OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau
Well-preserved paleo-shoreline systems suggest lake shrinkage occurred in a vast region of the Tibetan Plateau, indicating dramatic paleo-environmental changes that linked closely to variations in Asian monsoon precipitation, glacial meltwater, and evaporation. The elevation and chronology of these...
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Online Access: | http://ir.gig.ac.cn/handle/344008/68258 https://doi.org/10.3389/feart.2022.940013 |
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ftchacadscgigcas:oai:ir.gig.ac.cn:344008/68258 2023-05-15T16:39:17+02:00 OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau Wu, Yang Chen, Yiwei Huang, Long Ding, Ping Cui, Hao Wei, Gangjian 2022-07-11 http://ir.gig.ac.cn/handle/344008/68258 https://doi.org/10.3389/feart.2022.940013 英语 eng FRONTIERS MEDIA SA FRONTIERS IN EARTH SCIENCE http://ir.gig.ac.cn/handle/344008/68258 doi:10.3389/feart.2022.940013 Geology paleo-shoreline OSL dating Dagze Co lake level change Tibetan Plateau Geosciences Multidisciplinary SUMMER MONSOON ASIAN MONSOON QINGHAI LAKE BEACH RIDGES TANGRA YUMCO ICE CORE HOLOCENE LUMINESCENCE CLIMATE BASIN 期刊论文 2022 ftchacadscgigcas https://doi.org/10.3389/feart.2022.940013 2022-12-19T19:17:10Z Well-preserved paleo-shoreline systems suggest lake shrinkage occurred in a vast region of the Tibetan Plateau, indicating dramatic paleo-environmental changes that linked closely to variations in Asian monsoon precipitation, glacial meltwater, and evaporation. The elevation and chronology of these shoreline features can be used to reconstruct lake level fluctuation history and regional paleo-climate. Here, we report optically stimulated luminescence (OSL) dating of 14 sediment samples from three of seven paleo-shorelines at south of Dagze Co, central Tibetan Plateau, using coarse-grained quartz and K-feldspar. Two fine grain silt samples were also measured. The results suggest the following: 1) The highest paleo-shoreline for Dagze Co has an elevation around 4,525 m (+55 m above modern lake). Its age is estimated to be 9.1 +/- 0.5 to 9.6 +/- 0.6 ka, suggesting a relative humid condition in the early Holocene. 2) After that, the lake level dropped similar to 20 m and remained relatively stable (+35 m) from similar to 8 to 5 ka, implying a dry condition with reduced runoff. Lake level further declined for similar to 40 m since about 5 ka. 3) The general trend of shrinkage for Dagze Co broadly matches studies from adjacent lakes, suggesting a common pattern of lake's evolution on the south/central plateau in the late Quaternary. The long-term decreasing trend of Asian monsoon precipitation should be the main reason. Report ice core Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences) Tangra ENVELOPE(-60.100,-60.100,-62.667,-62.667) Frontiers in Earth Science 10 |
institution |
Open Polar |
collection |
Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchacadscgigcas |
language |
English |
topic |
Geology paleo-shoreline OSL dating Dagze Co lake level change Tibetan Plateau Geosciences Multidisciplinary SUMMER MONSOON ASIAN MONSOON QINGHAI LAKE BEACH RIDGES TANGRA YUMCO ICE CORE HOLOCENE LUMINESCENCE CLIMATE BASIN |
spellingShingle |
Geology paleo-shoreline OSL dating Dagze Co lake level change Tibetan Plateau Geosciences Multidisciplinary SUMMER MONSOON ASIAN MONSOON QINGHAI LAKE BEACH RIDGES TANGRA YUMCO ICE CORE HOLOCENE LUMINESCENCE CLIMATE BASIN Wu, Yang Chen, Yiwei Huang, Long Ding, Ping Cui, Hao Wei, Gangjian OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau |
topic_facet |
Geology paleo-shoreline OSL dating Dagze Co lake level change Tibetan Plateau Geosciences Multidisciplinary SUMMER MONSOON ASIAN MONSOON QINGHAI LAKE BEACH RIDGES TANGRA YUMCO ICE CORE HOLOCENE LUMINESCENCE CLIMATE BASIN |
description |
Well-preserved paleo-shoreline systems suggest lake shrinkage occurred in a vast region of the Tibetan Plateau, indicating dramatic paleo-environmental changes that linked closely to variations in Asian monsoon precipitation, glacial meltwater, and evaporation. The elevation and chronology of these shoreline features can be used to reconstruct lake level fluctuation history and regional paleo-climate. Here, we report optically stimulated luminescence (OSL) dating of 14 sediment samples from three of seven paleo-shorelines at south of Dagze Co, central Tibetan Plateau, using coarse-grained quartz and K-feldspar. Two fine grain silt samples were also measured. The results suggest the following: 1) The highest paleo-shoreline for Dagze Co has an elevation around 4,525 m (+55 m above modern lake). Its age is estimated to be 9.1 +/- 0.5 to 9.6 +/- 0.6 ka, suggesting a relative humid condition in the early Holocene. 2) After that, the lake level dropped similar to 20 m and remained relatively stable (+35 m) from similar to 8 to 5 ka, implying a dry condition with reduced runoff. Lake level further declined for similar to 40 m since about 5 ka. 3) The general trend of shrinkage for Dagze Co broadly matches studies from adjacent lakes, suggesting a common pattern of lake's evolution on the south/central plateau in the late Quaternary. The long-term decreasing trend of Asian monsoon precipitation should be the main reason. |
format |
Report |
author |
Wu, Yang Chen, Yiwei Huang, Long Ding, Ping Cui, Hao Wei, Gangjian |
author_facet |
Wu, Yang Chen, Yiwei Huang, Long Ding, Ping Cui, Hao Wei, Gangjian |
author_sort |
Wu, Yang |
title |
OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau |
title_short |
OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau |
title_full |
OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau |
title_fullStr |
OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau |
title_full_unstemmed |
OSL Dating of Paleo-Shorelines at Dagze Co, Central Tibetan Plateau |
title_sort |
osl dating of paleo-shorelines at dagze co, central tibetan plateau |
publisher |
FRONTIERS MEDIA SA |
publishDate |
2022 |
url |
http://ir.gig.ac.cn/handle/344008/68258 https://doi.org/10.3389/feart.2022.940013 |
long_lat |
ENVELOPE(-60.100,-60.100,-62.667,-62.667) |
geographic |
Tangra |
geographic_facet |
Tangra |
genre |
ice core |
genre_facet |
ice core |
op_relation |
FRONTIERS IN EARTH SCIENCE http://ir.gig.ac.cn/handle/344008/68258 doi:10.3389/feart.2022.940013 |
op_doi |
https://doi.org/10.3389/feart.2022.940013 |
container_title |
Frontiers in Earth Science |
container_volume |
10 |
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1766029617221599232 |