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DOI | 10.5194/cp-15-367-2019 |
The 4.2 ka BP Event in northeastern China: A geospatial perspective | |
Scuderi L.A.; Yang X.; Ascoli S.E.; Li H. | |
发表日期 | 2019 |
ISSN | 18149324 |
起始页码 | 367 |
结束页码 | 375 |
卷号 | 15期号:1 |
英文摘要 | The Hunshandake Sandy Lands of northeastern China, currently a semiarid lightly vegetated region, were characterized by perennial lakes and forest stands in the early and middle Holocene. Well-developed dark grassland-type paleosols (mollisols) at the southern edge of the Hunshandake-OSL (optically stimulated luminescence)-dated to between 6.93±0.61< and 4.27±0.38< ka along with lacustrine sands at higher elevations that date to between 5.7±0.3< and 5.2±0.2< ka-and thick gray lacustrine sediments suggest a wetter climate. Between 4.2 and 3.8 ka, the region experienced extreme drying that was exacerbated by lake overflow drainage and sapping that depleted the groundwater table. The region supported a robust population, the Hongshan Culture, but was depopulated post 4.2 ka with migration likely to the Yellow River Valley where the Hongshan introduced their characteristic cultural elements to early Chinese civilization. Evidence for extreme and sudden environmental change in northeastern China, at and following the 4.2 ka BP Event and like that we document in the Hunshandake, is widespread. However, no comprehensive overview of this climatic episode exists. Here, we discuss the relevant events in northeastern China and capture them in a spatially explicit Geographic Information Systems database that can be used to analyze the timing and spatial pattern of climate and environmental change associated with the 4.2 ka BP Event. This approach could serve as a prototype for a global 4.2 ka BP Event database. © 2019 Author(s). |
语种 | 英语 |
scopus关键词 | climate change; environmental change; groundwater; Holocene; lacustrine deposit; paleosol; semiarid region; water table; China; Hunshandak Sandland; Nei Monggol; Yellow River Valley |
来源期刊 | Climate of the Past |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/146849 |
作者单位 | Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM, United States; School of Earth Sciences, Zhejiang University, Hangzhou, Zhejiang Province, China |
推荐引用方式 GB/T 7714 | Scuderi L.A.,Yang X.,Ascoli S.E.,et al. The 4.2 ka BP Event in northeastern China: A geospatial perspective[J],2019,15(1). |
APA | Scuderi L.A.,Yang X.,Ascoli S.E.,&Li H..(2019).The 4.2 ka BP Event in northeastern China: A geospatial perspective.Climate of the Past,15(1). |
MLA | Scuderi L.A.,et al."The 4.2 ka BP Event in northeastern China: A geospatial perspective".Climate of the Past 15.1(2019). |
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