Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia

We describe the last glaciation climatic history Marine Isotope Stage (MIS, 2–4) from 66.7 ka to 14.5 ka in Hexigten, northeast Inner Mongolia, North China. The climate of the region experienced frequent and significant fluctuations between dry-cold and less dry-cold during the late MIS4. The climat...

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Published in:Geoscience Frontiers
Main Authors: Ji-Ling Song, Hong-Yan Sun, Ming-Zhong Tian, Xu-Jiao Zhang, Xue-Feng Wen, Miao Sun
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier 2018
Subjects:
Online Access:https://doi.org/10.1016/j.gsf.2017.03.005
https://doaj.org/article/6626eff32dc44a119946730d44c09582
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spelling ftdoajarticles:oai:doaj.org/article:6626eff32dc44a119946730d44c09582 2023-10-01T03:56:22+02:00 Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia Ji-Ling Song Hong-Yan Sun Ming-Zhong Tian Xu-Jiao Zhang Xue-Feng Wen Miao Sun 2018-03-01T00:00:00Z https://doi.org/10.1016/j.gsf.2017.03.005 https://doaj.org/article/6626eff32dc44a119946730d44c09582 EN eng Elsevier http://www.sciencedirect.com/science/article/pii/S1674987117300555 https://doaj.org/toc/1674-9871 1674-9871 doi:10.1016/j.gsf.2017.03.005 https://doaj.org/article/6626eff32dc44a119946730d44c09582 Geoscience Frontiers, Vol 9, Iss 2, Pp 431-439 (2018) Climate record Dune activity Inner Mongolia East Asian monsoon Marine isotope stage 2–4 Heinrich events Geology QE1-996.5 article 2018 ftdoajarticles https://doi.org/10.1016/j.gsf.2017.03.005 2023-09-03T00:35:52Z We describe the last glaciation climatic history Marine Isotope Stage (MIS, 2–4) from 66.7 ka to 14.5 ka in Hexigten, northeast Inner Mongolia, North China. The climate of the region experienced frequent and significant fluctuations between dry-cold and less dry-cold during the late MIS4. The climate was generally warm and humid during early MIS3 (MIS3c) and late MIS3 (MIS3a), whereas it was cold and dry in middle MIS3 (MIS3b) and during MIS2. In this study, the cold and dry conditions were correlated with a stronger East Asian winter monsoon and strong dune activity; whereas, warm and humid conditions were related to a stronger East Asian summer monsoon (EASM) and weak dune activity. This study establishes six distinct dry and cold intervals during the last glacial period (66.7–14.5 ka) based on optically stimulated luminescence data, multi-proxies record (magnetic susceptibility, grain size analysis, Rb/Sr, SiO2/TiO2) and chemical index of alteration (CIA). The last glacial period may be correlated with Heinrich events 1 to 6 which were further confirmed by comparison with the Hulu cave stalagmites and Greenland ice core records. It is concluded that the study area was substantially affected by the EASM, as compared with the loess–desert transition zone of the Chinese Loess Plateau, especially in MIS3c and suggested that the East Asian monsoon played a pivotal role in the last glacial period climate and dune activity. Article in Journal/Newspaper Greenland Greenland ice core ice core Directory of Open Access Journals: DOAJ Articles Greenland Hulu ENVELOPE(8.610,8.610,62.837,62.837) Geoscience Frontiers 9 2 431 439
institution Open Polar
collection Directory of Open Access Journals: DOAJ Articles
op_collection_id ftdoajarticles
language English
topic Climate record
Dune activity
Inner Mongolia
East Asian monsoon
Marine isotope stage 2–4
Heinrich events
Geology
QE1-996.5
spellingShingle Climate record
Dune activity
Inner Mongolia
East Asian monsoon
Marine isotope stage 2–4
Heinrich events
Geology
QE1-996.5
Ji-Ling Song
Hong-Yan Sun
Ming-Zhong Tian
Xu-Jiao Zhang
Xue-Feng Wen
Miao Sun
Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia
topic_facet Climate record
Dune activity
Inner Mongolia
East Asian monsoon
Marine isotope stage 2–4
Heinrich events
Geology
QE1-996.5
description We describe the last glaciation climatic history Marine Isotope Stage (MIS, 2–4) from 66.7 ka to 14.5 ka in Hexigten, northeast Inner Mongolia, North China. The climate of the region experienced frequent and significant fluctuations between dry-cold and less dry-cold during the late MIS4. The climate was generally warm and humid during early MIS3 (MIS3c) and late MIS3 (MIS3a), whereas it was cold and dry in middle MIS3 (MIS3b) and during MIS2. In this study, the cold and dry conditions were correlated with a stronger East Asian winter monsoon and strong dune activity; whereas, warm and humid conditions were related to a stronger East Asian summer monsoon (EASM) and weak dune activity. This study establishes six distinct dry and cold intervals during the last glacial period (66.7–14.5 ka) based on optically stimulated luminescence data, multi-proxies record (magnetic susceptibility, grain size analysis, Rb/Sr, SiO2/TiO2) and chemical index of alteration (CIA). The last glacial period may be correlated with Heinrich events 1 to 6 which were further confirmed by comparison with the Hulu cave stalagmites and Greenland ice core records. It is concluded that the study area was substantially affected by the EASM, as compared with the loess–desert transition zone of the Chinese Loess Plateau, especially in MIS3c and suggested that the East Asian monsoon played a pivotal role in the last glacial period climate and dune activity.
format Article in Journal/Newspaper
author Ji-Ling Song
Hong-Yan Sun
Ming-Zhong Tian
Xu-Jiao Zhang
Xue-Feng Wen
Miao Sun
author_facet Ji-Ling Song
Hong-Yan Sun
Ming-Zhong Tian
Xu-Jiao Zhang
Xue-Feng Wen
Miao Sun
author_sort Ji-Ling Song
title Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia
title_short Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia
title_full Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia
title_fullStr Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia
title_full_unstemmed Heinrich events recorded in a loess–paleosol sequence from Hexigten, Inner Mongolia
title_sort heinrich events recorded in a loess–paleosol sequence from hexigten, inner mongolia
publisher Elsevier
publishDate 2018
url https://doi.org/10.1016/j.gsf.2017.03.005
https://doaj.org/article/6626eff32dc44a119946730d44c09582
long_lat ENVELOPE(8.610,8.610,62.837,62.837)
geographic Greenland
Hulu
geographic_facet Greenland
Hulu
genre Greenland
Greenland ice core
ice core
genre_facet Greenland
Greenland ice core
ice core
op_source Geoscience Frontiers, Vol 9, Iss 2, Pp 431-439 (2018)
op_relation http://www.sciencedirect.com/science/article/pii/S1674987117300555
https://doaj.org/toc/1674-9871
1674-9871
doi:10.1016/j.gsf.2017.03.005
https://doaj.org/article/6626eff32dc44a119946730d44c09582
op_doi https://doi.org/10.1016/j.gsf.2017.03.005
container_title Geoscience Frontiers
container_volume 9
container_issue 2
container_start_page 431
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