Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia

Desertification and drought in inland Asia are closely related to human habitation and social sustainability in western China. The climate in western China has experienced multiple shifts in temperature and aridity since the Late Pleistocene. Investigating this region's Late Pleistocene paleocl...

Full description

Bibliographic Details
Main Authors: WEI Lijie, LI Zhenhong, LI Mingtao, DONG Xiaopeng, CUI Jiawei, KOU Linlin
Format: Article
Language:zho
Published: Institute of Geomechanics, Chinese Academy of Geological Sciences 2023-10-01
Series:Dizhi lixue xuebao
Subjects:
Online Access:https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2023015
_version_ 1797352454449266688
author WEI Lijie
LI Zhenhong
LI Mingtao
DONG Xiaopeng
CUI Jiawei
KOU Linlin
author_facet WEI Lijie
LI Zhenhong
LI Mingtao
DONG Xiaopeng
CUI Jiawei
KOU Linlin
author_sort WEI Lijie
collection DOAJ
description Desertification and drought in inland Asia are closely related to human habitation and social sustainability in western China. The climate in western China has experienced multiple shifts in temperature and aridity since the Late Pleistocene. Investigating this region's Late Pleistocene paleoclimatic changes contributes to predicting future climate trends. This study analyzes the pollen records from the Qingshuihe Basin in southern Ningxia during the middle to late Late Pleistocene, revealing four distinct pollen assemblage zones from bottom to top. These zones reflect paleovegetation and paleoclimate changes during the middle to late Late Pleistocene. The results indicate that during the middle Late Pleistocene (75-50 ka B.P.), the region featured a predominantly Artemisia-dominated steppe landscape with a cool and relatively dry climate. In the late Late Pleistocene (25-15 ka B.P.), the area experienced alternations between desert-steppe or steppe and forest-steppe, transitioning gradually to desert-steppe. During this period, the winter monsoon strengthened, leading to progressively cooler and drier conditions, with the climate shifting from cool and slightly moist to cold and arid. The further study of the palynological records during the middle and late Late Pleistocene in the Qingshuihe Basin of southern Ningxia holds significant implications for a proper understanding of the natural environmental history of the Loess Plateau and informs decision-making for its management.
first_indexed 2024-03-08T13:16:46Z
format Article
id doaj.art-d5be0297c68c46e5bb7063bfeaf8477b
institution Directory Open Access Journal
issn 1006-6616
language zho
last_indexed 2024-03-08T13:16:46Z
publishDate 2023-10-01
publisher Institute of Geomechanics, Chinese Academy of Geological Sciences
record_format Article
series Dizhi lixue xuebao
spelling doaj.art-d5be0297c68c46e5bb7063bfeaf8477b2024-01-18T06:51:52ZzhoInstitute of Geomechanics, Chinese Academy of Geological SciencesDizhi lixue xuebao1006-66162023-10-0129566267310.12090/j.issn.1006-6616.2023015Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, NingxiaWEI LijieLI ZhenhongLI Mingtao0DONG XiaopengCUI JiaweiKOU LinlinSchool of Earth Sciences and Resources, China University of Geosciences (Beijing), Beijing 100083, ChinaDesertification and drought in inland Asia are closely related to human habitation and social sustainability in western China. The climate in western China has experienced multiple shifts in temperature and aridity since the Late Pleistocene. Investigating this region's Late Pleistocene paleoclimatic changes contributes to predicting future climate trends. This study analyzes the pollen records from the Qingshuihe Basin in southern Ningxia during the middle to late Late Pleistocene, revealing four distinct pollen assemblage zones from bottom to top. These zones reflect paleovegetation and paleoclimate changes during the middle to late Late Pleistocene. The results indicate that during the middle Late Pleistocene (75-50 ka B.P.), the region featured a predominantly Artemisia-dominated steppe landscape with a cool and relatively dry climate. In the late Late Pleistocene (25-15 ka B.P.), the area experienced alternations between desert-steppe or steppe and forest-steppe, transitioning gradually to desert-steppe. During this period, the winter monsoon strengthened, leading to progressively cooler and drier conditions, with the climate shifting from cool and slightly moist to cold and arid. The further study of the palynological records during the middle and late Late Pleistocene in the Qingshuihe Basin of southern Ningxia holds significant implications for a proper understanding of the natural environmental history of the Loess Plateau and informs decision-making for its management.https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2023015ningxiaqingshuihe basinmiddle and late late pleistocenepalynological recordspaleovegetationpaleoclimate
spellingShingle WEI Lijie
LI Zhenhong
LI Mingtao
DONG Xiaopeng
CUI Jiawei
KOU Linlin
Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia
Dizhi lixue xuebao
ningxia
qingshuihe basin
middle and late late pleistocene
palynological records
paleovegetation
paleoclimate
title Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia
title_full Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia
title_fullStr Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia
title_full_unstemmed Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia
title_short Palynological records and paleoclimatic significance during the middle and late Late Pleistocene in the Qingshuihe Basin, Ningxia
title_sort palynological records and paleoclimatic significance during the middle and late late pleistocene in the qingshuihe basin ningxia
topic ningxia
qingshuihe basin
middle and late late pleistocene
palynological records
paleovegetation
paleoclimate
url https://journal.geomech.ac.cn//article/doi/10.12090/j.issn.1006-6616.2023015
work_keys_str_mv AT weilijie palynologicalrecordsandpaleoclimaticsignificanceduringthemiddleandlatelatepleistoceneintheqingshuihebasinningxia
AT lizhenhong palynologicalrecordsandpaleoclimaticsignificanceduringthemiddleandlatelatepleistoceneintheqingshuihebasinningxia
AT limingtao palynologicalrecordsandpaleoclimaticsignificanceduringthemiddleandlatelatepleistoceneintheqingshuihebasinningxia
AT dongxiaopeng palynologicalrecordsandpaleoclimaticsignificanceduringthemiddleandlatelatepleistoceneintheqingshuihebasinningxia
AT cuijiawei palynologicalrecordsandpaleoclimaticsignificanceduringthemiddleandlatelatepleistoceneintheqingshuihebasinningxia
AT koulinlin palynologicalrecordsandpaleoclimaticsignificanceduringthemiddleandlatelatepleistoceneintheqingshuihebasinningxia