Different grazing intensities affect soil nitrogen cycling by altering microbial nitrogen metabolism in alpine wetlands.

Among non-dominant phyla, only a few groups (bacterial Nitrospirota, unclassified archaea, Thermoproteota, and fungal Olpidiomycota) showed significant or highly significant responses to grazing intensity; most other taxa exhibited no significant changes.

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Pseudomonas exhibited significantly negative correlations with soil moisture content (SMC), organic matter (OM), and TN (r = −0.778 to −0.887, p < 0.01) and showed a positive trend with pH, indicating strong adaptability to high-pH and low-nutrient habitats.

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