Aerobic heterotrophic microorganisms (AH) play a significant role in carbon cycling in cyanobacterial mats; however, little is known about their abundance, diversity and interaction with cyanobacteria. Using catalyzed reporter deposition fluorescence in situ hybridization (CARD-FISH), bacterial counts in the mat's oxic layer reached a mean of 2.23 ± 0.4 × 1010 cells g-1. Cultivation of AH yielded strains belonging to Actinobacteria, Bacteroidetes, Firmicutes, Gammaproteobacteria and Haloarchaea. 16S rRNA bacterial sequences retrieved from the mat's oxic layer were related to Bacteroidetes, Chloroflexi and Proteobacteria, whereas archaeal sequences belonged to Crenarchaeota and Haloarchaea. Monocultures of cyanobacteria from the same mat were associated with different AH, although Bacteroidetes were found in most cultures. CARD-FISH showed that Bacteroidetes- and Chloroflexi-related bacteria were closely associated with filaments of Microcoleus chthonoplastes. The growth of an axenic culture of M. chthonoplastes PCC7420 was stimulated on the addition of a filtrate obtained from a non-axenic Microcoleus culture and containing only AH and released substances. In contrast, a similar filtrate from a non-axenic Cyanothece-related culture killed Cyanothece PCC 7418. We conclude that a diverse community of AH exist in close association with cyanobacteria in microbial mats and the interactions between AH and cyanobacteria are species-specific and involve the release of substances.
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Mar Pollut Bull
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CSIR-National Institute of Oceanography, Dona Paula, Goa 403004, India.
Coastal deoxygenation impacts phytoplankton communities crucial for marine productivity. The inter- and intra-annual variability in phytoplankton communities at a shallow (27 m) station over the Western Indian Shelf (CaTS site, off Goa) during deoxygenation events of the late southwest monsoon (LSWM September-October) were studied from 2020 to 2023. The water column (0-27 m depth) experienced seasonal hypoxia/anoxia at subsurface depths (0-1.
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January 2025
Key Laboratory of Lake and Watershed Science for Water Security, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; State Key Laboratory of Lake Science and Environment, Nanjing Institute of Geography and Limnology, Chinese Academy of Sciences, Nanjing 210008, China; The Fuxianhu Station of Deep Lake Research, Chinese Academy of Sciences, Chengjiang 652500, China. Electronic address:
Although considerable attention has been paid to the effects of eutrophication on aquatic methane (CH) emissions to the atmosphere, the ecosystem-level effects of oligotrophication/re-oligotrophication on aquatic CH production and subsequent ecological responses remain to be elucidated. It has been hypothesized that dissolved inorganic phosphorus (DIP)-deficient conditions drive the ecosystem to utilize poorly bioavailable organic phosphorus for biomass formation, thereby generating CH as a by-product. To test this hypothesis, a mass balance approach was used to estimate in situ oxic methane production (OMP) in an oligotrophic, deep Lake Fuxian.
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December 2024
State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China; University of Chinese Academy of Sciences, Beijing 100049, China; Guizhou Province Field Scientific Observation and Research Station of Hongfeng Lake Reservoir Ecosystem, Guiyang 551499, China. Electronic address:
Eutrophication has become one of the greatest threats to aquatic ecosystems. The release of phosphorus (P) from sediments exerts a critical role on eutrophication level. Both manganese (Mn) and iron (Fe), sensitive to redox conditions, own strong affinity for P.
View Article and Find Full Text PDFEnviron Sci Technol
August 2024
Centre for Microbiology and Environmental Systems Science, Department for Environmental Geosciences, University of Vienna, Josef-Holaubek-Platz 2, 1090 Vienna, Austria.
ISME J
January 2024
Department of Geosciences, Princeton University, Princeton, NJ 08544, United States.
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