Climate Reconstruction based on Pollen Analysis in Inner Mongolia, North China from 51.9 to 30.6 kaBP
文献类型：期刊论文
| 作者 | Li Suping; Ferguson, David K.; Wang Yong; Li Jinfeng1; Yao Jianxin |
| 刊名 | ACTA GEOLOGICA SINICA-ENGLISH EDITION
 |
| 出版日期 | 2013 |
| 卷号 | 87期号:5页码:1444-1459 |
| 关键词 | paleoclimate paleovegetation pollen analysis Late Pleistocene Inner Mongolia |
| ISSN号 | 1000-9515 |
| DOI | 10.1111/1755-6724.12141 |
| 文献子类 | Article |
| 英文摘要 | The palynomorph assemblage of lake sediments younger than 51.9 kaBP from Wulagai Gobi in Inner Mongolia was analyzed to reconstruct the vegetation and climate. From 51.9 to 30.6 kaBP, the vegetation was arid to semi-arid grassland with only slight changes. According to the palynomorphs, trees and shrubs were very rare. The large number and diversity of algae indicate the presence of a lake. Quantitative climatic conditions were reconstructed using the Best Analogues Method. The results indicate that the annual mean temperature was higher than that at present. The combination of temperature and annual precipitation suggests a change in the climate from cool dry to warm dry and then cool humid. Our results show that the annual precipitation values were mostly higher than that at present but were lower than 400 mm. It infers that the study area was already within the arid to semi-arid regions but with a stronger influence of the summer monsoon during 51.9 to 30.6 kaBP than at present. With slight differences mainly in time scale, the changing trend of the annual temperature curve is consistent with the other climatic records from Antarctica, Greenland, Hulu Cave (East China), and the Tibetan Plateau during the last glacial period. From 30.6 kaBP to present, very few palynomorphs were detected in the samples. Hence, no information about the vegetation and climate could be extracted. Combined with other studies during Late Pleistocene, we presume that the reason for the lack of pollen during this period was caused by an abrupt temperature fall after 30.6 kaBP or that the lacustrine conditions were unsuitable for pollen deposition. It was probably incurred by the oxidation on land prior to deposition. But for those samples only with algae, it might be caused by the fact that algae could finish their life history in a very short time in a seasonal lake. |
| 学科主题 | Geosciences, Multidisciplinary |
| 出版地 | HOBOKEN |
| 电子版国际标准刊号 | 1755-6724 |
| WOS关键词 | GREEN-ALGAE ; ICE-CORE ; PEDIASTRUM ; RECORD ; HOLOCENE ; INSTABILITY ; VEGETATION ; TIBET ; CHLOROPHYCEAE ; STRATIGRAPHY |
| WOS研究方向 | Science Citation Index Expanded (SCI-EXPANDED) |
| 语种 | 英语 |
| WOS记录号 | WOS:000325550700021 |
| 出版者 | WILEY |
| 资助机构 | China Geological Survey Projects(China Geological Survey) ; Basic Research Fund of Institute of Geology, Chinese Academy of Geological Sciences |
| 源URL | [http://ir.ibcas.ac.cn/handle/2S10CLM1/28137]  |
| 专题 | 植物研究所_系统与进化植物学研究中心_系统与进化植物学研究中心_学位论文 |
| 作者单位 | 1.Ferguson, David K.] Univ Vienna, Inst Palaeontol, A-1090 Vienna, Austria 2.Chinese Acad Geol Sci, Inst Geol, Key Lab Stratig & Palaeontol, Beijing 100037, Peoples R China 3.Chinese Acad Sci, Inst Bot, State Key Lab Systemat & Evolutionary Bot, Beijing 100093, Peoples R China |
| 推荐引用方式 GB/T 7714 | Li Suping,Ferguson, David K.,Wang Yong,et al. Climate Reconstruction based on Pollen Analysis in Inner Mongolia, North China from 51.9 to 30.6 kaBP[J]. ACTA GEOLOGICA SINICA-ENGLISH EDITION,2013,87(5):1444-1459. |
| APA | Li Suping,Ferguson, David K.,Wang Yong,Li Jinfeng,&Yao Jianxin.(2013).Climate Reconstruction based on Pollen Analysis in Inner Mongolia, North China from 51.9 to 30.6 kaBP.ACTA GEOLOGICA SINICA-ENGLISH EDITION,87(5),1444-1459. |
| MLA | Li Suping,et al."Climate Reconstruction based on Pollen Analysis in Inner Mongolia, North China from 51.9 to 30.6 kaBP".ACTA GEOLOGICA SINICA-ENGLISH EDITION 87.5(2013):1444-1459. |
入库方式： OAI收割
来源：植物研究所
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