Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1016/j.quascirev.2021.107246 |
Timing of late quaternary glaciations in the Yankti Kuti valley of the upper Kali Ganga catchment, Northern India | |
Bisht, Pinkey; Rawat, Ashish | |
通讯作者 | Bisht, P (corresponding author), Wadiai Inst Himalayan Geol, 33 GMS Rd, Dehra Dun 248001, Uttarakhand, India. |
来源期刊 | QUATERNARY SCIENCE REVIEWS
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ISSN | 0277-3791 |
EISSN | 1873-457X |
出版年 | 2021 |
卷号 | 273 |
英文摘要 | The Yankti Kuti valley which is located in the transitional climatic zone of the upper Kali Ganga catchment of northern India has witnessed multiple glacier advances since Marine Isotopic Stage 3 (MIS 3). The oldest glacial advance in the valley occurred during early MIS-3 and is dated to 52 +/- 3 ka (52.8 +/- 3 and 50.4 +/- 3 ka), the second advance occurred during late MIS 3 and is dated to 35 +/- 2 ka (36.4 +/- 1.8 and 34.5 +/- 2.2 ka). The termination of this stage occurred at similar to 30.3 +/- 2 ka and is reflected in the vertical shrinkage of the glacier. The third glacial advance which was more restricted is dated to the Last Glacial Maximum (LGM) 22 +/- 1 ka (22.2 +/- 1.1 and 21.4 +/- 1.2 ka). Following this, a glacial advance is dated to 16.1 +/- 1 ka corresponding to the Older Dryas cooling of the late glacial period. A subsequent minor re-advance is dated to 4.3 +/- 2.0 ka (4.4 +/- 0.4 and 4.2 +/- 0.1 ka) and can be attributed to the globally identified 4.2 ka cooling (arid) event. The study is in accordance with earlier observations made from the monsoon-dominated central Himalayan region. It provides a robust chronology and climatic evidence indicating significant ice volume depicted by the moraine height during MIS 3, implying that the moisture-deficient valleys of semi-arid Himalayan regions respond sensitively to enhance precipitation. The study suggests a regional synchronicity of glacier response to climate variability since MIS 3 and was in accordance with the synoptic-scale, climatic perturbation triggered by the North Atlantic millennial-scale climate oscillations. (C) 2021 Elsevier Ltd. All rights reserved. |
英文关键词 | Late quaternary glaciation Central himalaya Optical dating Holocene |
类型 | Article |
语种 | 英语 |
收录类别 | SCI-E |
WOS记录号 | WOS:000713693500005 |
WOS关键词 | CENTRAL HIMALAYA ; STIMULATED LUMINESCENCE ; GLACIER FLUCTUATIONS ; KARAKORAM HIMALAYA ; CLIMATIC DRIVERS ; SINGLE-ALIQUOT ; MONSOON ; HOLOCENE ; CHRONOLOGY ; QUARTZ |
WOS类目 | Geography, Physical ; Geosciences, Multidisciplinary |
WOS研究方向 | Physical Geography ; Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/374009 |
作者单位 | [Bisht, Pinkey] Wadiai Inst Himalayan Geol, 33 GMS Rd, Dehra Dun 248001, Uttarakhand, India; [Rawat, Ashish] HNB Garhwal Univ, Srinagar 246174, Uttarakhand, India |
推荐引用方式 GB/T 7714 | Bisht, Pinkey,Rawat, Ashish. Timing of late quaternary glaciations in the Yankti Kuti valley of the upper Kali Ganga catchment, Northern India[J],2021,273. |
APA | Bisht, Pinkey,&Rawat, Ashish.(2021).Timing of late quaternary glaciations in the Yankti Kuti valley of the upper Kali Ganga catchment, Northern India.QUATERNARY SCIENCE REVIEWS,273. |
MLA | Bisht, Pinkey,et al."Timing of late quaternary glaciations in the Yankti Kuti valley of the upper Kali Ganga catchment, Northern India".QUATERNARY SCIENCE REVIEWS 273(2021). |
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