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在季风驱动的热带河口,细菌在氨氧化过程中对古菌占据主导地位。

Bacterial domination over archaea in ammonia oxidation in a monsoon-driven tropical estuary.

作者信息

Puthiya Veettil Vipindas, Abdulaziz Anas, Chekidhenkuzhiyil Jasmin, Kalanthingal Ramkollath Lallu, Karayadi Hamza Fausia, Kizhakkepat Kalam Balachandran, Kallungal Ravunnikutty Muraleedharan, Nair Shanta

机构信息

Regional Centre, CSIR - National Institute of Oceanography, Cochin, Kerala, 682018, India.

出版信息

Microb Ecol. 2015 Apr;69(3):544-53. doi: 10.1007/s00248-014-0519-x. Epub 2014 Oct 26.

Abstract

Autotrophic ammonia oxidizing microorganisms, which are responsible for the rate-limiting step of nitrification in most aquatic systems, have not been studied in tropical estuaries. Cochin estuary (CE) is one of the largest, productive, and monsoon-driven estuary in India opening into the southeast Arabian Sea. CE receives surplus quantities of ammonia through industrial and domestic discharges. The distribution of ammonia-oxidizing bacteria (AOB), ammonia-oxidizing archaea (AOA), and anaerobic ammonia-oxidizing bacteria (anammox) were studied using fluorescence in situ hybridization (FISH) and their relative contribution to the process as well as the governing factors were examined and reported for the first time from CE. The order of occurrence of these assemblages was β-proteobacteria (0.79 to 2 × 10(5) cells ml(-1)) > γ-proteobacteria (0.9 to 4.6 × 10(4) cells ml(-1)) > anammox (0.49 to 1.9 × 10(4) cells ml(-1)) > AOA (0.56 to 6.3 × 10(3) cells ml(-1)). Phylogenetic analysis of DGGE bands showed major affiliation of AOB to β-proteobacteria, while AOA was affiliated to Crenarchaeota. The abundance of AOB was mostly influenced by ammonia concentrations. The recovered ammonia oxidation rate of AOB was in the range of 45-65%, whereas for AOA, it was 15-45%, indicating that AOB were mostly responsible for the ammonia oxidation in CE during the study period. Overall, the present study provides an insight into the relevance and contribution of different groups of ammonia oxidizing bacteria in CE and emphasizes the need for further in depth studies across space and on season scale.

摘要

自养氨氧化微生物负责大多数水生系统中硝化作用的限速步骤,然而在热带河口尚未对其进行研究。科钦河口(CE)是印度最大、最具生产力且受季风驱动的河口之一,通向阿拉伯海东南部。CE通过工业和生活排放接收大量氨。利用荧光原位杂交(FISH)研究了氨氧化细菌(AOB)、氨氧化古菌(AOA)和厌氧氨氧化细菌(anammox)的分布,并首次检测并报告了它们对该过程的相对贡献以及控制因素。这些菌群的出现顺序为β-变形菌(0.79至2×10⁵ 个细胞/毫升)>γ-变形菌(0.9至4.6×10⁴ 个细胞/毫升)>厌氧氨氧化菌(0.49至1.9×10⁴ 个细胞/毫升)>AOA(0.56至6.3×10³ 个细胞/毫升)。DGGE条带的系统发育分析表明,AOB主要隶属于β-变形菌,而AOA隶属于泉古菌门。AOB的丰度主要受氨浓度影响。AOB的氨氧化率恢复范围为45%至65%,而AOA的氨氧化率为15%至45%,这表明在研究期间,AOB是CE中氨氧化的主要责任者。总体而言,本研究深入了解了CE中不同氨氧化细菌群体的相关性和贡献,并强调了在空间和季节尺度上进一步深入研究的必要性。

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