Published July 2018 | Version v1
Journal article

Effects of long-term fertilization on phoD-harboring bacterial community in Karst soils

  • 1. Southern Regional Collaborative Innovation Center for Grain and Oil Crops in China, Hunan Agricultural University, Changsha 410128 (China)
  • 2. Key Laboratory of Agro-Ecological Processes in Subtropical Region, Institute of Subtropical Agriculture, The Chinese Academy of Sciences, Changsha 410125 (China)
  • 3. University of Chinese Academy of Sciences, Beijing 100049 (China)
  • 4. Institute of Groundwater Ecology, Helmholtz-Zentrum Muenchen (Germany)

Description

Highlights: • High-level organic inputs significantly changed the phoD community structure in Karst soils. • The positive correlation was found between available P, ALP activity and phoD gene abundance. • The P availability was also associated with soil Ca2+ concentration. Phosphorus (P) acquisition by plants from soil organic P mainly relies on microorganisms. Examining the community of functional microbes that encode phosphatases (e.g. PhoD) under different fertilization managements may provide valuable information for promoting soil organic P availability. Here, we investigated how the abundance and community diversity of phoD-harboring bacteria responded to long-term fertilization in Karst soils. Six fertilization treatments were designed as follows: non-fertilized control (CK), inorganic fertilization only (NPK), and inorganic fertilization combined with low- and high amounts of straw (LSNPK and HSNPK), or cattle manure (LMNPK and HMNPK). We found that soil available phosphorus (AP) content and the activity of alkaline phosphatase (ALP) were significantly higher in all combined inorganic/organic fertilization treatments, while the abundance of the phoD gene was only higher in the HMPNK treatment, compared to NPK. The combination of inorganic/organic fertilizations had no effect on the diversity of phoD genes compared to NPK alone, but the phoD gene richness was greater in these treatments as compared to the control. Only organic fertilization combinations with high amounts of organic matter (both HSNPK and HMNPK) significantly affected the phoD community structure. A structure equation model demonstrated that soil organic carbon (SOC), rather than P, greatly affected the phoD community structure, suggesting that organic P mineralization in soils is decoupled from C mineralization. Our results suggested that optimized combinations of inorganic/organic fertilizations could promote P availability via regulating soil phoD-harboring bacteria community diversity and ALP activity.

Availability note (English)

Available from http://dx.doi.org/10.1016/j.scitotenv.2018.01.314

Additional details

Identifiers

DOI
10.1016/j.scitotenv.2018.01.314;
PII
S0048969718303565;

Publishing Information

Journal Title
Science of the Total Environment
Journal Volume
628
Journal Page Range
p. 53-63
ISSN
0048-9697
CODEN
STENDL

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Copyright
Copyright (c) 2018 Elsevier B.V. All rights reserved.