Methylotrophs and Methylotroph Populations for Chloromethane Degradation Françoise Bringel1*, Ludovic Besaury2, Pierre Amato3, Eileen Kröber4, Stefen Kolb4, Frank Keppler5,6, Stéphane Vuilleumier1 and Thierry Nadalig1 1Université de Strasbourg UMR 7156 UNISTR CNRS, Molecular Genetics, Genomics, Microbiology (GMGM), Strasbourg, France. 2Université de Reims Champagne-Ardenne, Chaire AFERE, INR, FARE UMR A614, Reims, France. 3 Université Clermont Auvergne, CNRS, SIGMA Clermont, ICCF, Clermont-Ferrand, France. 4Microbial Biogeochemistry, Research Area Landscape Functioning – Leibniz Centre for Agricultural Landscape Research – ZALF, Müncheberg, Germany. 5Institute of Earth Sciences, Heidelberg University, Heidelberg, Germany. 6Heidelberg Center for the Environment HCE, Heidelberg University, Heidelberg, Germany. *Correspondence:
[email protected] htps://doi.org/10.21775/cimb.033.149 Abstract characterized ‘chloromethane utilization’ (cmu) Chloromethane is a halogenated volatile organic pathway, so far. Tis pathway may not be representa- compound, produced in large quantities by terres- tive of chloromethane-utilizing populations in the trial vegetation. Afer its release to the troposphere environment as cmu genes are rare in metagenomes. and transport to the stratosphere, its photolysis con- Recently, combined ‘omics’ biological approaches tributes to the degradation of stratospheric ozone. A with chloromethane carbon and hydrogen stable beter knowledge of chloromethane sources (pro- isotope fractionation measurements in microcosms, duction) and sinks (degradation) is a prerequisite indicated that microorganisms in soils and the phyl- to estimate its atmospheric budget in the context of losphere (plant aerial parts) represent major sinks global warming. Te degradation of chloromethane of chloromethane in contrast to more recently by methylotrophic communities in terrestrial envi- recognized microbe-inhabited environments, such ronments is a major underestimated chloromethane as clouds.