Hotspots of root-exuded amino acids are created within a rhizosphere-on-a-chip

Jayde Aufrecht, Muneeba Khalid, Courtney L. Walton, Kylee Tate, John F. Cahill, Scott T. Retterer

Research output: Contribution to journalArticlepeer-review

23 Scopus citations

Abstract

The rhizosphere is a challenging ecosystem to study from a systems biology perspective due to its diverse chemical, physical, and biological characteristics. In the past decade, microfluidic platforms (e.g. plant-on-a-chip) have created an alternative way to study whole rhizosphere organisms, like plants and microorganisms, under reduced-complexity conditions. However, in reducing the complexity of the environment, it is possible to inadvertently alter organism phenotype, which biases laboratory data compared to in situ experiments. To build back some of the complexity of the rhizosphere in a fully-defined, parameterized approach we have developed a rhizosphere-on-a-chip platform that mimics the physical structure of soil. We demonstrate, through computational simulation, how this synthetic soil structure can influence the emergence of molecular "hotspots"and "hotmoments"that arise naturally from the plant's exudation of labile carbon compounds. We establish the amenability of the rhizosphere-on-a-chip for long-term culture of Brachypodium distachyon, and experimentally validate the presence of exudate hotspots within the rhizosphere-on-a-chip pore spaces using liquid microjunction surface sampling probe mass spectrometry.

Original languageEnglish
Pages (from-to)954-963
Number of pages10
JournalLab on a Chip
Volume22
Issue number5
DOIs
StatePublished - Mar 7 2022

Funding

A portion of the research was conducted under the Laboratory Directed Research and Development (LDRD) program at Pacific Northwest National Laboratory, a multi-program national laboratory operated by Battelle for the U.S. Department of Energy. J. Aufrecht was supported by a Linus Pauling Distinguished Postdoctoral Fellowship. A portion of this research was conducted at the Center for Nanophase Material Sciences, which is a DOE Office of Science User Facility. J. F. Cahill and C. L. Walton were funded through the U.S. Department of Energy, Office of Science, Biological and Environmental Research, Bioimaging Science Program. M. Khalid and S. Retterer received support from the Genomic Science Program, U.S. Department of Energy, Office of Science, Biological and Environmental Research, as part of the Plant Microbe Interfaces Scientific Focus Area (http://pmi. ornl.gov).

FundersFunder number
Bioimaging Science Program
Plant Microbe Interfaces Scientific Focus Area
U.S. Department of Energy
Office of Science
Biological and Environmental Research

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