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首页> 外文期刊>Paleoceanography >Diploastrea heliopora Sr/Ca and O-18 records from northeast Luzon, Philippines: An assessment of interspecies coral proxy calibrations and climate controls of sea surface temperature and salinity
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Diploastrea heliopora Sr/Ca and O-18 records from northeast Luzon, Philippines: An assessment of interspecies coral proxy calibrations and climate controls of sea surface temperature and salinity

机译:Diploastrea Heliopora SR / CA和O-18来自Northeast Luzon,菲律宾的历史记录:评估Interspecies珊瑚代理校准和海面温度和盐度的气候控制

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摘要

The Indo-Pacific coral Diploastrea heliopora reveals regional multidecadal- to centennial- scale climate variability using coral carbonate O-18 (O-18(c)) as a combined proxy for sea surface temperature (SST) and sea surface salinity (SSS). However, to assess the coral's full potential in resolving climatic events, an independent SST proxy would be more advantageous. We examined both Sr/Ca and O-18 of Diploastrea against an adjacent Porites lobata core collected from northeast Luzon, Philippines. Winter Sr/Ca data from Diploastrea show a significant correlation to SST (r=-0.41, p<0.05, (root-mean-square of the residual) RMSR=0.81 degrees C) and provide a proxy with similar sensitivity as Porites (r=-0.57, p<0.05, RMSR=0.62 degrees C). An interspecies SST record is shown to be robust and used for a reconstruction of the Pacific Decadal Oscillation during boreal winter (r=-0.70, p=0.02). While we were unable to generate a robust Diploastrea O-18-SSS calibration at interannual timescale, the freshening trend toward the present, commonly observed in the region, is qualitatively captured in Diploastrea O-18. Comparison with Porites O-18 and instrumental SSS records shows that the magnitude of freshening is consistent between coral species. Wet and dry season Porites O-18 provide support for the relative influence of El Nino-Southern Oscillation events and local precipitation to SSS variability at our site. The multiproxy, multispecies approach of this study further strengthens the evidence for Diploastrea as an alternate climate archive in the Indo-Pacific region and seals its potential in helping resolve less understood global-scale climate phenomena.
机译:Indo-Pacific Coral Diploastrea Heliopora使用珊瑚碳酸盐O-18(O-18(C))作为海表面温度(SST)和海表面盐度(SSS)的组合代理,揭示了区域多数至百年气候变异性。但是,为了评估珊瑚在解决气候事件中的全部潜力,独立的SST代理将更有利于。我们审查了菲律宾东北吕宋岛收集的邻近Porites Lobata核心的Diploastea的SR / CA和O-18。来自Diploastea的冬季SR / CA数据显示与SST(r = -0.41,p <0.05,(残留)RMSR = 0.81摄氏度的根均线(均方根 - 平方)的显着相关性,并提供具有与Porites相似敏感性的代理(R. = -0.57,P <0.05,RMSR = 0.62℃)。 SST记录显示出稳健,并且用于在北冬(R = -0.70,P = 0.02)期间重建太平洋二等振荡的重建。虽然我们无法在际时间尺度处产生强大的Diploastrea O-18-SSS校准,但在该地区通常观察到的目前的新鲜趋势在Diploastrea O-18中被定性地捕获。与Porites O-18和仪器SSS记录的比较表明,珊瑚物种之间的新鲜幅度一致。湿季节豪华卫星O-18为我们网站提供了对EL Nino-Southern振荡事件和局部降水的相对影响的支持。本研究的多分歧方法进一步加强了Diploastrea作为互联地区的备选气候档案的证据,并密封其帮助解决较少理解的全球范围气候现象。

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