Pollen-based biome reconstruction at Middle Holocene (6 ka BP) and last glacial maximum (18 ka BP) in China
文献类型：期刊论文
| 作者 | Sun, XJ; Chen, XD; Song, CQ; Chen, XD; Luo, YL; Yang, DA; Yu, G; Kong, ZC; Liu, PM; Liu, GX |
| 刊名 | ACTA BOTANICA SINICA
 |
| 出版日期 | 2000-11-01 |
| 卷号 | 42期号:11页码:1201-1209 |
| 关键词 | Pollen Biome Middle Holocene The Last Glacial Maximum China |
| 文献子类 | Article |
| 英文摘要 | Biome (vegetation) reconstruction of the Middle Holocene ((6 000 +/- 500) a BP) and the Last Glacial Maximum ((18 000 +/- 2 000) a BP) in China was accomplished based on pollen data from "China Quternary Pollen data Base" and biomesation procedure. There are 116 pollen data used for 6 ka BP biome reconstruction. The 6 ka BP Biome shows the following differences as compared with the present vegetation: 1. Forests of eastern China expanded westwards to the steppe area, 2. Temperate deciduous forests shifted about 4 degrees latitudinally northwards and replaced by cool temperate mixed forest and taiga at present. 3. Tundra in Tibet Plateau was greatly shrunken. 4. Seasonal rainforest was replaced by rainforest in southern China. All these changes must be attributed to the increasing temperature and humidity during Middle Holocene, except some areas of southwestern and tropical areas of southern China where climate might be even cooler, but more humid than nowadays. Biome of 18 ka BP based on 39 pollen data displayed: 1. Steppe and desert expanded southwards and eastwards reaching the northern margin of the present evergreen broad-leaved forest. 2. Evergreen broad-leaved forest retracted southwards to the present tropical zone and the tropical forest banished completly. The vegetation changes must be resulted from cold and dry climate during the Last Glacial Maximum. |
| WOS关键词 | TERRESTRIAL BIOSPHERE ; SIMULATION ; CLIMATE ; LEVEL |
| 语种 | 英语 |
| WOS记录号 | WOS:000165668700018 |
| 出版者 | SCIENCE PRESS |
| 源URL | [http://ir.igsnrr.ac.cn/handle/311030/68285]  |
| 专题 | 中国科学院地理科学与资源研究所 |
| 通讯作者 | Sun, XJ |
| 作者单位 | 1.Chinese Acad Sci, Inst Bot, Beijing 100864, Peoples R China 2.Chinese Acad Sci, Nanjing Inst Geog & Limnol, Beijing 100864, Peoples R China 3.Nanjing Univ, Dept Geo & Ocean Sci, Nanjing 210008, Peoples R China 4.Chinese Acad Sci, Inst Geog, Beijing 100012, Peoples R China 5.Louisiana State Univ, Dept Geog & Anthropol, Baton Rouge, LA 70803 USA 6.Xian Coll Geol, Xian, Peoples R China 7.Natl Taiwan Univ, Taipei 10764, Taiwan 8.Chinese Acad Sci, Lanzhou Inst Glaciol & Geocryol, Beijing 100864, Peoples R China 9.Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Beijing 100864, Peoples R China 10.Chinese Acad Sci, Changchun Inst Geog, Beijing 100864, Peoples R China |
| 推荐引用方式 GB/T 7714 | Sun, XJ,Chen, XD,Song, CQ,et al. Pollen-based biome reconstruction at Middle Holocene (6 ka BP) and last glacial maximum (18 ka BP) in China[J]. ACTA BOTANICA SINICA,2000,42(11):1201-1209. |
| APA | Sun, XJ.,Chen, XD.,Song, CQ.,Chen, XD.,Luo, YL.,...&China Quaternary Pollen Data Base.(2000).Pollen-based biome reconstruction at Middle Holocene (6 ka BP) and last glacial maximum (18 ka BP) in China.ACTA BOTANICA SINICA,42(11),1201-1209. |
| MLA | Sun, XJ,et al."Pollen-based biome reconstruction at Middle Holocene (6 ka BP) and last glacial maximum (18 ka BP) in China".ACTA BOTANICA SINICA 42.11(2000):1201-1209. |
入库方式： OAI收割
来源：地理科学与资源研究所
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