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双壳贝类壳微量元素组成能否记录超高频率的环境变化?

Does trace element composition of bivalve shells record utra-high frequency environmental variations?

机构信息

Univ. Brest, CNRS, IRD, Ifremer, LEMAR, F-29280, Plouzané, France; Fisheries and Oceans Canada, Maurice Lamontagne Institute, Mont-Joli, QC, Canada.

Univ. Brest, CNRS, IRD, Ifremer, LEMAR, F-29280, Plouzané, France.

出版信息

Mar Environ Res. 2020 Jun;158:104943. doi: 10.1016/j.marenvres.2020.104943. Epub 2020 Mar 5.

Abstract

Saint-Pierre and Miquelon (SPM) is a small archipelago where instrumental measures based on water column velocity and temperature profiles compiled comprehensive evidence for strong near-diurnal (25.8h) current and bottom temperature oscillations (up to 11.5 °C) which is possibly the largest ever observed - at any frequency - on a stratified mid-latitude continental shelf. The main objective of our study was to identify if Placopecten magellanicus can record on its shell these high frequency environmental variations. To this end, we have tried to identify proxies for water temperature and food availability through development of a new ultra-high resolution LA-ICPMS analyses method capable of resolving shell surface elemental composition with a 10 μm resolution. This method was applied on two shell fragments, both representing the third year of growth and 2015 annual growth period, respectively coming from two environmentally contrasted sites, more (30 m depth) or less (10 m depth) affected by high frequency thermal oscillations. Our results strongly suggest a relationship between phytoplankton biomass and barium incorporation into P. magellanicus shells at both sites. Even if P. magellanicus might present a physiological control of magnesium incorporation, the shape of the two Mg/Ca profiles seems to illustrate that temperature also exerts a control on magnesium incorporation in P. magellanicus shells from SPM. While U/Ca and Mg/Ca profiles show a strong positive correlation for 30 m site shell, suggesting that uranium incorporation in P. magellanicus shell is at least partially temperature dependent. The absence of such correlation for 10 m site shell suggests differences in uranium environmental availability or in P. magellanicus biomineralization between these two sites. The resolution of this new analytical method raises questions about such data interpretation related to P. magellanicus growth dynamics and physiology or individual scale based environmental measurements.

摘要

圣皮埃尔和密克隆(SPM)是一个小群岛,基于水柱速度和温度剖面的仪器测量提供了强有力的近每日(25.8 小时)洋流和底层温度振荡的综合证据(最高可达 11.5°C),这可能是在任何频率下在分层中纬度大陆架上观察到的最大规模。我们研究的主要目的是确定褶牡蛎是否可以在其贝壳上记录这些高频环境变化。为此,我们试图通过开发一种新的超高分辨率激光烧蚀电感耦合等离子体质谱分析方法来确定水温和食物可用性的替代物,该方法能够以 10 μm 的分辨率解析贝壳表面的元素组成。该方法应用于两个贝壳碎片上,这两个贝壳分别代表生长的第三年和 2015 年的年度生长期,分别来自两个环境差异较大的地点,一个地点(30 米深)受高频热振荡的影响较大,另一个地点(10 米深)受高频热振荡的影响较小。我们的结果强烈表明,在这两个地点,浮游植物生物量和钡在褶牡蛎贝壳中的掺入之间存在关系。即使褶牡蛎可能对镁的掺入具有生理控制作用,但两个 Mg/Ca 剖面的形状似乎表明,温度也对来自 SPM 的褶牡蛎贝壳中镁的掺入具有控制作用。虽然 30 米深地点贝壳的 U/Ca 和 Mg/Ca 剖面显示出强烈的正相关,但 10 米深地点贝壳的 U/Ca 和 Mg/Ca 剖面没有显示出这种相关性,这表明铀在褶牡蛎贝壳中的掺入至少部分取决于温度。10 米深地点贝壳中铀的环境可用性或这两个地点褶牡蛎生物矿化之间存在差异,这对这种新分析方法的分辨率提出了有关褶牡蛎生长动态和生理学或个体尺度环境测量数据解释的问题。

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