Biological nitrogen fixation constitutes the main input of fixed nitrogen to Earth's ecosystems, and its isotope effect is a key parameter in isotope-based interpretations of the N cycle. The nitrogen isotopic composition (δ 15 N) of newly fixed N is currently believed to be ∼-1‰, based on measurements of organic matter from diazotrophs using molybdenum (Mo)-nitrogenases. We show that the vanadium (V)-and iron (Fe)-only "alternative" nitrogenases produce fixed N with significantly lower δ 15 N (-6 to -7‰). An important contribution of alternative nitrogenases to N 2 fixation provides a simple explanation for the anomalously low δ 15 N (<-2‰) in sediments from the Cretaceous Oceanic Anoxic Events and the Archean Eon. A significant role for the alternative nitrogenases over Mo-nitrogenase is also consistent with evidence of Mo scarcity during these geologic periods, suggesting an additional dimension to the coupling between the global cycles of trace elements and nitrogen. Mo is ∼+2‰ (3-6)], which is thought to be the most abundant in nature. As a result, the δ 15 N of newly fixed N is ∼-1‰ (i.e., ∼+2‰ lower than the δ 15 N of dissolved N 2 substrate, +0.7‰, Fig. 1A).In addition to Mo-nitrogenase (the most common form of the enzyme), diazotrophs can possess two other nitrogenase isozymes (7). These so-called "alternative" nitrogenases differ chiefly from Mo-nitrogenases in that V or Fe replaces Mo in the active site. They also contain an additional protein subunit and exhibit slower kinetics compared with the Mo-nitrogenase (8). Such differences could result in distinct isotope effects, a possibility supported by Rowell et al. (9), who reported small but significant variations in biomass δ 15 N from growth of wild-type diazotrophs possessing all three isozymes in media containing Fe and amendments of Mo, V, or neither metal. However, the use of multiple nitrogenase isozymes in the wild type (10) precludes the direct association between biomass δ 15 N and the isotope effect of a particular isozyme. Here we (i) measured directly the isotope effects for Mo-, V-, and Fe-only nitrogenases using diazotroph mutant strains that could express only a single nitrogenase isozyme, (ii) determined the impact of metal limitation on alternative nitrogenase use and N isotope fractionation in wild-type bacteria, and (iii) provide several examples of how these results on N isotope fractionation may change our understanding of the N cycle in the past.
Results and DiscussionIsotope Fractionation During Nitrogen Fixation by Mo-, V-, and Fe-only Nitrogenases. We measured the in vivo isotope effect associated with each type of nitrogenase in two phylogenetically and metabolically distinct diazotrophic bacteria, Rhodopseudomonas palustris and Azotobacter vinelandii. R. palustris is an alpha-proteobacterium. It fixes N 2 anaerobically and was grown under anaerobic and photoheterotrophic conditions. A. vinelandii is a gamma-proteobacterium. It fixes N 2 aerobically and was grown under aerobic chemoheterotrophic conditions. All three nitroge...