid for Scientific Research (A).

Allocation TypeSingle-year Grants
Section一般
Research Field Stratigraphy/Paleontology
Research InstitutionThe University of Tokyo

Principal Investigator

TAIRA Asahiko  Ocean Research Institute, The University of Tokyo Professor, 海洋研究所, 教授 (50112272)

Co-Investigator(Kenkyū-buntansha) MURAYAMA Masashi  Kochi Univ., Marine Core Research Center, Associate Prof., 海洋コアセンター, 助教授 (50261350)
ISHII Teruaki  Ocean Research Institute, The University of Tokyo Associate Prof., 海洋研究所, 助教授 (80111582)
TOKUYAMA Hidekazu  Ocean Research Institute, The University of Tokyo Professor, 海洋研究所, 教授 (10107451)
OKADA Makoto  Ibaragi Univ., Faculty of Scence, Assistant Prof., 理学部, 助手 (00250978)
大河内 直彦  北海道大学, 低温研究所, 助手 (00281832)
阿波根 直一  東京大学, 海洋研究所, COE研究員 (30359161)
Project Period (FY) 1998 – 2000
Project Status Completed (Fiscal Year 2000)
Budget Amount *help
¥20,200,000 (Direct Cost: ¥20,200,000)
Fiscal Year 2000: ¥4,900,000 (Direct Cost: ¥4,900,000)
Fiscal Year 1999: ¥6,000,000 (Direct Cost: ¥6,000,000)
Fiscal Year 1998: ¥9,300,000 (Direct Cost: ¥9,300,000)
KeywordsCretaceous / Chalk / Black Shale / Anoxic Event / Cyanobacteria / Carbon Isotope / Sulfur Isotope / Blue Tide / チヨーク
Research Abstract

A chalk/black shale sequence exposed in the Appenine Mis. in Italy was investigated in order to reveal the basic marine environmental setting in the Cretaceous warm period. Cenomanian/Turonian black shale (Bonalleli horizon) showed the following characteristics.
1. The source of organic matter is bacterial origin (Cyanobacteria and photosynthesic bacteria).
2. Large excursion of sulfur isotope suggests strong ocean stratification with anoxic bottom water. About 30% of total sulfur from the global ocean was fixed as pyrite. The ocean surface had to be highly oligotrophic.
3. Occasional instability of stratified ocean and upwelling caused events of nutrient supply to the surface that caused radiolarian blooming.

Report

(4 results)
  • 2000 Annual Research Report   Final Research Report Summary
  • 1999 Annual Research Report
  • 1998 Annual Research Report
  • Research Products

    (23 results)

All Other

All Publications (23 results)

  • [Publications] 平朝彦: "白亜紀の温暖地球環境"月刊地球. 22(9). 659-662 (2000)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      2000 Final Research Report Summary
  • [Publications] IKEHARA, Minoru: "Variations of terrestrial input and marine productivity in the Southern Ocean (48゜ S) during the last two deglaciations."PALEOCEANOGRAPHY. 15(2). 170-180 (2000)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      2000 Final Research Report Summary
  • [Publications] 村山雅史: "古海洋学における放射性炭素年代測定法とその問題点"月刊地球. 22. 645-650 (2000)

    • Description
      「研究成果報告書概要(和文)」より
    • Related Report
      2000 Final Research Report Summary
  • [Publications] TAIRA,Asahiko: "Cretaceous Warmed Earth's Climate (in Japanese)."EarthMonthly (Chikyu). 22(9). 659-662 (2000)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      2000 Final Research Report Summary
  • [Publications] IKEHARA,Minoru: "Variations of terrestrial input and marine productivity in the Southern Ocean (48°S) during the last two deglaciations."PALEOCEANOGRAPHY. 15(2). 170-180 (2000)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      2000 Final Research Report Summary
  • [Publications] M.Murayama: "Radiocarbon dating in Paleoceanography"Monthly Chikyu. 22. 645-650 (2000)

    • Description
      「研究成果報告書概要(欧文)」より
    • Related Report
      2000 Final Research Report Summary
  • [Publications] 平朝彦: "白亜紀の温暖地球環境"月刊地球. 22(9). 659-662 (2000)

    • Related Report
      2000 Annual Research Report
  • [Publications] IKEHARA,Minoru: "Variations of terrestrial input and marine productivity in the Southern Ocean (48°S)during the last two deglaciations."PALEOCEANOGRAPHY. 15(2). 170-180 (2000)

    • Related Report
      2000 Annual Research Report
  • [Publications] 村山雅史: "古海洋学における放射性炭素年代測定法とその問題点"月刊地球. 22. 645-650 (2000)

    • Related Report
      2000 Annual Research Report
  • [Publications] 平 朝彦: "深海堀削が目指す新しい地球生命科学"科学. 69. 723-728 (1999)

    • Related Report
      1999 Annual Research Report
  • [Publications] Pickering, K. T: "Glacio-eustatic control on deep-marine clastic forearcsedimentation,Pliocene-mid-Pleistonece(c.1180-600 Ka)Kazusa Group SEJapan."Journal of the Geological Society, London. 156. 125-137 (1999)

    • Related Report
      1999 Annual Research Report
  • [Publications] 徳山 英一: "日本周辺海域の地質構造マッピング"地質ニュース. 541. 10 (1999)

    • Related Report
      1999 Annual Research Report
  • [Publications] Tamura Y.: "Primary arc basalts from Daisen Volcano,Japan:equilibrium crystal fractionation versus disequilibrium"Journal of Petrology. 41. 431-448 (1999)

    • Related Report
      1999 Annual Research Report
  • [Publications] Murayama, M.: "10Be Record in Northwest Pacific during the last 140 kyr ; Implications of terrigenous input and paleoproductivity changes"Proceedung of the Intermational workshop on Frontiers in Accelerator Mass Spectrometry, National Institute for Environmental Studies, Tsukuba, Japan. 225-229 (1999)

    • Related Report
      1999 Annual Research Report
  • [Publications] Ohkouchi, N.: "Sulfur isotope records arounds Livello Bonarelli (northern Apennines, Italy) black shale at the Cenomanian-Turonian boundary"Geology. 27. 535-538 (1999)

    • Related Report
      1999 Annual Research Report
  • [Publications] 徳山 英一: "東海沖の海底活断層"東京大学出版会. 350 (1999)

    • Related Report
      1999 Annual Research Report
  • [Publications] Asahiko TAIRA: "Nature and growth rate of the Northern Izu-Bonin (Ogasawara) arc crust and their implications for continental crust formation" The Island Arc. 7. 395-407 (1998)

    • Related Report
      1998 Annual Research Report
  • [Publications] K.T.PICKERING: "Glacio-eustatic control on deep-marine clastic forearc sedimentation.Pliocene-mid-Pleistocene (c.1180-600 ka) Kazusa" Journal of the Geological Society,London. 156. 125-136 (1999)

    • Related Report
      1998 Annual Research Report
  • [Publications] Jin-Oh Park: "Seismic record of tectonic evolution and backarc rifitng in the southern Ryukyu island arc system" Tectonophysics. 294. 21-42 (1998)

    • Related Report
      1998 Annual Research Report
  • [Publications] Ohkouchi,N.: "Depth ranges of alkenone production in the Gentral Pacific Ocean" Global Biogeochemical Cycles. 13(in press). (1999)

    • Related Report
      1998 Annual Research Report
  • [Publications] 大河内直彦: "バイオマーカーによる古海洋環境の復元・太平洋における深海底堆積物を例として-" 地学雑誌. 197. 40-53 (1998)

    • Related Report
      1998 Annual Research Report
  • [Publications] Lund,S.P.: "Geomagnetic field excursions occurred often during the last million years" EOS,transactions,AGU. 79. 178-179 (1998)

    • Related Report
      1998 Annual Research Report
  • [Publications] Sato,T.: "Quatemary geomagnetic field intensity: Constant periodicity or variable period?" Geophys.Res.Lett.25. 2221-2224 (1998)

    • Related Report
      1998 Annual Research Report

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Published: 1998-04-01   Modified: 2016-04-21  

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