Wildfires can influence the earth’s radiative
forcing through
the emission of biomass-burning aerosols. To better constrain the
impacts of wildfires on climate and understand their evolution under
future climate scenarios, reconstructing their chemical nature, assessing
their past variability, and evaluating their influence on the atmospheric
composition are essential. Ice cores are unique to perform such reconstructions
representing archives not only of past biomass-burning events but
also of concurrent climate and environmental changes. Here, we present
a novel methodology for the quantification of five biomass-burning
proxies (syringic acid, vanillic acid, vanillin, syringaldehyde, and p-hydroxybenzoic acid) and one biogenic emission proxy (pinic
acid) using solid phase extraction (SPE) and ultrahigh-performance
liquid chromatography coupled with high-resolution mass spectrometry.
This method was also optimized for untargeted screening analysis to
gain a broader knowledge about the chemical composition of organic
aerosols in ice and snow samples. The method provides low detection
limits (0.003–0.012 ng g–1), high recoveries
(74 ± 10%), and excellent reproducibility, allowing the quantification
of the six proxies and the identification of 313 different molecules,
mainly constituted by carbon, hydrogen, and oxygen. The effectiveness
of two different sample storage strategies, i.e., re-freezing of previously
molten ice samples and freezing of previously loaded SPE cartridges,
was also assessed, showing that the latter approach provides more
reproducible results.