Habitat and distribution changes of Picea and Larix in central Honshu since the Last Glacial
Habitat and distribution changes of Picea and Larix in central Honshu since the Last Glacial
批准号:
10680097
负责人:
OKITSU Susumu
金额:
$0.64万
依托单位:
依托单位国家:
日本
项目类别:
Grant-in-Aid for Scientific Research (C)
财政年份:
1998
资助国家:
日本
项目状态:
已结题
起止时间:
1998 至 2000
中文摘要
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英文摘要
We clarified vertical distribution, temperature, snowdepth, and geography of the habitat of Picea and Larix in central Honshu and Northeastern Asia based on literatures and fieldworks in the areas where those taxa were distributed much. Especially, we studied microtopography and ground conditions of the habitat where those taxa grew and regenerated. We obtained the following results as for the process of distribution changes of Picea and Larix trees since the Last Glacial : 1) The vertical distributions of Picea and Larix trees in mountain areas in central Honshu are generally intervened between subalpine coniferous forest mainly composed by Abies and Tsuga trees and montane deciduous broadleaved forest mainly composed by Fagus crenata and Quercus crispula. 2) Distributions of Picea and Larix trees concentrate in mountains of less snowfall and in temperature ranges between montane and subalpine zone. 3) The site of their growth and regeneration concentrates on rocky place, scraggy ridges, and landslide areas along valley where growth of the other tree species are difficult. 4) Under the cooler and drier condition without disterbance in the Last Glacial stage, Picea and Larix trees dominated over central Honshu. Through warming and heavier snowfall with frequent disterbance in the Late Glacial stages, distribution of Abies and Tsuga trees with deciduous broad-leaved trees expanded and Picea and Larix trees have decreased their distribution into their recent habitat. 5) Picea trees were widely distributed and variation of their cone morphology were continuous in central Japan in the Last Glacial. Since the Late Glacial stage to recent, they were divided into small populations in the middle of mountain where some species and subspecies were formed.
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野手啓行,沖津進,百原新: "日本のトウヒ属バラモミ節樹木の現在の分布と最終氷期以来の分布変遷"植生史研究. 6. 3-13 (1998)
Hiroyuki Note、Susumu Okitsu 和 Arata Momohara:“日本云杉树的当前分布以及自最后一个冰河时代以来分布的变化”植被历史研究。 6. 3-13 (1998)。
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沖津進: "大雪山上部に分布する植物群落の植生地理学的位置づけ"Actinia. 12. 103-112 (1999)
Susumu Okitsu:“分布在大雪山上部的植物群落的生理定位”Actinia。 12. 103-112 (1999)
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沖津進: "サハリン最北端シュミット半島に分布するエゾマツ,グイマツの共存条件とそれから推定される最終氷期の北海道における両種の共存状態"植生史研究. 7. 3-10 (1999)
Susumu Okitsu:“分布在萨哈林岛最北端施密特半岛的苏格兰云杉和松树云杉的共存条件,以及末次冰河时期北海道这两个物种的共存状况”,《植被历史研究》7. 3-。 10 (1999)
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Note, H., Okitsu, S., and Momohara, A.: "Present distribution of Picea sect. Picea Farjon and distribution changes since the Last Glacial Age in Japan."Japanese Journal of Historical Botany. 6. 3-13 (1998)
注:H.、Okitsu, S. 和 Momohara, A.:“Picea sect. Picea Farjon 的当前分布以及日本末次冰期以来的分布变化。”《日本历史植物学杂志》。
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沖津進: "北東アジアの沿岸地域における森林分布と境界の決定機構"生態環境研究. 6. 143-145 (1999)
Susumu Okitsu:“东北亚沿海地区森林分布和边界的确定机制”《生态环境研究》6. 143-145 (1999)。
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共 35 条
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