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首页> 外文期刊>Geochimica et Cosmochimica Acta: Journal of the Geochemical Society and the Meteoritical Society >Multi-specimen and multi-site calibration of Aleutian coralline algal Mg/Ca to sea surface temperature
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Multi-specimen and multi-site calibration of Aleutian coralline algal Mg/Ca to sea surface temperature

机译:阿留申珊瑚藻Mg / Ca对海面温度的多标本和多地点标定

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摘要

Higher latitude oceanic and climatic reconstructions are needed to distinguish natural climate variability from anthropogenic warming in regions projected to experience significant increases in temperature during this century. Clathromorphum nereostratum is a long-lived coralline alga abundant along the Aleutian archipelago that records seasonal to centennial fluctuations in seawater temperatures in its high-Mg calcite skeleton. Thus, C. nereostratum is an important proxy archive to reconstruct past seawater temperature variability in this data-poor subarctic region. Here, we measured magnesium to calcium ratios (Mg/Ca) by laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) along the growth axis in six live-collected specimens from three islands in the Aleutian archipelago to assess Mg/Ca reproducibility and to calibrate algal Mg/Ca against modern gridded sea surface temperature (SST) data products. The master Mg/Ca-SST transfer function, determined by averaging the algal Mg/Ca-SST from each island (n=6), resulted in a reconstruction error of ±0.45 ℃, a 31-46% reduction in error compared to the reconstruction error for a single alga. The master algal-SST record interpolated to monthly and annual resolution significantly varied with gridded SST data products (r~2=0.98, p<0.0001, n=517 and r~2=.27, p<0.0003, n=44, respectively) for the period from 1960 to 2003. Therefore, coralline algal Mg/Ca-derived SST reconstructions record absolute changes in past SST variability in the Aleutian archipelago. The transfer functions developed here can be applied to Mg/Ca records generated from long-lived specimens of C. nereostratum to reconstruct northern North Pacific and Bering Sea SST variability for the past several hundred years.
机译:在本世纪预计气温将显着上升的地区,需要进行更高纬度的海洋和气候重建,以将自然气候变化与人为变暖区分开来。笼形藻是一种长寿的珊瑚藻,分布在阿留申群岛上,记录了高镁方解石骨架中海水温度的季节性至百年波动。因此,C。nereostratum是一个重要的代理档案,可以重建这个数据贫乏的亚北极地区过去的海水温度变化。在这里,我们通过激光烧蚀-电感耦合等离子体质谱法(LA-ICP-MS)沿生长轴测量了阿留申群岛三个岛屿的六个活体标本中的镁与钙之比(Mg / Ca),以评估Mg / Ca可再现性,并针对现代栅格化海面温度(SST)数据产品校准藻Mg / Ca。通过平均每个岛上的藻类Mg / Ca-SST(n = 6)求出的主Mg / Ca-SST传递函数导致重建误差为±0.45℃,与之相比,误差降低了31-46%。单个藻类的重建错误。藻类SST主记录插值到月度和年度分辨率随网格SST数据产品的变化显着(r〜2 = 0.98,p <0.0001,n = 517和r〜2 = .27,p <0.0003,n = 44 )从1960年到2003年。因此,珊瑚藻类Mg / Ca衍生的SST重建记录了阿留申群岛过去SST变异性的绝对变化。此处开发的传递函数可以应用于从长寿命神经纹层标本中生成的Mg / Ca记录,以重建北太平洋北部和白令海SST过去数百年的变异性。

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