Phosphorus (P) availability is a critical factor limiting the restoration of degraded ecosystems in nutrient-poor karst regions. Enclosure has been considered an effective strategy to restore degraded grasslands. However, the mechanisms through which grazing enclosure affects soil P fractions and microbial nutrient limitations in these fragile regions remain unclear. We investigated soil P fractions (resin-P, NaHCO3–P, NaOH–P, HCl–P, and residual-P) and microbial nutrient limitations along a subalpine grassland restoration chronosequence (3, 9, 15, 23 years enclosure) in the karst area of southwest China. The nutrient limitations of microbes were quantified by enzymatic vector analysis. The results showed that vector length initially increased, then declined, while the angle decreased with the restoration stage, indicating a microbial community shift from P to nitrogen (N) limitation. Residual-P was the dominant fraction, followed by HCl-P, highlighting stable P pool prevalence. Despite this, over the restoration chronosequence, resin-P content increased, and residual-P decreased progressively, indicating enhanced P bioavailability. Random forest model and structural equation model identified soil pH, extracellular enzymes related to carbon (C) and P cycle, and the relative abundance of microbial core taxa (i.e., Actinobacteriota, Glomeromycota) as primary drivers of P availability and microbial nutrient limitations. Overall, our results highlight that long-term enclosure is an effective management strategy for improving P availability and alleviating microbial P limitation in karst grasslands, and also emphasize the importance of specific microbial taxa (high relative abundance and high connectivity within the co-occurrence network) for soil nutrient cycling during grassland restoration.
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