Ahníkov (Most Basin, NW Czech Republic) is one of the most diverse and well-documented early Miocene sites in Central Europe. Apart from plant and invertebrate remains, to date, more than 150 species of fossil vertebrates have been reported (Dvořák et al. 2010). The fossil site is also known with the name of Merkur-North. Ahníkov is the name of a village destroyed due to the expansion of an opencast brown coal mine in the 1980s, which was called Merkur-North (Dvořák et al. 2010). According to Mach et al. (2017), both names (Ahníkov and Merkur-North) used for this palaeontological site are synonymous and the authors therefore referred to it as Ahníkov/Merkur Mine. However, we prefer to use just the name Ahníkov (for more details see Ekrt et al. 2016).Ahníkov is located between the cities of Kadaň and Chomutov, more specifically 2 km SW from the Zelená village in the westernmost part of the Most Basin (Fig. 1). The site was discovered in the 1960s during drill cores prospection and the geological profile was exposed in the 1980s (Čtyroký et al. 1964a, b;Bůžek et al. 1988;Dvořák et al. 2010;Ekrt et al. 2016).The Most Basin is the largest of the five Cenozoic freshwater basins along the Ohře/Eger Graben (Rajchl et al. 2009). The bedrock of the Most Basin consists of Proterozoic metamorphic rocks, covered by Carboniferous sediments and volcanic rocks; these are subsequently overlaid by Cretaceous marine sediments (Mach et al. 2014). At the site of Ahníkov, the bedrock is composed of deeply weathered biotitic paragneiss of pre-Variscian age. The Ohře/Eger Graben is the easternmost part of the European Cenozoic Rift System. The main volcanic activity and the beginning of sedimentation occurred