Nitrogen isotopic fractionation during abiotic synthesis of organic solid particles

TL;DR

This study investigates nitrogen isotope fractionation during abiotic organic synthesis via plasma discharge, revealing consistent N isotope depletion and implications for understanding organic formation in the solar system and planetary atmospheres.

Contribution

It demonstrates that plasma discharge synthesis causes specific nitrogen isotope fractionation, providing insights into abiotic organic formation and isotopic signatures in the solar system.

Findings

Nitrogen is incorporated into aerosols regardless of initial gas composition.

Synthesized aerosols are depleted in 15N by 15-25 permil relative to N2.

Kinetic effects likely cause the observed isotope fractionation.

Abstract

The formation of organic compounds is generally assumed to result from abiotic processes in the Solar System, with the exception of biogenic organics on Earth. Nitrogen-bearing organics are of particular interest, notably for prebiotic perspectives but also for overall comprehension of organic formation in the young solar system and in planetary atmospheres. We have investigated abiotic synthesis of organics upon plasma discharge, with special attention to N isotope fractionation. Organic aerosols were synthesized from N2-CH4 and N2-CO gaseous mixtures using low-pressure plasma discharge experiments, aimed at simulating chemistry occurring in Titan s atmosphere and in the protosolar nebula, respectively. Nitrogen is efficiently incorporated into the synthesized solids, independently of the oxidation degree, of the N2 content of the starting gas mixture, and of the nitrogen speciation in the aerosols. The aerosols are depleted in 15N by 15-25 permil relative to the initial N2 gas, whatever the experimental setup is. Such an isotopic fractionation is attributed to mass-dependent kinetic effect(s). Nitrogen isotope fractionation upon electric discharge cannot account for the large N isotope variations observed among solar system objects and reservoirs. Extreme N isotope signatures in the solar system are more likely the result of self-shielding during N2 photodissociation, exotic effect during photodissociation of N2 and/or low temperature ion-molecule isotope exchange. Kinetic N isotope fractionation may play a significant role in the Titan s atmosphere. We also suggest that the low delta15N values of Archaean organic matter are partly the result of abiotic synthesis of organics that occurred at that time.