Contrasting Trends in Plant Diversity and Soil Carbon Mineralization Under Precipitation-Driven Vegetation and Soil Carbon Dynamics in the Mongolian Plateau.

Furthermore, SOC mineralization accumulation in all three soil layers (0–5, 5–10, and 10–20 cm) showed an increasing trend with increasing MBC and fungal/bacterial biomass (Figure S4 ).

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The Shannon–Wiener index showed a decreasing trend with increasing MAT, while the Margalef richness index exhibited a significant “ U ‐shaped” relationship with MAT ( p < 0.05), indicating that both increases and decreases in MAT were accompanied by increases in the Margalef richness index.

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