首页> 美国卫生研究院文献>Applied and Environmental Microbiology >Microbial Manganese and Sulfate Reduction in Black Sea Shelf Sediments
【2h】

Microbial Manganese and Sulfate Reduction in Black Sea Shelf Sediments

机译:黑海陆架沉积物中微生物锰和硫酸盐的还原

代理获取
本网站仅为用户提供外文OA文献查询和代理获取服务,本网站没有原文。下单后我们将采用程序或人工为您竭诚获取高质量的原文,但由于OA文献来源多样且变更频繁,仍可能出现获取不到、文献不完整或与标题不符等情况,如果获取不到我们将提供退款服务。请知悉。

摘要

The microbial ecology of anaerobic carbon oxidation processes was investigated in Black Sea shelf sediments from mid-shelf with well-oxygenated bottom water to the oxic-anoxic chemocline at the shelf-break. At all stations, organic carbon (Corg) oxidation rates were rapidly attenuated with depth in anoxically incubated sediment. Dissimilatory Mn reduction was the most important terminal electron-accepting process in the active surface layer to a depth of ∼1 cm, while SO42− reduction accounted for the entire Corg oxidation below. Manganese reduction was supported by moderately high Mn oxide concentrations. A contribution from microbial Fe reduction could not be discerned, and the process was not stimulated by addition of ferrihydrite. Manganese reduction resulted in carbonate precipitation, which complicated the quantification of Corg oxidation rates. The relative contribution of Mn reduction to Corg oxidation in the anaerobic incubations was 25 to 73% at the stations with oxic bottom water. In situ, where Mn reduction must compete with oxygen respiration, the contribution of the process will vary in response to fluctuations in bottom water oxygen concentrations. Total bacterial numbers as well as the detection frequency of bacteria with fluorescent in situ hybridization scaled to the mineralization rates. Most-probable-number enumerations yielded up to 105 cells of acetate-oxidizing Mn-reducing bacteria (MnRB) cm−3, while counts of Fe reducers were <102 cm−3. At two stations, organisms affiliated with Arcobacter were the only types identified from 16S rRNA clone libraries from the highest positive MPN dilutions for MnRB. At the third station, a clone type affiliated with Pelobacter was also observed. Our results delineate a niche for dissimilatory Mn-reducing bacteria in sediments with Mn oxide concentrations greater than ∼10 μmol cm−3 and indicate that bacteria that are specialized in Mn reduction, rather than known Mn and Fe reducers, are important in this niche.
机译:研究了黑海陆架沉积物中厌氧碳氧化过程的微生物生态学,这些沉积物是由具有良好氧化底水的陆架中层到陆架断裂处的缺氧-缺氧趋化索。在所有站点,缺氧培养的沉积物中有机碳(Corg)的氧化速率随深度而迅速衰减。在活性表面层中,异化Mn还原是最重要的终端电子接受过程,深度约为1 cm,而SO4 2-还原则构成了下面整个Corg氧化。锰的还原由中等高的氧化锰浓度支持。不能看出微生物减少铁的贡献,并且添加三水铁矿不会刺激该过程。锰的还原导致碳酸盐沉淀,这使Corg氧化速率的定量变得复杂。在有氧底水站,厌氧培养中Mn还原对Corg氧化的相对贡献为25%到73%。在原地,Mn还原必须与氧气呼吸竞争的情况下,该过程的贡献将随着底部氧气浓度的波动而变化。总细菌数以及通过荧光原位杂交技术对细菌的检测频率与矿化率成比例。最多数量的枚举最多产生10 5 个醋酸盐氧化Mn还原菌(MnRB)cm -3 的细胞,而Fe还原剂的数量<10 < sup> 2 cm −3 。在两个站点上,从MnRB的最高MPN阳性正稀释液中,从16S rRNA克隆文库中鉴定出唯一与Arcobacter相关的生物。在第三站,还观察到了与杆状杆菌有关的克隆类型。我们的研究结果描绘了锰氧化物浓度大于约10μmolcm -3 的沉积物中异化Mn还原细菌的生态位,并表明专门从事Mn还原的细菌,而不是已知的Mn和Fe还原剂,在这个利基市场中很重要。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
代理获取

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