“…The next geological interval, that of the Aptian Age , includes several more putative Scoliidae, definitive Vespidae ( †Curiosivespa Rasnitsyn, 1975, †Priorvespa Carpenter & Rasnitsyn, 1990, putative Tiphiidae ( †Architiphia Darling, 1990 in Darling & Sharkey 1990), putative Sapygidae ( †Cretofedtschenkia Osten, 2007), and a potential crown ant based on our present analyses ( †Cariridris Brandão & Martins-Neto, 1990, see also Ohl 2004). These Aptian fossils have been recovered from several localities, most notably the Laiyang (e.g., Zhou et al 2020), Yixian (e.g., Chang et al 2017), Khurilt (= Dzun-Bain, Kopylov et al 2020), and Crato Formations (e.g., Martill et al 2009). No other first appearances of vespiform Aculeata occurs before the Kachin amber deposit, although definitive stem Formicidae are recovered from the late Albian Charentese and Baikura Formations, including the unplaceable male-based genus †Baikuris Dlussky, 1987, the sphecomyrmine †Gerontoformica cretacica Nel & Perrault, 2004, and the haidomyrmecine †Haidomyrmodes mammuthus Perrichot et al, 2008. Undoubtedly the most important fossil deposit for understanding the paleodiversity of the Aculeata is that of the mid Cretaceous Kachin (Burmese) amber (~ 99 Mya: Shi et al 2012, Mao et al 2018; see also Balashov 2021).…”