Effects of chitin and temperature on sub-Arctic soil microbial and fungal communities and biodegradation of hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX) and 2,4-dinitrotoluene (DNT).

Abstract

Climate warming in the Arctic and the thawing of frozen carbon stocks are leading to uncertainty as to how bacterial communities will respond, including pollutant degrading bacteria. This study investigated the effects of carbon stimulation and temperature on soil microbial community diversity and explosive biodegradation in two sub-Arctic soils. Chitin as a labile carbon source stimulated overall microbial activities as reflected by increases in basal respiration (three to tenfold) and potential nitrification activity (two to fourfold) compared to unamended soil. This stimulation extended to 2,4-dinitroluene- (DNT) and hexahydro-1,3,5-trinitro-1,3,5-triazine (RDX)-degrading microorganisms either directly or via co-metabolic reaction mechanisms. A stimulatory effect of the incubation temperature (2, 12, or 22°C) on these microbial activities was also observed, but the chitin stimulation caused greater shifts in the structure of the bacterial and fungal communities. The first reported occurrence of an associated role of chitinolytic bacteria belonging to Cellulomonadaceae and chitinolytic fungi belonging to Mortierellaceae in explosive biodegradation is described. This study found that sub-Arctic soil microbial communities were adapted to respond quickly to an increase in labile carbon sources over the range of temperatures used in this study. The warming climate in the Arctic could benefit explosive contaminated soil clean-up by providing non-recalcitrant carbon sources that stimulate overall microbial activity and correspondingly explosive biodegradation.