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J-GLOBAL ID：201802237358151816   整理番号：18A0609989

MuUs砂漠,中国北部,最終退氷以降における泥炭地の進化【Powered by NICT】

Evolution of Peatlands in the Mu Us Desert, Northern China, Since the Last Deglaciation

著者 (21件)： Liu Xiaokang (State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Liu Xiaokang (Engineering Center of Desertification and Blown-Sand Control of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Liu Xiaokang (Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Lu Ruijie (State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Lu Ruijie (Engineering Center of Desertification and Blown-Sand Control of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Lu Ruijie (Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Du Jing (State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Du Jing (Engineering Center of Desertification and Blown-Sand Control of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Du Jing (Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Lyu Zhiqiang (State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Lyu Zhiqiang (Engineering Center of Desertification and Blown-Sand Control of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Lyu Zhiqiang (Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Wang Lindong (State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Wang Lindong (Engineering Center of Desertification and Blown-Sand Control of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Wang Lindong (Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Gao Shangyu (State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Gao Shangyu (Engineering Center of Desertification and Blown-Sand Control of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Gao Shangyu (Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Wu Yongqiu (State Key Laboratory of Earth Surface Processes and Resource Ecology, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Wu Yongqiu (Engineering Center of Desertification and Blown-Sand Control of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China) ,  Wu Yongqiu (Key Laboratory of Environmental Change and Natural Disaster of Ministry of Education, Faculty of Geographical Science, Beijing Normal University, Beijing, China)
資料名： Journal of Geophysical Research: Earth Surface  (Journal of Geophysical Research: Earth Surface)
巻： 123  号： 2  ページ： 252-261  発行年： 2018年 
JST資料番号： W2385A  ISSN： 2169-9003  CODEN： JGREA2  資料種別： 逐次刊行物 (A)
記事区分： 原著論文  発行国： アメリカ合衆国 (USA)  言語： 英語 (EN)

抄録/ポイント： 泥炭堆積物からの気候再構成は,第四紀研究の重要な側面である。中国北部のMuUs砂漠の泥炭地の以前の研究は,古気候進化の過程に焦点を当てているが,泥炭地開発の歴史は比較研究の欠如のために不明のままである。ここでは,最終退氷期以来のMuUs砂漠内の泥炭地発達を実証した入手可能な記録の合成を提示した。12地点から以前に公表された結果と二種の新しい部位からプロファイルから古気候記録を組み合わせた。著者らの目的は,泥炭地発達の時間的及び空間的記録を再構成し,その駆動力を決定することである。結果は,それらの空間的範囲の有意な拡大した場合,泥炭地は二段階で開発から~15ka完新世初期まで6.5 3kaのことを示した。これらの相は,二つの異なるタイプの沼沢プロセスに対応し,両者は東アジアモンスーンの変化に密接に関係している。2ka以降の最終段階は,モンスーンの顕著な弱化,泥炭蓄積は停止によるものであった。Copyright 2018 Wiley Publishing Japan K.K. All Rights reserved. Translated from English into Japanese by JST.【Powered by NICT】

シソーラス用語： モンスーン ,  堆積物 ,  駆動力 ,  *砂漠 ,  古気候 ,  *泥炭 ,  *中国北部 ,  気候 ,  再構成
準シソーラス用語： 東アジアモンスーン ,  *泥炭地 ,  *最終退氷期 , 【Automatic Indexing@JST】

著者キーワード (3件)： 最終退氷 ,  MuUs砂漠 ,  泥炭地の進化

分類 (2件)： 農業土木  (FB02000W) ,  第四紀  (DE02070C)

タイトルに関連する用語 (5件)： 砂漠 ,  中国北部 ,  最終退氷 ,  泥炭地 ,  進化