CCPortal
DOI10.1016/j.palaeo.2024.112020
Reconstruction of Holocene precipitation patterns and vegetation evolution in the North China Plain: Deciphering the relative influence of climate and anthropogenic forcing
发表日期2024
ISSN0031-0182
EISSN1872-616X
起始页码638
卷号638
英文摘要In this paper, we investigate Holocene precipitation changes in northern China to improve the understanding of the East Asian summer monsoon (EASM) and provide an environmental context for the development of Chinese civilisation. Our study is based on an analysis of 260 pollen samples from Holocene lacustrine sediments at Ningjinpo in northern China, and employs the biomisation method to reconstruct regional vegetation types and vegetation changes, and to decipher their driving factors, by incorporating regional climatic data and information on human activities. Results indicate that, in the early Holocene (10,000-8100 cal yr B.P.), regional climate was dry, with annual precipitation of 470 mm. In the middle Holocene (8100-3000 cal yr B.P.), a rapid increase was observed in precipitation, reaching 580 mm. During the late Holocene (2600-600 cal yr B.P.), climate became drier again, with annual precipitation decreasing to 480 mm. Between 10,000-600 cal yr B.P., vegetation exhibited distinct successional patterns dominantly influenced by climate, transitioning from meadow-steppe to forest, and then back to meadow-steppe. After 600 cal yr B.P., vegetation succession decoupled from climate change, with human activities emerging as the primary driving force, as indicated by the substantial increase in anthropogenic pollen and charcoal concentrations. In the future, under the combined influence of global warming and intensified human activity, the implementation of scientific environmental planning measures will become increasingly important for the restoration and sustainable development of regional vegetation ecosystems.
英文关键词Pollen analysis; Annual average precipitation; Vegetation succession; Human activity; Holocene; North China Plain
语种英语
WOS研究方向Physical Geography ; Geology ; Paleontology
WOS类目Geography, Physical ; Geosciences, Multidisciplinary ; Paleontology
WOS记录号WOS:001170198400001
来源期刊PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/299706
作者单位Hebei Normal University; Lanzhou University
推荐引用方式
GB/T 7714
. Reconstruction of Holocene precipitation patterns and vegetation evolution in the North China Plain: Deciphering the relative influence of climate and anthropogenic forcing[J],2024,638.
APA (2024).Reconstruction of Holocene precipitation patterns and vegetation evolution in the North China Plain: Deciphering the relative influence of climate and anthropogenic forcing.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,638.
MLA "Reconstruction of Holocene precipitation patterns and vegetation evolution in the North China Plain: Deciphering the relative influence of climate and anthropogenic forcing".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 638(2024).
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
百度学术
百度学术中相似的文章
必应学术
必应学术中相似的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。