Nitrogen Cycling Capability Between Biocrusts and Soil Biocrusts’ δ 15 N ranged from 1.72 to 7.6 and followed a decreasing trend in the following order: bare soil > Cyanobacterial crust > Crustose lichen > Foliose lichen ( Figure 5 ).
← all excerpts
The Bacterial Microbiome Associated With Arid Biocrusts and the Biogeochemical Influence of Biocrusts Upon the Underlying Soil.
1
—
—