根室半島における後期更新世以降の植生変遷 Vegetation history in Nemuro Peninsula since the Late Pleistocene.

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Pollen analysis of deposits from Ochiishi Mire was made with special references to the vegetation history of Nemuro Peninsula in easternmost Hokkaido since the Late Pleistocene. A landscape consisting of grassland and birch forest was seen around this area ca. 11500 years ago. Thereafter, conifers such as spruce, fir and larch began to invade and formed boreal forests. These coniferous forests, excluding larch, continuously occupied this area until ca. 6000 years ago. Though the coniferous forests deteriorated due to climatic warming, cool temperate deciduous forest has not fully developed in this area yet. The cool temperate oak forest slightly decreased and boreal birch forest developed in the peninsula ca. 2500 years ago.

収録刊行物

  • 植生学会誌

    植生学会誌 18(1), 39-44, 2001

    植生学会

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各種コード

  • NII論文ID(NAID)
    110008145247
  • NII書誌ID(NCID)
    AA11347548
  • 本文言語コード
    JPN
  • 資料種別
    SHO
  • ISSN
    13422448
  • NDL 記事登録ID
    6382784
  • NDL 雑誌分類
    ZR3(科学技術--生物学--植物) // ZU4(書誌・図書館・一般年鑑--専門書誌)
  • NDL 請求記号
    Z18-3499
  • データ提供元
    CJP書誌  NDL  NII-ELS  J-STAGE 
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