bioRxiv Science⌕ Search

Biology subjects

Rucker, H.

Publications and source records attributed to Rucker, H..

3 recordsLinked to original sources

Persistent nitrogenase isotope signatures over two billion years of engineered evolution

Nitrogen isotope fractionation ({varepsilon}15N) 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 {varepsilon}15N values under controlled laboratory conditions. All engineered strains exhibit {varepsilon}15N 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.

evolutionary biology↗

Ecological resource competition as a driver of metallome evolution

The oldest nitrogenase isozyme, emerging a billion years or more before the Great Oxidation Event (GOE), required a molybdenum (Mo)-based cofactor. "Alternative" nitrogenases using iron (Fe) or vanadium (V) cofactors evolved only after the GOE. This history is puzzling because environmental Fe availability decreased after the GOE, while Mo availability increased, due to the contrasting environmental redox behaviors of these elements. Why, then, did the alternatives emerge only after the GOE? Using a model constrained by known microbial Mo quotas, we demonstrate that a strong selection pressure for the use of metals in nitrogenase other than Mo is a plausible consequence of competition between nitrogen-fixing prokaryotes and nitrate-reducing microbes, which require Mo for nitrate reduction and assimilation. This competition would have intensified after the GOE due to increasing availability of nitrate, explaining the evolutionary timing of nitrogenases isozymes. Ecological resource competition therefore emerges as a third driver of metallome evolution in deep-time, alongside the relative environmental availabilities and adaptive advantages of particular metals.

evolutionary biology↗

The Origins of ATP Dependence in Biological Nitrogen Fixation

Life depends on a conserved set of chemical energy currencies that are relics of early biochemistry. One of these is ATP, a molecule that, when paired with a divalent metal ion such as Mg2+, can be hydrolyzed to support numerous cellular and molecular processes. Despite its centrality to extant biochemistry, it is unclear whether ATP supported the function of ancient enzymes. We investigate the evolutionary necessity of ATP by experimentally reconstructing an ancestral variant of the key N2-reducing enzyme nitrogenase. We show that the ancestor has a strict requirement for ATP and its hydrolysis is coupled to electron transfer for N2 reduction. Our results provide direct laboratory evidence of ATP usage by an ancient enzyme, and underscore how biomolecular constraints can entirely decouple cofactor selection from environmental availability.

evolutionary biology↗