Journal of Tropical Oceanography ›› 2025, Vol. 44 ›› Issue (4): 45-55.doi: 10.11978/2024203

• Marine Climatology • Previous Articles     Next Articles

Graded responses of coral skeletal δ18O and Sr/Ca to ENSO in the southern South China Sea

LI Ruoan1(), LI Xuqing2, CHEN Tianran2()   

  1. 1. School of Geography Sciences, South China Normal University, Guangzhou 510631, China
    2. State Key Laboratory of Tropical Oceanography, South China Sea Institute of Oceanology (CAS), Guangzhou 510301, China
  • Received:2024-10-29 Revised:2024-11-23 Online:2025-07-10 Published:2025-07-31
  • Contact: CHEN Tianran
  • Supported by:
    Special Foundation for National Science and Technology Basic Research Program of China(2022FY100601); National Natural Science Foundation of China(42076065)

Abstract:

Understanding the differential responses of coral geochemical proxies to El Niño-Southern Oscillation (ENSO) events of various intensities and types is crucial for reconstructing pre-instrumental ENSO variability. This study extracts sea surface temperature (SST) data from the southern South China Sea (SCS) since 1950, along with published coral skeletal δ18O and Sr/Ca time series from four locations (from west to east: Hòn Tre Island, Yongshu Island, Anemone’s Garden, and Palawan Island). Employing methods such as frequency-domain analysis and lag correlation analysis, we investigate the responses of SST and coral geochemical proxies in the southern South China Sea to different types and grades of ENSO events. The results indicate that the accuracy of coral geochemical proxies in classifying EP (east Pacific)-El Niño and CP (central Pacific)-El Niño events increases from east to west, whereas the classification accuracy for SBW (strong basin-wide)-El Niño events gradually decreases from east to west. Similarly, for CP-La Niña events, the classification accuracy of coral geochemical proxy improves progressively from east to west, while the opposite trend is observed for EP-La Niña events. Overall, the classification capability of coral geochemical proxies in the southern SCS is weaker for EP-El Niño and CP-La Niña events compared to SBW-El Niño and EP-La Niña events, with better performance in classifying strong ENSO events than extreme ENSO events.

Key words: southern South China Sea, ENSO, coral, Sr/Ca, δ18O, graded response

CLC Number: 

  • P732