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4 results for “hypsodonty”
Fig. 2. A, B in Hypsodonty in Pleistocene ground sloths
Fig. 2. A, B. Paramylodon harlani (Owen, 1840), early Pleistocene, Hillsborough, Florida, USA. A. Left upper caniniform, UF 87042. B. Left M2, UF 87068. C, D. Glossotherium robustum (Owen, 1842), Pleistocene, General Belgrano, Buenos Aires province, Argentina. C. Left upper caniniform, MHM no catalogue number. D. Left M3, MHM no catalogue number.
Fig. 1. A. MLP 2−3 in Hypsodonty in Pleistocene ground sloths
Fig. 1. A. MLP 2−3, molariform of Megatherium americanum Cuvier, 1796, Pleistocene, Buenos Aires province, Argentina. B. UF 162356, molariform of Eremotherium eomigrans De Iuliis and Cartelle, 1999, Pleistocene, Alachua, Florida, USA. Because of the homodonty of the upper and lower megatheriine molariforms, determining the position of the isolated teeth is not reliable (except for M1, M5, and m5, but these do not have the ridges and grooves so prominent as in the illustrated material); thus, we have not attempted to identify the exact position of these teeth, but only figure them to show their occlusal features and the development of the tooth crown height.
Text-fig. 13. Hypsodonty in different Collimys species. a, b, d, f – M1, labial view; c, e, g – m1, lingual view; a – C. transversus, Steinheim, late Middle Miocene ("MN 7"); b, c – C. longidens, Nebelbergweg, Middle-Late Miocene transition, MN 8/9; d, e – C. primus, Eichkogel, Late Miocene, MN 11; f, g – C. caucasicus sp. nov., Gaverdovsky (f) and Volchaya Balka (g, holotype), Late Miocene, MN 11. a–e – modified after Kälin and Engesser (2001). in Late Miocene (Early Turolian) Vertebrate Faunas And Associated Biotic Record Of The Northern Caucasus: Geology, Taxonomy, Palaeoenvironment, Biochronology
Text-fig. 13. Hypsodonty in different Collimys species. a, b, d, f – M1, labial view; c, e, g – m1, lingual view; a – C. transversus, Steinheim, late Middle Miocene ("MN 7"); b, c – C. longidens, Nebelbergweg, Middle-Late Miocene transition, MN 8/9; d, e – C. primus, Eichkogel, Late Miocene, MN 11; f, g – C. caucasicus sp. nov., Gaverdovsky (f) and Volchaya Balka (g, holotype), Late Miocene, MN 11. a–e – modified after Kälin and Engesser (2001).
Comparison of environmental inference approaches for ecometric analyses: Using hypsodonty to estimate precipitation
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