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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >Sr/Ca–sea surface temperature calibration in the coral Porites lutea from subtropical northern South China Sea
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Sr/Ca–sea surface temperature calibration in the coral Porites lutea from subtropical northern South China Sea

机译:南海亚热带北部珊瑚Porites lutea中Sr / Ca-海面温度的标定

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摘要

Strontiumto calcium(Sr/Ca) ratios in annual bands of Porites corals are commonly used as past sea surface temperature proxy in tropical oceans, whereas studies that refer to Sr/Ca–SST calibration in high-latitude corals are rather rare in general. Here we present a 50-year (1961–2010) near-fortnightly Sr/Ca record in two Porites lutea corals living near the northern limit of reef-building corals in the subtropical northern South China Sea, where winter temperatures are extreme for hermatypic corals. The Sr/Ca time series shows a clear annual cyclicity, with marked sharparrow winter peaks. Comparison with an instrumental SST record (since 1961) indicates that this Sr/Ca record is chiefly modulated by SST. Two different methods are discussed for calibrating Sr/Ca with SST. The correlation between interpolated Sr/Ca and SST is significant, but the coefficient is relatively low, mainly attributed to extreme cold winter SSTs (<~16 °C) which cause a significant decrease or even cessation of coral skeletal extension. Another modified method using only annual low Sr/Ca values which could clearly bematchedwith the same features in the instrumental SST record ismore reliable. Themodified regression equation does not encompass SSTs below24 °C. The fidelity of the coral-based Sr/Ca–SST calibrationwas assessed and the precision of themethod is estimated to be 0.31 ± 0.62 °C based on the calibration–verification exercise. The modified method is suggested in marginal coral areas with extreme intra-annual SST variation (e.g., from 13 to 30 °C).
机译:在热带海洋中,Porites珊瑚的年波段中锶与钙(Sr / Ca)之比通常被用作过去的海面温度指标,而有关高纬度珊瑚中Sr / Ca–SST校准的研究通常很少。在这里,我们在南亚热带亚热带北部珊瑚礁建造珊瑚的北限附近生活的两种Porite lutea珊瑚中,提出了近五十年来(1961-2010)的Sr / Ca近两周记录,那里的冬季温度对于放牧珊瑚极为极端。 。 Sr / Ca时间序列显示出明显的年度周期性,并具有明显的尖锐/狭窄的冬季高峰。与仪器的SST记录(自1961年以来)进行比较表明,该Sr / Ca记录主要受SST调制。讨论了两种用SST校准Sr / Ca的方法。内插Sr / Ca与SST之间的相关性很显着,但是系数相对较低,主要归因于冬季极冷的SST(<〜16°C),这会导致珊瑚骨骼延伸的显着减少甚至停止。另一种仅使用年度低Sr / Ca值的改进方法更可靠,该方法可以与仪器SST记录中的相同特征明显地匹配。修改后的回归方程不包括低于24°C的SST。评估了基于珊瑚的Sr / Ca–SST校准的保真度,根据校准验证工作,该方法的精度估计为0.31±0.62°C。建议在边缘海域内SST年度变化极高(例如从13到30°C)的情况下使用这种改进的方法。

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