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Abstracts available here - Society for Conservation Biology

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25th International Congress <strong>for</strong> <strong>Conservation</strong> <strong>Biology</strong> • Auckland, New Zealand • 5-9 December 2011<br />

from 0.86 to 1.02% and from 0.75 to 2.43%, respectively. Microbial<br />

CO2 evolution values <strong>for</strong> crusts B-E fluctuated between 0.79 and 1.32 μg<br />

CO2-C g-1 dry soil h-1, which was two-fold lower in comparison to crust A.<br />

However, t<strong>here</strong> were no significant differences in microbial biomass between<br />

different crust types. The values of community-level physiological profiles<br />

were found to increase from 108.6 <strong>for</strong> crust A to 196.7 μg CO2-C g-1<br />

dry soil h-1<strong>for</strong> crust E, and the values <strong>for</strong> crusts C and E were significantly<br />

(P

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