Understanding the coupling relationships among lake physicochemical properties, internal nutrient recycling, and related microbes is key for the control of freshwater eutrophication. In this study, seasonal variations in microorganisms at the sediment-water interface (SWI) of the eutrophic Lake Chaohu in China were analyzed, in order to reveal changes in phosphorus (P)-cycling-related microbes in the sediments and its association with internal P release during the cyanobacterial life cycle. The identified P-cycling-related microbes include phosphorus-solubilizing bacteria (PSB) (dominant of Bacillus, Thiobacillus and Acinetobacter), sulfate-reducing bacteria (SRB) (dominant of Sva0081_ sediment_ group, norank_ c__ Thermodesulfovibrionia and Desulfatiglans) and iron-reducing bacteria (FeRB) (dominant of Geothermobacter, Anaeromyxobacter, Thermoanaerobaculum and Clostridium_sensu_stricto_1). Increased PSB and reduced proportions of iron-aluminum-bound P (Fe/Al-P) and calcium-bound P (Ca-P) from the benthic stage to initial cyanobacterial growth indicated that internal phosphorus was released through the solubilization of Fe/Al-P and Ca-P by PSB. Growth of cyanobacteria was accompanied by cyanobacteria death, deposition, and degradation during early algal blooms, which increased SRB caused by high organic matter and the net deposition of phosphorus in the western lake. Conversely, phosphorus release in eastern lake was observed because of organic phosphorus mineralization. High linear discriminant analysis effect size of SRB and FeRB and the decreased Fe/Al-P in sediments indicated sulfide-mediated chemical iron reduction (SCIR) and FeRB-mediated microbial iron reduction mechanisms for internal phosphorus release during late algal blooms. The observed seasonal pattern of P-cycling-related microbes and its mediation on internal phosphorus release provides a foundation for internal P management in Lake Chaohu.
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http://dx.doi.org/10.1016/j.jes.2024.07.028 | DOI Listing |
J Environ Sci (China)
August 2025
Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 211135, China.
Understanding the coupling relationships among lake physicochemical properties, internal nutrient recycling, and related microbes is key for the control of freshwater eutrophication. In this study, seasonal variations in microorganisms at the sediment-water interface (SWI) of the eutrophic Lake Chaohu in China were analyzed, in order to reveal changes in phosphorus (P)-cycling-related microbes in the sediments and its association with internal P release during the cyanobacterial life cycle. The identified P-cycling-related microbes include phosphorus-solubilizing bacteria (PSB) (dominant of Bacillus, Thiobacillus and Acinetobacter), sulfate-reducing bacteria (SRB) (dominant of Sva0081_ sediment_ group, norank_ c__ Thermodesulfovibrionia and Desulfatiglans) and iron-reducing bacteria (FeRB) (dominant of Geothermobacter, Anaeromyxobacter, Thermoanaerobaculum and Clostridium_sensu_stricto_1).
View Article and Find Full Text PDFSci Total Environ
July 2024
Soil Physics and Land Management Group, Wageningen University, P.O. Box 47, 6700 AA Wageningen, the Netherlands.
Fumigants and fungicides are effective at controlling soil-borne pathogens but might also adversely affect soil beneficial microbes, such as soil phosphorus (P) solubilizing microbes, further altering nutrient cycling processes. Therefore, this study investigated the effects of the fumigant chloropicrin (CP) and the fungicide azoxystrobin (AZO) on soil microeukaryotes and P-cycling related soil bacteria through a greenhouse experiment. Soil microeukaryotic communities and bacterial communities containing two phosphomonoesterase encoding genes (phoC and phoD) were analysed using high-throughput sequencing methods.
View Article and Find Full Text PDFSci Total Environ
April 2024
State Key Laboratory of Black Soils Conservation and Utilization, Northeast Institute of Geography and Agroecology, Chinese Academy of Sciences, Harbin 150081, China. Electronic address:
Soil biogeochemical cycles are essential for regulating ecosystem functions and services. However, little knowledge has been revealed on microbe-driven biogeochemical processes and their coupling mechanisms in soil profiles. This study investigated the vertical distribution of soil functional composition and their contribution to carbon (C), nitrogen (N) and phosphorus (P) cycling in the humus horizons (A-horizons) and parent material horizons (C-horizons) in Udic and Ustic Isohumosols using shotgun sequencing.
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