Articles | Volume 16, issue 6
https://doi.org/10.5194/bg-16-1133-2019
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, Hanan Ginat, Osnat Gillor, and Roey Angel

Viewed

Total article views: 3,629 (including HTML, PDF, and XML)
HTML PDF XML Total Supplement BibTeX EndNote
2,504 1,047 78 3,629 202 58 85
  • HTML: 2,504
  • PDF: 1,047
  • XML: 78
  • Total: 3,629
  • Supplement: 202
  • BibTeX: 58
  • EndNote: 85
Views and downloads (calculated since 06 Nov 2018)
Cumulative views and downloads (calculated since 06 Nov 2018)

Viewed (geographical distribution)

Total article views: 3,629 (including HTML, PDF, and XML) Thereof 3,354 with geography defined and 275 with unknown origin.
Country # Views %
  • 1
1
 
 
 
 

Cited

Latest update: 14 Dec 2024
Download
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.
Altmetrics
Final-revised paper
Preprint