Arid
DOI10.3390/su11216146
The Possible Stimulation of the Mid-Holocene Period's Initial Hydrological Recession on the Development of Neolithic Cultures along the Margin of the East Asian Summer Monsoon
Xue, Wenping1,2; Jin, Heling1; Liu, Bing1,3; Sun, Liangying1; Liu, Zhenyu1
通讯作者Jin, Heling ; Liu, Bing
来源期刊SUSTAINABILITY
EISSN2071-1050
出版年2019
卷号11期号:21
英文摘要A better understanding of past East Asian summer monsoonal (EASM) variations, which play a key role in the development of the largely rain-watered agriculture in China, could contribute to better appraising potential impacts on EASM with regard to global climate change. However, our knowledge of the relationship between mid-Holocene hydrological recession and the development of Neolithic culture is limited due to a lack of joint studies and a compilation of spatiotemporal data, especially on the episode of 6-5 ka from the mid-Holocene Optimum (HO) along the peripheral realm of the EASM. Here, we suggest that the hydrological recession between 6-5 ka, on the basis of lithology and geochemical element analysis, occurred not only in the Horqin sandy land, but also in other fluvial-lacustrine, stalagmitic, loess, and aeolian records across the whole monsoon-influenced boundary belt. These records indicated varied, more or less synchronous, and coherent moisture changes, yet with not entirely consistent onsets, durations, and degrees. We attributed this spatiotemporal complexity to the orbit-induced weakening of summer solar insolation, and the interactions of the Asian monsoon (AM) and westerlies, as well as topography and regional vegetation factors. Furthermore, the mid-Holocene initial hydroclimatic recession during 6-5 ka within the thresholds of an eco-environment bearing a capacity system, might have facilitated the development of mid-late Neolithic culture and stimulated the north and northwest expansion and integration of region-specific Neolithic culture.
英文关键词hydrological recession mid-Holocene geochemical elements EASM margin Neolithic culture
类型Article
语种英语
国家Peoples R China
开放获取类型gold
收录类别SCI-E ; SSCI
WOS记录号WOS:000501205200273
WOS关键词NORTHEASTERN TIBETAN PLATEAU ; HOLOCENE CLIMATIC-CHANGE ; INNER-MONGOLIA PLATEAU ; CAL. YR BP ; INTERTROPICAL CONVERGENCE ZONE ; SPATIAL-TEMPORAL DISTRIBUTION ; LOESS-PALEOSOL SEQUENCES ; BADAIN JARAN DESERT ; ARID CENTRAL-ASIA ; DALI-NOR AREA
WOS类目Green & Sustainable Science & Technology ; Environmental Sciences ; Environmental Studies
WOS研究方向Science & Technology - Other Topics ; Environmental Sciences & Ecology
EI主题词2019-11-01
来源机构兰州大学 ; 中国科学院西北生态环境资源研究院
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/310561
作者单位1.Chinese Acad Sci, Cold & Arid Reg Environm & Engn Res Inst, Key Lab Desert & Desertificat, 320 Donggang West Rd, Lanzhou 730000, Gansu, Peoples R China;
2.Univ Chinese Acad Sci, 19 Yuquan Rd, Beijing 100049, Peoples R China;
3.Lanzhou Univ, Key Lab ofWestern China Environm Syst, 222 Tianshui South Rd, Lanzhou 730000, Gansu, Peoples R China
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GB/T 7714
Xue, Wenping,Jin, Heling,Liu, Bing,et al. The Possible Stimulation of the Mid-Holocene Period's Initial Hydrological Recession on the Development of Neolithic Cultures along the Margin of the East Asian Summer Monsoon[J]. 兰州大学, 中国科学院西北生态环境资源研究院,2019,11(21).
APA Xue, Wenping,Jin, Heling,Liu, Bing,Sun, Liangying,&Liu, Zhenyu.(2019).The Possible Stimulation of the Mid-Holocene Period's Initial Hydrological Recession on the Development of Neolithic Cultures along the Margin of the East Asian Summer Monsoon.SUSTAINABILITY,11(21).
MLA Xue, Wenping,et al."The Possible Stimulation of the Mid-Holocene Period's Initial Hydrological Recession on the Development of Neolithic Cultures along the Margin of the East Asian Summer Monsoon".SUSTAINABILITY 11.21(2019).
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