Abstract

Animal excretion can be a significant nutrient flux within ecosystems, where it supports primary production and facilitates microbial decomposition of organic matter. The effects of excretory products on nutrient cycling have been documented for various species and ecosystems, but temporal variation in these processes is poorly understood. We examined variation in excretion rates of a dominant grazing snail, Elimia clavaeformis, and its contribution to nutrient cycling, over the course of 14 months in a well-studied, low-nutrient stream (Walker Branch, east Tennessee, USA). Biomass-specific excretion rates of ammonium varied over twofold during the study, coinciding with seasonal changes in food availability (measured as gross primary production) and water temperature (multiple linear regression, R 2 = 0.57, P = 0.053). The contribution of ammonium excretion to nutrient cycling varied with seasonal changes in both biological (that is, nutrient uptake rate) and physical (that is, stream flow) variables. On average, ammonium excretion accounted for 58% of stream water ammonium concentrations, 26% of whole-stream nitrogen demand, and 66% of autotrophic nitrogen uptake. Phosphorus excretion by Elimia was contrastingly low throughout the year, supplying only 1% of total dissolved phosphorus concentrations. The high average N:P ratio (89:1) of snail excretion likely exacerbated phosphorus limitation in Walker Branch. To fully characterize animal excretion rates and effects on ecosystem processes, multiple measurements through time are necessary, especially in ecosystems that experience strong seasonality.

Highlights

  • Animals can affect carbon and nutrient cycling through direct and indirect pathways

  • We examined the contribution of snail excretion to whole-stream nutrient cycling by comparing excretion rates to three ecosystem metrics: (1) whole-stream ammonium uptake measured using steady-state ammonium releases, (2) autotrophic nutrient uptake, calculated from gross primary production measurements and the C:N and C:P of periphyton, and (3) volumetric excretion and excretion turnover distance

  • Stream water concentrations of ammonium and total dissolved phosphorus were variable through time, with no clear temporal pattern

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Summary

INTRODUCTION

Animals can affect carbon and nutrient cycling through direct (that is, excretion, egestion) and indirect (that is, grazing, soil compaction, bioturbation) pathways. Nitrogen (N) and phosphorus (P) excretion rates vary widely across species (Vanni and others 2002; McIntyre and others 2008; McManamay and others 2011) due to differences in body composition and variation in the N and P of food sources (Elser and Urabe 1999) External factors such as temperature (Gardner and others 1981; Devine and Vanni 2002) and food availability and quality (James and others 2007; Wilson and Xenopoulos 2011; Moslemi and others 2012) can influence excretion rates. Temperature, and nutrient uptake vary temporally in Walker Branch (Mulholland and others 1985a; Mulholland and Hill 1997; Roberts and others 2007), so we predicted that snail excretion and its potential role supporting stream nutrient cycling would vary as well. Because Elimia occurs at high densities in oligotrophic streams, we predicted its excretion would be a major contribution to nutrient flux in Walker Branch

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