Spatial and temporal variabilities of δC and δN within lower trophic levels of a large lake: implications for estimating trophic relationships of consumers.

Stable isotopes of carbon (δC) and nitrogen (δN) often have unique values among lake habitats (e.g. benthic, littoral, pelagic), providing a widely used tool for measuring the structure and energy flow in aquatic food webs. However, there has been little recognition of the spatial and temporal variabilities of these isotopes within habitats of aquatic ecosystems. To address this, δC and δN were measured in seston, zebra mussels ( Dreissena polymorpha) and young-of-year (YOY) yellow ( Perca flavescens), and white perch ( Morone americana) collected from four sites across the offshore habitat of the western basin of Lake Erie during June-September 2009. Values of δC and δN showed significant spatial and temporal variations, with month accounting for >50% of the variation, for both stable isotopes and all the species except seston. Such variation in isotope values has the potential to significantly influence or confound interpretation of stable isotopes in measures, such as trophic position (TP) which use lower trophic level organisms as their baseline. For example, TP was found to vary up to 0.7 for yellow and white perch (TP = δN − δN/diet-tissue fractionation factor) depending on the zebra mussel data used (e.g., from a different location or a different collection month). As the use of stable isotopes continues to move from qualitative to more quantitative measures of trophic structure, food web research must recognize the importance of stable isotopes' variability in lower trophic level organisms, especially in large lake systems. [ABSTRACT FROM AUTHOR]