Microbe-cellulose hydrogels as a model system for particulate carbon degradation in soil aggregates

Author:

Candry Pieter123,Godfrey Bruce J1,Winkler Mari Karoliina-Henriikka1

Affiliation:

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

2. Laboratory of Systems and Synthetic Biology, Wageningen University & Research , 6708 WE, Wageningen, The Netherlands

3. Laboratory of Systems and Synthetic Biology , Wageningen University & Research, 6708 WE, Wageningen, The Netherlands . E-mail: pieter.candry@wur.nl

Abstract

Abstract Particulate carbon (C) degradation in soils is a critical process in the global C cycle governing greenhouse gas fluxes and C storage. Millimeter-scale soil aggregates impose strong controls on particulate C degradation by inducing chemical gradients of e.g. oxygen, as well as limiting microbial mobility in pore structures. To date, experimental models of soil aggregates have incorporated porosity and chemical gradients but not particulate C. Here, we demonstrate a proof-of-concept encapsulating microbial cells and particulate C substrates in hydrogel matrices as a novel experimental model for soil aggregates. Ruminiclostridium cellulolyticum was co-encapsulated with cellulose in millimeter-scale polyethyleneglycol-dimethacrylate (PEGDMA) hydrogel beads. Microbial activity was delayed in hydrogel-encapsulated conditions, with cellulose degradation and fermentation activity being observed after 13 days of incubation. Unexpectedly, hydrogel encapsulation shifted product formation of R. cellulolyticum from an ethanol-lactate-acetate mixture to an acetate-dominated product profile. Fluorescence microscopy enabled simultaneous visualization of the PEGDMA matrix, cellulose particles, and individual cells in the matrix, demonstrating growth on cellulose particles during incubation. Together, these microbe-cellulose-PEGDMA hydrogels present a novel, reproducible experimental soil surrogate to connect single cells to process outcomes at the scale of soil aggregates and ecosystems.

Funder

US Department of Energy, Office of Science, Office of Biological & Environmental Research

Publisher

Oxford University Press (OUP)

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