Microbial group specific uptake kinetics of inorganic phosphate and adenosine-5′-triphosphate (ATP) in the North Pacific Subtropical Gyre

dc.contributor.author Björkman, Karin M.
dc.contributor.author Duhamel, Solange
dc.contributor.author Karl, David M.
dc.date.accessioned 2014-11-13T19:36:50Z
dc.date.available 2014-11-13T19:36:50Z
dc.date.issued 2012-06-11
dc.description © The Author(s), 2012. This article is distributed under the terms of the Creative Commons Attribution License. The definitive version was published in Frontiers in Microbiology 3 (2012): 189, doi:10.3389/fmicb.2012.00189. en_US
dc.description.abstract We investigated the concentration dependent uptake of inorganic phosphate (Pi) and adenosine-5′-triphosphate (ATP) in microbial populations in the North Pacific Subtropical Gyre (NPSG). We used radiotracers to measure substrate uptake into whole water communities, differentiated microbial size classes, and two flow sorted groups; Prochlorococcus (PRO) and non-pigmented bacteria (NPB). The Pi concentrations, uptake rates, and Pi pool turnover times (Tt) were (mean, ±SD); 54.9 ± 35.0 nmol L−1 (n = 22), 4.8 ± 1.9 nmol L−1 day−1 (n = 19), and 14.7 ± 10.2 days (n = 19), respectively. Pi uptake into >2 μm cells was on average 12 ± 7% (n = 15) of the total uptake. The kinetic response to Pi (10–500 nmol L−1) was small, indicating that the microorganisms were close to their maximum uptake velocity (Vmax). Vmax averaged 8.0 ± 3.6 nmol L−1 day−1 (n = 19) in the >0.2 μm group, with half saturation constants (Km) of 40 ± 28 nmol L−1 (n = 19). PRO had three times the cell specific Pi uptake rate of NPB, at ambient concentrations, but when adjusted to cells L−1 the rates were similar, and these two groups were equally competitive for Pi. The Tt of γ-P-ATP in the >0.2 μm group were shorter than for the Pi pool (4.4 ± 1.0 days; n = 6), but this difference diminished in the larger size classes. The kinetic response to ATP was large in the >0.2 μm class with Vmax exceeding the rates at ambient concentrations (mean 62 ± 27 times; n = 6) with a mean Vmax for γ-P-ATP of 2.8 ± 1.0 nmol L−1 day−1, and Km at 11.5 ± 5.4 nmol L−1 (n = 6). The NPB contribution to γ-P-ATP uptake was high (95 ± 3%, n = 4) at ambient concentrations but decreased to ∼50% at the highest ATP amendment. PRO had Km values 5–10 times greater than NPB. The above indicates that PRO and NPB were in close competition in terms of Pi acquisition, whereas P uptake from ATP could be attributed to NPB. This apparent resource partitioning may be a niche separating strategy and an important factor in the successful co-existence within the oligotrophic upper ocean of the NPSG. en_US
dc.description.sponsorship This work was supported by grants from the Gordon and Betty Moore Foundation’s Marine Microbiology Initiative and The National Science Foundation OCE 0326616 and EF 04-24599, awarded to D. M. Karl. en_US
dc.format.mimetype application/pdf
dc.identifier.citation Frontiers in Microbiology 3 (2012): 189 en_US
dc.identifier.doi 10.3389/fmicb.2012.00189
dc.identifier.uri https://hdl.handle.net/1912/6947
dc.language.iso en_US en_US
dc.publisher Frontiers Media en_US
dc.relation.uri https://doi.org/10.3389/fmicb.2012.00189
dc.rights Attribution-NonCommercial 3.0 Unported *
dc.rights.uri http://creativecommons.org/licenses/by-nc/3.0/
dc.title Microbial group specific uptake kinetics of inorganic phosphate and adenosine-5′-triphosphate (ATP) in the North Pacific Subtropical Gyre en_US
dc.type Article en_US
dspace.entity.type Publication
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