“…Because plant 14 C reflects the CO 2 assimilated from the atmosphere during photosynthesis, differences in 14 C depletion between plant samples are driven by local differences in ambient 14 CO 2 composition and particularly the amount of fossil fuel influence. Studies around the world have mapped ffCO 2 patterns using a variety of plant species appropriate for their study area including tree rings in LA (e.g., Djuricin et al., 2012 ), evergreen tree leaves in Italy (Alessio et al., 2002 ), corn leaves in the United States (Hsueh et al., 2007 ) and Beijing, China (Xi et al., 2011 ), annual grasses in California (Riley et al., 2008 ; Wang & Pataki, 2010 ), ipê leaves in Rio de Janeiro (Santos et al., 2019 ), turfgrasses in New Zealand (Turnbull et al., 2022 ), and wheat crops in India (Sharma et al., 2023 ). Thus, cities can apply this technique to quantify ffCO 2 patterns by sampling a commonly found plant species that is photosynthetically active during the time integration period of interest.…”