Effects of CO<sub>2</sub> on diazotroph biomass δ<sup>15</sup>N
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Biological nitrogen (N<sub>2</sub>) fixation is the main input of fixed nitrogen to ecosystems on Earth. Nitrogen isotope fractionation during this process is a key parameter for understanding the nitrogen cycle, however, relatively little is known about its regulatory mechanisms. Here we examine the effects of varying CO<sub>2</sub> concentrations on biomass δ<sup>15</sup>N signatures of the cyanobacterial diazotrophs <i>Trichodesmium</i> <i>erythraeum</i><i> </i>and<i> </i><i>Crocosphaera watsonii</i>. We show that these organisms produce biomass up to ~3‰ lower in δ<sup>15</sup>N under either decreased (~180 µatm) or elevated (~1400 µatm) CO<sub>2</sub>concentrations in comparison to modern levels (~380 µatm). Our results pointed towards changes in nitrogenase enzyme efficiency in response to CO<sub>2</sub> perturbations impacting isotopic fractionation during N<sub>2</sub> fixation and thus the biomass δ<sup>15</sup>N. This study contributes to an improved interpretation of the observed fluctuations in the δ<sup>15</sup>N records, and thus the past nitrogen cycle on Earth.



