...
首页> 外文期刊>Geobiology >Low temperature S~0 biomineralization at a supraglacial springsystem in the Canadian High Arctic
【24h】

Low temperature S~0 biomineralization at a supraglacial springsystem in the Canadian High Arctic

机译:加拿大高北极地区冰缘春季系统的低温S〜0生物矿化

获取原文
获取原文并翻译 | 示例
   

获取外文期刊封面封底 >>

       

摘要

Elemental sulfur (S~0) is deposited each summer onto surface ice at Borup Fiord pass on Ellesmere Island, Canada,when high concentrations of aqueous H2S are discharged from a supraglacial spring system. 16S rRNA geneclone libraries generated fromsulfur deposits were dominated by b-Proteobacteria, particularly Ralstonia sp. Sulfur-cycling micro-organisms such as Thiomicrospira sp., and e-Proteobacteria such as Sulfuricurvales and Sulfurovumalesspp. were also abundant. Concurrent cultivation experiments isolated psychrophilic, sulfide-oxidizingconsortia, which produce S~0 in opposing gradients of Na2S and oxygen. 16S rRNA gene analyses of sulfur precipitatedin gradient tubes show stable sulfur-biomineralizing consortia dominated by Marinobacter sp. in associationwith Shewanella, Loktanella, Rubrobacter, Flavobacterium, and Sphingomonas spp. Organisms closelyrelated to cultivars appear in environmental 16S rRNA clone libraries; none currently known to oxidize sulfide.Once consortia were simplified to Marinobacter and Flavobacteria spp. through dilution-to-extinction and agarremoval, sulfur biomineralization continued. Shewanella, Loktanella, Sphingomonas, and Devosia spp. werealso isolated on heterotrophic media, but none produced S~0 alone when reintroduced to Na2S gradient tubes.Tubes inoculated with a Marinobacter and Shewanella spp. co-culture did show sulfur biomineralization, suggestingthat Marinobacter may be the key sulfide oxidizer in laboratory experiments. Light, florescence and scanningelectron microscopy of mineral aggregates produced in Marinobacter experiments revealed abundant cells,with filaments and sheaths variably mineralized with extracellular submicron sulfur grains; similar biomineralizationwas not observed in abiotic controls. Detailed characterization of mineral products associated with low temperaturemicrobial sulfur-cycling may provide biosignatures relevant to future exploration of Europa and Mars.
机译:每年夏天,当从冰川期泉水系统中排放出高浓度的H2S水溶液时,加拿大Ellesmere岛的Borup Fiord通道将元素硫(S〜0)沉积在地表冰上。由硫沉积物产生的16S rRNA基因克隆文库由b-变形杆菌,特别是Ralstonia sp。主导。硫循环微生物,如Thiomicrospira sp。和e-变形杆菌,如Sulfuricurvales和Sulfurovumalesspp。也很丰富。并行培养实验分离出耐高温,硫化物氧化的聚生体,该聚生体以相反的Na2S和氧气梯度生成S〜0。硫沉淀素梯度管的16S rRNA基因分析表明稳定的硫生物矿化财团主要由Marinobacter sp。与Shewanella,Loktanella,风杆菌,黄杆菌和鞘氨醇单胞菌一起。与品种密切相关的有机体出现在环境16S rRNA克隆文库中。目前尚无一个能氧化硫化物的物质。一旦将财团简化为Marinobacter和Flavobacteria spp。通过稀释至灭绝和琼脂去除,硫磺生物矿化继续进行。 Shewanella,Loktanella,鞘氨醇单胞菌和Devosia spp。在异养培养基上也分离到了三聚氰胺,但是当再引入Na2S梯度管中时,没有一个单独产生S〜0。用Marinobacter和Shewanella spp接种的管。共培养确实显示出硫的生物矿化作用,这表明Marinobacter可能是实验室实验中的关键硫化物氧化剂。在海洋细菌实验中产生的矿物质聚集体的光,荧光和扫描电镜观察显示,细胞丰富,细丝和鞘被细胞外亚微米硫颗粒矿化。在非生物对照中未观察到类似的生物矿化作用。与低温微生物硫循环相关的矿物产品的详细表征可能提供与欧罗巴和火星的未来勘探有关的生物特征。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号