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首页> 外文期刊>Palaeogeography, Palaeoclimatology, Palaeoecology: An International Journal for the Geo-Sciences >High-resolution analysis of trace elements in crustose coralline algae from the North Atlantic and North Pacific by laser ablation ICP-MS
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High-resolution analysis of trace elements in crustose coralline algae from the North Atlantic and North Pacific by laser ablation ICP-MS

机译:激光烧蚀ICP-MS对北大西洋和北太平洋地壳珊瑚藻中的微量元素进行高分辨率分析

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We have investigated the trace elemental composition in the skeleta of two specimens of attached-living coralline algae of the species Clathromorphum compactum from the North Atlantic (Newfoundland) and Clathromorphum nereostratum from the North Pacific/Bering Sea region (Amchitka Island, Aleutians). Samples were analyzed using Laser Ablation-Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS) yielding for the first time continuous individual trace elemental records of up to 69. years in length. The resulting algal Mg/Ca, Sr/Ca, U/Ca, and Ba/Ca ratios are reproducible within individual sample specimens. Algal Mg/Ca ratios were additionally validated by electron microprobe analyses (Amchitka sample). Algal Sr/Ca, U/Ca, and Ba/Ca ratios were compared to algal Mg/Ca ratios, which previously have been shown to reliably record sea surface temperature (SST). Ratios of Sr/Ca from both Clathromorphum species show a strong positive correlation to temperature-dependent Mg/Ca ratios, implying that seawater temperature plays an important role in the incorporation of Sr into algal calcite. Linear Sr/Ca-SST regressions have provided positive, but weaker relationships as compared to Mg/Ca-SST relationships. Both, algal Mg/Ca and Sr/Ca display clear seasonal cycles. Inverse correlations were found between algal Mg/Ca and U/Ca, Ba/Ca, and correlations to SST are weaker than between Mg/Ca, Sr/Ca and SST. This suggests that the incorporation of U and Ba is influenced by other factors aside from temperature.
机译:我们研究了来自北大西洋(纽芬兰)的致密藻物种(Clathromorphum compactum)和来自北太平洋/白令海地区(Amchitka岛,阿留申群岛)的Clathromorphum nereostratum的两个附着的活珊瑚藻的标本中的痕量元素组成。使用激光烧蚀-电感耦合等离子体质谱法(LA-ICP-MS)分析样品,首次获得连续的单个痕量元素记录,最长记录长达69年。生成的藻Mg / Ca,Sr / Ca,U / Ca和Ba / Ca之比在各个样品标本中均可重现。藻的Mg / Ca比值还通过电子探针分析(Amchitka样品)进行了验证。将藻类Sr / Ca,U / Ca和Ba / Ca之比与藻类Mg / Ca之比进行了比较,以前已证明它们能可靠地记录海表温度(SST)。两种笼形藻中Sr / Ca的比例与温度相关的Mg / Ca的比例均显示出很强的正相关关系,这表明海水温度在Sr掺入藻方解石中起着重要作用。与Mg / Ca-SST关系相比,线性Sr / Ca-SST回归提供了正相关但较弱的关系。藻类Mg / Ca和Sr / Ca均显示清晰的季节性周期。发现藻类Mg / Ca与U / Ca,Ba / Ca之间呈反相关,与SST的相关性比Mg / Ca,Sr / Ca和SST之间的相关性弱。这表明除了温度以外,U和Ba的掺入还受其他因素影响。

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