Laura Meredith

Laura Meredith

Assistant Professor, BIO5 Institute
Assistant Professor, Ecosystem Genomics
Assistant Professor, Genetics - GIDP
Assistant Professor, Global Change - GIDP
Assistant Professor, Hydrology / Atmospheric Sciences
Director, Biosphere 2 - Tropical Rain Forest
Primary Department
520 6264213

Work Summary

Work Summary
We aim to constrain the microbial drivers of soil-atmosphere trace gas fluxes across a range of scales. We constrain the genetic traits for trace gas metabolism and develop new tools for measuring genes and gases in heterogenous soil systems. New understanding is evaluated across a range of model to natural ecosystems where microbial trace gas cycling occurs in the context of environmental forcings and interactions. Lab website:

Research Interest

Research Interest
Our research is focused on microbe-mediated trace gas fluxes between the soil and atmosphere, their genomic basis, and methods to link gene to ecosystem function in the face of soil complexity and wide-ranging scales. Keywords: Soil Microbial Function, CO2, CH4, N2O, OCS, VOCs


Meredith, L. K., Commane, R., Keenan, T. F., Klosterman, S. T., Munger, J. W., Templer, P. H., Tang, J., Wofsy, S. C., & Prinn, R. G. (2017). Ecosystem fluxes of hydrogen in a mid-latitude forest driven by soil microorganisms and plants. GLOBAL CHANGE BIOLOGY, 23(2), 906-919.
Whelan, M. E., Lennartz, S. T., Gimeno, T. E., Wehr, R., Wohlfahrt, G., Wang, Y., Kooijmans, L., Hilton, T. W., Belviso, S., Peylin, P., Commane, R., Sun, W., Chen, H., Kuai, L., Mammarella, I., Maseyk, K., Berkelhammer, M., Li, K., Yakir, D., , Zumkehr, A., et al. (2017). Reviews and Syntheses: Carbonyl Sulfide as a Multi-scale Tracer for Carbon and Water Cycles. Biogeosciences Discussions, 2017, 1--97.
Wilson, R. M., Tfaily, M. M., Rich, V. I., Keller, J. K., Bridgham, S. D., Zalman, C. M., Meredith, L., Hanson, P. J., Hines, M., Pfeifer-Meister, L., Saleska, S. R., Crill, P., Cooper, W. T., Chanton, J. P., & Kostka, J. E. (2017). Hydrogenation of organic matter as a terminal electron sink sustains high CO2:CH4 production ratios during anaerobic decomposition. ORGANIC GEOCHEMISTRY, 112, 22-32.