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Soil carbon and nitrogen cycling at the atmosphere–soil interface: Quantifying the responses of biocrust–soil interactions to global change
1 INTRODUCTION In drylands, which constitute almost half of the Earth's terrestrial surface, water scarcity constrains the growth of vascular plants. Instead, primary production occurs directly at the soil surface by biological soil crusts (biocrusts) which establish at the top few millimeters of soil.
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