Journal of Tropical Oceanography ›› 2025, Vol. 44 ›› Issue (4): 45-55.doi: 10.11978/2024203
• Marine Climatology • Previous Articles Next Articles
LI Ruoan1(), LI Xuqing2, CHEN Tianran2(
)
Received:
2024-10-29
Revised:
2024-11-23
Online:
2025-07-10
Published:
2025-07-31
Contact:
CHEN Tianran
Supported by:
CLC Number:
LI Ruoan, LI Xuqing, CHEN Tianran. Graded responses of coral skeletal δ18O and Sr/Ca to ENSO in the southern South China Sea[J].Journal of Tropical Oceanography, 2025, 44(4): 45-55.
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Tab. 1
Data sources for coral geochemical indicators"
参考文献 | 采样地点 | 经纬度 | 样品年代 | 地球化学指标 | 分辨率 |
---|---|---|---|---|---|
Goodkin et al, | 竹岛(Hòn Tre Island) | 12°12′N, 109°18′E | 1950年1月—2010年10月 | Sr/Ca | 月 |
Yu et al, | 永暑岛(Yongshu Island) | 9°33′N, 112°54′E | 1951年1月—1999年4月 | δ18O | 季节、月 |
Wu et al, | 巴拉望岛(Palawan Island) | 11°28′N, 119°01′E | 1947年1月—1981年1月 | δ18O | 半年至双月 |
Krawczyk et al, | 海葵园(Anemone’s Garden) | 4°17′N, 113°49′E | 1982年1月—2016年1月 | δ18O、Sr/Ca | 月 |
Fig. 1
Spatial correlation between SST in the southern SCS (lagged by 4 months) and Niño3.4 index. Created by Climate Explorer, an online tool (Trouet et al, 2013). The SST in the southern SCS shows a significant positive correlation (P<0.1) with the Niño3.4 index. The SST data used for this analysis were derived from the monthly HadISST dataset, covering the period from 1950 to 2020 (https://www.metoffice.gov.uk/hadobs/hadisst/). Black dots on the map indicate coral sampling locations: (1) Hòn Tre Island; (2) Yongshu Island; (3) Anemone’s Garden, (4) Palawan Island"
Fig. 2
Correlation analyses (a-j) and time series (k-p) of monthly-resolution geochemical proxies in coral skeletons (black folded line) with sea surface temperature (SST) from southern SCS and local SST records (gray dotted line), both processed with a 13-month moving average. Asterisks (*) represent statistically significant correlations (P<0.05)"
Fig. 3
Signal processing of instrumental SST sequence: (a) time-domain plot of the Niño3.4 signal before and after processing, with the dotted line representing the raw signal sequence and the solid line representing the signal sequence after applying a 12~48 Hz filter; (b) frequency-domain plot of the original Niño3.4 signal, showing that the frequency distribution is primarily concentrated in the 12~48 Hz ( 1~4 years) frequency band; (c) frequency-domain plot of the Niño3.4 signal after 12~48 Hz filtering; (d) time series of Niño3.4 (solid line) and sea surface temperature anomaly (SSTA) (dotted line) in the southern SCS after 12~48 Hz band-pass filtering; (e) results of the lagged correlation analysis, showing that the correlation with Niño3.4 reaches its peak when the SST in the southern SCS is lagged by 4 months, with a correlation coefficient of 0.72 (P<0.05)"
Fig. 5
Different types and intensities of ENSO events as recorded by coral geochemical proxies: (a) different types and intensities of ENSO events recorded in the Niño3.4 index series from 1950 to 2020 as reference standard; (b) Sr/Ca anomalies from Hòn Tre Island, 1950-2010; (c) Sr/Ca anomalies from Anemone’s Garden, 1982-2016; (d) δ18O anomalies from Yongshu Island, 1951-1999; (e) δ18O anomalies from Palawan Island, 1950-1981; (f) δ18O anomalies from Anemone’s Garden, 1982-2016; Neutral warming events (▽) were excluded from subsequent statistical analyses"
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