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Variations of alkenone temperature in the Sea of Japan during the last 170 ka and its paleoceanographic implications

  • Article
  • Oceanology
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Chinese Science Bulletin

Abstract

Two sediment cores, KCES1 and ODP797, which were recovered from the Sea of Japan (JS), were measured for alkenone-derived sea surface temperatures (\(U^{{\text{K}}^{\prime}}_{37} {\text{-SSTs}}\)). Our results revealed that the SSTs closely follow the glacial-interglacial cycles during the last 170 ka, except in the last glacial maximum (LGM), during which the SST was higher than in the Holocene. The anomalous high temperature in the LGM is considered as an effect of the intrusion of a low salinity water mass into the JS when the sea level was almost below 130 m. On the glacial-interglacial to orbital timescale, the \( U^{{\text{K}}^{\prime }}_{37} {\text{-SSTs}} \) record in the JS correlated well with the benthic foraminiferal δ 18O record and solar insolation, which suggests the dominant control of solar insolation and its related sea ice development on the SST in the JS. On the sub-orbital/millennial timescale, reduced SST corresponds to an enhanced east asian winter monsoon (EAWM) during the last glacial period (MIS3 and MIS4), indicating the dominant control of sea ice expansion due to the enhanced EAWM on the SST in the JS. In contrast, during the last interglacial period (MIS5), the SST in the JS was controlled by variations in the east Asian summer monsoon. These results highlight the key role of solar insolation and associated glacial-interglacial conditions in the variations of the SST in the JS since the last 170 ka.

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Acknowledgments

This work was supported by the National Natural Science Foundation of China (41076038, 40710069004, 40606016 and 41006036), and the Project of Global Change and Air-Sea Interaction.

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Authors and Affiliations

  1. Key Laboratory of Marine Sedimentology and Environmental Geology, First Institute of Oceanography, State Oceanic Administration, Qingdao, 266061, China

    Yanguang Liu, Jiaojie Chen, Jinxia Chen, Jianjun Zou & Zhengquan Yao

  2. Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education/Qingdao Collaborative Innovation Center of Marine Science and Technology, Ocean University of China, Qingdao, 266100, China

    Lei Xing

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  1. Yanguang Liu
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Correspondence to Yanguang Liu.

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Liu, Y., Chen, J., Chen, J. et al. Variations of alkenone temperature in the Sea of Japan during the last 170 ka and its paleoceanographic implications. Chin. Sci. Bull. 59, 4498–4509 (2014). https://doi.org/10.1007/s11434-014-0367-6

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  • DOI: https://doi.org/10.1007/s11434-014-0367-6

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