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Fig. 1 in A Possible Heptaxodontine and Other Caviidan Rodents from the Quaternary of Jamaica

Fig. 1. Localities of specimens described in text: Wallingford Roadside Cave (holotype of Alterodon major), Sheep Pen (caviidan proximal femur), and Drum Cave (holotype of Xaymaca fulvopulvis). MacPhee (1984) provided detailed descriptions of Wallingford Roadside Cave and Sheep Pen. Survey map of Drum Cave (after Fincham, 1997) shows location of pit #2 in Brown Dust Passage, where type jaw of Xaymaca was recovered.

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FIGURE 5. Chiropteran mandibles. A. Mormoops blainvillei, B. Pteronotus macleayii, C. Pteronotus parnellii, D. Pteronotus quadridens, E. Brachyphylla nana, F. Erophylla bombifrons, G. Monophyllus redmani, H in Quaternary Bat Diversity in the Dominican Republic

FIGURE 5. Chiropteran mandibles. A. Mormoops blainvillei, B. Pteronotus macleayii, C. Pteronotus parnellii, D. Pteronotus quadridens, E. Brachyphylla nana, F. Erophylla bombifrons, G. Monophyllus redmani, H. Phyllonycteris poeyi. Scale bar = 5 mm.

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FIGURE 6. Chiropteran humeri. A in Quaternary Bat Diversity in the Dominican Republic

FIGURE 6. Chiropteran humeri. A. Mormoops blainvillei (extant, ROM 89973), B. Mormoops megalophylla (extant, AMNH 25589), C. †Mormoops magna, D. †Mormoops magna (mirror image), E. Pteronotus macleayii (mirror image), F. Brachyphylla nana (mirror image), G. Erophylla bombifrons (mirror image), H. Monophyllus redmani (mirror image), I. Phyllonycteris poeyi. Scale bar = 10 mm.

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FIGURE 4 in Quaternary Bat Diversity in the Dominican Republic

FIGURE 4. Phyllostomidae skulls: dorsal, lateral, and ventral views. A. Brachyphylla nana, B. Erophylla bombifrons, C. Monophyllus redmani, D. Phyllonycteris poeyi. Scale bar = 5 mm.

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FIGURE 3 in Quaternary Bat Diversity in the Dominican Republic

FIGURE 3. Mormoopidae skulls: dorsal, lateral, and ventral views. A. Mormoops blainvillei, B. Pteronotus macleayii, C. Pteronotus parnellii, D. Pteronotus quadridens. Scale bar = 5 mm.

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FIGURE 1 in Quaternary Bat Diversity in the Dominican Republic

FIGURE 1. Flooded floor of Oleg's Bat Cave in eastern Dominican Republic, where numerous bat cranial and postcranial remains can be observed. Photograph courtesy of the Dominican Republic Speleological Society and Phillip Lehman.

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FIGURE 2 in Quaternary Bat Diversity in the Dominican Republic

FIGURE 2. Map showing the localities where fossil bats have been recorded in Hispaniola. Circles indicate localities reported by other studies. Squares indicate localities presented by this study. Haiti: (1) Diquini, (2) Gonâve Island, (3) Port-de-Paix, (4) Saint-Michel-de-l'Atalaye, and (5) La Selle. Dominican Republic: (6) Cueva de Lily, (7) Oleg's Bat Cave, (8) Cerro de San Francisco, (9) Constanza, and (10) San Gabriel.

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FIG. 14. — A in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 14. — A, the two first axes of a PCA performed on the harmonics of Fourier for the ventral view; B, the same for the apical view; C, D, location of the the populations means in the canonical space corresponding to the amplitudes of the harmonics of Fourier for the apical view; C, the two first canonical axes CA1 versus CA2; D, canonical axes CA1 versus CA3; green triangle, Moroccan Atlantic; yellow triangle, Cap Rhir; green square, Oualidia (O. brevirobusta). Red group, Mediterranean forms (Ocenebra erinaceus (Linnaeus, 1758)); blue group, North Atlantic forms (O. erinaceus); green group, Moroccan Atlantic forms (O. brevirobusta Houart, 2000), black square (Ocinebrellus inornatus (Récluz, 1851)). Abbreviations: P, Pleistocene; Pl, Pliocene.

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FIG. 15. — A in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 15. — A, average Fourier power spectrum for the apical view, 99.95% of the power is described by the first nine harmonics, represented by the arrow; B, same for the ventral view, 99.95% of the power is described by the first 12 harmonics, represented by the arrow.

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FIG. 11 in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 11. — Majority rule consensus tree obtained by the comput- er program Winclada99 (Lenght: 100, CI: 0.48, RI: 0.67). Abbreviations: H, Holocene; Md, Middle Age; P, Pleistocene; Pl, Pliocene; R, Recent; s.f., subfossil; O., Ocenebra.

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FIG. 10 in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 10. — Strict consensus tree obtained by the computer programs Hennig86 (Lenght: 96, CI: 0.38, RI: 0.50) and Winclada99 (Lenght: 96, CI: 0.38, RI: 0.49). Abbreviations: Cl. 1-Cl. 6, number of the clades; in bold, the characters and in parenthesis, the character states; H, Holocene; Md, Middle Age; P, Pleistocene; Pl, Pliocene; R, Recent; s.f., subfossil; O., Ocenebra.

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FIG. 8 in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 8. — Spiral sculpture of recent Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (apertural view); A, B, O. erinaceus (Malaga, Mediterranean Sea, Spain) (MNHN, domaine de collection Botanique et Zoologie); C, D, O. brevirobusta (Casablanca, Atlantic, Morocco) (MNHN R11448 et R11449; Lecointre coll.). Abbreviations: see p. 267. Scale bars: A, C, 1 mm; B, D, 5 mm.

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FIG. 9 in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 9. — Spiral sculpture of Ocenebra erinaceus (Linnaeus, 1758) (apertural view); A, specimen from Asti (Pliocene, Italy) (MNHN R11447; Vibray coll.); B, specimen from Aigues-Mortes (Recent, Mediterranean Sea, France) (MNHN R63993; Merle coll.); C, specimen from Saint-Brieuc (English Channel, France) (MNHN R11445; Lhomme coll.); D, specimen from Oléron Island (Atlantic, France) (MNHN R11446; Lacour coll.). Abbreviations: see p. 267. Scale bar: 5 mm.

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FIG. 7 in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 7. — Simplistic representation of the ontogeny of the spiral cords of Ocenebra brevirobusta Houart, 2000 (population from Casablanca, Moroccan Atlantic). Abbreviations: adis, adapical secondary cord of the siphonal canal; ADP, adapical primary cord of the siphonal canal; ads, adapical secondary cord of the sutural ramp; IP, infrasutural primary cord; P1, shoulder cord; P2-P6, primary cords of the convex part of the whorl (w.); s2, s3, s6, secondary cords of the convex part of the whorl.

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FIG. 13. — A in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 13. — A, intra- and interpopulation analysis using the Procrustes analysis for five specimens of Ocenebra erinaceus (Linnaeus, 1758) from Malaga (red), from Quiberon (blue), and for five specimen from O. brevirobusta Houart, 2000 from Moroccan Atlantic (green); B, morphological comparisons using the Procrustes analysis for the Mediterranean populations of O. erinaceus (Recent: dark red; fossils: light red), the Atlantic Ocean populations of O. erinaceus (Recent: dark blue; fossils: light blue), O. brevirobusta (Recent: dark green; fossil: light green) and for Ocinebrellus inornatus (Récluz, 1851) (black). The populations from Cap Rhir and the Étang de Thau respectively are in yellow and brown colours.

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FIG. 3 in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 3. — Location of 14 landmarks on the ventral view of the Ocenebra Gray, 1847. The correspondence between the primary cords (P1 to P4) and the landmarks is given; photo of O. erinaceus (Linnaeus, 1758), V. Berrou.

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FIG. 2 in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 2. — Linear measures used for the biometric study of Ocenebra Gray, 1847. Abbreviations: BCS, distance between the base and the old siphonal canal; H, total height; HA, height of the aperture excluding the siphonal canal; HLW, height of the last whorl; HP1, height of the P1 cord spine; HS, height of the siphonal canal; TP1, thickness of P1; WA, width of the aperture; WS, width of the shoulder; photo of O. erinaceus (Linnaeus, 1758), courtesy of R. Houart.

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FIG. 1. — A in Quaternary and Recent shells of Ocenebra erinaceus (Linnaeus, 1758) and O. brevirobusta Houart, 2000 (Mollusca, Muricidae, Ocenebrinae): reflections on the intra- and interspecific variations

FIG. 1. — A, geographic range of the genus Ocenebra Gray, 1847 in Europe after Houart (2001a) modified; B, geographic location of the studied samples; photos of Ocenebra, courtesy of R. Houart.

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FIGURE 12 in The Cuban Crocodile (Crocodylus rhombifer) from Late Quaternary Underwater Cave Deposits in the Dominican Republic

FIGURE 12. Map of the West Indies showing the location of Late Quaternary sites containing crocodiles. Fossil samples from Abaco and Grand Bahama in the Bahamas, Cuba, Dominican Republic, and Grand Cayman include skulls or partial skulls that can be confidently identified as the Cuban crocodile (Crocodylus rhombifer). All other records consist of fragmentary or isolated specimens identified as either Crocodylus sp. or Crocodylia indeterminate. Site numbers are as follows (sites 1–22 are from various islands in the Bahamas): Abaco (see Morgan and Albury, 2013, for an enlarged map of Abaco showing the location of these fossil sites): 1. Sawmill Sink; 2. Dan's Cave; 3. Ralph's Cave; 4. Nancy's Cave; 5. Lost Reel Cave. 6. Gilpin Point. Grand Bahama: 7. Bell Channel; 8. Anaconda Pond; 9. Mermaid's Lair. Eleuthera: 10. White Lake Cave; 11. Kelly's Blue Hole (= Bung Hole); 12. Mermaid's Pool; 13. Preacher's Cave. New Providence: 14. Banana Hole. San Salvador: 15. Hanna's Bananas. Great Exuma: 16. Isaac Bay Cave. Rum Cay: 17. Bobby's Cave. Crooked Island: 18. Pittstown Landing; 19. 1702 Cave. Acklins: 20. Rupert's Pond; 21. Delectable Bay. Mayaguana: 22. The Fountain. Grand Cayman (see Morgan and Albury, 2013, for an enlarged map of Grand Cayman showing the location of these fossil sites): 23. Crocodile Canal; 24. Prospect; 25. Chisholm Cow Well; 26. Connally Cow Well; 27. Queen Elizabeth II Botanic Park; 28. Furtherland Farms Cow Well; 29. Crab Cave. Cuba: 30. Cueva Lamas; 31. Las Breas de San Felipe; 32. Ciego Montero; 33. Casimbas de las Llanadas; 34. Caves of Cueiba. Jamaica: 35. Wallingford Roadside Cave; 36. Dairy Cave; 37. Bellevue. Hispaniola (Dominican Republic): 38. Oleg's Bat Cave; 39. Ni-Rahu (= Cueva de Lynn). Puerto Rico: 40. Cueva Salida. Mona Island: 41. Cueva de los Losetas.

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FIGURE 11 in The Cuban Crocodile (Crocodylus rhombifer) from Late Quaternary Underwater Cave Deposits in the Dominican Republic

FIGURE 11. Modern skull of an American crocodile (Crocodylus acutus) from Lago Enriquillo, Dominican Republic (MNHNRD1) in A. dorsal, B. ventral, C. left lateral, and D. posterior views.

opencc-by-4.0Dec 2018View details →

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