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Palynological study of 200-meter core samples from Lake Biwa, Central Japan : I : The palaeovegetational and palaeoclimatic changes during the last 600, 000 years
http://hdl.handle.net/2297/38472
http://hdl.handle.net/2297/38472506e30fb-5390-47cd-b6ab-b825bfc3b088
名前 / ファイル | ライセンス | アクション |
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SC-PR-FUJI-N-230.pdf (2.2 MB)
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Item type | 学術雑誌論文 / Journal Article(1) | |||||
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公開日 | 2017-10-03 | |||||
タイトル | ||||||
タイトル | Palynological study of 200-meter core samples from Lake Biwa, Central Japan : I : The palaeovegetational and palaeoclimatic changes during the last 600, 000 years | |||||
言語 | ||||||
言語 | eng | |||||
資源タイプ | ||||||
資源タイプ識別子 | http://purl.org/coar/resource_type/c_6501 | |||||
資源タイプ | journal article | |||||
著者 |
Fuji, Norio
× Fuji, Norio |
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著者別表示 |
藤, 則雄
× 藤, 則雄 |
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書誌情報 |
日本古生物学會報告・紀事 新編 = Transactions and proceedings of the Paleontological Society of Japan. New series 巻 132, p. 230-252, 発行日 1983-01-01 |
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ISSN | ||||||
収録物識別子タイプ | ISSN | |||||
収録物識別子 | 0031-0204 | |||||
NCID | ||||||
収録物識別子タイプ | NCID | |||||
収録物識別子 | AA00867896 | |||||
DOI | ||||||
関連タイプ | isIdenticalTo | |||||
識別子タイプ | DOI | |||||
関連識別子 | https://doi.org/10.14825/prpsj1951.1983.132_230 | |||||
出版者 | ||||||
出版者 | 日本古生物学会 = Palaeontological Society of Japan | |||||
抄録 | ||||||
内容記述タイプ | Abstract | |||||
内容記述 | The samples of a 200-meter core obtained from the present bottom in Lake Biwa, Central Japan for the investigations of the palaeoclimatic and palaeovegetational changes in and around the lake during the last 600, 000 years can be divided into 19 pollen zones from the view point of palynology. The palaeoclimatic change and the ages of glacial and interglacial stages display similarity to the palaeotemperature curve by oxygen isotope ratio determination from the Caribbean Sea. During the glacial stages or stadials, the typical vegetation thriving today in the Subpolar or Subalpine zone of Japan prevailed at the summit area and/or the montane area around Lake Biwa, and in the lowland around the lake, plants growing today in the Cool Temperate zone were distributed. In the interglacials and interstadials, the palaeovegetation in the higher area was characterized mainly by plants of the Cool Temperate zone and the present Temperate zone, and in the lowland, the palaeovegetation was composed mainly of broadleaved deciduous and evergreen trees growing in the Warm Temperate zone. 日本における第四紀を通じての古植生の変遷とそれに基づく古気候の変化を究明して, 世界における第四紀の気候変化の標準の1つにすることを目的として, 1971年秋, 琵琶湖の水深65mの湖底から約200mに及ぶボーリングを実施した。そして, 殆んど完全に連続するコアを採集することに成功。このコア・サンプルは, 研究の第一段階として, 5m間隔で採集され, 花粉分析の視点から研究された。その結果, 200mコアは19の花粉帯に区分され, 約60万年間に12回の寒冷期(氷期)と10回の温和期の存在したことが確認された。このような琵琶湖における気候変化の記録をカリブ海からの酸素同位体による古水温変化と比較すると, 全般的にみてよく酷似する。なお, 琵琶湖底からのサンプルは, 有機化学, δ13C, 珪藻群集, フィッション・トラック法年代測定, 及び古地磁気変の諸視点からも究明され, 気候変化とそれらとの比較検討も併せて述べた。 | |||||
権利 | ||||||
権利情報 | Copyright © The Palaeontological Society of Japan | |||||
著者版フラグ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | http://www.palaeo-soc-japan.jp/ | |||||
関連URI | ||||||
識別子タイプ | URI | |||||
関連識別子 | https://www.jstage.jst.go.jp/browse/prpsj1951 |