The Origin of Earth's Mantle Nitrogen: Primordial or Early Biogeochemical Cycling?

Earth's mantle nitrogen (N) content is comparable to that found in its N-rich atmosphere. Mantle N has been proposed to be primordial or sourced by later subduction, yet its origin has not been elucidated. Here we model N partitioning during the magma ocean stage following planet formation and the subsequent cycling between the surface and mantle over Earth history using argon (Ar) and N isotopes as tracers. The partitioning model, constrained by Ar, shows that only about 10% of the total N content can be trapped in the solidified mantle due to N's low solubility in magma and low partitioning coefficients in minerals in oxidized conditions supported from geophysical and geochemical studies. A possible solution for the primordial origin is that Earth had about 10 times more N at the time of magma ocean solidification. We show that the excess N could be removed by impact erosion during late accretion. The cycling model, constrained by N isotopes, shows that mantle N can originate from efficient N subduction, if the sedimentary N burial rate on early Earth is comparable to that of modern Earth. Such a high N burial rate requires biotic processing. Finally, our model provides a methodology to distinguish the two possible origins with future analysis of the surface and mantle N isotope record.

Automated summary

The origin of nitrogen in Earth's mantle is still unclear, and this study explores possible explanations. Modelling the partitioning of nitrogen during the early stages of Earth's formation and subsequent cycling between the surface and mantle, it is found that only a small fraction of nitrogen can be trapped in the solidified mantle. The excess nitrogen may have been eroded through impact events, and the mantle nitrogen could have originated from efficient subduction processes.