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10 results for “Stephanocemas”
Figure 10 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 10. Species ranges, phyletic relationship, and zoogeographical positions of the Paradicrocerus–Stephanocemas clade. Most of the species ranges are approximate. Phyletic relationship is based on one of the shortest trees in our cladistic analysis, and some indeterminate taxa not included in the cladogram are inserted here based on our estimates of their relationships. The antlers are scaled to their approximate relative size, and dashed lines are mostly our own reconstructions of missing tines.
Figure 9 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 9. Strict consensus of four shortest trees (tree length = 12) of the Paradicrocerus–Stephanocemas clade found by the branch and bound option of the PAUP program on a ten taxa ¥ nine characters data matrix (Table 1).
Figure 8. IVPP V15726 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 8. IVPP V15726, Stephanocemas sp. from IVPP locality CD0406. A, dorsal, and B, ventral views of antler fragment. Scale is for both views.
Figure 6. IVPP V15724 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 6. IVPP V15724, referred specimen of Stephanocemas palmatus sp. nov. A, dorsal, B, ventral, and C, medial views of posterior palm portion of a juvenile antler.
Figure 7. IVPP V15725 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 7. IVPP V15725, Stephanocemas sp. from IVPP locality CD9818. A, stereophoto of dorsal view, B, lateral view, and C, ventral view of partial antler.
Figure 5. IVPP V15723 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 5. IVPP V15723, referred specimen of Stephanocemas palmatus sp. nov. A, dorsal, and B, ventral views of palm portion of antler.
Figure 4. IVPP V15722 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 4. IVPP V15722, left antler without pedicel, holotype of Stephanocemas palmatus sp. nov. from Qaidam Basin, northern Tibetan Plateau. A, medial, and B, ventral views. Left is posterior and right is anterior.
Figure 3 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 3. Stereophoto of dorsal view of IVPP V15722, left antler without pedicel, holotype of Stephanocemas palmatus sp. nov. from Qaidam Basin, northern Tibetan Plateau. Top is posterior and bottom is anterior.
Figure 2 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 2. Satellite image of the Barun Yawula anticline, with key fossil localities and their relative stratigraphical positions indicated. The east–west trending fold is asymmetrical with the south limb dipping more steeply than the north limb. A prominent resistant bed (a dark–light band combination, indicated by black dashed lines) within the rusty green sandstones layers helps to trace stratigraphical relationships between localities in eastern and western ends of the anticline, although multiple faults (with offsets ranging from 50 to 500 m), particularly those in the eastern end, complicate correlations. White lines are the measured section.
Figure 1 in A new species of crown-antlered deer Stephanocemas (Artiodactyla, Cervidae) from the middle Miocene of Qaidam Basin, northern Tibetan Plateau, China, and a preliminary evaluation of its phylogeny
Figure 1. Map of Qaidam Basin showing surrounding mountains and major vertebrate fossil localities.
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