Typhlomys hipparionum QIU , 1989
publication ID |
https://doi.org/ 10.2478/if-2019-0024 |
persistent identifier |
https://treatment.plazi.org/id/D035C10B-FF9A-FF8E-FC41-FA8907355343 |
treatment provided by |
Diego |
scientific name |
Typhlomys hipparionum QIU , 1989 |
status |
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Typhlomys hipparionum QIU, 1989
Text-figs 6 View Text-fig , 7 View Text-fig
H o l o t y p e. Right M 1 (IVPP V 8820).
T y p e l o c a l i t y. Shihuiba, Lufeng, Yunnan Province,
China.
R e f e r r e d m a t e r i a l. Yuanmou: 1 M 2, 1 M 3, 1 M 3 ( IVPP V 25885.1 – 3 View Materials ) from Loc. 9904; 1 M 1 ( IVPP V 25885.4 ) from Loc. 9905; 3 M 1, 2 M 2, 2 M 3, 4 M 1, 4 M 2, 2 M 3 ( IVPP V 25885.5 – 21 View Materials ) from Loc. 9906 .
M e a s u r e m e n t s. M 1: 1.75–1.90 × 1.15–1.30 mm; M 2: 1.60–1.65 × 1.00– 1.10 mm; M 3: 1.15–1.25 × 0.90–1.00 mm; M 1: 1.90–2.10 × 1.00– 1.10 mm; M 2: 1.50–1.55 × 1.05– 1.10 mm; M 3: 1.20–1.35 × 0.88–1.00 mm (length × width).
D e s c r i p t i o n. Typhlomys hipparionum from Leilao is larger than T. aff. T. primitivus in size, but closely matches in morphology and dimensions T. hipparionum from Shihuiba of Lufeng ( Text-fig. 6 View Text-fig ), the type locality of this species. However, minor differences between the two forms can be observed, which should not be overemphasized in view of the rather limited amount of material from the two sites.
All 4 M 1 s from Yuanmou are relatively wide and short in comparison with the holotype. Syncline Ia is slightly smaller than or equal to syncline IV, rather than slightly larger than syncline IV, as in the holotype. All 3 M 2 s show distinctly and laterally closed synclines Ia and IV, and continuous endoloph and ectoloph in this stage of wear. All 3 M 3 s have a distinct mesoloph and show a smaller syncline Ia at the anterobuccal corner of the tooth and a longer syncline IV at the posterobuccal corner .
The M 1 has a continuous endolophid, even in the fresh specimens. As in Typhlomys hipparionum from Lufeng and other species of the genus, the mesial angle of diagonal ridge/synclines to the longitudinal axis gradually increases toward the back. In 1 of 2 identifiable M 1 s, syncline Ia is long and narrow, and the other is short and separated by a crest. All 4 M 2 s have small and shallow synclines Ia and IV. All 3 M 3 s show discernable synclines Ia, but no hypolophid and synclines IV.
R |
Departamento de Geologia, Universidad de Chile |
IVPP |
Institute of Vertebrate Paleontology and Paleoanthropology |
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