Articles | Volume 16, issue 6
Biogeosciences, 16, 1133–1145, 2019
https://doi.org/10.5194/bg-16-1133-2019
Biogeosciences, 16, 1133–1145, 2019
https://doi.org/10.5194/bg-16-1133-2019

Research article 19 Mar 2019

Research article | 19 Mar 2019

The origin and role of biological rock crusts in rocky desert weathering

Nimrod Wieler et al.

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ED: Publish subject to minor revisions (review by editor) (15 Feb 2019) by Denise Akob
AR by Anna Wenzel on behalf of the Authors (20 Feb 2019)  Author's response    Manuscript
ED: Publish as is (27 Feb 2019) by Denise Akob
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Short summary
In stony deserts, when rocks are exposed to atmospheric conditions, they undergo weathering. The cavernous (honeycomb) weathering pattern is one of the most common, but it is still unclear exactly how it is formed. We show that microorganisms, which differ from the surrounding soil and dust, form biological crusts on exposed rock surfaces. These microbes secrete polymeric substances that mitigate weathering by reducing evaporation rates and, consequently, salt transport rates through the rock.
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