Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation

The common methods used for grain-size analysis have their own deficiencies and limitations in terms of explaining the genesis of grain-size components. In this study, the end-member modeling analysis method is applied to multi-mode grain-size distributions of core sediment from Anguli-nuur lake to...

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Published in:Atmosphere
Main Authors: Junfeng Li, Xingqi Liu, Xin Mao, Huiqing Yang
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2022
Subjects:
Online Access:https://doi.org/10.3390/atmos13111826
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spelling ftmdpi:oai:mdpi.com:/2073-4433/13/11/1826/ 2023-08-20T04:08:26+02:00 Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation Junfeng Li Xingqi Liu Xin Mao Huiqing Yang agris 2022-11-02 application/pdf https://doi.org/10.3390/atmos13111826 EN eng Multidisciplinary Digital Publishing Institute Climatology https://dx.doi.org/10.3390/atmos13111826 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 13; Issue 11; Pages: 1826 grain-size distribution last deglaciation northern China Anguli-nuur lake Asian monsoon Text 2022 ftmdpi https://doi.org/10.3390/atmos13111826 2023-08-01T07:10:06Z The common methods used for grain-size analysis have their own deficiencies and limitations in terms of explaining the genesis of grain-size components. In this study, the end-member modeling analysis method is applied to multi-mode grain-size distributions of core sediment from Anguli-nuur lake to help to understand the sediment provenance, transport processes and sedimentary environment. Four optimal end-members are unmixed, and three transport-deposition processes are revealed, including the runoff, wave and aeolian processes. The humidity index synthesized by the runoff and aeolian end-members in the core sediment is used to reconstruct the humidity variability in the East Asian monsoonal domain since the last deglaciation. Our record shows that the patterns of humidity variability are coincidentally linked with the monsoonal precipitation index from the same core and stalagmite record in southern China. The Holocene optimum is identified in early and middle Holocene. In addition, a series of millennial- and multi-centennial-scale dry events documented in our record are well correlated with the ice-rafted debris events in the North Atlantic. The results reveal that the grain-size record from Anguli-nuur lake is sensitive in response to moisture variability in northern China. Text North Atlantic MDPI Open Access Publishing Atmosphere 13 11 1826
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic grain-size distribution
last deglaciation
northern China
Anguli-nuur lake
Asian monsoon
spellingShingle grain-size distribution
last deglaciation
northern China
Anguli-nuur lake
Asian monsoon
Junfeng Li
Xingqi Liu
Xin Mao
Huiqing Yang
Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation
topic_facet grain-size distribution
last deglaciation
northern China
Anguli-nuur lake
Asian monsoon
description The common methods used for grain-size analysis have their own deficiencies and limitations in terms of explaining the genesis of grain-size components. In this study, the end-member modeling analysis method is applied to multi-mode grain-size distributions of core sediment from Anguli-nuur lake to help to understand the sediment provenance, transport processes and sedimentary environment. Four optimal end-members are unmixed, and three transport-deposition processes are revealed, including the runoff, wave and aeolian processes. The humidity index synthesized by the runoff and aeolian end-members in the core sediment is used to reconstruct the humidity variability in the East Asian monsoonal domain since the last deglaciation. Our record shows that the patterns of humidity variability are coincidentally linked with the monsoonal precipitation index from the same core and stalagmite record in southern China. The Holocene optimum is identified in early and middle Holocene. In addition, a series of millennial- and multi-centennial-scale dry events documented in our record are well correlated with the ice-rafted debris events in the North Atlantic. The results reveal that the grain-size record from Anguli-nuur lake is sensitive in response to moisture variability in northern China.
format Text
author Junfeng Li
Xingqi Liu
Xin Mao
Huiqing Yang
author_facet Junfeng Li
Xingqi Liu
Xin Mao
Huiqing Yang
author_sort Junfeng Li
title Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation
title_short Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation
title_full Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation
title_fullStr Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation
title_full_unstemmed Grain-Size End-Members of Anguli-Nuur Lake Core Sediments: Evidence for Moisture Variability in Northern China since the Last Deglaciation
title_sort grain-size end-members of anguli-nuur lake core sediments: evidence for moisture variability in northern china since the last deglaciation
publisher Multidisciplinary Digital Publishing Institute
publishDate 2022
url https://doi.org/10.3390/atmos13111826
op_coverage agris
genre North Atlantic
genre_facet North Atlantic
op_source Atmosphere; Volume 13; Issue 11; Pages: 1826
op_relation Climatology
https://dx.doi.org/10.3390/atmos13111826
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos13111826
container_title Atmosphere
container_volume 13
container_issue 11
container_start_page 1826
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