Sedimentary evolution revealed by aeolian and lacustrine depositions in the southern margin of the Weihe Basin during the Early Pleistocene

Wang Ting; Zhang Hang; Sun Youbin

doi:10.19509/j.cnki.dzkq.tb20220111

Volume 42 Issue 6

Nov. 2023

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Wang Ting, Zhang Hang, Sun Youbin. Sedimentary evolution revealed by aeolian and lacustrine depositions in the southern margin of the Weihe Basin during the Early Pleistocene[J]. Bulletin of Geological Science and Technology, 2023, 42(6): 95-105. doi: 10.19509/j.cnki.dzkq.tb20220111

Citation:

Wang Ting, Zhang Hang, Sun Youbin. Sedimentary evolution revealed by aeolian and lacustrine depositions in the southern margin of the Weihe Basin during the Early Pleistocene[J]. Bulletin of Geological Science and Technology, 2023, 42(6): 95-105. doi: 10.19509/j.cnki.dzkq.tb20220111

Citation:

Wang Ting, Zhang Hang, Sun Youbin. Sedimentary evolution revealed by aeolian and lacustrine depositions in the southern margin of the Weihe Basin during the Early Pleistocene[J]. Bulletin of Geological Science and Technology, 2023, 42(6): 95-105. doi: 10.19509/j.cnki.dzkq.tb20220111

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Sedimentary evolution revealed by aeolian and lacustrine depositions in the southern margin of the Weihe Basin during the Early Pleistocene

doi: 10.19509/j.cnki.dzkq.tb20220111

Wang Ting^{1a, 2, 3
,},
Zhang Hang^{1a, 3},
Sun Youbin^{1a, 1b
,
,}

1a.
State Key Laboratory of Loess and Quaternary Geology, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
1b.
Centerfor Excellencein Quaternary Science and Global Change, Institute of Earth Environment, Chinese Academy of Sciences, Xi'an 710061, China
2.
Hubei Engineering University, Xiaogan Hubei 432000, China
3.
University of Chinese Academy of Sciences, Beijing 100049, China

Received Date: 17 Mar 2022
Accepted Date: 10 May 2022
Rev Recd Date: 06 May 2022

Abstract

Abstract

<p>The Quaternary climate is characterized by a notable cooling and significant glacial-interglacial fluctuations driven by the influence of orbital-induced insolation and bipolar ice-volume variability. The Weihe Basin, located in the critical zone of the Asian monsoon region, accumulated thick fluvial-lacustrine deposition and aeolian deposition since the Cenozoic, which is a key placeto explore the environmental evolution during the Quaternary period.</p></sec><sec><title>Objective
The fluvial-lacustrine strata of the Sanmen Formation in the Weihe Basin are considered to be closely related to Palaeo-Sanmen Lake. However, the relationship among the stratigraphic age of the Sanmen Formation, the evolution of the palaeolake as well as the evolution of regional tectonics is still under much debated.
Methods
In this work, the magnetic susceptibility and grain size records from two sections (Yanyu and Wujiabu) in the southern margin of the Weihe Basin have been generated to investigate sedimentary evolution during the interval of 2.6-1.6 Ma.
Results
The mean grain size (MGS) and magnetic susceptibility (MS) of the Yanyu loess exhibit large-amplitude variations as proxies for the East Asian winter and summer monsoons. The MGS and MS variations in theWujiabu section show that lithology changes from lacustrine to aeolian facies occurred at 1.95 Ma in the southern margin of the Weihe Basin. In lacustrine environments, MGS is positively correlated with MS and is sensitive to fluctuations in lake level linked with monsoonal precipitation.
Conclusion
Overall, the climatic characteristics on the margin of the Weihe Basin during the early Pleistocene can be divided into two intervals: ① the lake level frequently fluctuated during 2.6-1.95 Ma, ② the lake shrank from 1.95 to 1.6 Ma. We suggest that the disappearance of Palaeo-Sanmen Lake was affected by the development and integration of the Yellow River.
- Weihe Basin,
- Early Pleistocene,
- lacustrine deposition,
- aeolian loess,
- Palaeo-Sanmen Lake

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References(83)

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Sedimentary evolution revealed by aeolian and lacustrine depositions in the southern margin of the Weihe Basin during the Early Pleistocene

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Sedimentary evolution revealed by aeolian and lacustrine depositions in the southern margin of the Weihe Basin during the Early Pleistocene

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