Abstract

This study aimed to determine the variability of carbon and nitrogen elemental content, stoichiometry and diet proportions of invertebrates in two sub-tropical estuaries in South Africa experiencing seasonal changes in rainfall and river inflow. The elemental ratios and stable isotopes of abiotic sources, zooplankton and macrozoobenthos taxa were analyzed over a dry/wet seasonal cycle. Nutrient content (C, N) and stoichiometry of suspended particulate matter exhibited significant spatio-temporal variations in both estuaries, which were explained by the variability in river inflow. Sediment particulate matter (%C, %N and C:N) was also influenced by the variability in river flow but to a lesser extent. The nutrient content and ratios of the analyzed invertebrates did not significantly vary among seasons with the exception of the copepod Pseudodiaptomus spp. (C:N) and the tanaid Apseudes digitalis (%N, C:N). These changes did not track the seasonal variations of the suspended or sediment particulate matter. Our results suggest that invertebrates managed to maintain their stoichiometry independent of the seasonality in river flow. A significant variability in nitrogen content among estuarine invertebrates was recorded, with highest % N recorded from predators and lowest %N from detritivores. Due to the otherwise general lack of seasonal differences in elemental content and stoichiometry, feeding guild was a major factor shaping the nutrient dynamics of the estuarine invertebrates. The nutrient richer suspended particulate matter was the preferred food source over sediment particulate matter for most invertebrate consumers in many, but not all seasons. The most distinct preference for suspended POM as a food source was apparent from the temporarily open/closed system after the estuary had breached, highlighting the importance of river flow as a driver of invertebrate nutrient dynamics under extreme events conditions. Moreover, our data showed that estuarine invertebrates concentrated C and N between 10–100 fold from trophic level I (POM) to trophic level II (detritivores/deposit feeders) and thus highlighted their importance not only as links to higher trophic level organisms in the food web, but also as providers of a stoichiometrically homeostatic food source for such consumers. As climate change scenarios for the east coast of South Africa predict increased rainfall as a higher number of rainy days and days with higher rainfall, our results suggest that future changes in rainfall and river inflow will have measurable effects on the nutrient content and stoichiometry of food sources and possibly also in estuarine consumers.

Highlights

  • Ecological stoichiometry focuses on studying the balance of elements in ecological interactions and processes [1]

  • Several principles have been developed in ecological stoichiometry theory, which aim to explain the characteristics of elemental composition and ratios in organisms

  • The analysis of elemental content (C, N), stoichiometry (C:N) and diet composition in relation to seasonal variations of river inflow and rainfall in the temporarily open/closed Mpenjati Estuary and permanently open Mlalazi Estuary revealed a large influence of river inflow on suspended organic matter and to a lesser extent on sediment organic matter

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Summary

Introduction

Ecological stoichiometry focuses on studying the balance of elements in ecological interactions and processes [1]. Persson et al [8] analyzed 132 datasets from published studies to test the generality of the strict homeostasis assumption; they found that autotrophs were generally less homeostatic than heterotrophs, but that heterotrophic species differed in their degree of homeostatic regulation. These authors suggest that the degree of homeostasis is strongly influenced by both environmental and physiological factors. Large elemental imbalances between primary food sources and consumers can modify the growth, reproduction and nutrient release of an organism, with consequences at the community and ecosystem level [3,9,11]

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