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Variation in δ<sup>15</sup>N and δ<sup>13</sup>C trophic fractionation: Implications for aquatic food web studies
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2001
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BiologyIsotope AnalysisBiogeochemistryBiodiversityEngineeringTrophic ImpactAquatic Food SystemIsotopic FractionationIsotope GeochemistryEcosystem InteractionTrophic InteractionsTrophic FractionationStable Isotope ProbingFood Web InteractionFood WebTrophic WebTrophic Transfer
Stable isotope techniques for food web analysis rely on a priori estimates of trophic fractionation (Δδ15N and Δδ13C), yet even unbiased estimates vary, contributing error to quantitative isotope models. The study performed a broad‑scale analysis of Δδ15N and Δδ13C in aquatic systems, added three new field estimates, and simulated error variance in trophic position and diet mixing models by incorporating observed fractionation variation and other error sources. Carnivores exhibited significantly higher Δδ15N and Δδ13C values than herbivores, with greater variability among carnivores, invertebrates, and lab‑derived estimates; excluding herbivores, the mean Δδ15N and Δδ13C were 3.4‰ and 0.8‰, respectively, and the simulated error in trophic position and mixing model outputs was generally minor when primary consumers served as baselines and end‑member d13C values were distinct.
Use of stable isotope techniques to quantify food web relationships requires a priori estimates of the enrichment or depletion in δ 15 N and δ 13 C values between prey and predator (known as trophic fractionation; hereafter Δδ 15 N and Δδ 13 C). We conducted a broad‐scale analysis of Δδ 15 N and Δδ 13 C from aquatic systems, including three new field estimates. Carnivores had significantly higher Δδ 15 N values than herbivores. Furthermore, carnivores, invertebrates, and lab‐derived estimates were significantly more variable than their counterparts ( f‐test, p < 0.00001). Δδ 13 C was higher for carnivores than for herbivores ( p = 0.001), while variances did not differ significantly. Excluding herbivores, the average Δδ 15 N and Δδ 13 C were 3.4‰ and 0.8‰, respectively. But even with unbiased fractionation estimates, there is variation in isotopic fractionation that contributes to error in quantitative isotope model outputs. We simulated the error variance in δ 15 N‐based estimates of trophic position and two‐source δ 13 C diet mixing models, explicitly considering the observed variation in Δδ 15 N and Δδ 13 C, along with the other potential error sources. The resultant error in trophic position and mixing model outputs was generally minor, provided that primary consumers were used as baseline indicators for estimating trophic position and that end member d13C values in dietary mixing models were sufficiently distinct.