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Dataset of Intensity of the Major Elements and Magnetic Susceptibility in Lake Core on the Western Loess Plateau over the Middle-Late Holocene


LEI Qianqian1GUO Chao*1
1 College of Resource Environment and Tourism,Hubei University of Arts and Science,Xiangyang 441053,China

DOI:10.3974/geodb.2024.11.05.V1

Published:Nov. 2024

Visitors:13       Data Files Downloaded:1      
Data Downloaded:0.08 MB      Citations:

Key Words:

Elemental chemistry,Holocene,Climate change,Human activity

Abstract:

The dataset is developed based on Chaona lake sediment core located in the western part of the Loess Plateau. A series of 970-cm sediment cores which were recovered from the lake basin using by a piston corer equipment in 2016. The data of chemical elements and magnetic susceptibility was determined at 0.1-0.5 cm resolution using X-ray fluorescence (XRF) core-scanning measurements. Based on a robust chronology sequence that was established by a multiple dating approach and high-resolution, continuous elemental geochemistry and magnetic susceptibility records, a sedimentological and geochemical reconstructions of environment and climate variations spanning the Middle-Late Holocene was conducted. The dataset includes: (1) the geo-location of sediment core; (2) the age sequence of a lake core on the Loess Plateau over the past 6000 years; (3) the variation of the major elements (Al, Si, S, K, Ca, Ti, Mn, Rb, Sr, Br and Fe) in lake core over the past 6000 years; (4) the variation of element ratios (Si/Ti and Rb/Sr) in lake core over the past 6000 years; (5) the variation of the magnetic susceptibility in lake core over the past 6000 years. The temporal resolution of the element and magnetic susceptibility data is 10 years. The dataset is archived in .shp and .xlsx formats, and consist of 9 data files with data size of 86.8 KB (Compressed into one file with 84.6 KB). The analysis paper based on this dataset has been published in Palaeogeography, Palaeoclimatology, Palaeoecology, Issue 644, 2024.

Foundation Item:

Nature Science Foundation of Hubei Province (2023AFD059)

Data Citation:

LEI Qianqian, GUO Chao*.Dataset of Intensity of the Major Elements and Magnetic Susceptibility in Lake Core on the Western Loess Plateau over the Middle-Late Holocene[J/DB/OL]. Digital Journal of Global Change Data Repository, 2024. https://doi.org/10.3974/geodb.2024.11.05.V1.

References:


     [1] Kylander, M. E., Ampel, L., Wohlfarth, B., et al. High-resolution X-ray fluorescence core scanning analysis of Les Echets (France) sedimentary sequence: new insights from chemical proxies [J]. Journal of Quaternary Science, 2011, 26 (1): 109-117.
     [2] Xu, D. K., Lu, H. Y., Chu, G. Q., et al. Synchronous 500- year oscillations of monsoon climate and human activity in Northeast Asia [J]. Nature Communication, 2019, 10: 4105.
     [3] Dykoski, C. A., Edwards, R. L., Cheng, H., et al. A high-resolution, absolute-dated Holocene and deglacial Asian monsoon record from Dongge cave, China [J]. Earth Planet Science Letter, 2005, 233(1-2): 71-86.
     [4] Dearing, J. A. Holocene environmental change from magnetic proxies in lake sediments [M]. In: Maher, B. A., Thompson, R. (Eds.), Quaternary Climates, Environments and Magnetism. Cambridge University Press, 1999: 231-278.
     [5] Wanner, H., Beer, J., Butikofer, J., et al, 2008. Mid- to late-Holocene climate change: An overview [J]. Quaternary Science Review, 2008, 27(19-20): 1791-1828.
     

Data Product:

ID Data Name Data Size Operation
1 Element&MSLakeCoreLP.rar 84.66KB
Co-Sponsors

Institute of Geographic Sciences and Natural Resources Research,Chinese Academy of Sciences

The Geographical Society of China

Parteners

Committee on Data for Science and Technology (CODATA) Task Group on Preservation of and Access to Scientific and Technical Data in/for/with Developing Countries (PASTD)

Jomo Kenyatta University of Agriculture and Technology

Digital Linchao GeoMuseum