岩手山南東麓春子谷地湿原の花粉分析からみた約13,000年前以降の植生変遷と気候変化

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タイトル別名
  • Vegetation and Climate Changes since ca. 13,000 cal yrs BP Based on Pollen Analysis in Harukoyachi Mire, Iwate Prefecture, Northeast Japan
  • イワテサン ナントウロク ハルコヤチ シツゲン ノ カフン ブンセキ カラ ミタ ヤク 13000ネンマエ イコウ ノ ショクセイ ヘンセン ト キコウ ヘンカ

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We performed pollen and tephra analyses and radiocarbon dating measurement on sedimentary drilling cores in Harukoyachi Mire (460m a. s. l.), Iwate Prefecture, northeast Japan. These cores included Akitakomagatake-Yanagisawa pumice, Akitakomagatake-Horikiri pumice, Towada-a volcanic ash, and Iwate-Kariya scoria. The local vegetation changes around the site since ca. 13, 000cal yrs BP were reconstructed as follows: Betula forest mixed with cool temperate broad-leaved forest in ca. 13.4-13.0ka; transitional forest from Betula forest to cool temperate broad-leaved forest in ca. 13.0-10.5ka; cool temperate broad-leaved forest composed mainly of Quercus subgen. Lepidobalanus in ca. 10.5-1.4ka; cool temperate broad-leaved forest and Cryptomeria japonica forest in ca. 1.4-0.2ka; and Pinus densiflora secondary forest and Cryptomeria japonica plantation forest in ca. 0.2ka-present. These vegetation changes indicate that the climate in this region was cool in ca. 13.0ka, followed by an abrupt increase in temperature during ca.13.0-10.5ka, and finally warm similar to the present.

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  • 地理学評論

    地理学評論 81 (4), 228-237, 2008

    公益社団法人 日本地理学会

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