Chemical evolution imprints in the rare isotopes of nearby M dwarfs

TL;DR

This study measures rare isotopes in nearby M dwarfs to trace galactic chemical evolution, revealing how isotope ratios correlate with metallicity and supporting models of interstellar enrichment by novae.

Contribution

First to measure carbon and oxygen isotope ratios in a large sample of M dwarfs, linking stellar isotopic composition to galactic chemical evolution models.

Findings

Higher metallicity stars have lower 12C/13C ratios.

Observed 16O/18O ratios align with theoretical predictions.

M dwarfs serve as effective tracers of cosmic chemical enrichment.

Abstract

Elements heavier than hydrogen and helium, collectively termed metals, were created inside stars and dispersed through space at the final stages of stellar evolution. The relative amounts of different isotopes (variants of the same element with different masses) in stellar atmospheres provide clues about how our galaxy evolved chemically over billions of years. M dwarfs are small, cool, long-lived stars that comprise three-quarters of all stars in our galaxy. Their spectra exhibit rich fingerprints of their composition, making them potential tracers of chemical evolution. We measure rare carbon and oxygen isotopes in 32 nearby M dwarfs spanning a range of metallicities using high-resolution infrared spectroscopy. We find that stars with higher metal content have lower 12C/13C ratios, indicating they formed from material progressively enriched in 13C over time. This pattern is consistent with models where novae eruptions contributed significant amounts of 13C to the interstellar medium over the past few billion years. Our measurements of 16O/18O ratio match theoretical predictions and suggest that metal-rich stars reach 16O/18O ratios significantly lower than the Sun. These results establish M dwarfs as tracers of chemical enrichment throughout cosmic history.