Increasing rates of long-term nitrogen deposition consistently increased litter decomposition in a semi-arid grassland

• The continuing nitrogen (N) deposition observed worldwide alters ecosystem nutrient cycling and ecosystem functioning. Litter decomposition is a key process contributing to these changes, but the numerous mechanisms for altered decomposition remain poorly identified. • We assessed these different...

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Published in:The New phytologist Vol. 229; no. 1; pp. 296 - 307
Main Authors: Hou, Shuang-Li, Hättenschwiler, Stephan, Yang, Jun-Jie, Sistla, Seeta, Wei, Hai-Wei, Zhang, Zhi-Wei, Hu, Yan-Yu, Wang, Ru-Zhen, Cui, Shu-Yan, Lü, Xiao-Tao, Han, Xing-Guo
Format: Journal Article
Language:English
Published: England Wiley 01.01.2021
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ISSN:0028-646X, 1469-8137, 1469-8137
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Summary:• The continuing nitrogen (N) deposition observed worldwide alters ecosystem nutrient cycling and ecosystem functioning. Litter decomposition is a key process contributing to these changes, but the numerous mechanisms for altered decomposition remain poorly identified. • We assessed these different mechanisms with a decomposition experiment using litter from four abundant species (Achnatherum sibiricum, Agropyron cristatum, Leymus chinensis and Stipa grandis) and litter mixtures representing treatment-specific community composition in a semi-arid grassland under long-term simulation of six different rates of N deposition. • Decomposition increased consistently with increasing rates of N addition in all litter types. Higher soil manganese (Mn) availability, which apparently was a consequence of N addition-induced lower soil pH, was the most important factor for faster decomposition. Soil C : N ratios were lower with N addition that subsequently led to markedly higher bacterial to fungal ratios, which also stimulated litter decomposition. • Several factors contributed jointly to higher rates of litter decomposition in response to N deposition. Shifts in plant species composition and litter quality played a minor role compared to N-driven reductions in soil pH and C : N, which increased soil Mn availability and altered microbial community structure. The soil-driven effect on decomposition reported here may have long-lasting impacts on nutrient cycling, soil organic matter dynamics and ecosystem functioning.
Bibliography:These authors contributed equally to this work.
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ISSN:0028-646X
1469-8137
1469-8137
DOI:10.1111/nph.16854