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Major odorous secondary metabolites produced by actinomycetes

Major odorous secondary metabolites produced by actinomycetes

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Actinomycetes are a complex group of bacteria present in a wide variety of environments, either as dormant spores or actively growing. Some actinomycetes produce two potent terpenoids (geosmin and 2-methylisoborneol (MIB)) and pyrazines, common causes of drinking water off flavours, and have been implicated in taste and odour episodes. However, iso...

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... chlorine, earthy/musty odours are the second most common type of reported T/O (Suffett, 1996), and most often caused by the metabolites geosmin and MIB (Wnorowski, 1992 and many others). As observed above, some actinomycetes (notably Streptomyces) produce one or both of these terpenoids, as well as other musty/earthy smelling metabolites (Table 4). Actinomycetes have been associated with musty/earthy odours in water and fish since the early 1900s (Adams, 1929;Thaysen, 1936). ...

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... Our results indicated that Proteobacteria, Actinobacteria, Cyanobacteria, and Bacteroidets accounted for 90% of the total microbial community at the phylum level ( Figure 5). This may be related to Proteobacteria, Actinobacteria and Bacteroidetes are all believed to degrade complex organic macromolecules (González et al., 2000;Kirchman, 2002;Zaitlin and Watson, 2006). Previous study showed that Proteobacteria and Actinobacteria were the dominant microbial community in surface water of reservoir which account for more than 50% of the total bacteria (Yu et al., 2014). ...
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... The presence of fungi genera in drinking water not only changes the odour and taste but also causes some operational and technological difficulties [3]. Water contamination by fungal activities can produce mycotoxicity and allergy to human health [4,5]. It can be transmitted or inhaled during the sauna or showering. ...
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... Both are terpenoids and are synthesized from linear isoprene diphosphate precursors with various chain lengths (Pham et al., 2020). They have also been reported to be produced (synthesized and secreted) as secondary metabolites by different types of cyanobacteria (Izaguirre et al., 1982;Carmichael, 2001;Pham et al., 2020), but other studies have shown actinomycetes, proteobacteria, myxobacteria and some fungi to be geosmin producers (Zaitlin and Watson, 2006;John et al., 2018). ...
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... Many microorganisms, including cyanobacteria, actinomycetes, and certain fungi, produce malodorous compounds [1]. In water reservoirs, several species of cyanobacteria produce earthy-or musty-smelling compounds as secondary metabolites [2][3][4]. ...
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... Widespread musty odor events caused by MIB have been increasingly reported in recent decades, raising considerable public attention (Devi et al., 2021;Lee et al., 2017). Cyanobacteria (Lee et al., 2017) and actinomycetes (Zaitlin and Watson, 2006;Zuo et al., 2010) have been widely accepted as the main MIB producers, although the dominant source for a specific water body is sometimes controversial. Previous studies have revealed that the cyclic nucleotide-binding protein genes (cnb A and cnb B), methyl transferase gene (mtf), and MIB cyclase gene (mic) are associated with MIB biosynthesis (Giglio et al., 2011;Komatsu et al., 2008). ...
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Cellular 2-methylisoborneol (MIB) yield of cyanobacteria varies under different conditions according to culture studies and field investigations, the causal mechanism remains unclear and results in ineffective MIB prediction. Through an intensive field survey during an MIB episode produced by Pseudanabaena cinerea in QCS reservoir, we demonstrated that MIB synthesis (mic) gene abundance (DNA) and expression (RNA) might be useful as parameters for early warning of MIB production. It was found that the abundance of mic DNA and RNA peaked ahead of MIB concentrations by 10 and 7 days, respectively. In addition, the RNA abundance (R2 = 0.45, p < 0.01) showed a slightly higher correlation with MIB compared to DNA abundance (R2 = 0.37, p < 0.01), suggesting that the conditions for the growth of Pseudanabaena cinerea might be slightly different from those for mic gene expression, which was verified by a culture experiment. The highest cell growth was obtained under 36 μmol photons m−2 s−1, while the highest cellular MIB yield and mic gene expression level were obtained under 85 μmol photons m−2 s−1. Our results clearly supported that light intensity was the virtual regulator governing the mic gene expression within the controlled culture experiment and the actual MIB episode in the reservoir. Besides these results, we developed an early warning model using mic gene abundance as an indicator of MIB episodes, which was verified in two other reservoirs. Our findings highlight the effect of light intensity on mic gene expression and MIB synthesis and provide an early warning tool targeting MIB episode prediction, which therefore should be of importance for source water authorities.