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Review

Methylotrophs and Methylotroph Populations for Chloromethane Degradation

by
Françoise Bringel
1,*,
Ludovic Besaury
2,
Pierre Amato
3,
Eileen Kröber
4,
Steffen Kolb
4,
Frank Keppler
5,6,
Stéphane Vuilleumier
1 and
Thierry Nadalig
1
1
Université de Strasbourg UMR 7156 UNISTRA CNRS, Laboratory of Molecular Genetics, Genomics, Microbiology (GMGM), Strasbourg, France
2
Université de Reims Champagne-Ardenne, Chaire AFERE, INRA, FARE UMR A614, Reims, France
3
Université Clermont Auvergne, CNRS, SIGMA Clermont, ICCF, Clermont-Ferrand, France
4
Microbial Biogeochemistry, Research Area Landscape Functioning – Leibniz Centre for Agricultural Landscape Research – ZALF, Müncheberg, Germany
5
Institute of Earth Sciences, Heidelberg University, Heidelberg, Germany
6
Heidelberg Center for the Environment HCE, Heidelberg University, Heidelberg, Germany
*
Author to whom correspondence should be addressed.
Curr. Issues Mol. Biol. 2019, 33(1), 149-172; https://doi.org/10.21775/cimb.033.149
Submission received: 5 March 2019 / Revised: 8 April 2019 / Accepted: 8 May 2019 / Published: 5 June 2019

Abstract

Chloromethane is a halogenated volatile organic compound, produced in large quantities by terrestrial vegetation. After its release to the troposphere and transport to the stratosphere, its photolysis contributes to the degradation of stratospheric ozone. A better knowledge of chloromethane sources (production) and sinks (degradation) is a prerequisite to estimate its atmospheric budget in the context of global warming. The degradation of chloromethane by methylotrophic communities in terrestrial environments is a major underestimated chloromethane sink. Methylotrophs isolated from soils, marine environments and more recently from the phyllosphere have been grown under laboratory conditions using chloromethane as the sole carbon source. In addition to anaerobes that degrade chloromethane, the majority of cultivated strains were isolated in aerobiosis for their ability to use chloromethane as sole carbon and energy source. Among those, the Proteobacterium Methylobacterium (recently reclassified as Methylorubrum) harbours the only characterisized 'chloromethane utilization' (cmu) pathway, so far. This pathway is not representative of chloromethane-utilizing populations in the environment as cmu genes are rare in metagenomes. Recently, combined 'omics' biological approaches with chloromethane carbon and hydrogen stable isotope fractionation measurements in microcosms, indicated that microorganisms in soils and the phyllosphere (plant aerial parts) represent major sinks of chloromethane in contrast to more recently recognized microbe-inhabited environments, such as clouds. Cultivated chloromethane-degraders lacking the cmu genes display a singular isotope fractionation signature of chloromethane. Moreover, 13CH3Cl labelling of active methylotrophic communities by stable isotope probing in soils identify taxa that differ from the taxa known for chloromethane degradation. These observations suggest that new biomarkers for detecting active microbial chloromethane-utilizers in the environment are needed to assess the contribution of microorganisms to the global chloromethane cycle.

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MDPI and ACS Style

Bringel, F.; Besaury, L.; Amato, P.; Kröber, E.; Kolb, S.; Keppler, F.; Vuilleumier, S.; Nadalig, T. Methylotrophs and Methylotroph Populations for Chloromethane Degradation. Curr. Issues Mol. Biol. 2019, 33, 149-172. https://doi.org/10.21775/cimb.033.149

AMA Style

Bringel F, Besaury L, Amato P, Kröber E, Kolb S, Keppler F, Vuilleumier S, Nadalig T. Methylotrophs and Methylotroph Populations for Chloromethane Degradation. Current Issues in Molecular Biology. 2019; 33(1):149-172. https://doi.org/10.21775/cimb.033.149

Chicago/Turabian Style

Bringel, Françoise, Ludovic Besaury, Pierre Amato, Eileen Kröber, Steffen Kolb, Frank Keppler, Stéphane Vuilleumier, and Thierry Nadalig. 2019. "Methylotrophs and Methylotroph Populations for Chloromethane Degradation" Current Issues in Molecular Biology 33, no. 1: 149-172. https://doi.org/10.21775/cimb.033.149

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