Fig. 17 in Taxonomy and palaeobiogeography of the Cenozoic Euro-Mediterranean rissoid gastropod Galeodinopsis and its relationship with close genera

Fig. 17. Distribution of European species of Galeodinopsis Sacco, 1895, based on material studied and that from the literature. Dark and light grey vertical segments roughly indicate the Late Paleogene Paris Basin and the southern part of the North Sea Basins, respectively; white segments represent the Mainzer Basin–Upper Rhine Graben (from Rögl 1999 and Rasser et al. 2008, modified). The horizontal black and dark grey segments approximate the Iberian Late Neogene and Aquitaine Late Oligocene–Early Miocene Atlantic domains, respectively; orange dots indicate the southernmost part of the Thule land-bridge joining England with continental Europe (from Vincent 1990, adapted and modified); green line indicates a hypothetical reconstruction of the Late Paleogene shoreline in the North Sea and Paris Basins, allowing communication (smaller red arrow) between the two areas from the Early Oligocene. The red line indicates part of the Central European shoreline (according to Rögl 1999) during very Early Neogene time, showing northwards shifting of the southern coasts of the North Sea Basin. The larger red arrow indicates the hypothesized connection to the Aquitaine Basin. 1, Upper Eocene/very early Oligocene, Latdorf Koenen 1867; Tembrock, 1964) and Magderburg (Müller 2011); 2, Oligocene, Rupelian, Söllingen (Speyer 1864; Koenen 1867); 3, Oligocene, Chattian, Sternberg (Wiechmann 1871; Anderson 1960); 4, Oligocene, Rupelian, Amsdorf (Gründel 1997); 5, Oligocene, Chattian, Freden (Anderson 1960); 6, Oligocene, Chattian, Ahnetal (Anderson 1960); 7, Oligocene, Chattian, Glimmerode; 8, Middle Oligocene, Magonza basin at Waldböckelheim (Sandberger 1863; Anderson 1960); 9, Oligocene, Chattian, Doberg (Wiechmann 1871); 10, Oligocene, Chattian, Krefeld (Wiechmann 1871), Rumeln (Anderson 1960), and Moers (Janssen 1978a); 11, Oligocene, early Rupelian, Klein-Spauwen (Nyst 1845); 12, Oligocene, Rupelian, Paris Basin (Deshayes 1864); 13, Middle Pliocene, Mondego (Landau et al. 2004); 14, Pliocene, Estepona (Landau et al. 2004); 15, Pliocene, Sidi Moussa (Cossmann 1921); 16, Pliocene, Altavilla and Trappeto (Garilli 2008); 17, Lower Pliocene, Magliano Sabina (Garilli 2008); 18, Lower Pliocene, Siena (Chirli 2006); 19, Mio-Pliocene, Modena, Parma, and Piacenza (Coppi 1876; Garilli 2008); 20, Lower to Upper Pliocene, Savona and Asti (Garilli, 2008).