京都市八丁平湿原周辺における最終氷期最盛期以降の植生変遷

• 高原 光

  大阪府農林技術センター環境部

• 竹岡 政治

  京都府立大学農学部林学科

書誌事項

タイトル別名

• VEGETATIONAL CHANGES SINCE THE LAST GLACIAL MAXIMUM AROUND THE HATCHODAIRA MOOR, KYOTO, JAPAN
• キョウトシ ハッチョウ ダイラシツゲン

抄録

The pollen analysis of core samples from the Hatchodaira moor (alt. 810m) in the montane zone at the northern part of Kyoto City, revealed seven vegetational changes to have occured there during the last 25,000 years. 1. Conifer・Betula stage (ca. 25,000-15,000 y.B.P.) : subarctic coniferous forest. 2. Fagus・Lepidodalanus-Conifer・Betula stage (ca. 15,000-12,000 y.B.P.) : the ecotone between subarctic coniferous and cool temperate broad-leaved forests. 3. Conifer・Betula stage (ca. 12,000-10,000 y.B.P.) : subarctic coniferous forest. 4. Fagus・Lepidobalanus・Betula stage (ca. 10,000-9,000 y.B.P.) : the ecotone between subarctic coniferous and cool temperate broad-leaved forests. 5. Fagus・Lepidobalanus・Carpinus stage (ca. 9,000-4,500 y.B.P.) : cool temperate beech (F. crenata) forest. 6. Lepidobanlanus・Carpinus・Betula stage (ca. 4,500-1,500 y.B.P.) : cool temperate oak (Quercus mongolica var. grosseserrata) forest. 7. Pinus stage (ca. 1,500 y.B.P.-present) : pine (P. densiflora) forest reflecting the destruction of natural forests by human activities.

収録刊行物

• 日本生態学会誌

  日本生態学会誌 36 (2), 105-116, 1986

  一般社団法人 日本生態学会

キーワード

• Pollen analysis
• Peat
• Vegetational changes
• Last glacial period
• Post glacial period.

詳細情報

• CRID: 1390001204292789376
• NII論文ID: 110001883144
• NII書誌ID: AN00193852
• DOI: 10.18960/seitai.36.2_105
• ISSN: 2424127X
• ISSN: 00215007
• NDL書誌ID: 3102518
• Web Site: https://ndlsearch.ndl.go.jp/books/R000000004-I3102518
• 本文言語コード: ja
• データソース種別:
  • JaLC
  • NDL
  • CiNii Articles
• 抄録ライセンスフラグ: 使用不可