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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Published in:Frontiers in Earth Science
Main Authors: Wu, Yang, Chen, Yiwei, Huang, Long, Ding, Ping, Cui, Hao, Wei, Gangjian
Format: Report
Language:English
Published: FRONTIERS MEDIA SA 2022
Subjects:
Online Access:http://ir.gig.ac.cn/handle/344008/68258
https://doi.org/10.3389/feart.2022.940013
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spelling 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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