若尔盖退化泥炭地土壤原核微生物群落结构对水位恢复的短期响应

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罗明没¹^,², 陈悦¹^,², 杨刚³, 胡斌¹, 李玮¹^,²^,^*(

), 陈槐⁴^,^*(

)

Short-term response of soil prokaryotic community structure to water level restoration in degraded peatland of the Zoigê Plateau

LUO Ming-Mo¹^,², CHEN Yue¹^,², YANG Gang³, HU Bin¹, LI Wei¹^,²^,^*(

), CHEN Huai⁴^,^*(

)

图4. 水位恢复处理下若尔盖退化泥炭地土壤化学性质与原核微生物优势类群相对丰度间相关性。SOC, 土壤有机碳; TN, 总氮; TP, 总磷; Water level, 水位。**, p < 0.01; *, p < 0.05。

Fig. 4. Correlation between soil chemical properties and relative abundance of prokaryotic microbial dominant groups in Zoigê degraded peatland under water level restoration. SOC, soil organic carbon; TN, total nitrogen; TP, total phosphorus. **, p < 0.01; *, p < 0.05.