The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert
Through nine trace elements of the Shenmu section, Mu Us Desert is analyzed for the climate changes during Early Holocene. Except Sr, a migration process of P, Mn, Cr, Rb, Nb, Cu, Zn, and V is found in the dune sands, indicating the accumulation processes of the Asian winter monsoon-driven wind eros...
Published in: | Geochemistry International |
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Online Access: | http://ir.gig.ac.cn/handle/344008/43546 https://doi.org/10.1134/S0016702917140038 |
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ftchacadscgigcas:oai:ir.gig.ac.cn:344008/43546 2023-05-15T17:30:20+02:00 The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert Liu Haibo Li Baosheng Zheng Chunhong Si Yuejun Wen Xiaohao Niu Dongfeng Du Shuhuan Shu Peixian 2017-12-01 http://ir.gig.ac.cn/handle/344008/43546 https://doi.org/10.1134/S0016702917140038 英语 eng MAIK NAUKA/INTERPERIODICA/SPRINGER GEOCHEMISTRY INTERNATIONAL http://ir.gig.ac.cn/handle/344008/43546 doi:10.1134/S0016702917140038 Geochemistry & Geophysics Shenmu section early Holocene trace elements paleo climate changes NORTH-ATLANTIC CLIMATE HIGH-RESOLUTION ASIAN MONSOON CYCLES CHINA 期刊论文 2017 ftchacadscgigcas https://doi.org/10.1134/S0016702917140038 2020-12-22T07:21:49Z Through nine trace elements of the Shenmu section, Mu Us Desert is analyzed for the climate changes during Early Holocene. Except Sr, a migration process of P, Mn, Cr, Rb, Nb, Cu, Zn, and V is found in the dune sands, indicating the accumulation processes of the Asian winter monsoon-driven wind erosion and transport and deposition under the cold climatic phase. And accumulation of these elements in different layers of paleo sol dune sands is related to regional geomorphology and element properties. 8.5 winter-summer monsoon cycles in the early Holocene are observed. The duration time and climate of the stronger winter monsoon phases can be compared with the cold climate in the North Atlantic and other parts of China. The result of Red fit 3.8 power spectra shows 310a, 210a, 90a, and 70a centennial cycles for the element, which are consistent with the solar oscillation cycles. These suggest that the external solar activities of the Earth may have great influences on driving the winter and summer monsoon cycles during early Holocene. Report North Atlantic Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences) Geochemistry International 55 12 1171 1179 |
institution |
Open Polar |
collection |
Guangzhou Institute of Geochemistry: GIG OpenIR (Chinese Academy of Sciences) |
op_collection_id |
ftchacadscgigcas |
language |
English |
topic |
Geochemistry & Geophysics Shenmu section early Holocene trace elements paleo climate changes NORTH-ATLANTIC CLIMATE HIGH-RESOLUTION ASIAN MONSOON CYCLES CHINA |
spellingShingle |
Geochemistry & Geophysics Shenmu section early Holocene trace elements paleo climate changes NORTH-ATLANTIC CLIMATE HIGH-RESOLUTION ASIAN MONSOON CYCLES CHINA Liu Haibo Li Baosheng Zheng Chunhong Si Yuejun Wen Xiaohao Niu Dongfeng Du Shuhuan Shu Peixian The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert |
topic_facet |
Geochemistry & Geophysics Shenmu section early Holocene trace elements paleo climate changes NORTH-ATLANTIC CLIMATE HIGH-RESOLUTION ASIAN MONSOON CYCLES CHINA |
description |
Through nine trace elements of the Shenmu section, Mu Us Desert is analyzed for the climate changes during Early Holocene. Except Sr, a migration process of P, Mn, Cr, Rb, Nb, Cu, Zn, and V is found in the dune sands, indicating the accumulation processes of the Asian winter monsoon-driven wind erosion and transport and deposition under the cold climatic phase. And accumulation of these elements in different layers of paleo sol dune sands is related to regional geomorphology and element properties. 8.5 winter-summer monsoon cycles in the early Holocene are observed. The duration time and climate of the stronger winter monsoon phases can be compared with the cold climate in the North Atlantic and other parts of China. The result of Red fit 3.8 power spectra shows 310a, 210a, 90a, and 70a centennial cycles for the element, which are consistent with the solar oscillation cycles. These suggest that the external solar activities of the Earth may have great influences on driving the winter and summer monsoon cycles during early Holocene. |
format |
Report |
author |
Liu Haibo Li Baosheng Zheng Chunhong Si Yuejun Wen Xiaohao Niu Dongfeng Du Shuhuan Shu Peixian |
author_facet |
Liu Haibo Li Baosheng Zheng Chunhong Si Yuejun Wen Xiaohao Niu Dongfeng Du Shuhuan Shu Peixian |
author_sort |
Liu Haibo |
title |
The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert |
title_short |
The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert |
title_full |
The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert |
title_fullStr |
The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert |
title_full_unstemmed |
The climate change during early Holocene recorded by trace elements of Shenmu section, Mu Us Desert |
title_sort |
climate change during early holocene recorded by trace elements of shenmu section, mu us desert |
publisher |
MAIK NAUKA/INTERPERIODICA/SPRINGER |
publishDate |
2017 |
url |
http://ir.gig.ac.cn/handle/344008/43546 https://doi.org/10.1134/S0016702917140038 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
GEOCHEMISTRY INTERNATIONAL http://ir.gig.ac.cn/handle/344008/43546 doi:10.1134/S0016702917140038 |
op_doi |
https://doi.org/10.1134/S0016702917140038 |
container_title |
Geochemistry International |
container_volume |
55 |
container_issue |
12 |
container_start_page |
1171 |
op_container_end_page |
1179 |
_version_ |
1766126688522993664 |