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Sea Ice Microbial Communities: Distribution, Abundance, and Diversity of Ice Bacteria in McMurdo Sound, Antarctica, in 1980

机译:海冰微生物群落:1980年南极麦克默多湾的冰细菌分布,数量和多样性

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An abundant and diverse bacterial community was found within brine channels of annual sea ice and at the ice-seawater interface in McMurdo Sound, Antarctica, in 1980. The mean bacterial standing crop was 1.4 × 1011 cells m?2 (9.8 mg of C m?2); bacterial concentrations as high as 1.02 × 1012 cells m?3 were observed in ice core melt water. Vertical profiles of ice cores 1.3 to 2.5 m long showed that 47% of the bacterial numbers and 93% of the bacterial biomass were located in the bottom 20 cm of sea ice. Ice bacterial biomass concentration was more than 10 times higher than bacterioplankton from the water column. Scanning electron micrographs showed a variety of morphologically distinct cell types, including coccoid, rod, fusiform, filamentous, and prosthecate forms; dividing cells were commonly observed. Approximately 70% of the ice bacteria were free-living, whereas 30% were attached to either living algal cells or detritus. Interactions between ice bacteria and microalgae were suggested by a positive correlation between bacterial numbers and chlorophyll a content of the ice. Scanning and transmission electron microscopy revealed a close physical association between epibacteria and a dominant ice alga of the genus Amphiprora. We propose that sea ice microbial communities are not only sources of primary production but also sources of secondary microbial production in polar ecosystems. Furthermore, we propose that a detrital food web may be associated with polar sea ice.
机译:1980年,在南极州麦克默多湾的一年一度海冰的盐水通道内和冰-海水界面处发现了一个丰富多样的细菌群落。平均细菌现存量为1.4×1011细胞m?2(9.8 mg C 2);在冰芯融化水中观察到细菌浓度高达1.02×1012细胞m?3。 1.3至2.5 m长的冰芯的垂直剖面表明,47%的细菌数量和93%的细菌生物量位于海冰底部20 cm。冰细菌的生物量浓度比水柱中的浮游生物高10倍以上。扫描电子显微镜照片显示了多种形态学上不同的细胞类型,包括球形,棒状,梭形,丝状和假体形式。通常观察到分裂细胞。大约70%的冰细菌是自由活动的,而30%的细菌附着在活的藻类细胞或碎屑上。冰细菌和微藻之间的相互作用通过细菌数量与冰中叶绿素a含量之间的正相关来暗示。扫描和透射电子显微镜显示,附生细菌与两栖类属的优势冰藻之间存在紧密的物理联系。我们提出,海冰微生物群落不仅是极地生态系统中初级生产的来源,而且还是次级微生物生产的来源。此外,我们建议破坏性食物网可能与极地海冰有关。

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