A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake
文献类型:期刊论文
作者 | Shen, J; Liu, XQ; Matsumoto, R; Wang, SM; Yang, XD |
刊名 | SCIENCE IN CHINA SERIES D-EARTH SCIENCES
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出版日期 | 2005 |
卷号 | 48期号:6页码:742-751 |
关键词 | Qinghai Lake Late-Glacial Age to Holocene multi-proxy analysis high-resolution palaeoclimate |
ISSN号 | 1006-9313 |
英文摘要 | Based on multi-proxy analysis of pollen, carbonate, TOC, TN and delta(13)C of organic matters, a high-resolution climatic evolution of Qinghai Lake since the Late Glacial Age is reconstructed. The results indicate that the boundary between the Last Glacial Maximum and the Late Glacial Age is at about 18.2 cal.ka BP. The warm and wet period, which began at about 15.4 cal.ka BP, culminated at 7.4 cal.ka BP and came to its end at about 4.5 cal.ka. BP. After that, the climate gradually became cold and dry. The multi-proxy analysis indicates that the climate fluctuated greatly during the transitional period from the Late glacial Age to the Holocene, and this is in good accordance with that reflected by deep sea cores of North Atlantic, ice cores of Greenland, lake sediments in Europe, loess sequences and Guliya ice core in China. The climatic evolutional characteristic of the Qinghai Lake since the Late Glacial Age shows that the driving force of the East-Asia Monsoon correlates with solar radiation on the ten-thousand-year scale. |
公开日期 | 2012-03-07 |
源URL | [http://159.226.73.51/handle/332005/2801] ![]() |
专题 | 南京地理与湖泊研究所_湖泊室 |
推荐引用方式 GB/T 7714 | Shen, J,Liu, XQ,Matsumoto, R,et al. A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake[J]. SCIENCE IN CHINA SERIES D-EARTH SCIENCES,2005,48(6):742-751. |
APA | Shen, J,Liu, XQ,Matsumoto, R,Wang, SM,&Yang, XD.(2005).A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake.SCIENCE IN CHINA SERIES D-EARTH SCIENCES,48(6),742-751. |
MLA | Shen, J,et al."A high-resolution climatic change since the Late Glacial Age inferred from multi-proxy of sediments in Qinghai Lake".SCIENCE IN CHINA SERIES D-EARTH SCIENCES 48.6(2005):742-751. |
入库方式: OAI收割
来源:南京地理与湖泊研究所
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