後期第四紀における海洋での炭酸カルシウムの堆積変動史 –炭酸カルシウムの溶解変動–  [in Japanese] Carbonate preservation and climatic change during late quaternary –Fluctuation of carbonate dissolution–  [in Japanese]

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Author(s)

Abstract

Carbonate has played an important role on global carbon cycle. The fossil carbonate component of deep-sea sediments provides much of our knowledge of its fluctuation as well as paleoclimatic change. The compiled data on the distribution, preservation, and accumulation of carbonate on the seafloor indicate that depth of sedimentary lysocline has fluctuated markedly in conjunction with late Quaternary climate cycles and that carbonate sedimentation is much affected by the fluctuation of the abyssal carbonate ion concentration. Also it is suggested that the fluctuations of the dissolution are largely controlled by changes in the global mass balance of carbonate and ocean circulation, which have a close relationship with climatic conditions.

Journal

  • Chikyukagaku

    Chikyukagaku 28(2), 123-142, 1994

    The Geochemical Society of Japan

Cited by:  3

Codes

  • NII Article ID (NAID)
    110008679894
  • NII NACSIS-CAT ID (NCID)
    AN00141280
  • Text Lang
    JPN
  • Article Type
    Journal Article
  • ISSN
    0386-4073
  • NDL Article ID
    3889427
  • NDL Source Classification
    ME61(地質・地史)
  • NDL Source Classification
    ZM41(科学技術--地球科学)
  • NDL Call No.
    Z15-645
  • Data Source
    CJPref  NDL  NII-ELS  J-STAGE 
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