Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau
A periglacial ground wedge in bajada gravel near the northern base of the Qinghai Nan Shan underlies loess of late- and postglacial age. The composition and structure of the wedge fill are consistent with an ice-wedge origin, implying former permafrost and relatively moist conditions at this localit...
Published in: | Permafrost and Periglacial Processes |
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Language: | English |
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JOHN WILEY & SONS LTD
2001
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Online Access: | http://ir.ieecas.cn/handle/361006/11926 https://doi.org/10.1002/ppp.386 |
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ftchinacascieeca:oai:ir.ieecas.cn:361006/11926 2023-06-11T04:09:38+02:00 Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau Porter, SC Singhvi, A An, ZS Lai, ZP 2001 http://ir.ieecas.cn/handle/361006/11926 https://doi.org/10.1002/ppp.386 英语 eng JOHN WILEY & SONS LTD PERMAFROST AND PERIGLACIAL PROCESSES http://ir.ieecas.cn/handle/361006/11926 doi:10.1002/ppp.386 null ice-wedge cast Pleistocene permafrost palaeoenvironment Tibet Physical Geography Geology WESTERN CHINA QAIDAM BASIN LAKE PERMAFROST EVOLUTION QINGHAI LOESS Geography Physical Article 期刊论文 2001 ftchinacascieeca https://doi.org/10.1002/ppp.386 2023-05-08T13:23:58Z A periglacial ground wedge in bajada gravel near the northern base of the Qinghai Nan Shan underlies loess of late- and postglacial age. The composition and structure of the wedge fill are consistent with an ice-wedge origin, implying former permafrost and relatively moist conditions at this locality. A luminescence date of 15,100 +/- 1600 years from the wedge fill marks the end of ice-wedge activity, which is inferred to have been during the last glaciation. The present mean annual air temperature (MAAT) (-0.7 degreesC) is too high to produce frost cracking and ice-wedge formation, but snowline depression of ca. 700-800 m in the adjacent mountains is consistent with a reduction in MAAT of at least 3.8 degreesC during the last glacial maximum. Such a temperature depression would reduce MAAT to values equivalent to Arctic regions now experiencing active ice-wedge growth. The absence of loess of full-glacial age and the presence of a weakly developed palaeosol atop the bajada gravel imply a stable, cold land surface. Qinghai Lake, although reduced in size at that time, likely raised local humidity to levels that favoured ice-wedge growth in this low-altitude sector (ca. 3000-3400 m) of the Tibetan Plateau. Copyright (C) 2001 John Wiley & Sons, Ltd. Article in Journal/Newspaper Arctic permafrost Permafrost and Periglacial Processes Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) Arctic Bajada ENVELOPE(-67.433,-67.433,-66.717,-66.717) Basin Lake ENVELOPE(-71.750,-71.750,67.083,67.083) Permafrost and Periglacial Processes 12 2 203 210 |
institution |
Open Polar |
collection |
Institute of Earth Environment: IEECAS OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchinacascieeca |
language |
English |
topic |
ice-wedge cast Pleistocene permafrost palaeoenvironment Tibet Physical Geography Geology WESTERN CHINA QAIDAM BASIN LAKE PERMAFROST EVOLUTION QINGHAI LOESS Geography Physical |
spellingShingle |
ice-wedge cast Pleistocene permafrost palaeoenvironment Tibet Physical Geography Geology WESTERN CHINA QAIDAM BASIN LAKE PERMAFROST EVOLUTION QINGHAI LOESS Geography Physical Porter, SC Singhvi, A An, ZS Lai, ZP Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau |
topic_facet |
ice-wedge cast Pleistocene permafrost palaeoenvironment Tibet Physical Geography Geology WESTERN CHINA QAIDAM BASIN LAKE PERMAFROST EVOLUTION QINGHAI LOESS Geography Physical |
description |
A periglacial ground wedge in bajada gravel near the northern base of the Qinghai Nan Shan underlies loess of late- and postglacial age. The composition and structure of the wedge fill are consistent with an ice-wedge origin, implying former permafrost and relatively moist conditions at this locality. A luminescence date of 15,100 +/- 1600 years from the wedge fill marks the end of ice-wedge activity, which is inferred to have been during the last glaciation. The present mean annual air temperature (MAAT) (-0.7 degreesC) is too high to produce frost cracking and ice-wedge formation, but snowline depression of ca. 700-800 m in the adjacent mountains is consistent with a reduction in MAAT of at least 3.8 degreesC during the last glacial maximum. Such a temperature depression would reduce MAAT to values equivalent to Arctic regions now experiencing active ice-wedge growth. The absence of loess of full-glacial age and the presence of a weakly developed palaeosol atop the bajada gravel imply a stable, cold land surface. Qinghai Lake, although reduced in size at that time, likely raised local humidity to levels that favoured ice-wedge growth in this low-altitude sector (ca. 3000-3400 m) of the Tibetan Plateau. Copyright (C) 2001 John Wiley & Sons, Ltd. |
format |
Article in Journal/Newspaper |
author |
Porter, SC Singhvi, A An, ZS Lai, ZP |
author_facet |
Porter, SC Singhvi, A An, ZS Lai, ZP |
author_sort |
Porter, SC |
title |
Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau |
title_short |
Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau |
title_full |
Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau |
title_fullStr |
Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau |
title_full_unstemmed |
Luminescence age and palaeoenvironmental implications of a late Pleistocene ground wedge on the northeastern Tibetan Plateau |
title_sort |
luminescence age and palaeoenvironmental implications of a late pleistocene ground wedge on the northeastern tibetan plateau |
publisher |
JOHN WILEY & SONS LTD |
publishDate |
2001 |
url |
http://ir.ieecas.cn/handle/361006/11926 https://doi.org/10.1002/ppp.386 |
long_lat |
ENVELOPE(-67.433,-67.433,-66.717,-66.717) ENVELOPE(-71.750,-71.750,67.083,67.083) |
geographic |
Arctic Bajada Basin Lake |
geographic_facet |
Arctic Bajada Basin Lake |
genre |
Arctic permafrost Permafrost and Periglacial Processes |
genre_facet |
Arctic permafrost Permafrost and Periglacial Processes |
op_relation |
PERMAFROST AND PERIGLACIAL PROCESSES http://ir.ieecas.cn/handle/361006/11926 doi:10.1002/ppp.386 |
op_rights |
null |
op_doi |
https://doi.org/10.1002/ppp.386 |
container_title |
Permafrost and Periglacial Processes |
container_volume |
12 |
container_issue |
2 |
container_start_page |
203 |
op_container_end_page |
210 |
_version_ |
1768383596552257536 |