†Cebupithecia sarmientoi (Pitheciidae)
Cebupithecia sarmientoi ist eine Primatenart innerhalb der Familie Pitheciidae, die ab dem Neogen (Miozän) im Langhium lebte, das vor rund 16 Millionen Jahren begann und bis vor 13,8 Millionen Jahren andauerte.
Fundorte
Die Funddaten, die Systematik sowie die unten folgende Literatursammlung stammen aus der Paleobiology Database, Lizenz
Daten zu den einzelnen Funden von Cebupithecia sarmientoi
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung |
|---|---|---|---|
| UCMP Locality V 4517 | "adjacent to the Villavieja-San Alfonso trail, several meters beyond the house called La Venta, Huila" (coordinate based on Loma La Venta) | Serravallian zwischen 11.61 und 15.97 Millionen Jahren |
La Venta; Royo no. 1999 |
| Kommentar z. Stratigraphie | Lithographie | Museum | |
| "Approximately 8 meters of gray clays overlying concretionary mudstone which rests on conglomerates so conspicuously exposed in the middle of the Villavieja-Cerro Gordo section" | "Found in the [gray] clays" | UCMP |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung |
|---|---|---|---|
| Cebupithecia Cerro Gordo; Monkey Locality; UCMP V-4517 | Fossils recorded from the Monkey locality were found in the clay adjacent to the Villavieja - San Alfonso trail, several hundred yards beyond the house called La Venta, Hulia, Colombia. 4.1 km NE of Villavieja, a few meters north of the Villavieja-San Alfonso trail, 675 m NE of house called La Venta | Serravallian zwischen 11.8 und 13.8 Millionen Jahren |
UCMP V4517 |
| Lithographie | Museum | ||
| Aproximately 25 feet of gray clays overlying concretionary sandstones which rest on the conglomerates so conspicuously exposed in the middle of the Villaviaja - Cerro Gordo section. This unit varies somewhat and in places grades laterally into sandstone, but is predominantely clay. Fossils recorded from the Monkey locality were found in the clay. | UCMP |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
|---|---|---|---|
| Duke Locality 21 | Nearby landmark is Cerro Gordo | Serravallian zwischen 11.8 und 13.8 Millionen Jahren |
La Victoria |
| Kommentar z. Stratigraphie | |||
| this locality lies immediately above cerro gordo sandstone beds Note: Stirton (1953) elevated the term Honda to the Group category. Wellman (1967), included "Grupo Honda" in the Villavieja Formation and La Dorada Formation and makes a good description of the fragments of these formations, which contributes to the definition of the area of origin of the sediments. However, the evolution of diagenetic processes in the rocks studied was not detailed. Finally, Guerrero (1993) established that the Honda Group is comprised of La Victoria Formation to the base and the overlying Villavieja Formation. This collection had formation = La Dorada assigned. La Dorada formation is considered a synonym of the La Victoria formation now (the latter having a Laventan age). |
| Sammlung | Epoche, Alter | Geologie, Formation |
|---|---|---|
| Duke locality 21 | Serravallian zwischen 11.8 und 13.8 Millionen Jahren |
La Victoria |
| Kommentar z. Stratigraphie | ||
| Unit between Cerro Gordo Ss Beds and Chunchullo Ss Beds |
Literatur
R. A. Stirton, D. E. Savage 1950, A new Monkey from the La Venta Miocene of Colombia. Compilación de los estudios geológicos oficiales en Colombia. 8, p. 345 - 356A. H. Miller, D. E. Savage 1953, A fossil hoatzin from the Miocene of Colombia. Auk. 70:4, p. 484 - 489
D. J. Meldrum, J. G. Fleagle, R. F. Kay 1990, Partial humeri of two Miocene Colombian primates. American Journal of Physical Anthropology. 81:3, p. 413 - 422
D. J. Meldrum, R. F. Kay, R. F. Kay 1997, Postcranial skeleton of Laventan Platyrrhines. Vertebrate Paleontology in the Neotropics. The Miocene fauna of La Venta, Colombia. :3, p. 459 - 472