Biogeochemical N signatures from rate-yield trade-offs during in vitro chemosynthetic NO3− reduction by deep-sea vent ε-Proteobacteria and Aquificae growing at different temperatures

NO3− reduction is a metabolism that is widespread among ε-Proteobacteria and Aquificae, two abundant classes of microorganisms found at deep-sea vents. In this study, we used Sulfurovum lithotrophicum, Caminibacter mediatlanticus and Thermovibrio ammonificans as representatives of these groups to study ecophysiological, metabolic and biogeochemical parameters associated with chemolithoautotrophic NO3− reduction under different temperature regimes. We observed that while S. lithotrophicum and C. mediatlanticus achieved higher cell densities than T. ammonificans, the overall NO3− consumption by the latter was on average ∼9 and ∼5 times faster on a per cell basis, respectively. Comparison with previously published data from other cultured vent ε-Proteobacteria and Aquificae suggests that the rate-yield trade-offs observed in our experiments are generally conserved between these two groups in line with their ecophysiologies. Kinetic isotope effects of N from NO3− reduction were 9.6 ± 2.7‰ for S. lithotrophicum, 6.4 ± 0.7‰ for C. mediatlanticus and 8.8 ± 0.6‰ for T. ammonificans. Our results help evaluate how metabolic partitioning between growth efficiency and reaction kinetics during chemolithoautotrophic NO3− reduction affect the concentration and isotope composition of N compounds at deep-sea hydrothermal vents.