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首页> 外文期刊>Aquatic Microbial Ecology >Temperature, organic matter, and the control of bacterioplankton in the Neuse River and Pamlico Sound estuarine system
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Temperature, organic matter, and the control of bacterioplankton in the Neuse River and Pamlico Sound estuarine system

机译:Neuse河和Pamlico Sound河口系统中的温度,有机质以及浮游细菌的控制

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摘要

A 4 yr, spatially extensive study of the Neuse River and Pamlico Sound estuarine system, North Carolina, was used to evaluate the temporal patterns and bottom-up controls of the resident bacterioplankton community. This meso- to eutrophic estuarine system had high concentrations of dissolved and particulate organic matter and supported an active and abundant phytoplankton community. Temporal analysis of bacterioplankton productivity (BP) revealed a strong seasonal pattern, similar to water temperature. Comparisons of BP and several environmental variables grouped by season and year showed little correspondence between the bacteria and either river discharge or organic matter at either scale. Temperature explained about half of the variation in BP data, but without any obvious threshold in the semi-log temperature productivity relationship, implying the absence of a shift to substrate limitation at higher temperatures. The temperature effect varied in space and was lower at the freshwater station, suggesting differential substrate availability or the presence of a different resident microbial community. Proxies for bacterial substrates, including dissolved organic carbon, particulate organic nitrogen, and chlorophyll a, improved the predictive power in multiple regression models, but at least one-third of the variation in BP remained unexplained. The regression models differed by station group, further highlighting the possible difference in biota and/or resources between the freshwater and brackish sites.
机译:对北卡罗来纳州的Neuse河和Pamlico Sound河口系统进行了为期4年的空间广泛研究,以评估居民浮游细菌群落的时间格局和自下而上的控制。中到富营养化的河口系统具有高浓度的溶解性和颗粒状有机质,并支持活跃而丰富的浮游植物群落。对浮游细菌生产力(BP)的时间分析显示出强烈的季节性模式,类似于水温。 BP与按季节和年份分组的几个环境变量的比较表明,细菌与河流排放或任何规模的有机物之间几乎没有对应关系。温度解释了BP数据中大约一半的变化,但在半对数温度生产率关系中没有任何明显的阈值,这意味着在更高的温度下没有向底物极限的转变。温度效应在空间中变化并且在淡水站处较低,表明底物可利用性不同或存在不同的常驻微生物群落。细菌底物的代理(包括溶解的有机碳,颗粒状的有机氮和叶绿素a)在多个回归模型中提高了预测能力,但至少有三分之一的血压变化尚无法解释。回归模型因站点组的不同而不同,这进一步突出了淡水和咸淡站点之间生物群和/或资源的可能差异。

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