首页> 外文期刊>Biogeosciences >Mussel shells of iMytilus edulis/i as bioarchives of the distribution of rare earth elementsand yttrium in seawater and the potential impact of pH and temperature ontheir partitioning behavior
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Mussel shells of iMytilus edulis/i as bioarchives of the distribution of rare earth elementsand yttrium in seawater and the potential impact of pH and temperature ontheir partitioning behavior

机译:贻贝壳的 mytilus edulis 作为海水中稀土元素分布的生物分配,以及钇在海水中的潜在影响和温度对他的分区行为的潜在影响

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Mussel shells are potential bioarchives of proxies for changes in thephysicochemical conditions in the bivalve's habitat. One such proxy is thedistribution of rare earths and yttrium (REY) in seawater, as REYspeciation in seawater is sensitive to pH and temperature variations, due tothe impact of these parameters on the activity of CO32? inseawater. We present a new protocol for sample preparation and determinationof ultratrace concentrations of REY in bulk bivalve shells (comprised ofcalcite and aragonite) that includes sample treatment with NaOCl followedby REY separation and preconcentration. The data obtained were used tocalculate REY partition coefficients between bulk bimineralic shellsof Mytilus edulis (calcite aragonite mix) and ambient seawater, and the results acquired werethen used to investigate the potential effects of pH and temperature on REYpartitioning.Shells of Mytilus edulis mussels from the North Sea show consistent shale-normalized(SN) REY patterns that increase from the light REY to the middle REY anddecrease from the middle REY to the heavy REY. Despite being different from the general seawater REYSN pattern, the shells still display distinctREY features of seawater, such as a negative CeSN anomaly and smallpositive YSN and GdSN anomalies. Apparent REY partitioncoefficients between shells and seawater (appDTot.REYshell/seawater) are low and decrease stronglyfrom the light REY (4.04 for La) to the heavy REY (0.34 for Lu). However,assuming that only the free REY3+ are incorporated into the shell,modDFreeREY3+shell/seawater values are higher andcomparatively similar for all REY (102.46 for La; 113.44 for Lu) but show a slightmaximum at Tb (199.18). Although the impact of vital effects, such as REYspeciation in a mussel's extrapallial fluid from which the carbonateminerals precipitate, cannot be quantified yet, it appears that M. edulis shells arebioarchives of some REY features of seawater.We modeled the REYSN patterns of a hypothetical mussel shell at pH 8.2and 7.6 and at temperatures of 25 and 5?°C, assumingthat only free REY3+ are incorporated into the carbonate's crystallattice and that vital effects do not obliterate the REY signal of theshells. The results suggest that with lower pH, REY concentrations in shellsincrease, but with little effect on the shape of the REYSN patterns,while a temperature change has an impact on the REYSN pattern but onlyminor effects on REY concentrations. Hence, after additional calibrationstudies, the REY systematics in mussel shells may become a valuable proxyfor paleo-pH and ocean acidification.
机译:贻贝贝壳是双向栖息地中物理化学条件的变化的潜在生物学。一个这样的代理是海水中稀土和钇(Rey)的分布,因为海水中的重新分析对pH和温度变化敏感,因此这些参数对CO 3 活性的影响。 2?内部水。我们提出了一种新的样品制备方法,用于散装双壳壳中的富含芦苇浓度(由甲酰胺和金属石),包括用NaoCL随后的rey分离和前浓缩的样品处理。获得的数据被用来在散装丛生壳(Capite Aragite Mix)和环境海水中的散装酰胺壳之间的rey分区系数在散装酰胺壳(Calcite Aragite Mix)和环境海水中,并且结果获得了Werethen用于研究pH和温度对再现的潜在影响。< br> 米蒂斯的贝壳 mytilus edulis 来自北海的贻贝显示一致的页岩标准化(sn)rey模式,从中间芦苇到中间芦苇到沉重的芦苇。尽管与普通海水Rey Sn 模式不同,但壳牌仍然显示海水的独特植物特征,例如负CE sn 异常和小型y sn 和GD sn 异常。贝壳和海水之间的表观芦苇分区( app d tot.rey shell / seawater )很低,并从灯光rey(4.04 for la for la for la )到沉重的芦苇(Lu 0.34)。然而,假设仅将自由Rey 3 + 纳入壳体中, mod d freerey3 + shell / seawater 对于所有Rey(La的102.46,LU的102.46),值更高且不可变地相似,但在TB(199.18)中显示出略微达到的。虽然迄今为止乌斯特的挤压液中的重新分析等生命影响的影响尚不能量,但尚不定量碳原态沉淀物,似乎是 m。 Edulis 贝壳是海水的一些rey特征的贝壳。 在pH8.2和7.6和25和5的温度下,我们建模了假设贻贝壳的rey 模式。 °C,假设仅免费Rey 3 + 被掺入碳酸盐的晶体中,并且生命效应不会抹去TheShells的rey信号。结果表明,贝壳中的pH值较低,rey浓度较少,但对rey sn 图案的形状几乎没有影响,而温度变化对rey sn 图案,但仅对芦苇浓度的影响。因此,在额外的次次校准中,贻贝壳中的芦苇系统可能成为古pH和海洋酸化的有价值的。

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