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

Xiaohua Qiu; Tiegang Li; Fengming Chang; Qingyun Nan; Zhifang Xiong; Hanjie Sun

doi:10.1007/s00343-014-3073-y

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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

Updated：2023-05-16

- 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
- Journal of Oceanology and Limnology Vol. 32, Issue 1, Pages: 187-200(2014)
- Affiliations：
  
  1. Key Laboratory of Marine Geology and Environment Institute of Oceanology Chinese Academy of Sciences
  2. University of Chinese Academy of Sciences
- Author bio：
- Funds：
- DOI：10.1007/s00343-014-3073-y
  CLC：
- Online First：21 February 2014，
  
  Published：2014
- Accepted：
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Qiu, X., Li, T., Chang, F. et al. 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., Chin. J. Ocean. Limnol. 32, 187–200 (2014). https://doi.org/10.1007/s00343-014-3073-y
DOI：

Qiu, X., Li, T., Chang, F. et al. 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., Chin. J. Ocean. Limnol. 32, 187–200 (2014). https://doi.org/10.1007/s00343-014-3073-y DOI：

摘要

Abstract

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 δ18O sw exhibited very similar variations to those of mean ocean δ18Osw

owing to the past sea-level changes on glacial-interglacial timescale. Calculated values of δ18Osw-ss reflect a more saline condition during high local summer insolation (SI) periods. Such correspondence between δ18Osw-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.

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