College of Horticulture, South China Agricultural University, Guangdong Province Key Laboratory of Microbial Signals and Disease Control, Guangdong Engineering Research Center for Grass Science, Guangdong Engineering Center for Litchi, Guangzhou, 510642, China.
State Key Laboratory of Applied Microbiology Southern China, Guangdong Provincial Key Laboratory of Microbial Culture Collection and Application, Guangdong Institute of Microbiology, Guangzhou, 510070, China.
Environ Microbiol Rep. 2018 Jun;10(3):310-319. doi: 10.1111/1758-2229.12641. Epub 2018 Apr 16.
Phosphorus (P) cycling is a fundamental process driven by microorganisms, and plants can regulate P cycling directly or via their influence on the soil microbial community. However, the differential P cycling patterns associated with legumes and grass are largely unknown. Therefore, we investigated the microbial community involved in P cycling in subtropical soil grown with stylo (Stylosanthes guianensis, legume) or bahiagrass (Paspalum notatum, grass) using metagenomic sequencing. P fractionation indicated that sparingly soluble inorganic P (Pi) accounted for approximately 75% of P pool. Bacteria involved in sparingly soluble Pi solubilization (pqq, gad, JEN) were more abundant in bahiagrass soil, with Candidatus Pelagibacter, Trichodesmium, Neorickettsia, Nitrobacter, Paraburkholderia, Candidatus Solibacter, Burkholderia as major contributors. In contrast, bacteria involved in organic P (Po) mineralization (php, glpQ, phn) were more abundant in stylo soil, consistent with phosphatase activity and Frankia, Kyrpidia, Thermobispora, Streptomyces, Rhodococcus were major contributors. Bacteria taking up low molecular-weight Po were more abundant in stylo soil than in bahiagrass soil, while those taking up Pi were less abundant. These data suggest that bacterial communities associated with legumes and grass develop contrasting P acquisition strategies, highlighting the possibility of intercropping with legumes and grass for better P cycling.
磷(P)循环是由微生物驱动的基本过程,植物可以直接或通过其对土壤微生物群落的影响来调节 P 循环。然而,豆科植物和禾本科植物之间与 P 循环相关的差异模式在很大程度上尚不清楚。因此,我们使用宏基因组测序研究了亚热带土壤中与柱花草(Stylosanthes guianensis,豆科植物)或百喜草(Paspalum notatum,禾本科植物)生长相关的参与 P 循环的微生物群落。P 分组表明,难溶性无机磷(Pi)约占 P 库的 75%。参与难溶性 Pi 溶解的细菌(pqq、gad、JEN)在百喜草土壤中更为丰富,而 Pelagibacter、Trichodesmium、Neorickettsia、Nitrobacter、Paraburkholderia、Candidatus Solibacter 和 Burkholderia 是主要贡献者。相比之下,参与有机磷(Po)矿化的细菌(php、glpQ、phn)在柱花草土壤中更为丰富,与磷酸酶活性和 Frankia、Kyrpidia、Thermobispora、Streptomyces 和 Rhodococcus 等为主要贡献者相一致。低分子量 Po 的摄取细菌在柱花草土壤中比在百喜草土壤中更为丰富,而摄取 Pi 的细菌则较少。这些数据表明,与豆科植物和禾本科植物相关的细菌群落发展出了不同的 P 获取策略,突出了与豆科植物和禾本科植物间作以改善 P 循环的可能性。