Trading oxygen for iron II. Oxygen- versus iron-dependent cosmic star formation history
Martyna Chruślińska, Mirko Curti, Ruediger Pakmor, Annalisa De Cia, Jorryt Matthee, Aniket Bhagwat, Stephanie Monty
TL;DR
This paper argues that oxygen and iron track different cosmic enrichment histories and should be treated separately in galaxy evolution modeling. It builds an observationally motivated framework to derive independent iron- and oxygen-based cosmic star formation histories by leveraging the redshift-invariant $[O/Fe]-sSFR$ relation and updated high-redshift constraints from JWST. The study finds that near-solar $[O/Fe]$ star formation is rare (at least 70% of stellar mass forms with non-solar O/Fe), and that the SFRD-weighted mean metallicity is typically lower in $[Fe/H]$ than in $[O/H]$, with the offset peaking around $z\sim3$ and then plateauing. These results bear on interpreting spectra and rates of metal-poor transients and highlight biases introduced by solar-scaling in common SPS and galaxy evolution diagnostics.
Abstract
Due to their different nucleosynthetic origin, a stellar population produces oxygen (O) and iron (Fe) on different timescales and their relative abundance can deviate strongly from solar. Galaxy formation models should treat these elements separately, as they play a distinct role in shaping physical phenomena. For example, oxygen mainly sets the gas cooling rate, while the iron abundance sets stellar atmosphere opacities impacting stellar evolution, spectra and feedback. Observations of star-forming galaxies usually only constrain gas-phase oxygen abundance, vastly limiting our capabilities of separating the cosmic evolution of oxygen and iron. Here, we present an observationally-motivated framework to scale the cosmic evolution of O and Fe abundances. We apply the relation between the alpha-enhancement and galaxies' specific star formation rate ([O/Fe]-sSFR; Chruslinska et al. 2024) to derive the Fe and O-dependent cosmic star formation history (cSFH). We find that star formation with near-solar O/Fe is rare: at least 70% of the integrated cosmic stellar mass forms at non-solar O/Fe. The cosmic average metallicity is generally lower in [Fe/H] than in [O/H] (by up to a factor 3), with the offset increasing from redshifts z=0 to z~3 and then approaching the core-collapse O/Fe ratio. We validate our results against samples that probe the Fe-dependent cSFH in different regimes such as absorption-derived <[Fe/H]> from long gamma-ray bursts. Our results impact the interpretations of stellar and galaxy spectra and the predicted rates of transients, especially those linked to metal-poor progenitors (e.g., black hole mergers).
