Temperature Drives the Continental-Scale Distribution of Key Microbes in Topsoil Communities

Author:

Garcia-Pichel Ferran1,Loza Virginia12,Marusenko Yevgeniy1,Mateo Pilar12,Potrafka Ruth M.1

Affiliation:

1. School of Life Sciences, Arizona State University, Tempe, AZ 85287, USA.

2. Departamento de Biología, Facultad de Ciencias, Universidad Autónoma de Madrid, Madrid, Spain.

Abstract

Desert Soil Shuffle Soil microorganisms make up a substantial fraction of global biomass, turning over carbon and other key nutrients on a massive scale. Although the soil protects them somewhat from daily temperature fluxes, the distribution of these communities will likely respond to gradual climate change. Garcia-Pichel et al. (p. 1574 , see the cover; see the Perspective by Belnap ) surveyed bacterial diversity across a range of North American desert soils, or biocrusts—ecosystems in which photosynthetic bacteria determine soil fertility and control physical soil properties such as erodability and water retention. Most of the sites were dominated by one of two cyanobacterial species, but their relative proportions were controlled largely by factors related to temperature. Laboratory enrichment cultures of the two species at different temperatures also showed temperature as a primary determining factor of bacterial diversity. It is unknown if temperature will affect the distribution of other soil microorganisms, but the marked shifts of these two keystone bacterial species suggest further change is in store for these delicate ecosystems.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference42 articles.

1. J. Belnap O. L. Lange Eds. Biological Soil Crusts: Structure Function and Management (Springer-Verlag Berlin 2001) vol. 150.

2. F. Garcia-Pichel in Encyclopedia of Environmental Microbiology G. Bitton Ed. (Wiley New York 2002) pp. 1019–1023.

3. Vulnerability of desert biological soil crusts to wind erosion: the influences of crust development, soil texture, and disturbance

4. Nitrogen cycling in desert biological soil crusts across biogeographic regions in the Southwestern United States

5. Export of nitrogenous compounds due to incomplete cycling within biological soil crusts of arid lands

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