Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka
Changes in sea surface temperature (SST), seawater oxygen isotope (delta O-18(sw)), and local salinity proxy (delta O-18(sw-ss)) in the past 155 ka were studied using a sediment core (MD06-3052) from the northern edge of the western Pacific Warm Pool (WPWP), within the flow path of the bifurcation o...
Published in: | Chinese Journal of Oceanology and Limnology |
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ftchinacasciocas:oai:ir.qdio.ac.cn:337002/23842 2023-05-15T13:40:37+02:00 Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka Qiu Xiaohua Li Tiegang Chang Fengming Nan Qingyun Xiong Zhifang Sun Hanjie Li, TG (reprint author), Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Peoples R China. 2014 http://ir.qdio.ac.cn/handle/337002/23842 https://doi.org/10.1007/s00343-014-3073-y 英语 eng CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY http://ir.qdio.ac.cn/handle/337002/23842 doi:10.1007/s00343-014-3073-y cn.org.cspace.api.content.CopyrightPolicy@4ccda880 Mg/ca Sea Surface Temperature (Sst) Western Pacific Warm Pool (Wpwp) Enso Monsoon Marine & Freshwater Biology Oceanography Article 期刊论文 2014 ftchinacasciocas https://doi.org/10.1007/s00343-014-3073-y 2022-06-27T05:36:40Z Changes in sea surface temperature (SST), seawater oxygen isotope (delta O-18(sw)), and local salinity proxy (delta O-18(sw-ss)) in the past 155 ka were studied using a sediment core (MD06-3052) from the northern edge of the western Pacific Warm Pool (WPWP), within the flow path of the bifurcation of the North Equatorial Current. Our records reveal a lead-lag relationship between paired Mg/Ca-SST and delta O-18 during Termination II and the last interglacial period. Similarity in SST between our site and the Antarctic temperature proxy and in CO2 profile showed a close connection between the WPWP and the Antarctic. Values of delta O-18 sw exhibited very similar variations to those of mean ocean delta O-18(sw), owing to the past sea-level changes on glacial-interglacial timescale. Calculated values of delta O-18(sw-ss) reflect a more saline condition during high local summer insolation (SI) periods. Such correspondence between delta O-18(sw-ss) and local SI in the WPWP may reflect complex interaction between ENSO and monsoon, which was stimulated by changes in solar irradiance and their influence on the local hydrologic cycle. This then caused a striking reorganization of atmospheric circulation over the WPWP. Article in Journal/Newspaper Antarc* Antarctic Planktonic foraminifera Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR Antarctic The Antarctic Pacific Chinese Journal of Oceanology and Limnology 32 1 187 200 |
institution |
Open Polar |
collection |
Institute of Oceanology, Chinese Academy of Sciences: IOCAS-IR |
op_collection_id |
ftchinacasciocas |
language |
English |
topic |
Mg/ca Sea Surface Temperature (Sst) Western Pacific Warm Pool (Wpwp) Enso Monsoon Marine & Freshwater Biology Oceanography |
spellingShingle |
Mg/ca Sea Surface Temperature (Sst) Western Pacific Warm Pool (Wpwp) Enso Monsoon Marine & Freshwater Biology Oceanography Qiu Xiaohua Li Tiegang Chang Fengming Nan Qingyun Xiong Zhifang Sun Hanjie Li, TG (reprint author), Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Peoples R China. Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka |
topic_facet |
Mg/ca Sea Surface Temperature (Sst) Western Pacific Warm Pool (Wpwp) Enso Monsoon Marine & Freshwater Biology Oceanography |
description |
Changes in sea surface temperature (SST), seawater oxygen isotope (delta O-18(sw)), and local salinity proxy (delta O-18(sw-ss)) in the past 155 ka were studied using a sediment core (MD06-3052) from the northern edge of the western Pacific Warm Pool (WPWP), within the flow path of the bifurcation of the North Equatorial Current. Our records reveal a lead-lag relationship between paired Mg/Ca-SST and delta O-18 during Termination II and the last interglacial period. Similarity in SST between our site and the Antarctic temperature proxy and in CO2 profile showed a close connection between the WPWP and the Antarctic. Values of delta O-18 sw exhibited very similar variations to those of mean ocean delta O-18(sw), owing to the past sea-level changes on glacial-interglacial timescale. Calculated values of delta O-18(sw-ss) reflect a more saline condition during high local summer insolation (SI) periods. Such correspondence between delta O-18(sw-ss) and local SI in the WPWP may reflect complex interaction between ENSO and monsoon, which was stimulated by changes in solar irradiance and their influence on the local hydrologic cycle. This then caused a striking reorganization of atmospheric circulation over the WPWP. |
format |
Article in Journal/Newspaper |
author |
Qiu Xiaohua Li Tiegang Chang Fengming Nan Qingyun Xiong Zhifang Sun Hanjie Li, TG (reprint author), Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Peoples R China. |
author_facet |
Qiu Xiaohua Li Tiegang Chang Fengming Nan Qingyun Xiong Zhifang Sun Hanjie Li, TG (reprint author), Chinese Acad Sci, Key Lab Marine Geol & Environm, Inst Oceanol, Qingdao 266071, Peoples R China. |
author_sort |
Qiu Xiaohua |
title |
Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka |
title_short |
Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka |
title_full |
Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka |
title_fullStr |
Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka |
title_full_unstemmed |
Sea surface temperature and salinity reconstruction based on stable isotopes and Mg/Ca of planktonic foraminifera in the western Pacific Warm Pool during the last 155 ka |
title_sort |
sea surface temperature and salinity reconstruction based on stable isotopes and mg/ca of planktonic foraminifera in the western pacific warm pool during the last 155 ka |
publishDate |
2014 |
url |
http://ir.qdio.ac.cn/handle/337002/23842 https://doi.org/10.1007/s00343-014-3073-y |
geographic |
Antarctic The Antarctic Pacific |
geographic_facet |
Antarctic The Antarctic Pacific |
genre |
Antarc* Antarctic Planktonic foraminifera |
genre_facet |
Antarc* Antarctic Planktonic foraminifera |
op_relation |
CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY http://ir.qdio.ac.cn/handle/337002/23842 doi:10.1007/s00343-014-3073-y |
op_rights |
cn.org.cspace.api.content.CopyrightPolicy@4ccda880 |
op_doi |
https://doi.org/10.1007/s00343-014-3073-y |
container_title |
Chinese Journal of Oceanology and Limnology |
container_volume |
32 |
container_issue |
1 |
container_start_page |
187 |
op_container_end_page |
200 |
_version_ |
1766137525442707456 |