FIG. 1 in A revision of the late early Eocene mammal faunas from Mas de Gimel and Naples (Montpellier, Southern France) and the description of a new theridomorph rodent

FIG. 1. — Geographic (A) and geological map (B) showing the location of Mas de Gimel, Naples, and Naples 2 (Montpellier, Herault). Numbers: 1, Callovian; 2, lower Oxfordian; 3, upper Oxfordian; 4, lower Kimmeridgian; 5, Maastrichtian; 6, Paleocene ["Vitrollian"]; 7, late Ypresian; 8, Ypresian/Lutetian; 9, Oligocene; 10, Miocene; 11, Pliocene; 12, Holocene. Actual view (C) and schematic diagram in 1968 (D, modified from Cappetta et al. 1968) of Mas de Gimel outcrop, showing that fossiliferous deposits are now inaccessible (under the road level); Numbers: 1, lower Kimmeridgian; 2, late Ypresian brecciated limestone; 3, late Ypresian brownish marl; 4, late Ypresian/early Lutetian lacustrine limestone. View of Naples and Naples 2 localities in 1988 during urban development works (E) and detailed view of Naples 2 fossiliferous level, showing two mandibles of Lophiodon Cuvier, 1822 during excavations (F).