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 （δ18Osw）, and local salinity proxy （δ18Osw-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 Equ...

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Published in:Chinese journal of oceanology and limnology 2014, Vol.32 (1), p.187-200
Main Author: 仇晓华 李铁刚 常凤鸣 南青云 熊志方 孙晗杰
Format: Article
Language:English
Subjects:
Atmospheric circulation
Calcium
Carbon dioxide
Earth and Environmental Science
Earth Sciences
El Nino
El Nino phenomena
Foraminifera
Geology
Hydrologic cycle
Hydrological cycle
Interglacial periods
Irradiance
Isotopes
Magnesium
Marine
monsoon season
Ocean currents
Oceanography
oxygen
Oxygen isotopes
Salinity
Salinity effects
sea level
Sea level changes
Sea surface
Sea surface temperature
Seawater
sediments
solar radiation
Southern Oscillation
Stable isotopes
summer
Surface temperature
Surface water
Temperature effects
太阳辐射
末次间冰期
浮游有孔虫
海面温度
盐度
稳定同位素
西太平洋暖池
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cited_by cdi_FETCH-LOGICAL-c399t-ba5e4c167767b0ddc82a0028e0061ea53f734c85b3f7b1375fa86bea2ba312b43
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description Changes in sea surface temperature （SST）, seawater oxygen isotope （δ18Osw）, and local salinity proxy （δ18Osw-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 δ18O 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 818Osw exhibited very similar variations to those of mean ocean δ18Osw, owing to the past sea-level changes on glacial-interglacial timescale. Calculated values of δ18O reflect a more saline condition during high local summer insolation （SI） periods. Such correspondence between δ18O 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.
doi_str_mv 10.1007/s00343-014-3073-y
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J. Ocean. Limnol</addtitle><addtitle>Chinese Journal of Oceanology and Limnology</addtitle><description>Changes in sea surface temperature （SST）, seawater oxygen isotope （δ18Osw）, and local salinity proxy （δ18Osw-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 δ18O 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 818Osw exhibited very similar variations to those of mean ocean δ18Osw, owing to the past sea-level changes on glacial-interglacial timescale. Calculated values of δ18O reflect a more saline condition during high local summer insolation （SI） periods. 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identifier ISSN: 0254-4059
ispartof Chinese journal of oceanology and limnology, 2014, Vol.32 (1), p.187-200
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subjects Atmospheric circulation
Calcium
Carbon dioxide
Earth and Environmental Science
Earth Sciences
El Nino
El Nino phenomena
Foraminifera
Geology
Hydrologic cycle
Hydrological cycle
Interglacial periods
Irradiance
Isotopes
Magnesium
Marine
monsoon season
Ocean currents
Oceanography
oxygen
Oxygen isotopes
Salinity
Salinity effects
sea level
Sea level changes
Sea surface
Sea surface temperature
Seawater
sediments
solar radiation
Southern Oscillation
Stable isotopes
summer
Surface temperature
Surface water
Temperature effects
太阳辐射
末次间冰期
浮游有孔虫
海面温度
盐度
稳定同位素
西太平洋暖池
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
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