Smith Cindy J, Nedwell David B, Dong Liang F, Osborn A Mark
Department of Biological Sciences, University of Essex, Colchester, UK.
Appl Environ Microbiol. 2007 Jun;73(11):3612-22. doi: 10.1128/AEM.02894-06. Epub 2007 Mar 30.
Estuarine systems are the major conduits for the transfer of nitrate from agricultural and other terrestrial-anthropogenic sources into marine ecosystems. Within estuarine sediments some microbially driven processes (denitrification and anammox) result in the net removal of nitrogen from the environment, while others (dissimilatory nitrate reduction to ammonium) do not. In this study, molecular approaches have been used to investigate the diversity, abundance, and activity of the nitrate-reducing communities in sediments from the hypernutrified Colne estuary, United Kingdom, via analysis of nitrate and nitrite reductase genes and transcripts. Sequence analysis of cloned PCR-amplified narG, napA, and nrfA gene sequences showed the indigenous nitrate-reducing communities to be both phylogenetically diverse and also divergent from previously characterized nitrate reduction sequences in soils and offshore marine sediments and from cultured nitrate reducers. In both the narG and nrfA libraries, the majority of clones (48% and 50%, respectively) were related to corresponding sequences from delta-proteobacteria. A suite of quantitative PCR primers and TaqMan probes was then developed to quantify phylotype-specific nitrate (narG and napA) and nitrite reductase (nirS and nrfA) gene and transcript numbers in sediments from three sites along the estuarine nitrate gradient. In general, both nitrate and nitrite reductase gene copy numbers were found to decline significantly (P < 0.05) from the estuary head towards the estuary mouth. The development and application, for the first time, of quantitative reverse transcription-PCR assays to quantify mRNA sequences in sediments revealed that transcript numbers for three of the five phylotypes quantified were greatest at the estuary head.
河口系统是硝酸盐从农业和其他陆地人为源向海洋生态系统转移的主要通道。在河口沉积物中,一些微生物驱动的过程(反硝化作用和厌氧氨氧化)导致环境中氮的净去除,而其他过程(异化硝酸盐还原为铵)则不会。在本研究中,通过分析硝酸盐和亚硝酸盐还原酶基因及转录本,采用分子方法研究了英国超富营养化的科尔恩河口沉积物中硝酸盐还原群落的多样性、丰度和活性。对克隆的PCR扩增的narG、napA和nrfA基因序列进行序列分析表明,本地硝酸盐还原群落不仅在系统发育上具有多样性,而且与先前在土壤和近海海洋沉积物中表征的硝酸盐还原序列以及培养的硝酸盐还原菌不同。在narG和nrfA文库中,大多数克隆(分别为48%和50%)与δ-变形菌门的相应序列相关。然后开发了一套定量PCR引物和TaqMan探针,以量化沿河口硝酸盐梯度的三个地点沉积物中特定系统发育型的硝酸盐(narG和napA)和亚硝酸盐还原酶(nirS和nrfA)基因及转录本数量。一般来说,从河口源头到河口口,硝酸盐和亚硝酸盐还原酶基因拷贝数均显著下降(P < 0.05)。首次开发并应用定量逆转录PCR测定法来量化沉积物中的mRNA序列,结果表明,在五个定量的系统发育型中,有三个的转录本数量在河口源头最高。