Miocaperea pulchra, Bisconti, 2012
publication ID |
https://doi.org/ 10.1111/j.1096-3642.2012.00862.x |
DOI |
https://doi.org/10.5281/zenodo.5480048 |
persistent identifier |
https://treatment.plazi.org/id/A41CEE52-D764-FFD0-39A6-FF2DFA73FB78 |
treatment provided by |
Marcus |
scientific name |
Miocaperea pulchra |
status |
sp. nov. |
MIOCAPEREA PULCHRA SP. NOV.
Holotype. SMNS 46978 About SMNS of the Palaeontological Collection. The specimen consists of a skull subdivided into two parts: one including the rostrum and the other including the neurocranium. The tympanic bullae are missing.
Type locality. Aguada de Lomas (Sacaco area, Arequipa Department, Peru) is a well-known fossil-bearing site located around 550 km south-east of Lima ( Fig. 1 View Figure 1 ) in the Pisco Formation ( De Muizon & Bellon, 1981; De Muizon & DeVries, 1985). The locality is close to the southern coast of Peru and its height is around 250– 300 m a.s.l. The approximate geographic co-ordinates for the locality are: 15°5′S, 74°8′W.
Formation and age. Pisco Formation. The Pisco Formation outcrop at Aguada de Lomas has been extensively studied ( De Muizon & Bellon, 1981; De Muizon & DeVries, 1985; De Muizon et al., 2003) because this locality yielded several well-preserved marine vertebrate fossils, including whales and aquatic sloths ( De Muizon, 1988; Pilleri, 1989; De Muizon et al., 2003). Mollusc and vertebrate biostratigraphies together with radioisotopic dating constrain the age of the sediments to late Tortonian (Late Miocene), 7–8 Mya ( De Muizon & Bellon, 1981; De Muizon & DeVries, 1985).
Diagnosis. As for genus.
Etymology. Pulchra, Latin, beautiful, referring to the exquisite condition of preservation of the type specimen.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.