Affiliation:
1. State Key Laboratory of Environmental Aquatic Chemistry, Research Center for Eco-Environmental Sciences, Chinese Academy of Sciences, Beijing 100085, China
2. Water Quality Monitoring Center, Beijing Waterworks Group, Beijing 100085, China
Abstract
ABSTRACT
The role of bacteria in the occasional emergence of red water, which has been documented worldwide, has yet to be determined. To better understand the mechanisms that drive occurrences of red water, the bacterial community composition and the relative abundance of several functional bacterial groups in a water distribution system of Beijing during a large-scale red water event were determined using several molecular methods. Individual clone libraries of the 16S rRNA gene were constructed for three red water samples and one sample of normal water.
Beta
-,
Alpha
-, and
Gammaproteobacteria
comprised the major bacterial communities in both red water and normal water samples, in agreement with previous reports. A high percentage of red water clones (25.2 to 57.1%) were affiliated with or closely related to a diverse array of iron-oxidizing bacteria, including the neutrophilic microaerobic genera
Gallionella
and
Sideroxydans
, the acidophilic species
Acidothiobacillus ferrooxidans
, and the anaerobic denitrifying
Thermomonas
bacteria. The genus
Gallionella
comprised 18.7 to 28.6% of all clones in the three red water libraries. Quantitative real-time PCR analysis showed that the 16S rRNA gene copy concentration of
Gallionella
spp. was between (4.1 ± 0.9) × 10
7
(mean ± standard deviation) and (1.6 ± 0.3) × 10
8
per liter in red water, accounting for 13.1% ± 2.9% to 17.2% ± 3.6% of the total
Bacteria
spp. in these samples. By comparison, the percentages of
Gallionella
spp. in the normal water samples were 0.1% or lower (below the limit of detection), suggesting an important role of
Gallionella
spp. in the formation of red water.
Publisher
American Society for Microbiology
Subject
Ecology,Applied Microbiology and Biotechnology,Food Science,Biotechnology
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