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FIG. 4. — Crocodylidae indet. 1 in Crocodile remains from the Burdigalian (lower Miocene) of Gebel Zelten (Libya)

FIG. 4. — Crocodylidae indet. 1 (MNHN.LBE.311), skull table and braincase in ventral view. Abbreviations: bo, basioccipital; boc, basioccipital condyle; bs, basisphenoid; f, frontal; ls, laterosphenoid; m.e.f, median eustachian foramen; po, postorbital; pob, postorbital bar; q, quadrate; stf, supratemporal fenestra. Scale bar: 2 cm.

FIG. 3. — Crocodylidae indet. 1 in Crocodile remains from the Burdigalian (lower Miocene) of Gebel Zelten (Libya)

FIG. 3. — Crocodylidae indet. 1 (MNHN.LBE.311), skull table in dorsal view. Abbreviations: boc, basioccipital condyle; exoc, exoccipital; f, frontal; p, parietal; po, postorbital; pop, paraoccipital process; q, quadrate; soc, supraoccipital; sq, squamosal; sqp, squamosal projection; stf, supratemporal fenestra. Scale bar: 2 cm.

FIG. 2 in Crocodile remains from the Burdigalian (lower Miocene) of Gebel Zelten (Libya)

FIG. 2. — Tomistoma lusitanica Antunes, 1967 (MNHN.LBE.300), anterior portion of the snout; A, dorsal view; B, ventral view. Abbreviations: e.n, external naris; n, nasals; mx, maxillae; pmx, premaxillae. Scale bars: 2 cm.

FIG. 7. — Crocodylidae indet. 2 in Crocodile remains from the Burdigalian (lower Miocene) of Gebel Zelten (Libya)

FIG. 7. — Crocodylidae indet. 2; A, fragmentary skull table in dorsal view (MNHN.LBE.306); B, anterior portion of right dentary in dorsal view (MNHN.LBE.307). Abbreviations: f, frontal; p, parietal; po, postorbital; pop, paraoccipital process; q, quadrate; qj, quadratojugal; soc, supraoccipital process; sq, squamosal; sqp, squamosal projection; stf, supratemporal fenestra. Scale bars: 2 cm.

FIG. 6. — Crocodylidae indet. 1 in Crocodile remains from the Burdigalian (lower Miocene) of Gebel Zelten (Libya)

FIG. 6. — Crocodylidae indet. 1 (MNHN.LBE.311), skull table and braincase in right lateral view. Abbreviations: bo, basioccipital; boc, basioccipital condyle; bs, basisphenoid; e.a.m, external auditory meatus; f, frontal; f.o, foramen ovale; ls, laterosphenoid; po, postorbital; pob, postorbital bar; q, quadrate; sq, squamosal. Scale bar: 2 cm.

FIG. 5 in Fossil sea turtles (Chelonii, Dermochelyidae and Cheloniidae) from the Miocene of Pietra Leccese (late Burdigalian-early Messinian), Southern Italy

FIG. 5. — Trachyaspis lardyi Meyer, 1843 (MAUL 988/1 detail), photograph and interpretative drawing. Note the hexagonal, narrow and elongated shape of the neural plate, and the proximal portion of the adjoining left pleural plate. Keels are represented by hard lines, and sectioned surface in grey. Abbreviations: n, neural; pl, pleural. Scale bar: 10 mm.

FIG. 4 in Fossil sea turtles (Chelonii, Dermochelyidae and Cheloniidae) from the Miocene of Pietra Leccese (late Burdigalian-early Messinian), Southern Italy

FIG. 4. — Trachyaspis lardyi Meyer, 1843 (MAUL 992/1), photograph and interpretative drawing of a large portion of a cheloniid carapace. Note the presence of three parallel ridges, the scute sulci pattern (where visible) and the sculptured surface. Abbreviations: bj, bone junction (dotted line); fs, fragmented surface (grey); r, ridge (continuous line); ss, scute sulci (dashed line). Scale bar: 50 mm.

FIG. 1. — A in Fossil sea turtles (Chelonii, Dermochelyidae and Cheloniidae) from the Miocene of Pietra Leccese (late Burdigalian-early Messinian), Southern Italy

FIG. 1. — A, Testudo varicosa Costa, 1851 (MP-CMSNN 8448), type specimen, original drawing by Costa (1864) and photograph of the slab as preserved nowadays. Note that Costa did not follow the original position of the specimen in the slab. T. varicosa is here considered a junior synonym of Trachyaspis lardyi Meyer, 1843; B, Euclastes melii Misuri, 1910 remains, photo and reconstruction (modified from Misuri 1910). Note that a large portion of the reconstructed carapace is not represented in the fossil. Scale bars: A, 40 mm; B, 50 mm.

FIG. 2 in Fossil sea turtles (Chelonii, Dermochelyidae and Cheloniidae) from the Miocene of Pietra Leccese (late Burdigalian-early Messinian), Southern Italy

FIG. 2. — Psephophorus polygonus Meyer, 1846 (MAUL 1008/1), photographs and interpretative drawings: A, dorsal view of the slab and the detail of some elongated ossicles. At left, note the two longitudinal and almost parallel ridges, indicated by hard lines, and that more than five ossicles are present between two ridges; at right, some elongated ossicles that form the ridge are shown; B, transversal section of a ridge: the visceral surface is flat and the dorsal one is convex, the ridge sides are low tilted and the apex is rounded. Abbreviations: sec, section; sed, sediment. Grey areas indicate fragmented surfaces. Scale bars: 50 mm.

FIG. 3 in Fossil sea turtles (Chelonii, Dermochelyidae and Cheloniidae) from the Miocene of Pietra Leccese (late Burdigalian-early Messinian), Southern Italy

FIG. 3. — Psephophorus polygonus Meyer, 1846 (MAUL 990/1a-l), geometric relationships among the slabs belonging to a single specimen. At present, this is the largest known portion of a P. polygonus carapace so far reported in the literature. The ridges are indicated by hard lines. Scale bar: 200 mm.

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Text-fig. 1. Sampling areas in Çankırı province: the village of Sakarcaören near to the town of Orta (green circle) in the east of GVP, and the other sites (yellow circles), volcanic centers (red circles) and the border of GVP. The sites marked as yellow circles: ELM, Elmali village; SOG, Soguksu National Park; BUG, Bugralar village; INO, Inozu Valley South Side; INL, Inozu Valley North Side; KAR, Karasar village; MEN, Menceler Plateau; KIR, Kiraluc Site near Nuhhoca village; AGU, Asagiguney village; KUZ, Kuzca village (Bayam et al. 2018); PEL, Pelitcik village (Akkemik et al. 2009); GUD, Gudul (Akkemik et al. 2017); HOC, Hoçaş village and KOZ, Kozyaka village (Akkemik et al. 2016). The sites located in the western part (INO, INL, KAR, MEN, KIR, AGU, KUZ, HOC and KUZ) are from early – middle Burdigalian and Hancili Formation (Altun et al. 2002, Akbaş et al. 2002). The sites in the central part (GUD, BUG, ELM, PEL and SOG) are from middle – late Burdigalian, Pazar Formation (Kazancı 2012, Sen et al. 2017), and finally the fossil site in the east part of GVP is the late Miocene, Hüyükköy Formation (Sengüler 2007). in The First Glyptostroboxylon And Taxodioxylon Descriptions From The Late Miocene Of Turkey And Palaeoclimatological Evaluation

Text-fig. 1. Sampling areas in Çankırı province: the village of Sakarcaören near to the town of Orta (green circle) in the east of GVP, and the other sites (yellow circles), volcanic centers (red circles) and the border of GVP. The sites marked as yellow circles: ELM, Elmali village; SOG, Soguksu National Park; BUG, Bugralar village; INO, Inozu Valley South Side; INL, Inozu Valley North Side; KAR, Karasar village; MEN, Menceler Plateau; KIR, Kiraluc Site near Nuhhoca village; AGU, Asagiguney village; KUZ, Kuzca village (Bayam et al. 2018); PEL, Pelitcik village (Akkemik et al. 2009); GUD, Gudul (Akkemik et al. 2017); HOC, Hoçaş village and KOZ, Kozyaka village (Akkemik et al. 2016). The sites located in the western part (INO, INL, KAR, MEN, KIR, AGU, KUZ, HOC and KUZ) are from early – middle Burdigalian and Hancili Formation (Altun et al. 2002, Akbaş et al. 2002). The sites in the central part (GUD, BUG, ELM, PEL and SOG) are from middle – late Burdigalian, Pazar Formation (Kazancı 2012, Sen et al. 2017), and finally the fossil site in the east part of GVP is the late Miocene, Hüyükköy Formation (Sengüler 2007).

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FIG. 1 in Crocodile remains from the Burdigalian (lower Miocene) of Gebel Zelten (Libya)

FIG. 1. — Map of Africa showing location of the Gebel Zelten locality (*) in Northern Libya.