Plant diversity of the Tianshui Basin in the western Loess Plateau during the mid-Holocene - Charcoal records from archaeological sites
文献类型:期刊论文
作者 | Sun, Nan(孙楠) ; Li, Xiaoqiang(李小强) ; Dodson, John ; Zhou, Xinying(周新郢) ; Zhao, Keliang(赵克良) ; Yang, Qing(杨青) |
刊名 | QUATERN INT
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出版日期 | 2013 |
卷号 | 308期号:0页码:27—35 |
关键词 | POLLEN DATA GLACIAL-MAXIMUM YR BP VEGETATION CHINA HOLOCENE RECONSTRUCTIONS AGRICULTURE CALIBRATION EMISSION |
ISSN号 | 1040-6182 |
通讯作者 | lixiaoqiang@ivpp.ac.cn |
英文摘要 | Assessing the potential impact of increased temperature needs examination of robust palaeorecords that contain analogues. The fossil charcoal (anthracological) records from the mid-Holocene archaeological sites can provide palaeo-analogues on the impacts of climate change. The Xishanping and Dadiwan sites were continuously developed during the Neolithic Culture in the Tianshui Basin, western Loess Plateau. A total of 24 samples of fossil charcoal were recovered using a floatation method. At least 100 fragments were examined from each sample, and these fragments were identified following standard procedures, and the results were used to reconstruct the vegetation and plant diversity between 5200 and 4300 cal BP, which was a warm period for the region. The charcoal evidence from the Xishanping and Dadiwan sites confirm that woody plants were widely available, including temperate taxa such as Betula, Litmus, Quercus, Carpinus, Acer, Corylus and Padus, and typical subtropical taxa such as Bambusoideae, Liquidambar formosana, Castanopsis, Pseudotsuga sinensis, and Eucommia ulmoides. The assemblages of fossil charcoal show that mixed forests of north-subtropical evergreen and deciduous broadleaved trees existed. This is a broader range of woody plants than at present in the Tianshui Basin. This leads to the conclusion that the warmer and increasing monsoon precipitation resulted in a northward shift in the southern vegetation zones. And that the natural botanical diversity between 5200 and 4300 cal BP was also greater than at present in the Tianshui Basin, western Loess Plateau. (c) 2013 Elsevier Ltd and INQUA. All rights reserved. |
原文出处 | 10.1016/j.quaint.2013.05.014 |
公开日期 | 2013-11-27 |
源URL | [http://119.78.100.205/handle/311034/4106] ![]() |
专题 | 古脊椎动物与古人类研究所_古人类及旧石器研究室 |
推荐引用方式 GB/T 7714 | Sun, Nan,Li, Xiaoqiang,Dodson, John,et al. Plant diversity of the Tianshui Basin in the western Loess Plateau during the mid-Holocene - Charcoal records from archaeological sites[J]. QUATERN INT,2013,308(0):27—35. |
APA | Sun, Nan,Li, Xiaoqiang,Dodson, John,Zhou, Xinying,Zhao, Keliang,&Yang, Qing.(2013).Plant diversity of the Tianshui Basin in the western Loess Plateau during the mid-Holocene - Charcoal records from archaeological sites.QUATERN INT,308(0),27—35. |
MLA | Sun, Nan,et al."Plant diversity of the Tianshui Basin in the western Loess Plateau during the mid-Holocene - Charcoal records from archaeological sites".QUATERN INT 308.0(2013):27—35. |
入库方式: OAI收割
来源:古脊椎动物与古人类研究所
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