首页> 美国卫生研究院文献>Frontiers in Microbiology >Microbial Group Specific Uptake Kinetics of Inorganic Phosphate and Adenosine-5′-Triphosphate (ATP) in the North Pacific Subtropical Gyre
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Microbial Group Specific Uptake Kinetics of Inorganic Phosphate and Adenosine-5′-Triphosphate (ATP) in the North Pacific Subtropical Gyre

机译:北太平洋亚热带环流中无机磷酸盐和5-三磷酸腺苷(ATP)的微生物群特异性吸收动力学

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摘要

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.
机译:我们调查了北太平洋亚热带环流(NPSG)中微生物种群中无机磷酸盐(Pi)和5'-三磷酸腺苷(ATP)的浓度依赖性吸收。我们使用放射性示踪剂来测量整个水群落,不同微生物大小类别和两个流量分类组的底物吸收。原球菌(PRO)和无色素细菌(NPB)。 Pi的浓度,摄取率和Pi库转换时间(Tt)为(平均值,±SD); 54.9±35.0 nmol L −1 (n = 22),4.8±1.9 nmol L -1 day −1 (n = 19),和14.7±10.2天(n = 19)。 Pi对>2μm细胞的摄取平均占总摄取的12%±7%(n = 15)。对Pi(10–500 nmol L -1 )的动力学响应很小,表明微生物接近其最大吸收速度(Vmax)。 >0.2μm组中的Vmax平均为8.0±3.6 nmol L −1 day -1 (n = 19),半饱和常数(Km)为40±28 nmol L -1 (n = 19)。在环境浓度下,PRO具有NPB的细胞特异性Pi吸收速率的三倍,但当调整为L -1 细胞时,速率相似,并且这两组对Pi的竞争性相同。 >0.2μm组的γ-P-ATP的Tt短于Pi库(4.4±1.0 d天; n = 6),但是在较大尺寸的类中这种差异减小了。 ATP的动力学响应在>0.2μm级中很大,Vmax超过环境浓度下的速率(平均62±27倍; n = 6),γ-P-ATP的平均Vmax为2.8±1.0 nmol L -1 day -1 ,Km为11.5±±5.4 nmol L -1 (n = 6)。在环境浓度下,NPB对γ-P-ATP吸收的贡献较高(95%±3%, n = 4),而在最高的ATP修正下降低至约50%。 PRO的 K m值是NPB的5-10倍。以上表明PRO和NPB在Pi获取方面竞争激烈,而来自ATP的P吸收可归因于NPB。这种明显的资源划分可能是利基分离策略,也是NPSG贫营养上层海洋成功共存的重要因素。

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