“…James Ross Island (JRI) has been relatively well‐studied compared to typical Antarctic localities due to the presence of nearby Argentinian, Czech, and Chilean bases, which facilitate frequent visits by scientists from these countries as well as American and British scientists. The geology of the area has been the subject of numerous studies, most of which focused on igneous petrology (e.g., Košler et al., 2009; Sykes, 1988), geochronology (compilation of ages in Smellie, 2021b), glaciology (Carrivick et al., 2012; Engel et al., 2012), sedimentology/stratigraphy (Milanese et al., 2020; Tobin et al., 2012, 2020), and paleontology (Olivero, 2012; Roberts et al., 2014). The area consists of a thick Cretaceous‐Paleogene sedimentary basin, capped by a large basaltic polygenetic shield volcano along with several smaller outlying volcanoes (Figures 1 and 2a) (Smellie et al., 2013).…”