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  1. F300 宇宙地球環境研究所
  2. F300b 紀要
  3. 名古屋大学加速器質量分析計業績報告書
  4. 8

東シベリアコリマ河下流域及びヤクーツク周辺の永久凍土中の有機物年代測定

https://doi.org/10.18999/sumrua.8.134
https://doi.org/10.18999/sumrua.8.134
61f47d05-34a9-4bcb-baad-b92862aa892e
名前 / ファイル ライセンス アクション
KJ00000187810.pdf KJ00000187810.pdf (844.1 kB)
Item type 紀要論文 / Departmental Bulletin Paper(1)
公開日 2010-05-18
タイトル
タイトル 東シベリアコリマ河下流域及びヤクーツク周辺の永久凍土中の有機物年代測定
その他のタイトル
その他のタイトル Radio Carbon Dating Results of Organic Materials Obtained from the Lowland Kolyma River and the Middle of Lena River
著者 福田, 正己

× 福田, 正己

WEKO 80367

福田, 正己

Search repository
Fukuda, Masami

× Fukuda, Masami

WEKO 80368

Fukuda, Masami

Search repository
仙頭, 宣幸

× 仙頭, 宣幸

WEKO 80369

仙頭, 宣幸

Search repository
Sento, Nobuyuki

× Sento, Nobuyuki

WEKO 80370

Sento, Nobuyuki

Search repository
中村, 俊夫

× 中村, 俊夫

WEKO 80371

中村, 俊夫

Search repository
Nakamura, Toshio

× Nakamura, Toshio

WEKO 80372

Nakamura, Toshio

Search repository
クニツキー, V. V.

× クニツキー, V. V.

WEKO 80373

クニツキー, V. V.

Search repository
Kunitsky, V. V.

× Kunitsky, V. V.

WEKO 80374

Kunitsky, V. V.

Search repository
権利
権利情報 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会
権利
権利情報 本文データは学協会の許諾に基づきCiNiiから複製したものである
抄録
内容記述 The field expeditions in Eastern Siberian Permafrost was conducted in both 1995 and 1996 as to get detail information of the permafrost response to climate change. In the low land area of Kolyma River, there exist the unique deposit of permafrost with large ground ice accumulation, which is locally "Edoma or Ice Complex". The genesis and occurrence of Edmoa reflect the long term climate change at high arctic Siberia. Because of the active response of Permafrost under present climate warming trend, it is important to understand the process of accumulation of Edmoa. Present authors sampled the organic materials from Edoma at various locations in these regions. Edoma tends to thaw in large scale after the Last Glacial Periods. By thawing and melting of ground ice, ground surface subsides and results in formation of Thermo-Karst depression, which is locally names as Alas. ^<14> dating results indicated the thawing of Edoma started at about 8000yBP ago and continued until about 4000yBP. As lowest boundary of Edoma was not detected, the initiation period of Edoma was not estimated yet. However at three locations in low land Kolyma, organic materials including fossil of Mammal were dated as the time of Karginsky Interstadial and Sartan Stadial in Last Glacial. Edoma in this region was categorized into two groups. Edoma along the coast of arctic sea near river mouth of Kolyma, named as Ambarchik started its accumulation in karginsky Interstadial and terminated its accumulation at the late karginsky Interstadial. On the other hand, two sites along Kolyma River, Plaxina Yar and Krasivoe, results of dating suggested accumulation of Edoma might continued in the middle of Sartan Stadial. These dated values newly imply Edoma in this region is the most latest accumulation in Eastern Siberian Permafrost.
内容記述タイプ Abstract
内容記述
内容記述 タンデトロン加速器質量分析計業績報告 Summaries of Researches Using AMS 1996 (平成8)年度
内容記述タイプ Other
出版者
出版者 名古屋大学年代測定資料研究センター 天然放射性元素測定小委員会
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
ID登録
ID登録 10.18999/sumrua.8.134
ID登録タイプ JaLC
関連情報
関連タイプ isVersionOf
識別子タイプ URI
関連識別子 http://ci.nii.ac.jp/naid/110000476030/
書誌情報 名古屋大学加速器質量分析計業績報告書

巻 8, p. 134-145, 発行日 1997-03
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著者版フラグ
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