Abstract

The present study was performed to assess the feeding performance of five detritivore species in a microcosm design. The test animals were four millipede species, Telodeinopus aoutii (Demange), Epibolus pulchripes (Gerstäcker), Cylindroiulus caeruleocinctus (Wood), Glomeris hexasticha (Brandt), and one isopod species, Porcellio scaber (Latreille), all feeding on Alnus glutinosa L. leaf litter for five consecutive weeks. At the end of each one-week interval, litter consumption, animal fresh weight, and excrement production were measured. Then, the feeding activity parameters for each species were calculated. Between big-size animal species, higher leaf consumption rates of 12.3–30.9 mg dry weight day−1 individual−1 were calculated for T. aoutii compared to those of 3.72–8.25 mg dry weight day−1 individual−1 for E. pulchripes. However, there was no difference in the consumption rates among small-size animals ranging from 0.46 to 1.65 mg dry weight day−1 individual−1. Excrement production rates followed a similar trend, as the consumption rates and the animals’ body weight remained constant during the experiment. Time was an important factor influencing the feeding activity of the animals, especially for the big-size group. Overall, the average assimilation efficiency of these species varied from 13.7% to 53.3%. The results of the present work will be the first step for understanding the ecological needs of these decomposer species in soil ecosystems.

Highlights

  • Decomposition of organic matter is an important stage in soil formation and its developmental process and soil functions [1,2]

  • Higher leaf consumption was observed in the big-size animals (T. aoutii and E. pulchripes; Figure 1a) compared to the small-size animals (C. caeruleocinctus, G. hexastica, and P. scaber)

  • Litter consumption was significantly decreased till the end of experiment for T. aoutii (Figure S2a, Supplementary Materials; F4,15 = 17.4, p < 0.001), C. caeruleocinctus (F4,15 = 3.66, p < 0.05), and P. scaber (F4,15 = 4.93, p < 0.01), but not for E. pulchripes (F4,15 = 2.75, p = 0.07) and G. hexastica (F4,15 = 2.54, p = 0.08)

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Summary

Introduction

Decomposition of organic matter is an important stage in soil formation and its developmental process and soil functions [1,2]. During litter decomposition, inorganic nutrients are released to the surrounding environment [6,7]. In this way, detritivore species may contribute to the nutrient cycling and availability of these nutrients to other soil organisms. Soil invertebrate may facilitate microbial colonization due to the fragmentation of leaf litter and increasing its surface area [8,9,10]. Their interaction is very important for plant material decomposition [11]

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