Soil carbon and nitrogen cycling at the atmosphere-soil interface: Quantifying the responses of biocrust-soil interactions to global change
Abstract
In drylands, where water scarcity limits vascular plant growth, much of the primary production occurs at the soil surface. This is where complex macro- and microbial communities, in an intricate bond with soil particles, form biological soil crusts (biocrusts). Despite their critical role in regulating C and N cycling in dryland ecosystems, there is limited understanding of the fate of biologically fixed C and N from biocrusts into the mineral soil, or how climate change will affect C and N fluxes between the atmosphere, biocrusts, and subsurface soils. To address these gaps, we subjected biocrustsoil systems to experimental warming and drought under controlled laboratory conditions, monitored CO
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| Título según WOS: | Soil carbon and nitrogen cycling at the atmosphere-soil interface: Quantifying the responses of biocrust-soil interactions to global change |
| Título según SCOPUS: | Soil carbon and nitrogen cycling at the atmospheresoil interface: Quantifying the responses of biocrustsoil interactions to global change |
| Título de la Revista: | Global Change Biology |
| Volumen: | 30 |
| Número: | 10 |
| Editorial: | John Wiley and Sons Inc. |
| Fecha de publicación: | 2024 |
| Idioma: | English |
| DOI: |
10.1111/gcb.17519 |
| Notas: | ISI, SCOPUS |