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チベット高原南東域における過去19,000 年間に亘る水循環の歴史的変動
https://doi.org/10.18999/sumrua.20.81
https://doi.org/10.18999/sumrua.20.8126c0a65a-0345-4613-a743-663a1dec2f98
名前 / ファイル | ライセンス | アクション |
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Item type | 紀要論文 / Departmental Bulletin Paper(1) | |||||
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公開日 | 2011-04-28 | |||||
タイトル | ||||||
タイトル | チベット高原南東域における過去19,000 年間に亘る水循環の歴史的変動 | |||||
言語 | ja | |||||
その他のタイトル | ||||||
その他のタイトル | Historical change in water circulation on the southeastern Tibetan Plateau over the past 19,000 years | |||||
言語 | en | |||||
著者 |
松中, 哲也
× 松中, 哲也× 西村, 弥亜× 中村, 俊夫× 渡邊, 隆広× Zhu, Liping× 寺井, 久慈× 中野, 志穂× 奈良, 郁子× 今井, 章雄× Matsunaka, Tetsuya× Nishimura, Mitsugu× Nakamura, Toshio× Watanabe, Takahiro× Terai, Hisayoshi× Nakano, Shiho× Nara, Watanabe Fumiko× Imai, Akio |
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アクセス権 | ||||||
アクセス権 | open access | |||||
アクセス権URI | http://purl.org/coar/access_right/c_abf2 | |||||
抄録 | ||||||
内容記述 | The reconstruction of palaeoenvironmental history on the Tibetan Plateau after the Last Glacial Maximum (LGM) is important for understanding the relationship of climate change between the Tibetan Plateau and various area in the world. Since 2001, we have been attempting to elucidate the historical change in water circulation after the LGM on the southeastern Tibetan Plateau, where little have been obtained about high resolution palaeoclimate records, using three sediment cores from Lake Pumayum Co located in a basin close to Himalayas. In the present study, we aimed at making clear in detail the change in land water inflow, based on δ^<13>C of TOC, Sand, and Ca-Carbonate records from PY104 and PY409 cores (ca. 4m in length) which date back to 18.4 cal. ka BP and 10.6 cal. ka BP, respectively. The following results have been obtained so far : 1) In the Oldest Dryas period (19 - 14.7 cal. ka BP), the inflow of land water which derived from glaciers and frozen soils began to be intensified at 18 cal. ka BP due to deglaciation and gradually increased toward 15 cal. ka BP. 2) Before beginning of the Bølling / Allerød period (14.7 - 12.8 cal. ka BP), the inflow of land water rapidly became active from 15 cal. ka BP, and the contribution of precipitation remarkably increased together with increase in melting water. 3) In the Younger Dryas period (12.8 - 11.6 cal. ka BP), although relatively dry condition prevailed temporarily, the land water gradually increased. Therefore, the climate in this area was not always cold and dry. 4) From the beginning of the Hypsithermal (ca. 9 cal. ka BP), the inflow of land water further increased and have been kept until present. | |||||
言語 | en | |||||
内容記述タイプ | Abstract | |||||
内容記述 | ||||||
内容記述 | 第21回名古屋大学年代測定総合研究センターシンポジウム平成20(2008)年度報告 | |||||
言語 | ja | |||||
内容記述タイプ | Other | |||||
出版者 | ||||||
言語 | ja | |||||
出版者 | 名古屋大学年代測定資料研究センター | |||||
言語 | ||||||
言語 | jpn | |||||
資源タイプ | ||||||
資源 | http://purl.org/coar/resource_type/c_6501 | |||||
タイプ | departmental bulletin paper | |||||
出版タイプ | ||||||
出版タイプ | VoR | |||||
出版タイプResource | http://purl.org/coar/version/c_970fb48d4fbd8a85 | |||||
ID登録 | ||||||
ID登録 | 10.18999/sumrua.20.81 | |||||
ID登録タイプ | JaLC | |||||
書誌情報 |
ja : 名古屋大学加速器質量分析計業績報告書 巻 20, p. 81-87, 発行日 2009-03 |
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著者版フラグ | ||||||
値 | publisher |