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首页> 外文期刊>Biogeosciences >High frequency Barium profiles in shells of the Great Scallop iPecten maximus/i: a methodical long-term and multi-site survey in Western Europe
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High frequency Barium profiles in shells of the Great Scallop iPecten maximus/i: a methodical long-term and multi-site survey in Western Europe

机译:大扇贝贝壳中的高频钡剖面:西欧有条不紊的长期多站点调查

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Skeletal barium/calcium ([Ba]/[Ca])shell ratios were measured everythird daily striae in 39 flat valves of the Great Scallop Pecten maximus collected intemperate coastal environments of Western Europe. A methodical evaluation ofthe ([Ba]/[Ca])shell ratio was performed for the first time anddemonstrates that ([Ba]/[Ca])shell profiles are reproducible forseveral scallop individuals from the same population (2-year old; 3shells/year), over a 7-year period (1998–2004), and from different coastalenvironments in France (42–49° N). As previously determined in the shellsof other bivalve species, ([Ba]/[Ca])shell profiles generally exhibiteda background ratio punctuated by two transient maxima occurring in early andlate summer. Background partition coefficient (DBa=0.11±0.03,in 2000) was similar to that previously reported in P. maximus shells, suggesting adirect shell uptake of dissolved seawater Ba (Gillikin et al.,2008). The 7-year survey in the Bay of Brest of the high frequency([Ba]/[Ca])shell profiles in the scallop's shell was exploited tobetter constrain both the occurrence and the amplitude of the summer Barelative enrichments as influenced by environmental processes. Seawater Bacontents in 2000 underlined significant particulate Ba inputs at thesediment water interface (SWI) during ([Ba]/[Ca])shell peak events.These Ba inputs are thus suggested to be subsequently induced by a pelagicbiogenic process, which mainly occurs under summer post-bloom conditions inrelationship to the cycling of particulate organic matter and associated Ba.The long term survey reveals that such pelagic Ba cycling processes areresponsible for particulate Ba inputs to the sediment water interface (SWI).Subsequent indirect Ba uptake by the bivalve results in higher([Ba]/[Ca])shell ratios, in that archived Ba within the shell cannot beused as a direct paleo productivity tracer. Our methodical approach, basedon a multi-year and multi-site-survey of ([Ba]/[Ca])shell ratio inScallop bivalves, allows us to establish the potential application of suchhigh frequency archives for further biogeochemical and ecologicalinvestigations of bivalves in the coastal environment.
机译:在大扇贝的39个扁平瓣中收集的西部不温带沿海环境中,每三天每天测量一次骨骼钡/钙([Ba] / [Ca]) shell 比欧洲。首次对([Ba] / [Ca]) shell 比率进行了系统的评估,证明([Ba] / [Ca]) shell 轮廓是可重现的来自同一人口(2岁; 3壳/年),在过去7年(1998-2004年)中以及来自法国不同沿海环境(北纬42-49°)的数个扇贝个体。如先前在其他双壳类物种的壳中所确定的那样,([Ba] / [Ca]) shell 剖面通常表现出背景比率,该比率被夏季和初夏出现的两个瞬时最大值所打断。背景分配系数(D Ba = 0.11±0.03,在2000年)与以前在 P中报道的相似。壳最大,表明直接吸收了溶解的海水Ba(Gillikin等,2008)。在布雷斯特湾对扇贝贝壳中的高频([Ba] / [Ca]) shell 剖面进行了为期7年的调查,目的是更好地限制夏季Barelative的发生和幅度受环境过程影响的浓缩。在([Ba] / [Ca]) shell 峰值事件期间,2000年海水中的Ba含量突显了这些沉积物水界面(SWI)上大量的Ba颗粒输入,因此,这些Ba输入被认为是由远洋生物成因引起的。长期调查显示,这种中上层Ba循环过程对沉积物水界面(SWI)中的Ba颗粒输入负有责任。双壳类对钡的吸收导致较高的[[Ba] / [Ca]) shell 比,这是因为壳中的已归档Ba不能用作直接的古生产力示踪剂。我们的方法基于扇贝双壳类([Ba] / [Ca]) shell 比率的多年期和多地点调查,使我们能够建立此类高频档案的潜在应用,以进一步沿海环境中双壳类动物的生物地球化学和生态调查。

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