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Published on: June 30, 2020
Limited ecosystem recovery from simulated chronic nitrogen deposition
William D Bowman1, Asma Ayyad2, Clifton P Bueno de Mesquita1
1Department of Ecology and Evolutionary Biology and Institute of Arctic and Alpine Research, University of Colorado, Boulder, Colorado, 80309-0334, USA.
Even after nitrogen (N) deposition stops, ecosystems show slow recovery. Legacy effects like high N cycling and low soil nutrients persist, impacting plant and microbial communities long-term.
Area of Science:
- Ecology
- Biogeochemistry
- Environmental Science
Background:
- Anthropogenic nitrogen (N) deposition causes significant ecosystem changes.
- Ecosystem recovery after reduced N deposition can be slow due to long-lasting impacts and inertia.
Purpose of the Study:
- To investigate recovery patterns in an alpine ecosystem after a 12-year nitrogen (N) addition experiment.
- To identify factors contributing to slow or absent recovery following declines in N deposition.
Main Methods:
- Monitoring plant species composition, microbial abundance, N cycling rates, soil pH, and cation pools.
- Assessing changes over nine years post-cessation of simulated N deposition (0, 20, 40, 60 kg N·ha⁻¹·yr⁻¹).
Main Results:
- Simulated N deposition altered plant communities (increased nitrophilic species, decreased dominant sedges) and soil chemistry (decreased pH and Mg²⁺, increased Al³⁺ and Mn²⁺).
- Nine years post-cessation, only one plant species showed recovery; microbial abundance remained lower.
- Elevated nitrification rates, NO₃⁻ pools, and depressed base cations (Ca²⁺, Mg²⁺) persisted, alongside elevated toxic metals (Al³⁺, Mn²⁺).
Conclusions:
- Long-term legacy effects of N deposition, including altered N cycling and soil chemistry, impede ecosystem recovery.
- Environmental standards for nitrogen deposition must consider these persistent legacy effects for accurate critical load assessments.
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