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南大洋和大西洋不同区域多糖降解过程中的细菌群落动态

Bacterial community dynamics during polysaccharide degradation at contrasting sites in the Southern and Atlantic Oceans.

作者信息

Wietz Matthias, Wemheuer Bernd, Simon Heike, Giebel Helge-Ansgar, Seibt Maren A, Daniel Rolf, Brinkhoff Thorsten, Simon Meinhard

机构信息

Institute for Chemistry and Biology of the Marine Environment, University of Oldenburg, Oldenburg, 26129, Germany.

Genomic and Applied Microbiology and Göttingen Genomics Laboratory, Institute of Microbiology and Genetics, University of Göttingen, Göttingen, 37077, Germany.

出版信息

Environ Microbiol. 2015 Oct;17(10):3822-31. doi: 10.1111/1462-2920.12842. Epub 2015 Apr 8.

Abstract

The bacterial degradation of polysaccharides is central to marine carbon cycling, but little is known about the bacterial taxa that degrade specific marine polysaccharides. Here, bacterial growth and community dynamics were studied during the degradation of the polysaccharides chitin, alginate and agarose in microcosm experiments at four contrasting locations in the Southern and Atlantic Oceans. At the Southern polar front, chitin-supplemented microcosms were characterized by higher fractions of actively growing cells and a community shift from Alphaproteobacteria to Gammaproteobacteria and Bacteroidetes. At the Antarctic ice shelf, chitin degradation was associated with growth of Bacteroidetes, with 24% higher cell numbers compared with the control. At the Patagonian continental shelf, alginate and agarose degradation covaried with growth of different Alteromonadaceae populations, each with specific temporal growth patterns. At the Mauritanian upwelling, only the alginate hydrolysis product guluronate was consumed, coincident with increasing abundances of Alteromonadaceae and possibly cross-feeding SAR11. 16S rRNA gene amplicon libraries indicated that growth of the Bacteroidetes-affiliated genus Reichenbachiella was stimulated by chitin at all cold and temperate water stations, suggesting comparable ecological roles over wide geographical scales. Overall, the predominance of location-specific patterns showed that bacterial communities from contrasting oceanic biomes have members with different potentials to hydrolyse polysaccharides.

摘要

多糖的细菌降解是海洋碳循环的核心,但对于降解特定海洋多糖的细菌类群却知之甚少。在此,我们在南大洋和大西洋四个不同地点的微观实验中,研究了几丁质、藻酸盐和琼脂糖等多糖降解过程中的细菌生长和群落动态。在南极极锋,添加几丁质的微观环境中,活跃生长细胞的比例更高,群落从α-变形菌纲向γ-变形菌纲和拟杆菌门转变。在南极冰架,几丁质降解与拟杆菌门的生长有关,细胞数量比对照高24%。在巴塔哥尼亚大陆架,藻酸盐和琼脂糖的降解与不同交替单胞菌科种群的生长相关,每个种群都有特定的时间生长模式。在毛里塔尼亚上升流区,仅藻酸盐水解产物古洛糖醛酸被消耗,这与交替单胞菌科丰度增加以及可能的交叉取食SAR11同时发生。16S rRNA基因扩增子文库表明,在所有寒冷和温带水域站点,几丁质都刺激了与拟杆菌门相关的赖兴巴赫氏菌属的生长,这表明在广泛的地理尺度上具有可比的生态作用。总体而言,特定地点模式的主导地位表明,来自不同海洋生物群落的细菌群落具有水解多糖潜力不同的成员。

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