Drought re-routes soil microbial carbon metabolism towards emission of volatile metabolites in an artificial tropical rainforest
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Author
Honeker, L.K.Pugliese, G.
Ingrisch, J.
Fudyma, J.
Gil-Loaiza, J.
Carpenter, E.
Singer, E.
Hildebrand, G.
Shi, L.
Hoyt, D.W.
Chu, R.K.
Toyoda, J.
Krechmer, J.E.
Claflin, M.S.
Ayala-Ortiz, C.
Freire-Zapata, V.
Pfannerstill, E.Y.
Daber, L.E.
Meeran, K.
Dippold, M.A.
Kreuzwieser, J.
Williams, J.
Ladd, S.N.
Werner, C.
Tfaily, M.M.
Meredith, L.K.
Affiliation
Biosphere II, University of ArizonaSchool of Natural Resources and the Environment, University of Arizona
Department of Environmental Sciences, University of Arizona
Issue Date
2023-07-31
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Honeker, L.K., Pugliese, G., Ingrisch, J. et al. Drought re-routes soil microbial carbon metabolism towards emission of volatile metabolites in an artificial tropical rainforest. Nat Microbiol 8, 1480–1494 (2023). https://doi.org/10.1038/s41564-023-01432-9Journal
Nature MicrobiologyRights
© The Author(s) 2023. This article is licensed under a Creative Commons Attribution 4.0 International License.Collection Information
This item from the UA Faculty Publications collection is made available by the University of Arizona with support from the University of Arizona Libraries. If you have questions, please contact us at repository@u.library.arizona.edu.Abstract
Drought impacts on microbial activity can alter soil carbon fate and lead to the loss of stored carbon to the atmosphere as CO2 and volatile organic compounds (VOCs). Here we examined drought impacts on carbon allocation by soil microbes in the Biosphere 2 artificial tropical rainforest by tracking 13C from position-specific 13C-pyruvate into CO2 and VOCs in parallel with multi-omics. During drought, efflux of 13C-enriched acetate, acetone and C4H6O2 (diacetyl) increased. These changes represent increased production and buildup of intermediate metabolites driven by decreased carbon cycling efficiency. Simultaneously,13C-CO2 efflux decreased, driven by a decrease in microbial activity. However, the microbial carbon allocation to energy gain relative to biosynthesis was unchanged, signifying maintained energy demand for biosynthesis of VOCs and other drought-stress-induced pathways. Overall, while carbon loss to the atmosphere via CO2 decreased during drought, carbon loss via efflux of VOCs increased, indicating microbially induced shifts in soil carbon fate. © 2023, The Author(s).Note
Open access articleISSN
2058-5276PubMed ID
37524975Version
Final Published Versionae974a485f413a2113503eed53cd6c53
10.1038/s41564-023-01432-9
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Except where otherwise noted, this item's license is described as © The Author(s) 2023. This article is licensed under a Creative Commons Attribution 4.0 International License.
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