The potential for bacteria from carbon-limited deep terrestrial environments to participate in chlorine cycling

Author:

Bhattarai Susma1ORCID,Temme Hanna2,Jain Abhiney3,Badalamenti Jonathan P4,Gralnick Jeffrey A35,Novak Paige J13

Affiliation:

1. Department of Civil, Environmental and Geo- Engineering, University of Minnesota Twin Cities , Minneapolis, MN 55455 , United States

2. AECOM, 800 LaSalle Ave, Minneapolis, MN 55402, United States

3. BioTechnology Institute, University of Minnesota Twin Cities , Saint Paul, MN 55108 , United States

4. University of Minnesota Genomics Center, University of Minnesota Twin Cities , Minneapolis, MN 55455 , United States

5. University of Minnesota Twin Cities Plant and Microbial Biology, , Saint Paul, MN 55108 , United States

Abstract

Abstract Bacteria capable of dehalogenation via reductive or hydrolytic pathways are ubiquitous. Little is known, however, about the prevalence of bacterial dechlorination in deep terrestrial environments with a limited carbon supply. In this study we analyzed published genomes from three deep terrestrial subsurface sites: a deep aquifer in Western Siberia, the Sanford Underground Research Facility in South Dakota, USA, and the Soudan Underground Iron Mine (SUIM) in Minnesota, USA to determine if there was evidence to suggest that microbial dehalogenation was possible in these environments. Diverse dehalogenase genes were present in all analyzed metagenomes, with reductive dehalogenase and haloalkane dehalogenase genes the most common. Taxonomic analysis of both hydrolytic and reductive dehalogenase genes was performed to explore their affiliation; this analysis indicated that at the SUIM site, hydrolytic dehalogenase genes were taxonomically affiliated with Marinobacter species. Because of this affiliation, experiments were also performed with Marinobacter subterrani strain JG233 (‘JG233’), an organism containing three predicted hydrolytic dehalogenase genes and isolated from the SUIM site, to determine whether hydrolytic dehalogenation was an active process and involved in growth on a chlorocarboxylic acid. Presence of these genes in genome appears to be functional, as JG233 was capable of chloroacetate dechlorination with simultaneous chloride release. Stable isotope experiments combined with confocal Raman microspectroscopy demonstrated that JG233 incorporated carbon from 13C-chloroacetate into its biomass. These experiments suggest that organisms present in these extreme and often low-carbon environments are capable of reductive and hydrolytic dechlorination and, based on laboratory experiments, may use this capability as a competitive advantage by utilizing chlorinated organic compounds for growth, either directly or after dechlorination.

Funder

Minnesota Environment and Natural Resources Trust Fund

LCCMR

National Science Foundation

Materials Research Science and Engineering Center

Publisher

Oxford University Press (OUP)

Subject

Applied Microbiology and Biotechnology,Ecology,Microbiology

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