tag: biocrust

Biological soil crusts: spatio-temporal development and ecological functions of soil surface microbial communities across different scales

Editorial for a special issue on Biocrusts in Frontiers in Microbiology can be found here. The special issue consists of 25 articles which can be downloaded as an e-book here. The remit for submissions is reproduced below: Biological soil crusts (biocrusts) are widely distributed throughout the world, and cover approximately …

Spatial organisation of fungi in soil biocrusts of the Kalahari is related to bacterial community structure and may indicate ecological functions of fungi in drylands

Biological soil crusts, or biocrusts, are microbial communities found in soil surfaces in drylands and in other locations where vascular plant cover is incomplete. They are functionally significant for numerous ecosystem services, most notably in the C fixation and storage due to the ubiquity of photosynthetic microbes. Whereas carbon fixation …

Soil biocrusts affect metabolic response to hydration on dunes in west Queensland, Australia

Soil biocrusts, formed from communities of microbes and their extracellular products are a common feature of dryland soil surfaces. Biocrust organisms are only intermittently metabolically active, but due to their ubiquity they make a significant contribution to the carbon cycle. Quantification of the controls and insights into the interlinked process of photosynthesis and respiration are …

Do some microbes exploit biocrusts?

Biocrusts are recognised for numerous beneficial functions in dryland environments including the promotion of surface stability, moisture retention, and sequestration of carbon and nitrogen from the air which enriches the soil. In microbial biocrusts these benefits are delivered as a consequence of the microbial community adaptations for survival. The biocrust …

Wetlands in Drylands: Hidden Hotspots of Carbon Sequestration and Storage?

Although the term ‘wetlands in drylands’ sounds like a contradiction, many drylands host a range of ephemeral wetlands. Pans, for example, are widespread features in many drylands, representing topographic depressions of varying size and shape that host ephemeral, sometimes saline, bodies of shallow water following infrequent precipitation or river flooding …

Microbial transport and soil integrity in drylands

Dryland soils are particularly vulnerable to erosion because of low plant cover and low organic matter which is linked with water availability and biological constraints. It is increasingly recognised that dryland soils can be managed to minimise erosion, which has benefits such as increasing soil fertility, carbon storage, and prevention …

Pastoralism and soil quality in the Kalahari

Land use change in the rangelands of Botswana is affecting soil properties. Pastoralism is the only viable livelihood for many rural poor in Botswana, and privatization of communal land is reducing the area of grazing available to those without land tenure. This has elevated stocking densities in communal areas, increasing …