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Updated: May 15, 2026

Linking Predation Risk, Herbivore Physiological Stress and Microbial Decomposition of Plant Litter
Published on: March 12, 2013
Herbivore trampling as an alternative pathway for explaining differences in nitrogen mineralization in moist
Maarten Schrama1, Pieter Heijning, Jan P Bakker
1Community and Conservation Ecology, University of Groningen, PO Box 11103, 9700 CC Groningen, The Netherlands. m.schrama@nioo.knaw.nl
Large herbivores impact nitrogen cycling differently based on soil type. In clay soils, grazing reduces nitrogen mineralization by compacting soil, while sandy soils show no such effect, highlighting the importance of soil texture.
Area of Science:
- Ecology
- Soil Science
- Biogeochemistry
Background:
- Large herbivores influence nitrogen cycling in grasslands, with effects varying by soil fertility.
- Recent findings indicate herbivores can reduce nitrogen mineralization in some fertile soils, prompting further investigation.
Purpose of the Study:
- To test the hypothesis that large herbivores affect nitrogen mineralization based on soil texture.
- To elucidate the mechanisms behind herbivore impacts on nitrogen mineralization in different soil types.
Main Methods:
- A 37-year field experiment on a salt marsh comparing herbivore-grazed and hand-mown treatments.
- Analysis of nitrogen mineralization rates, soil physical properties (compaction, water-filled porosity, redox potential), and soil macrofauna abundance.
- Investigation of decomposition activity in clay and sandy soil types.
Main Results:
- Herbivore presence decreased nitrogen mineralization in clay soil but not in sandy soil.
- Differences were attributed to herbivore-induced soil physical changes, not biomass removal.
- Clay soils showed increased water-filled porosity, negative redox potentials, reduced macrofauna, and lower decomposition under grazing.
Conclusions:
- Soil texture is a critical factor in understanding herbivore effects on nitrogen mineralization.
- Herbivore impacts are mediated by soil compaction, leading to anoxia and reduced decomposition in clay soils.
- Soil moisture and macrofauna dynamics are essential components of herbivore-ecosystem interactions.
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