Effects of Climate and Atmospheric Nitrogen Deposition on Early to Mid-Term Stage Litter Decomposition Across Biomes

Litter decomposition is a key process for carbon and nutrient cycling in terrestrial ecosystems and is mainly controlled by environmental conditions, substrate quantity and quality as well as microbial community abundance and composition. In particular, the effects of climate and atmospheric nitroge...

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Detalles Bibliográficos
Autores: Kwon, TaeOh, Shibata, Hideaki, Kepfer-Rojas, Sebastian, Schmidt, Inger K., Larsen, Klaus S, Beier, Claus, Berg, Björn, Verheyen, Kris, Lamarque, Jean-Francois, Hagedorn, Frank, Eisenhauer, Nico, Djukic, Ika, Peri, Pablo Luis
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2021
País:Argentina
Institución:Instituto Nacional de Tecnología Agropecuaria
Repositorio:INTA Digital (INTA)
Idioma:inglés
OAI Identifier:oai:localhost:20.500.12123/9826
Acceso en línea:http://hdl.handle.net/20.500.12123/9826
https://www.frontiersin.org/articles/10.3389/ffgc.2021.678480/full
https://doi.org/10.3389/ffgc.2021.678480
Access Level:acceso abierto
Palabra clave:Degradation
Carbon
Nitrogen
Nutrients
Climate Change
Microbial Flora
Soil
Temperature
Precipitation
Degradación
Carbono
Nitrógeno
Nutrientes
Cambio Climático
Flora Microbiana
Suelo
Temperatura
Precipitación Atmosférica
Terrestrial Ecosystems
Liter Descomposition
Nutrient Cycling
Global Scale
Biomes
Tea Bag
Green Tea
Rooibos Tea
Ecosistemas Terrestres
Descomposición de Hojas
Ciclo de Nutrientes
Escala Global
Biomas
Bolsa de Té
Té Verde
Té Rooibos
Descripción
Sumario:Litter decomposition is a key process for carbon and nutrient cycling in terrestrial ecosystems and is mainly controlled by environmental conditions, substrate quantity and quality as well as microbial community abundance and composition. In particular, the effects of climate and atmospheric nitrogen (N) deposition on litter decomposition and its temporal dynamics are of significant importance, since their effects might change over the course of the decomposition process. Within the TeaComposition initiative, we incubated Green and Rooibos teas at 524 sites across nine biomes. We assessed how macroclimate and atmospheric inorganic N deposition under current and predicted scenarios (RCP 2.6, RCP 8.5) might affect litter mass loss measured after 3 and 12 months. Our study shows that the early to mid-term mass loss at the global scale was affected predominantly by litter quality (explaining 73% and 62% of the total variance after 3 and 12 months, respectively) followed by climate and N deposition. The effects of climate were not litter-specific and became increasingly significant as decomposition progressed, with MAP explaining 2% and MAT 4% of the variation after 12 months of incubation. The effect of N deposition was litter-specific, and significant only for 12-month decomposition of Rooibos tea at the global scale. However, in the temperate biome where atmospheric N deposition rates are relatively high, the 12-month mass loss of Green and Rooibos teas decreased significantly with increasing N deposition, explaining 9.5% and 1.1% of the variance, respectively. The expected changes in macroclimate and N deposition at the global scale by the end of this century are estimated to increase the 12-month mass loss of easily decomposable litter by 1.1– 3.5% and of the more stable substrates by 3.8–10.6%, relative to current mass loss. In contrast, expected changes in atmospheric N deposition will decrease the mid-term mass loss of high-quality litter by 1.4–2.2% and that of low-quality litter by 0.9–1.5% in the temperate biome. Our results suggest that projected increases in N deposition may have the capacity to dampen the climate-driven increases in litter decomposition depending on the biome and decomposition stage of substrate.