Chinese Science Bulletin

, Volume 59, Issue 31, pp 4115–4122

Higher sea surface temperature in the northern South China Sea during the natural warm periods of late Holocene than recent decades

Authors

  • Hong Yan
    • Institute of Polar Environment, School of Earth and Space SciencesUniversity of Science and Technology of China
    • State Key Laboratory of Loess and Quaternary Geology, Institute of Earth EnvironmentChinese Academy of Sciences
    • Institute of Polar Environment, School of Earth and Space SciencesUniversity of Science and Technology of China
  • Da Shao
    • Institute of Polar Environment, School of Earth and Space SciencesUniversity of Science and Technology of China
  • Yuhong Wang
    • Advanced Management Research CenterNingbo University
  • Gangjian Wei
    • Guangzhou Institute of GeochemistryChinese Academy of Sciences
Article Geology

DOI: 10.1007/s11434-014-0317-3

Cite this article as:
Yan, H., Sun, L., Shao, D. et al. Chin. Sci. Bull. (2014) 59: 4115. doi:10.1007/s11434-014-0317-3

Abstract

The large-scale syntheses of global mean temperatures in IPCC fourth report suggested that the Northern Hemisphere temperature in the second half of the 20th century was likely the highest in at least the past 1,300 years and the 1990s was likely the warmest decade. However, this remains debated and the controversy is centered on whether temperatures during the recent half century were higher than those during the Medieval Climate Anomaly (MCA, AD 800–1300) and the Roman Warm Period (RWP, BC 200–AD 400), the most recent two natural warm periods of the late Holocene. Here the high resolution sea surface temperatures (SSTs) of two time windows around AD 990 (±40) and AD 50 (±40), which located in the MCA and RWP respectively, were reconstructed by the Sr/Ca ratio and δ 18O of Tradacna gigas shells from the northern South China Sea. The results suggested that the mean SSTs around AD 990 (±40) and AD 50 (±40) were 28.1 °C and 28.7 °C, 0.8 °C and 1.4 °C higher than that during AD 1994–2005, respectively. These records, together with the tree ring, lake sediment and literature records from the eastern China and northwest China, imply that the temperatures in recent decades do not seem to exceed the natural changes in MCA, at least in eastern Asia from northwest China to northern SCS.

Keywords

Tridacna South China Sea Late Holocene Natural warm periods Sea surface temperature

Copyright information

© Science China Press and Springer-Verlag Berlin Heidelberg 2014