2005
DOI: 10.1016/s0380-1330(05)70309-9
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Relationship Between Labile Dissolved Organic Carbon (LDOC), Bacterioplankton Cell Phosphorus Quota, and Bacterial Phosphate Uptake Rate in Lakes

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Cited by 4 publications
(3 citation statements)
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“…Examining the phylogenetic distribution of nifH reads revealed that both heterocystous Cyanobacteria and heterotrophic Proteobacteria exhibited the genetic potential to fix nitrogen. Since Sandusky Bay is a eutrophic system with abundant organic carbon, relationships between heterotrophic bacteria capable of fixing nitrogen (free-living and epiphytic) and nondiazotrophic cyanobacteria cannot be overlooked , which may lead to more effective “phycosphere” N and P recycling. These relationships have never been explored for Planktothrix spp.…”
Section: Discussionmentioning
confidence: 99%
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“…Examining the phylogenetic distribution of nifH reads revealed that both heterocystous Cyanobacteria and heterotrophic Proteobacteria exhibited the genetic potential to fix nitrogen. Since Sandusky Bay is a eutrophic system with abundant organic carbon, relationships between heterotrophic bacteria capable of fixing nitrogen (free-living and epiphytic) and nondiazotrophic cyanobacteria cannot be overlooked , which may lead to more effective “phycosphere” N and P recycling. These relationships have never been explored for Planktothrix spp.…”
Section: Discussionmentioning
confidence: 99%
“…The results of this study combined with the aforementioned studies, and other laboratory, , microcosm, , mesocosm and whole lake , studies strengthen the argument that in certain systems, N management is equally as important as P management for the reduction of bloom biomass and toxicity. Furthermore, Sandusky Bay must have strong N-sinks such as assimilatory N-reduction and dissimilatory sediment N-reduction given the high organic carbon inputs, but to our knowledge no study has investigated these processes in Sandusky Bay and management efforts would certainly need to consider these processes.…”
Section: Discussionmentioning
confidence: 99%
“…Significantly positive linear relationships between free-living bacterial abundance and protein-like C1 fluorescence were also found in the algal-derived filtrate group ( R 2 = 0.78, p < 0.001) and algal residual exudative organic matter group ( R 2 = 0.59, p < 0.01) throughout the entire experimental period. This indicated that labile algal-derived filtrate or algal residual exudative organic matter derived from algal degradation became an important factor in controlling bacterial abundance, which would play an important role in microbial food webs and carbon cycling during the decay of algal blooms through the bacterial enzymolysis mechanism [ 69 ]. At the final stable phase of the two groups (algal-derived filtrate group, day 20–80; algal residual exudative organic matter group, day 31–80), the humic-like C2 component accumulated with the decrease in free-living bacterial abundance, and free-living bacterial abundance showed a significant negative linear relationship with humic-like C2 fluorescence (algal-derived filtrate group, R 2 = 0.63, p < 0.05; algal residual exudative organic matter group, R 2 = 0.96, p < 0.01).…”
Section: Resultsmentioning
confidence: 99%