Last-glacial to postglacial climate formation in the continental interior inferred from multi-proxy records of Lake Hovsgol, Mongolia

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Last-glacial to postglacial climate formation in the continental interior inferred from multi-proxy records of Lake Hovsgol, Mongolia

机译：从蒙古霍夫斯高尔湖的多代理记录推断，大陆内部的最后冰期至冰期后气候形成

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《Climate of the Past Discussions》 |2010年第1期|共2页
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1. Last-glacial to postglacial climate formation in the continental interior inferred from multi-proxy records of Lake Hovsgol, Mongolia [J] . K. Minoura, D. Sugawara, T. Kawai Climate of the Past Discussions . 2010,第1期

机译：从蒙古霍夫斯高尔湖的多代理记录推断，大陆内部的最后冰期至冰期后气候形成
2. Last-glacial to postglacial climate formation in the continental interior inferred from multi-proxy records of Lake Hovsgol, Mongolia [J] . Climate of the Past Discussions . 2010,第5期

机译：从蒙古霍夫斯高尔湖的多代理记录推断，大陆内部的最后冰期至冰期后气候形成
3. Last glacial to post glacial climate changes in continental Asia inferred from multi-proxy records (geochemistry, clay mineralogy, and paleontology) from Lake Hovsgol, northwest Mongolia [J] . Takahiro Watanabe, Koji Minoura, Fumiko Watanabe Nara, Global and planetary change . 2012,第May期

机译：根据蒙古西北部霍夫斯高尔湖的多代记录（地球化学，粘土矿物学和古生物学）推断，亚洲大陆最后一次冰期至冰期后的气候变化
4. A MULTI-PROXY STUDY OF HOLOCENE PALEOCLIMATE AND DEPOSITIONAL ENVIRONMENT, HOVSGOL, MONGOLIA [C] . MELLISSA CROSS Keck Research Symposium in Geology . 2011

机译：全新型古古古古古古古古古古古古古古古古古古古（Hovsgol）的多功能研究，蒙古
5. A multi-proxy record of Holocene paleoenvironmental and paleoclimate change at Lake Tokun, south-central Alaska. [D] . Griffith, Jonathan Gilbert. 2014

机译：阿拉斯加中南部托昆湖全新世古环境和古气候变化的多代理记录。
6. Lake Sediment Records on Climate Change and Human Activities in the Xingyun Lake Catchment SW China [O] . Wenxiang Zhang, Qingzhong Ming, Zhengtao Shi, -1

机译：中国西南地区星云湖集水区气候变化和人类活动的湖泊沉积物记录
7. Last-glacial to postglacial climate formation in the continental interior inferred from multi-proxy records of Lake Hovsgol, Mongolia [O] . K. Minoura, D. Sugawara, T. Kawai 2010

机译：从蒙古霍夫斯高尔湖的多代理记录推断，大陆内部的最后冰期至冰期后气候形成

Last-glacial to postglacial climate formation in the continental interior inferred from multi-proxy records of Lake Hovsgol, Mongolia

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