Factors Controlling Coral Skeletal U/Ca Ratios with Implications for their Use as a Proxy for Past Ocean Conditions

Emily Patterson, S. Eanes, Penelope Lancrete, Anne Gothman, P. Roback
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Abstract

Seawater temperature, salinity and carbonate chemistry have been shown to influence the uranium/calcium (U/Ca) ratios of scleractinian coral skeletons. This apparent sensitivity of U/Ca to multiple environmental parameters calls into question whether there is one environmental variable that most strongly controls coral U/Ca, and whether U/Ca can be straightforwardly applied as a paleoenvironmental proxy due to the tendency of environmental variables to covary in space and time. In this study, uranium concentration data from an existing compilation of tropical scleractinian coral U-series measurements is paired with environmental data from the World Ocean Atlas (WOA) and the Global Ocean Data Analysis Project (GLODAP) to examine the sensitivity of coral skeletal U/Ca to multiple seawater properties including temperature, salinity, pH, and saturation state. First, univariate linear regressions and multiple linear regressions were used to compare relationships between uranium and environmental parameters in the dataset with relationships observed in previous studies. Next, principal component analysis and regularized regression were used to identify the most likely predictors of coral U/Ca in order to create a multiple linear regression model. Results indicate that pH, Ω, alkalinity, and temperature are all significant predictors of uranium concentrations in coral. The magnitude and strength of relationships between U/Ca and environmental variables also differ across different genera. Seawater properties with strong correlations and small ranges make interpretation of these results difficult. However, results of these analyses indicate that U/Ca is dependent on multiple environmental parameters and that previously developed univariate regressions may be insufficient to characterize the full range of variables that influence coral [238U]. KEYWORDS: Coral; Paleoceanography; Proxy Calibration; Uranium; Multiple Linear Regression; Regularized Regression; Environmental Change; Oceanographic Databases
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珊瑚骨骼U/Ca比值的控制因素及其作为过去海洋条件代理的含义
海水温度、盐度和碳酸盐化学已被证明会影响硬核珊瑚骨骼的铀/钙(U/Ca)比率。U/Ca对多种环境参数的明显敏感性引发了一个问题,即是否存在一个最强烈控制珊瑚U/Ca的环境变量,以及由于环境变量在空间和时间上的协变趋势,U/Ca是否可以直接用作古环境代理。在这项研究中,来自热带核状珊瑚U系列测量的现有汇编的铀浓度数据与世界海洋地图集(WOA)和全球海洋数据分析项目(GLODAP)的环境数据配对,以检查珊瑚骨骼U/Ca对多种海水特性的敏感性,包括温度、盐度、pH值和饱和状态。首先,利用单变量线性回归和多元线性回归,将数据集中铀与环境参数之间的关系与以往研究中观察到的关系进行比较。接下来,利用主成分分析和正则化回归来确定珊瑚U/Ca最可能的预测因子,以创建多元线性回归模型。结果表明,pH、Ω、碱度和温度都是珊瑚中铀浓度的重要预测因子。U/Ca与环境变量之间关系的大小和强度在不同属之间也存在差异。相关性强、范围小的海水性质使这些结果难以解释。然而,这些分析的结果表明,U/Ca依赖于多种环境参数,以前开发的单变量回归可能不足以表征影响珊瑚的所有变量[238U]。关键词:珊瑚;古海洋学;代理校准;铀;多元线性回归;正规化的回归;环境变化;海洋数据库
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