Increasing microbial carbon use efficiency with warming predicts soil heterotrophic respiration globally
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http://hdl.handle.net/10045/96187
Título: | Increasing microbial carbon use efficiency with warming predicts soil heterotrophic respiration globally |
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Autor/es: | Ye, Jian‐Sheng | Bradford, Mark A. | Dacal, Marina | Maestre, Fernando T. | García-Palacios, Pablo |
Centro, Departamento o Servicio: | Universidad de Alicante. Instituto Multidisciplinar para el Estudio del Medio "Ramón Margalef" |
Palabras clave: | CO2 efflux | Global warming | Microbe | Soil carbon stock | Soil respiration |
Área/s de conocimiento: | Ecología |
Fecha de publicación: | oct-2019 |
Editor: | John Wiley & Sons |
Cita bibliográfica: | Global Change Biology. 2019, 25(10): 3354-3364. doi:10.1111/gcb.14738 |
Resumen: | The degree to which climate warming will stimulate soil organic carbon (SOC) losses via heterotrophic respiration remains uncertain, in part because different or even opposite microbial physiology and temperature relationships have been proposed in SOC models. We incorporated competing microbial carbon use efficiency (CUE)–mean annual temperature (MAT) and enzyme kinetic–MAT relationships into SOC models, and compared the simulated mass‐specific soil heterotrophic respiration rates with multiple published datasets of measured respiration. The measured data included 110 dryland soils globally distributed and two continental to global‐scale cross‐biome datasets. Model–data comparisons suggested that a positive CUE–MAT relationship best predicts the measured mass‐specific soil heterotrophic respiration rates in soils distributed globally. These results are robust when considering models of increasing complexity and competing mechanisms driving soil heterotrophic respiration–MAT relationships (e.g., carbon substrate availability). Our findings suggest that a warmer climate selects for microbial communities with higher CUE, as opposed to the often hypothesized reductions in CUE by warming based on soil laboratory assays. Our results help to build the impetus for, and confidence in, including microbial mechanisms in soil biogeochemical models used to forecast changes in global soil carbon stocks in response to warming. |
Patrocinador/es: | J.‐S.Y. was funded by the Second Tibetan Plateau Scientific Expedition and Research Program (2019QZKK0305) and the Fundamental Research Funds for the Central Universities (lzujbky‐2019‐kb36). This research was supported by the European Research Council (ERC Grant Agreements 242658 [BIOCOM] and 647038 [BIODESERT]). M. D. is supported by a FPU fellowship from the Spanish Ministry of Education, Culture and Sports (Ref. FPU‐15/00392). P.G.P. acknowledges the Spanish Ministry of Economy and Competitiveness for financial support via the Juan de la Cierva Incorporación Program (IJCI‐2014‐20058). |
URI: | http://hdl.handle.net/10045/96187 |
ISSN: | 1354-1013 (Print) | 1365-2486 (Online) |
DOI: | 10.1111/gcb.14738 |
Idioma: | eng |
Tipo: | info:eu-repo/semantics/article |
Derechos: | © 2019 John Wiley & Sons Ltd |
Revisión científica: | si |
Versión del editor: | https://doi.org/10.1111/gcb.14738 |
Aparece en las colecciones: | INV - DRYLAB - Artículos de Revistas Personal Investigador sin Adscripción a Grupo |
Archivos en este ítem:
Archivo | Descripción | Tamaño | Formato | |
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2019_Ye_etal_GlobalChangeBiol_final.pdf | Versión final (acceso restringido) | 1,37 MB | Adobe PDF | Abrir Solicitar una copia |
2019_Ye_etal_GlobalChangeBiol_accepted.pdf | Accepted Manuscript (acceso abierto) | 641,71 kB | Adobe PDF | Abrir Vista previa |
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