Arid
DOI10.1016/j.quascirev.2021.107100
Late Quaternary glacial advances and equilibrium-line altitude changes in a semi-arid region, Suru Basin, western Himalaya
Kumar, Vinit; Mehta, Manish; Shukla, Aparna; Kumar, Anil; Garg, Siddhi
通讯作者Kumar, V (corresponding author), Wadia Inst Himalayan Geol, 33 GMS Rd, Dehra Dun 248001, Uttarakhand, India.
来源期刊QUATERNARY SCIENCE REVIEWS
ISSN0277-3791
EISSN1873-457X
出版年2021
卷号267
英文摘要This study examines the late Quaternary glacial history of Suru Basin and its associated tributary valleys (i.e., Achambur, Kangriz, Shafat, Rangdum, and Pensilugnpa), western Himalaya, based on the data collected from field surveys (2015-2019), satellite images, and optically stimulated luminescence (OSL) dating. The glaciers in Suru Basin have fluctuated greatly throughout the Marine Isotope Stages (MIS) 3 and 2 to the Little Ice Age (LIA), and are critical in understanding the linkages between regional and global climate change. Here, we present a detailed record of five major glacial advances of decreasing magnitude, dated 33-23 ka, 16 ka, 13-11 ka, 10-7.3 ka, 2.8-2.3 ka, and a minor advance dated 0.7-0.4 ka. These five major glacial advances are named from oldest to youngest as Suru- I to V, based on their optical chronology, geographical position, moraine stratigraphy, and glacially polished rock surfaces. Whereas, the equilibrium-line altitude (ELA) ascended by similar to 538 m from the oldest glacial advance (SuruI) to the present-day, followed by four other events (Suru-II, III, IV, and V) with ascended ELAs of similar to 522, similar to 399, similar to 243, and 215 m, respectively. Suru Basin has lost similar to 502 km(2) in its glaciated area and similar to 163 km(3) in ice volume from Suru-I to the present-day. The magnitude of glacier extent decreased from the MIS 3 and 2, early to late-Holocene, and LIA. The timing of these glacial advances is coarsely in agreement with North Atlantic millennial-scale climate oscillations (Heinrich events), signifying the probable correlation between these abrupt climate changes and glacial fluctuations in this semi-arid region of the Himalaya. (C) 2021 Elsevier Ltd. All rights reserved.
英文关键词Suru Basin MIS 3 and LIA Optically stimulated luminescence dating Equilibrium-line altitude North Atlantic millennia-scale climate oscillations Glacial advances Western Himalaya
类型Article
语种英语
收录类别SCI-E
WOS记录号WOS:000689256400004
WOS关键词INDIAN-SUMMER MONSOON ; LATE PLEISTOCENE GLACIATIONS ; SEA-SURFACE TEMPERATURE ; CHHOTA SHIGRI GLACIER ; NORTHERN-HEMISPHERE ; LADAKH HIMALAYA ; ZANSKAR RANGE ; ICE-AGE ; STIMULATED LUMINESCENCE ; MIDLATITUDE WESTERLIES
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/2XILL650/364448
作者单位[Kumar, Vinit; Mehta, Manish; Shukla, Aparna; Kumar, Anil; Garg, Siddhi] Wadia Inst Himalayan Geol, 33 GMS Rd, Dehra Dun 248001, Uttarakhand, India; [Shukla, Aparna] Minist Earth Sci, Lodhi Rd, New Delhi 110003, India
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GB/T 7714
Kumar, Vinit,Mehta, Manish,Shukla, Aparna,et al. Late Quaternary glacial advances and equilibrium-line altitude changes in a semi-arid region, Suru Basin, western Himalaya[J],2021,267.
APA Kumar, Vinit,Mehta, Manish,Shukla, Aparna,Kumar, Anil,&Garg, Siddhi.(2021).Late Quaternary glacial advances and equilibrium-line altitude changes in a semi-arid region, Suru Basin, western Himalaya.QUATERNARY SCIENCE REVIEWS,267.
MLA Kumar, Vinit,et al."Late Quaternary glacial advances and equilibrium-line altitude changes in a semi-arid region, Suru Basin, western Himalaya".QUATERNARY SCIENCE REVIEWS 267(2021).
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