Geological Society of America

29 Microbial Interactions with Metal, Mineral, and Nutrient Cycling

Tuesday, 14 March 2023
1:30 PM - 4:30 PM
Room 109

TAMING THE UNCULTURED: MODELING MICROBIAL LIFE UNDER VERY LOW REDOX POTENTIAL IN THE SUBSURFACE AND DEEP-SEA BIOSPHERE

Paper number: 29-5
Program: Theme Sessions
Time: 2:50 PM – 3:10 PM

Authors

Sabrina Beckmann Presenting Author
Oklahoma State University, Stillwater, OK
Ibrahim Farag
College of Earth, Ocean and Environment, Lewes, DE
Sabrina Beckmann
Oklahoma State University, Stillwater, OK
Malique Bowen
College of Earth, Ocean and Environment, Lewes, DE
Christina Baughan
University of Arizona, Tucson, AZ
Kara Heathman
Oklahoma State University, Stillwater, OK
Zoe Siftar
Oklahoma State University, Stillwater, OK
Nancy Prouty
U.S. Geological Survey, Santa Cruz, CA
Jennifer Biddle
College of Earth, Ocean and Environment, Lewes, DE
Jennifer Biddle
Oklahoma State University, Stillwater, OK

Abstract

The subsurface biosphere is a hot spot for microorganisms that carry out anaerobic methane oxidation which plays an important role in the long-term storage and removal of methane from the marine and estuarine carbon cycle. Recent research identified the significance of new metabolic pathways that are used by microbial communities in deep-sea carbonates to carry out methane oxidation (Beckmann et al., 2020, ISMEJ). Questions remain on the search of potential electron acceptors that microbes use to oxidize methane. We used river sediment (Broadkill River, DE) and deep-sea carbonates (Pacific Ocean, Queen Charlotte Fault) and a culturing-dependent approach maintaining a very low redox potentials down to -570 mV, a variety of electron acceptors and C1-C5 organic compounds with the goal to enrich a higher diversity of methane oxidisers. We successfully enriched distinct methanotrophic consortia where the main methane oxidizers vary in response to the prevalent redox potentials from ANME to Bathyarchaeota for -310 mV and -570 mV, respectively, from the subsurface of the river sediment. The final acceptor of electrons is likely sulfate, mediated by Dehalococcoides. The microbial community structures showed high degree of similarity across the enrichments and the major players primarily perform substrate-level phosphorylation, including the Coatesbacteria, Patescibacteria, Actinobacteria and Bacteriodeta along with others. The metagenomes of these enrichments have shown that the Coatesbacteria and CPR are performing supporting functions for the microbial community, including the production of cofactors such as vitamin B12 for the Dehalococcoidia. In enrichments using deep-sea carbonates, isoprene initiated the methane-oxidation in enrichment cultures at low redox potential (from -250 to -500mV) suggesting an important reductive role of isoprene or isoprenoid compounds in the subsurface. We are currently characterizing the microorganism’s metabolizing methane and isoprene in the enrichment cultures. These unique enrichments demonstrate the influence of life at low reduction potential, which is common throughout the subsurface, and show how microbes are partnered to gain the most energy out to fuel their metabolic processes in energy limited systems.

Geological Society of America Abstracts with Programs. Vol. 55, No. 1

doi: 10.1130/abs/2023SC-385145

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