Articles | Volume 8, issue 2
https://doi.org/10.5194/soil-8-717-2022
https://doi.org/10.5194/soil-8-717-2022
Original research article
 | 
07 Dec 2022
Original research article |  | 07 Dec 2022

Biocrust-linked changes in soil aggregate stability along a climatic gradient in the Chilean Coastal Range

Nicolás Riveras-Muñoz, Steffen Seitz, Kristina Witzgall, Victoria Rodríguez, Peter Kühn, Carsten W. Mueller, Rómulo Oses, Oscar Seguel, Dirk Wagner, and Thomas Scholten

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Cited articles

Abed, R. M. M., Tamm, A., Hassenrück, C., Al-Rawahi, A. N., Rodríguez-Caballero, E., Fiedler, S., Maier, S., and Weber, B.: Habitat-dependent composition of bacterial and fungal communities in biological soil crusts from Oman, Sci. Rep.-UK, 9, 6468, https://doi.org/10.1038/s41598-019-42911-6, 2019. 
Allison, L. E. and Richards, L. A.: Diagnosis and improvement of saline and alkali soils (No. 60), Soil and Water Conservative Research Branch, Agricultural Research Service, US Department of Agriculture, https://www.ars.usda.gov/ARSUserFiles/20360500/hb60_pdf/hb60complete.pdf (last access: 30 November 2022), 1954. 
Armesto, J. J., Arroyo, M. T., and Hinojosa Opazo, L.: The Mediterranean environment of central Chile, in: The Physical Geography of South America, edited by: Veblen, T., Young, K., and Orme, A., Oxford University Press, 184–199, https://doi.org/10.1093/oso/9780195313413.003.0019, 2007. 
Bachar, A., Al-Ashhab, A., Soares, M. I. M., Sklarz, M. Y., Angel, R., Ungar, E. D., and Gillor, O.: Soil Microbial Abundance and Diversity Along a Low Precipitation Gradient, Microb. Ecol., 60, 453–461, https://doi.org/10.1007/s00248-010-9727-1, 2010. 
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Short summary
Biological soil crusts (biocrusts) stabilize the soil surface mainly in arid regions but are also present in Mediterranean and humid climates. We studied this stabilizing effect through wet and dry sieving along a large climatic gradient in Chile and found that the stabilization of soil aggregates persists in all climates, but their role is masked and reserved for a limited number of size fractions under humid conditions by higher vegetation and organic matter contents in the topsoil.
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