A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea)
Using a radiolarian-based transfer function, mean annual sea surface temperature (SST) and seasonal temperature range are reconstructed through the last 10,500yrs in the northern Okinawa Trough. Down-core SST estimates reveal that throughout the Holocene the changes of mean annual SST display a thre...
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Online Access: | http://ir.qdio.ac.cn/handle/337002/5029 https://doi.org/10.1016/j.quaint.2006.12.007 |
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/5028 2023-05-15T16:38:50+02:00 A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea) Chang Fengming Li Tiegang Zhuang Lihua Yan Jun 2008-05-15 http://ir.qdio.ac.cn/handle/337002/5029 https://doi.org/10.1016/j.quaint.2006.12.007 英语 eng QUATERNARY INTERNATIONAL Chang Fengming; Li Tiegang; Zhuang Lihua; Yan Jun.A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea),QUATERNARY INTERNATIONAL,2008,183():115-122 http://ir.qdio.ac.cn/handle/337002/5029 doi:10.1016/j.quaint.2006.12.007 Ice-core Climate Oscillations Surface Temperature Age Calibration Pacific-ocean Circulation Instability South Gisp2 Biogeography Geography Physical Geosciences Multidisciplinary Article 期刊论文 2008 ftchinacasciocas https://doi.org/10.1016/j.quaint.2006.12.007 2022-06-27T05:32:35Z Using a radiolarian-based transfer function, mean annual sea surface temperature (SST) and seasonal temperature range are reconstructed through the last 10,500yrs in the northern Okinawa Trough. Down-core SST estimates reveal that throughout the Holocene the changes of mean annual SST display a three-step trend: (i) an early Holocene continuous warming between 10,500 and 8500yr BP which ends up with a abrupt cooling at about 8200yr BP; (ii) a relatively stable middle Holocene with high SST that lasted until 3200yr BP; and (iii) a late-Holocene distinct SST decline between 3200 and 500yr BP. This pattern is in agreement with the ice core and terrestrial paleoclimatic records in the Chinese continent and other regions of the world. Five cooling events with abrupt mean annual SST drops, which occur at similar to 300-600, 1400, 3100, 4600-5100 and 8200yr BP, are recognized during the last 10,500yrs. Comparison of our results with records of GISP2 ice core and marine sediment in North Atlantic region suggests these cooling events are strongly coupled, which implies a possible significant climatic correlation between high- and low-latitude areas. (C) 2007 Elsevier Ltd and INQUA. All rights reserved. Using a radiolarian-based transfer function, mean annual sea surface temperature (SST) and seasonal temperature range are reconstructed through the last 10,500yrs in the northern Okinawa Trough. Down-core SST estimates reveal that throughout the Holocene the changes of mean annual SST display a three-step trend: (i) an early Holocene continuous warming between 10,500 and 8500yr BP which ends up with a abrupt cooling at about 8200yr BP; (ii) a relatively stable middle Holocene with high SST that lasted until 3200yr BP; and (iii) a late-Holocene distinct SST decline between 3200 and 500yr BP. This pattern is in agreement with the ice core and terrestrial paleoclimatic records in the Chinese continent and other regions of the world. Five cooling events with abrupt mean annual SST drops, which occur at similar to 300-600, ... Article in Journal/Newspaper ice core North Atlantic Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Pacific Quaternary International 183 1 115 122 |
institution |
Open Polar |
collection |
Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
op_collection_id |
ftchinacasciocas |
language |
English |
topic |
Ice-core Climate Oscillations Surface Temperature Age Calibration Pacific-ocean Circulation Instability South Gisp2 Biogeography Geography Physical Geosciences Multidisciplinary |
spellingShingle |
Ice-core Climate Oscillations Surface Temperature Age Calibration Pacific-ocean Circulation Instability South Gisp2 Biogeography Geography Physical Geosciences Multidisciplinary Chang Fengming Li Tiegang Zhuang Lihua Yan Jun A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea) |
topic_facet |
Ice-core Climate Oscillations Surface Temperature Age Calibration Pacific-ocean Circulation Instability South Gisp2 Biogeography Geography Physical Geosciences Multidisciplinary |
description |
Using a radiolarian-based transfer function, mean annual sea surface temperature (SST) and seasonal temperature range are reconstructed through the last 10,500yrs in the northern Okinawa Trough. Down-core SST estimates reveal that throughout the Holocene the changes of mean annual SST display a three-step trend: (i) an early Holocene continuous warming between 10,500 and 8500yr BP which ends up with a abrupt cooling at about 8200yr BP; (ii) a relatively stable middle Holocene with high SST that lasted until 3200yr BP; and (iii) a late-Holocene distinct SST decline between 3200 and 500yr BP. This pattern is in agreement with the ice core and terrestrial paleoclimatic records in the Chinese continent and other regions of the world. Five cooling events with abrupt mean annual SST drops, which occur at similar to 300-600, 1400, 3100, 4600-5100 and 8200yr BP, are recognized during the last 10,500yrs. Comparison of our results with records of GISP2 ice core and marine sediment in North Atlantic region suggests these cooling events are strongly coupled, which implies a possible significant climatic correlation between high- and low-latitude areas. (C) 2007 Elsevier Ltd and INQUA. All rights reserved. Using a radiolarian-based transfer function, mean annual sea surface temperature (SST) and seasonal temperature range are reconstructed through the last 10,500yrs in the northern Okinawa Trough. Down-core SST estimates reveal that throughout the Holocene the changes of mean annual SST display a three-step trend: (i) an early Holocene continuous warming between 10,500 and 8500yr BP which ends up with a abrupt cooling at about 8200yr BP; (ii) a relatively stable middle Holocene with high SST that lasted until 3200yr BP; and (iii) a late-Holocene distinct SST decline between 3200 and 500yr BP. This pattern is in agreement with the ice core and terrestrial paleoclimatic records in the Chinese continent and other regions of the world. Five cooling events with abrupt mean annual SST drops, which occur at similar to 300-600, ... |
format |
Article in Journal/Newspaper |
author |
Chang Fengming Li Tiegang Zhuang Lihua Yan Jun |
author_facet |
Chang Fengming Li Tiegang Zhuang Lihua Yan Jun |
author_sort |
Chang Fengming |
title |
A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea) |
title_short |
A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea) |
title_full |
A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea) |
title_fullStr |
A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea) |
title_full_unstemmed |
A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea) |
title_sort |
holocene paleotemperature record based on radiolaria from the northern okinawa trough (east china sea) |
publishDate |
2008 |
url |
http://ir.qdio.ac.cn/handle/337002/5029 https://doi.org/10.1016/j.quaint.2006.12.007 |
geographic |
Pacific |
geographic_facet |
Pacific |
genre |
ice core North Atlantic |
genre_facet |
ice core North Atlantic |
op_relation |
QUATERNARY INTERNATIONAL Chang Fengming; Li Tiegang; Zhuang Lihua; Yan Jun.A Holocene paleotemperature record based on radiolaria from the northern Okinawa Trough (East China Sea),QUATERNARY INTERNATIONAL,2008,183():115-122 http://ir.qdio.ac.cn/handle/337002/5029 doi:10.1016/j.quaint.2006.12.007 |
op_doi |
https://doi.org/10.1016/j.quaint.2006.12.007 |
container_title |
Quaternary International |
container_volume |
183 |
container_issue |
1 |
container_start_page |
115 |
op_container_end_page |
122 |
_version_ |
1766029182219845632 |