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首页> 外文期刊>Ecological indicators >Taxon-specific variation in δ~(13)C and δ~(15)N of subfossil invertebrate remains: Insights into historical trophodynamics in lake food-webs
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Taxon-specific variation in δ~(13)C and δ~(15)N of subfossil invertebrate remains: Insights into historical trophodynamics in lake food-webs

机译:亚化石无脊椎动物的δ〜(13)C和δ〜(15)N的分类群特异性变化:对湖泊食物网中历史营养动力学的认识

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摘要

Carbon and nitrogen stable isotope ratios of sub-fossil invertebrate remains are potentially powerful indicators of nutrient flux, habitat-specific resource utilization, and trophic interactions in lentic food webs, but are rarely estimated for multiple species within lakes. Here we examined historical time series of delta C-13 and delta N-15 in remains of individual invertebrate taxa representing pelagic, littoral and benthic habitats during the 20th century in five boreal lakes of central Canada. We applied a novel statistical approach based on Generalized Additive Models (GAMs) to quantify the differences in centennial means and trends (i) between invertebrate remains and sedimentary organic matter (SOM), and (ii) among different taxa within each lake to evaluate the coherence of isotope signals during the 20th century. Differences in mean delta C-13 and delta N-15 were usually significant (p 0.05) between SOM and invertebrate taxa, and among individual taxa, reflecting selective feeding by invertebrates and differences in trophic position within food webs. In contrast, patterns of historical variance in isotope values varied among lakes with few consistent differences between long-term isotopic trends of SOM and invertebrate remains. In particular, SOM and invertebrate isotopic trends were similar in relatively dystrophic lakes, likely due to the importance of terrestrial carbon in both SOM and invertebrate diets. However, significant SOM-invertebrate trend differences were observed for both delta C-13 and delta N-15 in relatively clear-water lakes, possibly reflecting temporal variation in diets or tissue fractionation. Comparisons of historical trends in isotope values among taxa revealed few consistent patterns, likely indicating uncoupled carbon and nitrogen fluxes through invertebrate consumers with different habitat specializations or feeding modes. Together, our findings suggest that evaluation of taxon-specific delta C-13 and delta N-15 can provide valuable insights into historical tropho-dynamics in lake food webs.
机译:化石无脊椎动物残骸的碳和氮稳定同位素比是潜在的有力的养分通量,特定栖息地资源利用和片状食物网中营养相互作用的指标,但很少对湖泊中的多种物种进行估算。在这里,我们研究了代表加拿大中部五个北方湖泊在20世纪中上层,沿海和底栖生境的无脊椎动物分类单元的残骸中C-13和N-15的历史时间序列。我们应用了基于广义加性模型(GAM)的新颖统计方法来量化百年平均值和趋势的差异(i)无脊椎动物残骸和沉积有机物(SOM)之间的差异,以及(ii)每个湖泊内不同分类群之间的差异,以评估20世纪同位素信号的相干性。在SOM和无脊椎动物类群之间以及各个类群之间,平均C-13和N-15的差异通常很明显(p <0.05),这反映了无脊椎动物的选择性觅食和食物网中营养位置的差异。相反,湖泊中同位素值的历史变化模式各不相同,SOM和无脊椎动物的长期同位素趋势之间几乎没有一致的差异。特别是,在营养不良的湖泊中,SOM和无脊椎动物同位素的趋势相似,这可能是由于SOM和无脊椎动物饮食中陆地碳的重要性。然而,在相对清澈的水域湖泊中,在C-13和N-15三角洲均观测到明显的SOM无脊椎动物趋势差异,这可能反映了饮食或组织分离的时间变化。比较各类群中同位素值的历史趋势发现,几乎没有一致的模式,这可能表明通过具有不同生境专业化或摄食模式的无脊椎动物消费者的碳和氮通量是不相关的。在一起,我们的研究结果表明,评估特定分类群的C-13和N-15可以提供有关湖泊食物网中历史营养动力学的有价值的见解。

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