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Water chemistry, bacterial abundance and anoxygenic photosynthetic bacteria in an estuarine blue hole, Andros Island, The Bahamas.

机译:巴哈马群岛安德罗斯岛河口蓝洞中的水化学,细菌丰度和产氧光合细菌。

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Blue Holes of Andros Island, The Bahamas are chemically extreme, highly reducing environments with hydrogen sulfide (H2S) concentrations reaching 18 mM, the highest reported for my marine-salts system. The karstic topography, created by moving seawater and slightly acidic rainfall, resulted in sinkholes filled with seawater at depth and surface fresh water. Numerous blue holes on Andros Island include completely marine forms as well as estuarine and inland systems. This research focused on Tarpon Blue Hole (TBH), 7m deep and 40 m in diameter, located in the shallow, near-shore zone of Stafford Creek estuary. Despite limited depth, TBH was usually highly stratified with a salt driven pycnocline varying from about 3.5 to 5.0 m deep. Beneath the pycnocline the water column was anoxic, with (H2S) ranging up to 3.5 mM, and temperatures up to 41°C. TBH, which is affected by tidal and wind forces, was physically and chemically much more dynamic than inland blue holes, even to the extent that it completely destratified twice, May 1992 and January 1998, during the study. It restratified in less than six months in each case and returned to its anoxic, highly sulfidic condition. Bacteria were very abundant (100 × 106 ml−1) in the deep water. A red layer of presumptive purple sulfur bacteria (PSB) was always present at depths of about 4.5 to 5.5 m when TBH was stratified. PSB dominate planktonic, primary production with photosynthetic rates ten times higher in the “red layer” then in the epilimnion. Enrichment cultures from this “red layer” were established, and extinction dilutions resulted in a pure culture that was microscopically and physiologically identified as a (presumptive) purple sulfur bacterium. Using refined protocols for extraction of molecular 16S rDNA, PCR and DNA sequencing resulted in its identification as a novel strain of Marichromatium purpuratum TAR (http://www.ncbi.nlm.nih.gov: GenBank Accession Number AF294030). This is the first report of M. purpuratum from an anoxic, estuarine water column, and of an anoxygenic, photosynthetic bacterium from Bahamian blue holes. Biolog® Anaerobe Microplates indicate that this strain metabolizes: fructose, fucose, galaturonic acid, palatinose, ketobutyric acid, pyruvic acid, ramnose, glyoxylic acid, and succinic acid.
机译:巴哈马安德罗斯岛的蓝洞是化学性质极端的高还原性环境,硫化氢(H 2 S)浓度达到18 mM,这是我的海洋盐系统中报告的最高值。由移动的海水和轻微的酸性降雨形成的岩溶地形导致井坑中充满了一定深度的海水和地表淡水。安德罗斯岛上的许多蓝洞包括完全的海洋形态以及河口和内陆系统。这项研究的重点是塔福德蓝洞(TBH),深7m,直径40m,位于斯塔福德河口浅水近岸区域。尽管深度有限,但TBH通常用深约3.5至5.0 m的盐驱动的比高可宁高度分层。在比诺可林下,水柱是缺氧的,(H 2 S)的范围高达3.5 mM,温度高达41°C。 TBH受潮汐和风力的影响,在物理和化学上比内陆蓝洞具有更大的动态,甚至在研究过程中它在1992年5月和1998年1月两次完全被破坏。在每种情况下,它在不到六个月的时间内就重新恢复了状态,并恢复到缺氧,高度硫化的状态。深水中细菌非常丰富(100×10 6 ml -1 )。当TBH分层时,红色的推测性紫色硫细菌(PSB)始终存在于约4.5至5.5 m的深度。 PSB在浮游生物的初级生产中占主导地位,其“红色层”的光合作用速率是其上层期的十倍。建立了来自该“红色层”的富集培养物,并且消光稀释产生了一种纯培养物,在显微镜下和生理上被鉴定为(假定的)紫色硫细菌。使用精细的提取分子16S rDNA的方案,PCR和DNA测序结果将其鉴定为 Marichromatium purpuratum TAR 的新型菌株(http://www.ncbi.nlm.nih.gov:GenBank加入编号AF294030)。这是 M的第一份报告。来自缺氧河口水柱的紫癜,以及来自巴哈马蓝洞的产氧光合细菌。 Biolog ®厌氧菌微孔板表明该菌株代谢:果糖,岩藻糖,半乳糖醛酸,帕拉金糖,酮丁酸,丙酮酸,拉姆糖,乙醛酸和琥珀酸。

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