Hypolithic Communities: Important Nitrogen Sources in Antarctic Desert
Environmental Microbiology Reports (2011) 3(5), 581–586 doi:10.1111/j.1758-2229.2011.00266.x Hypolithic communities: important nitrogen sources in Antarctic desert soilsemi4_266 581..586 D. A. Cowan,1* J. A. Sohm,2 T. P. Makhalanyane,1 light while providing protection from the deleterious D. G. Capone,2 T. G. A. Green,3 S. C. Cary3,4 and effects of extreme desiccation, physical disturbance and I. M. Tuffin1 high UVa/b fluxes (Cockell and Stokes, 2004). 1Institute for Microbial Biotechnology and Hypolithic communities are typically dominated by pho- Metagenomics, University of the Western Cape, Cape toautotrophs including cyanobacteria and green algae Town, South Africa. (Cockell and Stokes, 2004; Wood et al., 2008), but moss- 2Wrigley Institute for Environmental Studies, University dominated hypolithons have recently been identified in of Southern California, Los Angeles, CA, USA. Antarctic desert soils (Cowan et al., 2010). These com- 3Department of Biological Sciences, University of munities are now thought to make an important contribu- Waikato, Hamilton, New Zealand. tion to the carbon input budget in depauperate habitats 4College of Earth and Ocean Science, University of such as polar deserts (Burkins et al., 2001). Delaware, Lewes, DE 19958, USA. However, little is known of the nitrogen budgets in Ant- arctic desert soils. Organic nitrogen inputs may be derived from legacy biomass or from lake-derived cyanobacterial Summary biomass distributed within the Dry Valleys by aeolian Hypolithic microbial communities (i.e. cryptic micro- action (Moorhead et al., 1999). Here we demonstrate, for bial assemblages found on the undersides of translu- the first time, that hypolithic communities both possess cent rocks) are major contributors of carbon input the genetic capacity for N2 fixation and exhibit significant into the oligotrophic hyper-arid desert mineral soils of nitrogenase activity, making them an important, and hith- the Eastern Antarctic Dry Valleys.
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