Phod-harboring bacterial communities mediated slow and fast phosphorus transformation in alkaline soil of a Robinia pseudoacacia afforestation chronosequence

Background and aims Soil phosphorus (P) availability is a key factor determining primary productivity in forest ecosystems in arid and semiarid regions. Under P deficient conditions, phoD -harboring microorganisms secrete alkaline phosphatase, improving P bioavailability. However, their roles in agi...

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Published inPlant and soil Vol. 488; no. 1-2; pp. 517 - 532
Main Authors Wang, Ying, Yang, Lin, Zhang, Jiawen, Li, Yan, Kang, Haibin, Bai, Xiaoxiong, Cui, Yongxing, Zhang, Min, Dong, Liguo, Yu, Xuan
Format Journal Article
LanguageEnglish
Published Cham Springer International Publishing 01.07.2023
Springer
Springer Nature B.V
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Summary:Background and aims Soil phosphorus (P) availability is a key factor determining primary productivity in forest ecosystems in arid and semiarid regions. Under P deficient conditions, phoD -harboring microorganisms secrete alkaline phosphatase, improving P bioavailability. However, their roles in aging plantations of leguminous trees is still unclear. Methods Soil samples were collected from 8-, 18-, and 30-year-old stands of a Robinia pseudoacacia afforestation of degraded agricultural land. Soil P fractions, alkaline phosphatase activity, phoD gene abundance, and bacterial community structure were determined. An experiment with P addition in pots with tree seedlings was set up to check for short-term P transformation processes. Results Soil inorganic P (Pi) and organic P (Po) in R. pseudoacacia afforestation stands mainly existed as stable Pi (NaOH-Pi) and moderately easily available Po (HCl-Po). The contents of all these soil P fractions except for HCl-Pi decreased with stand age, while alkaline phosphatase activity increased. Structural equation modelling (SEM) revealed that soil organic carbon (SOC), available phosphorus (AP) and labile-Po contents mediated the community composition, α diversity or abundance of phoD genes, thereby affecting alkaline phosphatase activity. SOC showed the strongest positive effect on alkaline phosphatase activity. The P addition experiment suggests that alkaline phosphatase activity was mainly regulated via soil C:P stoichiometry. Conclusion SOC appears to be an important regulator of Po turnover in P deficient soils via phoD gene-harboring microbes.
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ISSN:0032-079X
1573-5036
DOI:10.1007/s11104-023-05990-z