Increasing aggregate size reduces single-cell organic carbon incorporation by hydrogel-embedded wetland microbes

Author:

Johnston Juliet T1,Quoc Bao Nguyen2,Abrahamson Britt2,Candry Pieter2,Ramon Christina1,Cash Kevin J34,Saccomano Sam C3,Samo Ty J1,Ye Congwang1,Weber Peter K1,Winkler Mari-Karoliina Henriikka2,Mayali Xavier1

Affiliation:

1. Physical and Life Sciences, Lawrence Livermore National Laboratory , 7000 East Ave, Livermore CA 94550 , United States

2. Civil and Environmental Engineering, University of Washington , 201 More Hall, Box 352700, Seattle, WA 98195-2700 , United States

3. Chemical and Biological Engineering, Colorado School of Mines , 1500 Illinois St, Golden, CO 80401 , United States

4. Quantitative Biosciences and Engineering, Colorado School of Mines , 1500 Illinois St, Golden, CO 80401 , United States

Abstract

Abstract Microbial degradation of organic carbon in sediments is impacted by the availability of oxygen and substrates for growth. To better understand how particle size and redox zonation impact microbial organic carbon incorporation, techniques that maintain spatial information are necessary to quantify elemental cycling at the microscale. In this study, we produced hydrogel microspheres of various diameters (100, 250, and 500 μm) and inoculated them with an aerobic heterotrophic bacterium isolated from a freshwater wetland (Flavobacterium sp.), and in a second experiment with a microbial community from an urban lacustrine wetland. The hydrogel-embedded microbial populations were incubated with 13C-labeled substrates to quantify organic carbon incorporation into biomass via nanoSIMS. Additionally, luminescent nanosensors enabled spatially explicit measurements of oxygen concentrations inside the microspheres. The experimental data were then incorporated into a reactive-transport model to project long-term steady-state conditions. Smaller (100 μm) particles exhibited the highest microbial cell-specific growth per volume, but also showed higher absolute activity near the surface compared to the larger particles (250 and 500 μm). The experimental results and computational models demonstrate that organic carbon availability was not high enough to allow steep oxygen gradients and as a result, all particle sizes remained well-oxygenated. Our study provides a foundational framework for future studies investigating spatially dependent microbial activity in aggregates using isotopically labeled substrates to quantify growth.

Funder

United States Department of Energy’s Office of Science Biological and Environmental Research

Lawrence Livermore National Laboratory

DOE-BER

Publisher

Oxford University Press (OUP)

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