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An isotopic (Δ14C, δ13C, and δ15N) investigation of the composition of particulate organic matter and zooplankton food sources in Lake Superior and across a size-gradient of aquatic systems

机译:同位素(Δ14C,δ13C和δ15N)研究了苏底湖中颗粒有机质和浮游动物食物来源的组成,以及水产系统的尺寸梯度

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Food webs in aquatic systems can be supported both by carbon from recent local primary productivity and by carbon subsidies, such as material from terrestrial ecosystems, or past in situ primary productivity. The importance of these subsidies to respiration and biomass production remains a topic of debate. While some studies have reported that terrigenous organic carbon supports disproportionately high zooplankton production, others have suggested that phytoplankton preferentially support zooplankton production in aquatic ecosystems. Here we apply natural abundance radiocarbon (Δ14C) and stable isotope (δ13C, δ15N) analyses to show that zooplankton in Lake Superior selectively incorporate recently fixed, locally produced (autochthonous) organic carbon even though other carbon sources are readily available. Estimates from Bayesian isotopic modeling based on 14C and 13C values show that the average lake-wide median contributions of recent in-lake primary production and terrestrial, sedimentary, and bacterial organic carbon to the bulk POM in Lake Superior were 58%, 5%, 33%, and 3%, respectively. However, isotopic modeling estimates also show that recent in situ production contributed a disproportionately large amount (median, 91%) of the carbon in mesozooplankton biomass in Lake Superior. Although terrigenous organic carbon and old organic carbon from resuspended sediments were significant portions (median, 38%) of the available basal food resources, these contributed only a small amount to mesozooplankton biomass. Comparison of zooplankton food sources based on their radiocarbon composition showed that terrigenous organic carbon was relatively more important in rivers and small lakes, and the proportion of terrestrially derived material used by zooplankton correlated with the hydrologic residence time and the ratio of basin area to water surface area.
机译:水产系统中的食物网可以通过近期局部初级生产力和碳补贴等碳来支持,例如来自地面生态系统的材料,或以原位的初级生产力。这些补贴对呼吸和生物质生产的重要性仍然是辩论的主题。虽然有些研究报告说,人造有机碳支持不成比例的高浮游生物,但其他人提出浮游植物优先支持水生生态系统中的浮游植物生产。在这里,我们应用天然丰富的radiocarbon(Δ14c)和稳定的同位素(Δ13c,Δ15n)分析,以表明湖泊中的浮游动物在湖泊中选择性地掺入最近固定的,本地产生的(自身加载的)有机碳,即使其他碳源很容易获得。基于14C和13C价值的贝叶斯同位素建模估计表明,湖泊湖湖初级生产和陆地,沉积和细菌有机碳的普通湖泊宽的中位数贡献为优越湖的散装POM为58%,5%,分别为33%和3%。然而,同位素建模估计也表明,最近的原位生产促进了湖泊中湖中的Mesozooplankton生物质中的碳含量不成比例的大量(中位数,91%)。虽然来自重悬的沉积物的人造有机碳和旧有机碳是可用的基础食品资源的重要部分(中位数,38%),但这些额外的含量仅为Mesozooplankton生物量贡献。基于其无线电碳组合物的浮游植物食物来源的比较显示,河流和小湖泊中的堆积有机碳是相对更重要的,浮游动物与水文停留时间相关的北方衍生材料的比例和盆地区域与水面的比例区域。

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