DOI: 10.1007/s10584-017-2111-0
Scopus记录号: 2-s2.0-85033731720
论文题名: Interplay of environmental and socio-political factors in the downfall of the Eastern Türk Empire in 630 CE
作者: Di Cosmo N. ; Oppenheimer C. ; Büntgen U.
刊名: Climatic Change
ISSN: 0165-0009
EISSN: 1573-1480
出版年: 2017
卷: 145, 期: 2018-03-04 起始页码: 383
结束页码: 395
语种: 英语
英文关键词: Asian history
; Paleoclimatology
; Tree rings
; Volcanism
Scopus关键词: Agriculture
; Climate change
; Climatology
; Forestry
; Sulfur compounds
; Climate fluctuations
; Comprehensive analysis
; Demographic changes
; Environmental change
; Greenland ice cores
; Paleoclimatology
; Tree rings
; Volcanism
; Social sciences
; climate effect
; environmental change
; environmental factor
; environmental history
; episodic event
; historical record
; leadership
; nomadic people
; paleoclimate
; political history
; political relations
; tree ring
; volcanism
; vulnerability
; Central Asia
; China
英文摘要: The collapse of the Eastern Türk Empire (ETE, ca. 584–630 CE) in 630 CE marked the rise of Tang China as the paramount power on the Silk Road. It was followed by the Tang defeat of the Western Türk Empire in 659 and opened a phase of Chinese expansion into central Asia. Climate-induced environmental changes as well as economic and political consequences are mentioned in medieval Chinese records as major factors in the ETE collapse. The role of cooler temperatures has also been discussed in current scholarship. Here, we re-evaluate this question by assessing the available historical sources in the light of a global network of 16 tree-ring chronologies for this period, which reveal distinct summer cooling in the ETE heartland between 626 and 632 CE. Reconstructed peak cooling of up to − 3.4 °C in 627 and 628 CE (relative to the 1961–90 mean climatology) coincided with heavy snowfall and severe frost events in the territory of the ETE. A strong sulfate spike in Greenland ice cores that has been dated circa 626 CE is implicated in the abrupt surface cooling. We argue that the climatic perturbation and associated reduction in vegetation growth and livestock mortality are relevant in understanding the causes of the fall of the ETE but these indirect drivers must be evaluated within a comprehensive analysis of political relations within both the Türk and the Tang leadership. Our study underscores and contextualizes the vulnerability of past nomadic societies to small and episodic climate fluctuations, particularly when coupled with concurrent socioeconomic, political, and demographic changes. © 2017, Springer Science+Business Media B.V., part of Springer Nature.
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/83863
Appears in Collections: 气候减缓与适应 气候变化事实与影响
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作者单位: Institute for Advanced Study, School of Historical Studies, Princeton, NJ, United States; Princeton University, Princeton, NJ, United States; Department of Geography, University of Cambridge, Cambridge, United Kingdom; Swiss Federal Research Institute WSL, Birmensdorf, Switzerland; CzechGlobe, Global Change Research Institute CAS and Masaryk University, Brno, Czech Republic
Recommended Citation:
Di Cosmo N.,Oppenheimer C.,Büntgen U.. Interplay of environmental and socio-political factors in the downfall of the Eastern Türk Empire in 630 CE[J]. Climatic Change,2017-01-01,145(2018-03-04)