Abstract:Bacterial adaptation to growth with toxic halogenated chemicals was explored in the context of methylotrophic metabolism of Methylobacterium extorquens, by comparing strains CM4 and DM4, which show robust growth with chloromethane and dichloromethane, respectively. Dehalogenation of chlorinated methanes initiates growth-supporting degradation, with intracellular release of protons and chloride ions in both cases. The core, variable and strain-specific genomes of strains CM4 and DM4 were defined by comparison w… Show more
“…On the other hand, the small number of differentially abundant proteins shared by strains MC8b and DM4 growing with DCM contrasts with the fact that the two strains share 1136 homologous proteins with over 50% identity at the protein level, with a similar number of detected proteins in the two studies (2453 proteins for strain MC8b versus 2878 for strain DM4 [39]). To us, this suggests that adaptation to dehalogenation of DCM involves specific changes in expression of the taxonomically defined core genome following acquisition of genes for DCM utilisation [49,50], in keeping with the broad functional categories associated with transformation of DCM (Supplementary Table S5), and as suggested by transcriptional studies [51]. In other words, genes involved in adaptation to DCM are not limited to a specific set of genes of DCM-degrading strains, as evidenced by differentially abundant proteins shared by many and sometimes all 13 Hyphomicrobium strains of the pan-proteomics database (Supplementary Figure S1).…”
Several bacteria are able to degrade the major industrial solvent dichloromethane (DCM) by using the conserved dehalogenase DcmA, the only system for DCM degradation characterised at the sequence level so far. Using differential proteomics, we rapidly identified key determinants of DCM degradation for Hyphomicrobium sp. MC8b, an unsequenced facultative methylotrophic DCM-degrading strain. For this, we designed a pan-proteomics database comprising the annotated genome sequences of 13 distinct Hyphomicrobium strains. Compared to growth with methanol, growth with DCM induces drastic changes in the proteome of strain MC8b. Dichloromethane dehalogenase DcmA was detected by differential pan-proteomics, but only with poor sequence coverage, suggesting atypical characteristics of the DCM dehalogenation system in this strain. More peptides were assigned to DcmA by error-tolerant search, warranting subsequent sequencing of the genome of strain MC8b, which revealed a highly divergent set of dcm genes in this strain. This suggests that the dcm enzymatic system is less strongly conserved than previously believed, and that substantial molecular evolution of dcm genes has occurred beyond their horizontal transfer in the bacterial domain. Our study showed the power of pan-proteomics for quick characterization of new strains belonging to branches of the Tree of Life that are densely genome-sequenced.
“…On the other hand, the small number of differentially abundant proteins shared by strains MC8b and DM4 growing with DCM contrasts with the fact that the two strains share 1136 homologous proteins with over 50% identity at the protein level, with a similar number of detected proteins in the two studies (2453 proteins for strain MC8b versus 2878 for strain DM4 [39]). To us, this suggests that adaptation to dehalogenation of DCM involves specific changes in expression of the taxonomically defined core genome following acquisition of genes for DCM utilisation [49,50], in keeping with the broad functional categories associated with transformation of DCM (Supplementary Table S5), and as suggested by transcriptional studies [51]. In other words, genes involved in adaptation to DCM are not limited to a specific set of genes of DCM-degrading strains, as evidenced by differentially abundant proteins shared by many and sometimes all 13 Hyphomicrobium strains of the pan-proteomics database (Supplementary Figure S1).…”
Several bacteria are able to degrade the major industrial solvent dichloromethane (DCM) by using the conserved dehalogenase DcmA, the only system for DCM degradation characterised at the sequence level so far. Using differential proteomics, we rapidly identified key determinants of DCM degradation for Hyphomicrobium sp. MC8b, an unsequenced facultative methylotrophic DCM-degrading strain. For this, we designed a pan-proteomics database comprising the annotated genome sequences of 13 distinct Hyphomicrobium strains. Compared to growth with methanol, growth with DCM induces drastic changes in the proteome of strain MC8b. Dichloromethane dehalogenase DcmA was detected by differential pan-proteomics, but only with poor sequence coverage, suggesting atypical characteristics of the DCM dehalogenation system in this strain. More peptides were assigned to DcmA by error-tolerant search, warranting subsequent sequencing of the genome of strain MC8b, which revealed a highly divergent set of dcm genes in this strain. This suggests that the dcm enzymatic system is less strongly conserved than previously believed, and that substantial molecular evolution of dcm genes has occurred beyond their horizontal transfer in the bacterial domain. Our study showed the power of pan-proteomics for quick characterization of new strains belonging to branches of the Tree of Life that are densely genome-sequenced.
“…Bacteria able to degrade CH 3 Cl have been isolated from plant leaves and may utilize the cmu chloromethane utilization pathway (Nadalig et al, 2014). The only CH 3 Cl degradation pathway characterized in detail, was mainly studied in Methylobacterium extorquens CM4, an aerobic methylotrophic strain able to use CH 3 Cl as the sole source of carbon and energy (Chaignaud et al, 2017;Roselli et al, 2013;Vanelli et al, 1999). In this pathway, the CH 3 Cl dehalogenase includes a corrinoid methyltransferase (CmuA) and a tetrahydrofolate-dependent methyltransferase (CmuB) (Studer et al, 2001(Studer et al, , 1999.…”
Chloromethane (CHCl) is the most abundant halogenated trace gas in the atmosphere. It plays an important role in natural stratospheric ozone destruction. Current estimates of the global CHCl budget are approximate. The strength of the CHCl global sink by microbial degradation in soils and plants is under discussion. Some plants, particularly ferns, have been identified as substantial emitters of CHCl. Their ability to degrade CHCl remains uncertain. In this study, we investigated the potential of leaves from 3 abundant ferns (Osmunda regalis, Cyathea cooperi, Dryopteris filix-mas) to produce and degrade CHCl by measuring their production and consumption rates and their stable carbon and hydrogen isotope signatures. Investigated ferns are able to degrade CHCl at rates from 2.1 to 17 and 0.3 to 0.9μggday for C. cooperi and D. filix-mas respectively, depending on CHCl supplementation and temperature. The stable carbon isotope enrichment factor of remaining CHCl was -39±13‰, whereas negligible isotope fractionation was observed for hydrogen (-8±19‰). In contrast, O. regalis did not consume CHCl, but produced it at rates ranging from 0.6 to 128μggday, with stable isotope values of -97±8‰ for carbon and -202±10‰ for hydrogen, respectively. Even though the 3 ferns showed clearly different formation and consumption patterns, their leaf-associated bacterial diversity was not notably different. Moreover, we did not detect genes associated with the only known chloromethane utilization pathway "cmu" in the microbial phyllosphere of the investigated ferns. Our study suggests that still unknown CHCl biodegradation processes on plants play an important role in global cycling of atmospheric CHCl.
“…Such low concentrations likely do not yield sufficient energy for substantial bacterial growth with CH 3 Cl. However, many known alphaproteobacterial CH 3 Cl degraders also grow with methanol (CH 3 OH) [ 13 , 21 ], and this is also true in situ for soil methylotrophs of a deciduous forest [ 22 ]. Abundance of methylotrophs in O and A soil horizons is high, and ranges from 10 6 to 3 × 10 8 cells g soil −1 , consistent with their frequent isolation from soils [ 23 , 24 ].…”
Section: Introductionmentioning
confidence: 99%
“…Which organisms define the bacterial CH 3 Cl sink in soils is largely unknown at present. The only biochemically characterized pathway for CH 3 Cl utilization is the cmu pathway, characterized in detail for Methylobacterium extorquens CM4 [ 21 ]. It has been found in various CH 3 Cl-degrading bacterial strains, including several strains from forest soil [ 7 , 18 , 25 – 27 ].…”
Halogenated volatile organic compounds (VOCs) emitted by terrestrial ecosystems, such as chloromethane (CH3Cl), have pronounced effects on troposphere and stratosphere chemistry and climate. The magnitude of the global CH3Cl sink is uncertain since it involves a largely uncharacterized microbial sink. CH3Cl represents a growth substrate for some specialized methylotrophs, while methanol (CH3OH), formed in much larger amounts in terrestrial environments, may be more widely used by such microorganisms. Direct measurements of CH3Cl degradation rates in two field campaigns and in microcosms allowed the identification of top soil horizons (i.e., organic plus mineral A horizon) as the major biotic sink in a deciduous forest. Metabolically active members of Alphaproteobacteria and Actinobacteria were identified by taxonomic and functional gene biomarkers following stable isotope labeling (SIP) of microcosms with CH3Cl and CH3OH, added alone or together as the [13C]-isotopologue. Well-studied reference CH3Cl degraders, such as Methylobacterium extorquens CM4, were not involved in the sink activity of the studied soil. Nonetheless, only sequences of the cmuA chloromethane dehalogenase gene highly similar to those of known strains were detected, suggesting the relevance of horizontal gene transfer for CH3Cl degradation in forest soil. Further, CH3Cl consumption rate increased in the presence of CH3OH. Members of Alphaproteobacteria and Actinobacteria were also 13C-labeled upon [13C]-CH3OH amendment. These findings suggest that key bacterial CH3Cl degraders in forest soil benefit from CH3OH as an alternative substrate. For soil CH3Cl-utilizing methylotrophs, utilization of several one-carbon compounds may represent a competitive advantage over heterotrophs that cannot utilize one-carbon compounds.
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