. Bulletin of the Natural Histort Museum. Geology series. 98 SMITH Fig. 8 Camera lucida drawing of plating: a-c, Camewgalerus cantabricus sp. nov. BMNH EE6132 (holotype); Maastrichtian. coast west of Cabo Mayor (Santander. Cantabria); a, apical disc; b, oral surface; c, supraambital interambulacral plates, d, e, Coenholectypus nachtigali (Krumbeck. 1906), Maastrichtian, coast west of Cabo Mayor (Santander, Cantabria); d, BMNH EE6129; supraambital interambulacral plates; e, BMNH EE6131, oral view. Scale bars = 1 mm. with ambitus set low down. Periproct longitudinal, just subambital


. Bulletin of the Natural Histort Museum. Geology series. 98 SMITH Fig. 8 Camera lucida drawing of plating: a-c, Camewgalerus cantabricus sp. nov. BMNH EE6132 (holotype); Maastrichtian. coast west of Cabo Mayor (Santander. Cantabria); a, apical disc; b, oral surface; c, supraambital interambulacral plates, d, e, Coenholectypus nachtigali (Krumbeck. 1906), Maastrichtian, coast west of Cabo Mayor (Santander, Cantabria); d, BMNH EE6129; supraambital interambulacral plates; e, BMNH EE6131, oral view. Scale bars = 1 mm. with ambitus set low down. Periproct longitudinal, just subambital and clearly visible in posterior view. Oral surface pulvinate with small subcircular central peristome. Ambulacral pore-pairs forming broad bands over much of the oral surface. Material STUDIED. BMNHEE4351-5,EE6131-33,MGB 37471, 37511,37542,37557. Occurrence. Maastrichtian, horizons 4, 5, 6 and 7/8, Santander. Lower Maastrichtian of the Homes Morts Member at Sapeira, Santa Engracia and Salas de Pallars, Tremp Basin (Gallemi, 1992). Maastrichtian, top of bed 1, Olazagutia Pass, Navarra. Maastrichtian of Mas de Santa Maria, near Ibi, Alicante province (Gallemi et al. 1995). The type comes from the Maastrichtian of Saint Proupiary, near Auzas, Haute-Garonne, France and it has also been recorded from numerous other localities in Haute-Garonne, including Ausseing Massif, Picou near Roquefort, Mont Saunes, Beauchalot, Saint- Martory and Salies (Lambert, 1907). Remarks. Differs from C. magnificus (d'Orbigny) in having a longitudinal rather than transverse periproct, and from C. douvillei (Cotteau & Gauthier) in having a small, almost circular peristome as opposed to the distinctly oblique and large peristome of that species. This species becomes most common between levels 6 and 8 in the Maastrichtian of Santander. i PLATE 3 Figs 1,2 Conulus gigas (Cotteau, 1856), BMNH EE4354, Maastrichtian of Santander, Cantabria. Oral and lateral views, x 1. Figs 3-5 Clypeolampas ovatus (Lamarck,


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