Resurrected Nitrogenases Recapitulate Canonical N-isotope Biosignatures Over Two Billion Years

Nitrogen isotope fractionation (ε¹⁵N) in sedimentary rocks has provided evidence for biological nitrogen fixation, and thus primary productivity, on the early Earth.

However, the extent to which molecular evolution has influenced the isotopic signatures of nitrogenase, the enzyme that catalyzes the conversion of atmospheric nitrogen (N₂) to bioavailable ammonia, remains unresolved.

Here, we reconstruct and experimentally characterize a library of synthetic ancestral nitrogenase genes, spanning over 2 billion years of evolutionary history. By engineering modern microbes to express these ancient nitrogenases, we assess the resulting ε¹⁵N values under controlled laboratory conditions.

All engineered strains exhibit ε¹⁵N values within a narrow range comparable to that of modern microbes, suggesting that molybdenum (Mo)-dependent nitrogenase has been largely invariant throughout evolutionary time since the origins of this pathway.

These results confirm the robustness of N-isotope biosignatures in the ancient rock record and bolster their utility in the search for life in extraterrestrial environments.

a, Protein phylogeny of resurrected ancestral nitrogenases (nifHDK). Node colors represent extant taxonomy. b, Close-up of Group I nitrogenases. The ancestral nodes targeted in this study are labeled with circles. Heterocystous cyanobacteria (highlighted in teal) serve as a minimum age constraint for the ancestral nitrogenase nodes based on fossil evidence. c, Approximate ages for the origin of nitrogenase isoforms are based on geochemical and phylogenetic data. — biorxiv.org

Resurrected nitrogenases recapitulate canonical N-isotope biosignatures over two billion years, biorxiv.org (open access)

Astrobiology, evolution, genomics,