Paradolichopithecus arvernensis (Cercopithecidae)



Paradolichopithecus arvernensis ist eine Primatenart innerhalb der Familie Cercopithecidae, die ab dem Pliozän lebte, das vor rund 5,333 Millionen Jahren begann und bis vor vor 2,588 Millionen Jahren andauerte.

Fundorte

Systematik

Daten zu den einzelnen Funden von Paradolichopithecus arvernensis
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Valea Graunceanului, Tetoiu 1 lower faunal horizon Between Tetoiu (on which co-ordinates are based) and Irimesti (9km apart), in the Oltet river valley, in a valley called Valea Graunceanului (also called Valea Tetoi), on the western slope of a hill named Dealul Viilor. 2.5km north of La Pietris. Piacenzian
zwischen 2.59 und 3.6 Millionen Jahren
Valea Tetoi, Graunceanu
Kommentar z. Stratigraphie
Late Pliocene, just before the Olduvai event (based on palaeomagnetism). Faunal comparison indicates that the Lower Faunal Horizon (Tetoiu 1) correlates with the upper part of the Khaprov faunal complex, upper MN17 (St Vallier Zone), probably equivalent to the Tiglian warm stage. It is suggested that Valea Graunceanului correlates with zone 5C of the Tiglian, and is a warmer pahse than that represnted by La Pietris. Site is approximately 88m below the top of the section, at the base of a silty sand, about 1.5m thick.
Sammlung Kommentar zum Fundort Epoche, Alter
Slivnitsa In a hilly carst area ('Kozyaka') within 30km NW of Sofia, close to the western part of the town of Slivnitsa. Co-ordinates based on Slivnitsa. -
zwischen 0.01 und 5.33 Millionen Jahren
Kommentar z. Stratigraphie Kommentar z. Taxonomie
Similar date to Seneze, latest Pliocene rather than early Pleistocene, MNQ 18. Seven members of the Caprinae are present.
Sammlung Kommentar zum Fundort Epoche, Alter Kommentar zur Sammlung
Vatera F-Site This is the richest site of the Formation . It has been named after the discovery of Funny fragments of bones at the initial stages of the research. The site was systematically excavated for 4 continues seasons (1997-2000), yielding 550 fossils belonging to 15 different species of mammals, one bird and one reptile (the giant tortoise). Based on the fauna composition the site has been attributed to the MN 17 (about 2 Ma) (from Lyras and van der Geer, 2007) Calabrian
zwischen 0.78 und 2.59 Millionen Jahren
Vatera
Sammlung Epoche, Alter Kommentar zur Sammlung
Dafnero 3 Piacenzian
zwischen 2.59 und 3.6 Millionen Jahren
DFN3
Lithographie
DFN and DFN3 are part of the same fossiliferous layer of ochre silty sands exposed on the opposite slopes of an erosional crest. Stratigraphically, the fossil-yielding horizon is found ~0.5 m below a 1e2 m thick, dense conglomerate in a 20 m high section. The fossiliferous deposits belong to the basal part of a 60 m thick terrestrial lithostratigraphic unit of fluviatile origin that overlies unconformably molassic palustrial sediments ascribed to the Tsotylion Formation of the Mesohellenic Trench (Fountoulis et al., 2001 and references therein)

Literatur

C. Radulesco, P. Samson 1990, The Plio-Pleistocene mammalian succession of the Oltet Valley, Dacic Basin, Romania. Quatarpalaontologie. 8, p. 225 - 232
N. Spassov, P. Samson 1998, A new Late Villafranchian locality of vertebrate fauna - Slivnitsa (Bulgaria) and the carnivore dispersal events in Europe on the Pliocene/Pleistocene boundary. Historia naturalis bulgarica. 9, p. 101 - 113
J. de Vos, J. van der Made, A. Athanassiou, G. Lyras, P. Y. Sondaar, M. D. Dermitzakis 2002, Preliminary report on the late Pliocene fauna from Vatera (Lesvos, Greece). Annales Geologiques des Pays Helleniques. 39, p. 37 - 70
D. S. Kostopoulos, F. Guy, Z. Kynigopoulou, G. D. Koufos, X. Valentin, G. Merceron 2018, A 2Ma old baboon-like monkey from Northern Greece and new evidence to support the Paradolichopithecus e Procynocephalus synonymy (Primates: Cercopithecidae). Journal of Human Evolution. , p. 1 - 15, DOI: 10.1016/j.jhevol.2018.02.012