Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene
AMS(14)C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoo...
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2010
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Online Access: | http://ir.qdio.ac.cn/handle/337002/5131 https://doi.org/10.1007/s11434-010-3215-3 |
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/5130 2024-09-15T18:12:00+00:00 Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene Liu ShengFa Shi Xuefa Liu YanGuang Qia ShuQing Yang Gang Fang XiSheng Wu YongHua Li ChaoXin Li XiaoYan Zhu AiMei Gao JingJing 2010-07-01 http://ir.qdio.ac.cn/handle/337002/5131 https://doi.org/10.1007/s11434-010-3215-3 英语 eng CHINESE SCIENCE BULLETIN Liu ShengFa; Shi Xuefa; Liu YanGuang; Qia ShuQing; Yang Gang; Fang XiSheng; Wu YongHua; Li ChaoXin; Li XiaoYan; Zhu AiMei; Gao JingJing.Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene,CHINESE SCIENCE BULLETIN,2010,55(21):2306-2314 http://ir.qdio.ac.cn/handle/337002/5131 doi:10.1007/s11434-010-3215-3 Holocene Inner Shelf Of The East China Sea Mud Areas Grain Size Clay Mineral Elemental Analysis East Asia Winter Monsoon Multidisciplinary Sciences Article 期刊论文 2010 ftchinacasciocas https://doi.org/10.1007/s11434-010-3215-3 2024-08-09T03:18:11Z AMS(14)C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed. These three proxies, mean grain size (>9.71 mu m), chemical index of alteration (CIA) and ratio of smectite to kaolinite in particular, show similar fluctuation patterns. Furthermore, 10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene; these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon. The cooling events correlated well with the results of the delta(18)O curves of the Dunde ice core and GISP2, which therefore revealed a regional response to global climate change. Four stages of the East Asia winter monsoon were identified, i.e. 8300-6300 a BP, strong and unstable; 6300-3800 a BP, strong but stable; 3800-1400 a BP, weak and unstable; after 1400 a BP, weak but stable. AMS(14)C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed. These three proxies, mean grain size (>9.71 mu m), chemical index of alteration (CIA) and ratio of smectite to kaolinite in particular, show similar fluctuation patterns. Furthermore, 10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene; these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon. The cooling events correlated well with the results of the delta O-18 curves of the Dunde ice core and GISP2, which therefore revealed a regional ... Article in Journal/Newspaper ice core Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Chinese Science Bulletin 55 21 2306 2314 |
institution |
Open Polar |
collection |
Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
op_collection_id |
ftchinacasciocas |
language |
English |
topic |
Holocene Inner Shelf Of The East China Sea Mud Areas Grain Size Clay Mineral Elemental Analysis East Asia Winter Monsoon Multidisciplinary Sciences |
spellingShingle |
Holocene Inner Shelf Of The East China Sea Mud Areas Grain Size Clay Mineral Elemental Analysis East Asia Winter Monsoon Multidisciplinary Sciences Liu ShengFa Shi Xuefa Liu YanGuang Qia ShuQing Yang Gang Fang XiSheng Wu YongHua Li ChaoXin Li XiaoYan Zhu AiMei Gao JingJing Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene |
topic_facet |
Holocene Inner Shelf Of The East China Sea Mud Areas Grain Size Clay Mineral Elemental Analysis East Asia Winter Monsoon Multidisciplinary Sciences |
description |
AMS(14)C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed. These three proxies, mean grain size (>9.71 mu m), chemical index of alteration (CIA) and ratio of smectite to kaolinite in particular, show similar fluctuation patterns. Furthermore, 10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene; these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon. The cooling events correlated well with the results of the delta(18)O curves of the Dunde ice core and GISP2, which therefore revealed a regional response to global climate change. Four stages of the East Asia winter monsoon were identified, i.e. 8300-6300 a BP, strong and unstable; 6300-3800 a BP, strong but stable; 3800-1400 a BP, weak and unstable; after 1400 a BP, weak but stable. AMS(14)C dating and analysis of grain size, major elements and clay minerals were applied to Core MZ01 from the mud area on the inner shelf of the East China Sea. Based on the environmentally sensitive grain size, clay mineral and major element assemblages, the history of the East Asia winter monsoon since the mid-Holocene could be reconstructed. These three proxies, mean grain size (>9.71 mu m), chemical index of alteration (CIA) and ratio of smectite to kaolinite in particular, show similar fluctuation patterns. Furthermore, 10 extreme values corresponding to the contemporary cooling events could be recognized since the mid-Holocene; these extreme values are likely to have been caused by the strengthening of the East Asia winter monsoon. The cooling events correlated well with the results of the delta O-18 curves of the Dunde ice core and GISP2, which therefore revealed a regional ... |
format |
Article in Journal/Newspaper |
author |
Liu ShengFa Shi Xuefa Liu YanGuang Qia ShuQing Yang Gang Fang XiSheng Wu YongHua Li ChaoXin Li XiaoYan Zhu AiMei Gao JingJing |
author_facet |
Liu ShengFa Shi Xuefa Liu YanGuang Qia ShuQing Yang Gang Fang XiSheng Wu YongHua Li ChaoXin Li XiaoYan Zhu AiMei Gao JingJing |
author_sort |
Liu ShengFa |
title |
Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene |
title_short |
Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene |
title_full |
Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene |
title_fullStr |
Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene |
title_full_unstemmed |
Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene |
title_sort |
records of the east asian winter monsoon from the mud area on the inner shelf of the east china sea since the mid-holocene |
publishDate |
2010 |
url |
http://ir.qdio.ac.cn/handle/337002/5131 https://doi.org/10.1007/s11434-010-3215-3 |
genre |
ice core |
genre_facet |
ice core |
op_relation |
CHINESE SCIENCE BULLETIN Liu ShengFa; Shi Xuefa; Liu YanGuang; Qia ShuQing; Yang Gang; Fang XiSheng; Wu YongHua; Li ChaoXin; Li XiaoYan; Zhu AiMei; Gao JingJing.Records of the East Asian winter monsoon from the mud area on the inner shelf of the East China Sea since the mid-Holocene,CHINESE SCIENCE BULLETIN,2010,55(21):2306-2314 http://ir.qdio.ac.cn/handle/337002/5131 doi:10.1007/s11434-010-3215-3 |
op_doi |
https://doi.org/10.1007/s11434-010-3215-3 |
container_title |
Chinese Science Bulletin |
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55 |
container_issue |
21 |
container_start_page |
2306 |
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2314 |
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1810449591546413056 |