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Microscale investigations of microbial communities in coastal surficial sediments

机译:沿海表层沉积物中微生物群落的微观调查

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The upper millimeters of sediments are considered major locations of microbial colonization and activity. The goal of our study was to investigate variations of microbial communities in the uppermost sediment layers of the coastal Baltic Sea with emphasis on the complex interplay between microbiology and physico-chemical sediment properties. We selected a high-resolution methodological approach that combined the cryolanding sampling technique (spatial resolution of 250 μm) with microsensor-, spectrophotometric and microscopic analyses. While the oxygen penetration depths in dark conditions ranged from 1.4 mm to 2.6 mm during the study period, this zone expanded by about 1 mm in light and could be divided into three micro-horizons: (ⅰ) an upper zone with a high net O_2 production, (ⅱ) an intermediate zone with increased O_2 consumption on account of light-stimulated respiration and (ⅲ) a lower zone with lower O_2 consumption. Time-series experiments revealed a rapid response of the benthic microbial community to altered light intensities. In May and July, the net O_2 budget in the porewater of sediments was positive within 35 and 22 min after illumination, respectively, whereas in June O_2 production exceeded O_2 consumption after 112 min. The thickness of the O_2 production and O_2 consumption micro-zones decreased from May to July coinciding with an increase in temperature. In May, sites of enhanced O_2 consumption were closely associated with subsurface maxima of microbial numbers and enzymatic activities indicating a tight coupling between photoautotrophic and heterotrophic processes between 1- and 2-mm depth. In June and July, the microbial abundance and enzymatic activity hardly varied with depth. Spatial and temporal microheterogeneity of microbial distribution and activity in O_2 gradients was seen as a reflection of the complex interplay between microbiology and physico-chemical sediment properties.
机译:沉积物的上毫米被认为是微生物定殖和活动的主要位置。我们研究的目的是调查波罗的海沿岸最上层沉积层中微生物群落的变化,重点是微生物学与理化沉积物特性之间的复杂相互作用。我们选择了一种高分辨率的方法学方法,将冰冻着陆采样技术(空间分辨率为250μm)与微传感器,分光光度法和显微镜分析相结合。在研究期间,尽管在黑暗条件下氧气的渗透深度范围为1.4毫米至2.6毫米,但该区域在光照下扩展了约1毫米,并且可以分为三个微地平线:(ⅰ)具有较高净O_2的上部区域生产中,(ⅱ)由于光刺激呼吸而增加了O_2消耗的中间区域,以及(ⅲ)了较低O_2消耗的较低区域。时间序列实验显示底栖微生物群落对改变的光强度具有快速反应。 5月和7月,沉积物孔隙水中O_2的净预算分别在光照后35分钟和22分钟内为正,而6月O_2的产量在112分钟后超过了O_2的消耗。从5月到7月,O_2产生量和O_2消耗量微区的厚度减小,这与温度升高相吻合。 5月,O_2消耗增加的部位与地下最大微生物数量和酶活性密切相关,表明光自养和异养过程之间的紧密耦合在1和2毫米深度之间。在六月和七月,微生物的丰度和酶活性几乎没有变化。 O_2梯度中微生物分布和活动的时空微异质性被认为反映了微生物学与理化沉积物特性之间复杂的相互作用。

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