Fig. 1 in Climate-driven diversity changes of Mediterranean echinoids over the last 6 Ma

Fig. 1. Stratigraphy (A) and location (B) of some echinoid key sites from Italy, showing some of the most significant appearances, disappearances and other occurrences of Mediterranean late Cenozoic echinoids. Lithology and stratigraphy are reconstructed from Borghi and Garilli (2017) and Crippa et al. (2019) for Stirone east; Cau et al. (2015) for Stirone west; Ceregato et al. (2007) for Campore; Capozzi and Picotti (2003) for Castrocaro; Di Bella et al. (2005) for Anzio; Borghi and Garilli (2017) for Sant'Andrea. The nannofossil biozones (CNPL) and the age of Discoaster tamalis last occurrence are after Backman et al. (2012). The foraminifer biozonation (MPL) is according to Lirer et al. (2019).