Biosynthetic and catabolic pathways control amino acid δ²H values in aerobic heterotrophs
Abstract
The hydrogen isotope ratios (δ2HAA values) of amino acids in all organisms are substantially fractionated relative to growth water. In addition, they exhibit large variations within microbial biomass, animals, and human tissues, hinting at rich biochemical information encoded in such signals. In lipids, such δ2H variations are thought to primarily reflect NADPH metabolism. Analogous biochemical controls for amino acids remain largely unknown, but must be elucidated to inform the interpretation of these measurements. Here, we measured the δ2H values of amino acids from five aerobic, heterotrophic microbes grown on different carbon substrates, as well as five Escherichia coli mutant organisms with perturbed NADPH metabolisms. We observed similar δ2HAA patterns across all organisms and growth conditions, which–consistent with previous hypotheses–suggests a first-order control by biosynthetic pathways. Moreover, δ2HAA values varied systematically with the catabolic pathways activated for substrate degradation, with variations explainable by the isotopic compositions of important cellular metabolites, including pyruvate and NADPH, during growth on each substrate. As such, amino acid δ2H values may be useful for interrogating organismal physiology and metabolism in the environment, provided we can further elucidate the mechanisms underpinning these signals.
Copyright and License
© 2024 Silverman, Wijker and Sessions. This is an open-access article distributed under the terms of the Creative Commons Attribution License (CC BY). The use, distribution or reproduction in other forums is permitted, provided the original author(s) and the copyright owner(s) are credited and that the original publication in this journal is cited, in accordance with accepted academic practice. No use, distribution or reproduction is permitted which does not comply with these terms.
Acknowledgement
The authors would like to thank Tyler Fulton and Dr. Brian Stoltz for assistance with the chemical reactions used to measure the isotope composition of methyl chloroformate, as well as Fenfang Wu, Patrick Almhjell, and Elliott Mueller for informative discussions. We would also like to thank both reviewers for their constructive comments.
Funding
The author(s) declare that financial support was received for the research, authorship, and/or publication of this article. This work was supported by an NSF GRFP and CEMI (Center for Environmental Microbial Interactions) award to SS and an NSF award OCE-2023687 and NSF Geobiology and Low-Temperature Geochemistry Program award (#1921330) to AS.
Contributions
SS: Conceptualization, Formal analysis, Funding acquisition, Investigation, Methodology, Writing—original draft, Writing—review & editing. RW: Conceptualization, Methodology, Writing—review & editing. AS: Conceptualization, Formal analysis, Funding acquisition, Methodology, Project administration, Resources, Supervision, Writing—review & editing.
Conflict of Interest
The authors declare that the research was conducted in the absence of any commercial or financial relationships that could be construed as a potential conflict of interest.
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Additional details
- PMCID
- PMC11026604
- National Science Foundation
- NSF Graduate Research Fellowship
- California Institute of Technology
- Caltech Center for Environmental and Microbial Interactions
- National Science Foundation
- OCE-2023687
- National Science Foundation
- EAR-1921330`
- Caltech groups
- Division of Geological and Planetary Sciences, Caltech Center for Environmental Microbial Interactions (CEMI)