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DOI | 10.1111/bor.12201 |
Modern pollen assemblages from surface lake sediments and their environmental implications on the southwestern Tibetan Plateau | |
Ma, Qingfeng; Zhu, Liping; Lu, Xinmiao; Wang, Yong; Guo, Yun; Wang, Junbo; Ju, Jianting; Peng, Ping; Tang, Lingyu | |
通讯作者 | Ma, QF (通讯作者) |
发表日期 | 2017 |
ISSN | 0300-9483 |
EISSN | 1502-3885 |
起始页码 | 242 |
结束页码 | 253 |
卷号 | 46期号:2 |
英文摘要 | The relationships amongst modern pollen assemblages, vegetation, climate and human activity are the basis for reconstructing palaeoenvironmental changes using pollen records. It is important to determine these relationships at regional scales due to the development of vegetation under different climatic conditions and human activities. In this paper, we report on an analysis of modern pollen assemblages of 31 surface lake samples from 31 lakes (one sample per lake) on the southwestern Tibetan Plateau where the knowledge of modern pollen and their relationships with vegetation, climate and human activities is insufficient. The region includes five vegetation zones: sub- alpine shrub steppe, alpine steppe, alpine meadow and steppe ecotone, mountain desert and alpine desert. The lakes span a wide range of mean annual precipitation (50- 500 mm) and mean annual temperature (-8 to 6 degrees C). Modern pollen assemblages from our samples mainly consist of herb taxa (Artemisia, Cyperaceae, Poaceae, Chenopodiaceae, etc.) and some tree taxa (Pinus, Fagaceae, Alnus, etc.). The results indicate that modern pollen assemblages are able to reflect the main vegetation distribution. Redundancy analysis for the main pollen types and environmental variables shows that precipitation is the leading factor that influences the pollen distribution in the study area with the first axis capturing 13.7% of the variance in the pollen data set. The Artemisia/ Chenopodiaceae ratio is valid for separating the desert component (< 2) from the steppe and other vegetation zones (> 2) but is unable to distinguish moisture variations. The Artemisia/ Cyperaceae ratio is able to identify meadows (< 1) and steppes (> 1) and can be used as a moisture index on the southwestern Tibetan Plateau. Our results show that an appropriate range is needed for a modern pollen data set in order to perform pollen- based quantitative climate reconstructions in one region. It is essential to perform modern studies before using pollen ratios to reconstruct palaeovegetation and palaeoclimate at a regional scale. |
关键词 | QAIDAM BASINQUANTITATIVE RECONSTRUCTIONCLIMATE RECONSTRUCTIONSHOLOCENE VEGETATIONALPINE VEGETATIONSOURCE AREACHINAMOUNTAINSLASTMONGOLIA |
语种 | 英语 |
WOS研究方向 | Physical Geography ; Geology |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS记录号 | WOS:000398048200007 |
来源期刊 | BOREAS |
来源机构 | 中国科学院青藏高原研究所 |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/258907 |
推荐引用方式 GB/T 7714 | Ma, Qingfeng,Zhu, Liping,Lu, Xinmiao,et al. Modern pollen assemblages from surface lake sediments and their environmental implications on the southwestern Tibetan Plateau[J]. 中国科学院青藏高原研究所,2017,46(2). |
APA | Ma, Qingfeng.,Zhu, Liping.,Lu, Xinmiao.,Wang, Yong.,Guo, Yun.,...&Tang, Lingyu.(2017).Modern pollen assemblages from surface lake sediments and their environmental implications on the southwestern Tibetan Plateau.BOREAS,46(2). |
MLA | Ma, Qingfeng,et al."Modern pollen assemblages from surface lake sediments and their environmental implications on the southwestern Tibetan Plateau".BOREAS 46.2(2017). |
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