globalchange  > 过去全球变化的重建
DOI: 10.1016/j.ancene.2019.100197
WOS记录号: WOS:000477641500001
论文题名:
Glacio-archaeological evidence of permanent settlements within a glacier end moraine complex during 980-1840 AD: The Miyar Basin, Lahaul Himalaya, India
作者: Saini, Rakesh1; Sharma, Milap Chand2; Deswal, Sanjay3; Barr, Iestyn David4; Kumar, Pawan2; Kumar, Parvendra1; Kumar, Pankaj5; Chopra, Sundeep5
通讯作者: Saini, Rakesh
刊名: ANTHROPOCENE
ISSN: 2213-3054
出版年: 2019
卷: 26
语种: 英语
英文关键词: Glacio-archaeology ; Little Ice Age ; Glacier fluctuations ; Lahaul Himalaya
WOS关键词: LATE QUATERNARY GLACIATION ; ICE-AGE ; WESTERN HIMALAYA ; LAHUL-HIMALAYA ; ZANSKAR RANGE ; COLLAGEN EXTRACTION ; TIBETAN PLATEAU ; NORTHERN INDIA ; HINDU-KUSH ; HOLOCENE
WOS学科分类: Environmental Sciences ; Geography, Physical ; Geosciences, Multidisciplinary
WOS研究方向: Environmental Sciences & Ecology ; Physical Geography ; Geology
英文摘要:

This study presents glacio-archaeological evidence from the Miyar basin, Lahaul Himalaya, that points towards the former presence of a well settled agricultural society, within a glacier end moraine complex. Three high altitude villages (Tharang, Phundang and Patam, now in ruins) with elaborate irrigation networks thrived within the end moraine complex of Tharang glacier at 3700 m a.s.l. Evidence exists in the form of dilapidated houses which had an organised internal space, chronologically constrained by radiocarbon (C-14) dating. These settlements occupied the end moraine complex between 980 and 1840 CE, thereby encompassing the majority of Little Ice Age period (1300-1600 CE), as defined elsewhere. The existence of settlements along with an irrigation system and associate fields at similar to 3700-3800 m a.s.l. for almost similar to 860 years during the late 10th to early 19th centuries suggests more favourable climatic (warm) conditions that at present. By contrast, present habitation is restricted to areas below similar to 3500 m a.s.l. However, the slope controlled irrigation system also suggests moisture stressed conditions during the 980-1840 CE period, similar to present. The available temperature and snowfall proxies for the region support our proposed timing, and suggest favourable climatic conditions for the survival of these settlements. (C) 2019 Elsevier Ltd. All rights reserved.


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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/139259
Appears in Collections:过去全球变化的重建

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作者单位: 1.Dr Harisingh Gour Cent Univ, Dept Gen & Appl Geog, Sagar 470003, India
2.Jawaharlal Nehru Univ, Ctr Study Reg Dev, New Delhi 110067, India
3.Govt Coll Dujana, Dept Geog, Dujana, India
4.Manchester Metropolitan Univ, Sch Sci & Environm, Manchester, Lancs, England
5.IUAC, New Delhi 110067, India

Recommended Citation:
Saini, Rakesh,Sharma, Milap Chand,Deswal, Sanjay,et al. Glacio-archaeological evidence of permanent settlements within a glacier end moraine complex during 980-1840 AD: The Miyar Basin, Lahaul Himalaya, India[J]. ANTHROPOCENE,2019-01-01,26
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