Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet

We present a record of monsoon variations for the early and middle Holocene that is inferred from the geochemistry of sediment cores from Ahung Co, a lake in central Tibet. The resolution of this record is better than 50 yr and the age model is derived from radiocarbon ages of terrestrial charcoal,...

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Published in:Quaternary Research
Main Authors: Morrill, C, Overpeck, JT, Cole, JE, Liu, KB, Shen, CM, Tang, LY
Format: Report
Language:English
Published: ACADEMIC PRESS INC ELSEVIER SCIENCE 2006
Subjects:
Online Access:http://ir.nigpas.ac.cn/handle/332004/19149
https://doi.org/10.1016/j.yqres.2005.02.014
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spelling ftchinacscnigpas:oai:ir.nigpas.ac.cn:332004/19149 2023-05-15T16:39:18+02:00 Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet Morrill, C Overpeck, JT Cole, JE Liu, KB Shen, CM Tang, LY 2006-03-01 http://ir.nigpas.ac.cn/handle/332004/19149 https://doi.org/10.1016/j.yqres.2005.02.014 英语 eng ACADEMIC PRESS INC ELSEVIER SCIENCE QUATERNARY RESEARCH http://ir.nigpas.ac.cn/handle/332004/19149 doi:10.1016/j.yqres.2005.02.014 precipitation monsoon Holocene climate change oxygen stable isotopes paleoclimate hard-water effect aquatic macrophytes BASIN WESTERN TIBET SUMMER MONSOON ENVIRONMENTAL-CHANGES INDIAN MONSOON EUTROPHIC LAKES 2 SHALLOW ICE CORE CLIMATE PLATEAU QINGHAI Physical Geography Geology Geography Physical Geosciences Multidisciplinary 期刊论文 2006 ftchinacscnigpas https://doi.org/10.1016/j.yqres.2005.02.014 2019-08-14T12:44:08Z We present a record of monsoon variations for the early and middle Holocene that is inferred from the geochemistry of sediment cores from Ahung Co, a lake in central Tibet. The resolution of this record is better than 50 yr and the age model is derived from radiocarbon ages of terrestrial charcoal, which eliminates errors associated with the lake hard-water effect. We made down-core geochemical measurements of % carbonate, % organic carbon, C/N and delta C-13 of bulk organic matter, delta C-13 and delta O-18 of carbonate, and % dolomite. Proxy calibration and modern water-balance reconstruction show that these are proxies for lake depth and the amount of monsoon precipitation. We find that lake level and monsoon precipitation have been decreasing at Ahung Co since the early Holocene (similar to 7500 cal yr B.P.). Superimposed on this trend are rapid declines in monsoon rainfall at 7000-7500 and 4700 cal yr B.P. and seven century-scale wet-dry oscillations. The cores do not contain sediment from the last similar to 4000 yr. Surface sediments from the lake accumulated during the 20th century, however. From this, we argue that lake levels have risen again recently following a late Holocene dry period. (c) 2005 University of Washington. All rights reserved. Report ice core Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences) Indian Quaternary Research 65 02 232 243
institution Open Polar
collection Nanjing Institute of Geology and Palaeontology: NIGPAS OpenIR (Chinese Academy of Sciences)
op_collection_id ftchinacscnigpas
language English
topic precipitation
monsoon
Holocene
climate change
oxygen stable isotopes
paleoclimate
hard-water effect
aquatic macrophytes
BASIN WESTERN TIBET
SUMMER MONSOON
ENVIRONMENTAL-CHANGES
INDIAN MONSOON
EUTROPHIC LAKES
2 SHALLOW
ICE CORE
CLIMATE
PLATEAU
QINGHAI
Physical Geography
Geology
Geography
Physical
Geosciences
Multidisciplinary
spellingShingle precipitation
monsoon
Holocene
climate change
oxygen stable isotopes
paleoclimate
hard-water effect
aquatic macrophytes
BASIN WESTERN TIBET
SUMMER MONSOON
ENVIRONMENTAL-CHANGES
INDIAN MONSOON
EUTROPHIC LAKES
2 SHALLOW
ICE CORE
CLIMATE
PLATEAU
QINGHAI
Physical Geography
Geology
Geography
Physical
Geosciences
Multidisciplinary
Morrill, C
Overpeck, JT
Cole, JE
Liu, KB
Shen, CM
Tang, LY
Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet
topic_facet precipitation
monsoon
Holocene
climate change
oxygen stable isotopes
paleoclimate
hard-water effect
aquatic macrophytes
BASIN WESTERN TIBET
SUMMER MONSOON
ENVIRONMENTAL-CHANGES
INDIAN MONSOON
EUTROPHIC LAKES
2 SHALLOW
ICE CORE
CLIMATE
PLATEAU
QINGHAI
Physical Geography
Geology
Geography
Physical
Geosciences
Multidisciplinary
description We present a record of monsoon variations for the early and middle Holocene that is inferred from the geochemistry of sediment cores from Ahung Co, a lake in central Tibet. The resolution of this record is better than 50 yr and the age model is derived from radiocarbon ages of terrestrial charcoal, which eliminates errors associated with the lake hard-water effect. We made down-core geochemical measurements of % carbonate, % organic carbon, C/N and delta C-13 of bulk organic matter, delta C-13 and delta O-18 of carbonate, and % dolomite. Proxy calibration and modern water-balance reconstruction show that these are proxies for lake depth and the amount of monsoon precipitation. We find that lake level and monsoon precipitation have been decreasing at Ahung Co since the early Holocene (similar to 7500 cal yr B.P.). Superimposed on this trend are rapid declines in monsoon rainfall at 7000-7500 and 4700 cal yr B.P. and seven century-scale wet-dry oscillations. The cores do not contain sediment from the last similar to 4000 yr. Surface sediments from the lake accumulated during the 20th century, however. From this, we argue that lake levels have risen again recently following a late Holocene dry period. (c) 2005 University of Washington. All rights reserved.
format Report
author Morrill, C
Overpeck, JT
Cole, JE
Liu, KB
Shen, CM
Tang, LY
author_facet Morrill, C
Overpeck, JT
Cole, JE
Liu, KB
Shen, CM
Tang, LY
author_sort Morrill, C
title Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet
title_short Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet
title_full Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet
title_fullStr Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet
title_full_unstemmed Holocene variations in the Asian monsoon inferred from the geochemistry of lake sediments in central Tibet
title_sort holocene variations in the asian monsoon inferred from the geochemistry of lake sediments in central tibet
publisher ACADEMIC PRESS INC ELSEVIER SCIENCE
publishDate 2006
url http://ir.nigpas.ac.cn/handle/332004/19149
https://doi.org/10.1016/j.yqres.2005.02.014
geographic Indian
geographic_facet Indian
genre ice core
genre_facet ice core
op_relation QUATERNARY RESEARCH
http://ir.nigpas.ac.cn/handle/332004/19149
doi:10.1016/j.yqres.2005.02.014
op_doi https://doi.org/10.1016/j.yqres.2005.02.014
container_title Quaternary Research
container_volume 65
container_issue 02
container_start_page 232
op_container_end_page 243
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