Changes in plant richness and evenness since Marine Isotope Stage 2 on the Chinese Loess Plateau
文献类型:期刊论文
作者 | Yang, Xiaoxiao2; Jiang, Wenying; Yang, Shiling; Kong, Zhaochen3; Luo, Yunli3 |
刊名 | PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
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出版日期 | 2018 |
卷号 | 509页码:137-143 |
关键词 | Richness Evenness Pollen MIS 2 Mid-Holocene Chinese Loess Plateau |
ISSN号 | 0031-0182 |
DOI | 10.1016/j.palaeo.2017.02.021 |
文献子类 | Article |
英文摘要 | The warming period from Marine Isotope Stage 2 (MIS 2) to the mid-Holocene provides a useful analog for assessing the impact of global warming on plant diversity. Previously published pollen records from ten loess sections across the Chinese Loess Plateau (CLP) have shown that herbs were dominant during both MIS 2 and the mid-Holocene. During MIS 2, the vegetation in the eastern part was characterized mainly by Artemisia, together with Taraxacum-type, Echinops-type and Chenopodiaceae; and by Echinops-type, Chenopodiaceae, Nitraria, Ephedra and Picea in the western part. During the mid-Holocene, Artemisia remained dominant, while Echinops-type, Chenopodiaceae, Nitraria, Ephedra and Picea decreased, and Poaceae became more prevalent. From west to east during the mid-Holocene, Corylus, Quercus and Pinus increased, while Artemisia and Taraxacum-type decreased. In the present study, two indices of plant diversity (richness and evenness) were analyzed using these published pollen data. The results demonstrate that from MIS 2 to the mid-Holocene, plant richness increased at most of the studied sites, while plant evenness decreased. The increase in plant richness during the warming interval is in accordance with numerous geological records, but differs from modern observations of the response of biodiversity to ongoing global warming. The decrease in plant evenness is attributed to the increase in precipitation, associated with the intensification of the East Asian summer monsoon, which resulted in an increase in the dominance of Artemisia, and the corresponding inhibition in the growth of other species. Therefore, our results imply that plant richness in northern China would be expected to increase in a climate warming scenario, while changes in plant evenness would largely depend on interspecific competition within a plant community. (C) 2017 Elsevier B.V. All rights reserved. |
学科主题 | Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology |
出版地 | AMSTERDAM |
电子版国际标准刊号 | 1872-616X |
WOS关键词 | LAST GLACIAL MAXIMUM ; PALYNOLOGICAL RICHNESS ; CLIMATE-CHANGE ; NORTHERN CHINA ; GRAIN-SIZE ; GEOMORPHOLOGICAL HETEROGENEITY ; ENVIRONMENTAL HETEROGENEITY ; TERRESTRIAL ECOSYSTEMS ; MONSOON PRECIPITATION ; FLORISTIC DIVERSITY |
语种 | 英语 |
WOS记录号 | WOS:000447578200012 |
出版者 | ELSEVIER |
资助机构 | National Natural Science Foundation of ChinaNational Natural Science Foundation of China (NSFC) [41472318, 41611530697, 41172157] |
源URL | [http://ir.ibcas.ac.cn/handle/2S10CLM1/20678] ![]() |
专题 | 植被与环境变化国家重点实验室 |
作者单位 | 1.Chinese Acad Sci, Inst Bot, State Key Lab Vegetat & Environm Change, Beijing 100093, Peoples R China 2.Chinese Acad Sci, Inst Geol & Geophys, Key Lab Cenozo Geol & Environm, Beijing 100029, Peoples R China 3.Univ Chinese Acad Sci, Beijing 100049, Peoples R China |
推荐引用方式 GB/T 7714 | Yang, Xiaoxiao,Jiang, Wenying,Yang, Shiling,et al. Changes in plant richness and evenness since Marine Isotope Stage 2 on the Chinese Loess Plateau[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2018,509:137-143. |
APA | Yang, Xiaoxiao,Jiang, Wenying,Yang, Shiling,Kong, Zhaochen,&Luo, Yunli.(2018).Changes in plant richness and evenness since Marine Isotope Stage 2 on the Chinese Loess Plateau.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,509,137-143. |
MLA | Yang, Xiaoxiao,et al."Changes in plant richness and evenness since Marine Isotope Stage 2 on the Chinese Loess Plateau".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 509(2018):137-143. |
入库方式: OAI收割
来源:植物研究所
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