†Plesiadapis remensis (Plesiadapidae)
Plesiadapis remensis ist eine Primatenart innerhalb der Familie Plesiadapidae, die ab dem Paläogen (Paläozän) im Thanetium lebte, das vor rund 59,2 Millionen Jahren begann und bis vor 56 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 Plesiadapis remensis
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Cernay | "près de Cernay-lès-Reims" (basis of coordinate) according to Russell 1981 | Thanetian zwischen 56 und 59.2 Millionen Jahren |
Conglomérat de Cernay | Cernay-lès-Reims; carrières Lemoine; Lemoine Quarry |
| Kommentar z. Stratigraphie | Museum | Kommentar z. Taxonomie | ||
| "Thanétien supérieur" | MNHN | remaining fauna not discussed | ||
| U.a. am Fundort ausgegraben: | Sarnacius gingerichi | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Mont Berru | coordinate based on Berru | Thanetian zwischen 56 und 59.2 Millionen Jahren |
Sables de Bracheux | Berru bed 5; Mouras Quarry; Cernay |
| Kommentar z. Stratigraphie | Lithographie | |||
| younger than carrière Lemoine, which is late Thanetian (Russell 1981); NP9, MP6 (Smith and Smith 2003) bed 5 (Hooker and Russell 2012) | conglomerate (Smith and Smith 2003) | |||
| U.a. am Fundort ausgegraben: | Berruvius lasseroni | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung | |
|---|---|---|---|---|
| Lentille de Berru | coordinate based on Berru | Thanetian zwischen 56 und 59.2 Millionen Jahren |
Berru bed 4 | |
| Kommentar z. Stratigraphie | Lithographie | Kommentar z. Taxonomie | ||
| said to correlate with Cernay based on the presence of P. remensis, i.e., P. tricuspidens zone, equivalent to the latest Tiffanian P. simonsi zone; Cernay is now thought to be late Thanetian bed 4 (Hooker and Russell 2012) | shelly lens | underlies the main Berru horizon | ||
| U.a. am Fundort ausgegraben: | Plesiadapis tricuspidens | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Kyson | "Kyson" (apparently modern-day Kingston near Woodbridge, basis of coordinate) | Ypresian zwischen 47.8 und 56 Millionen Jahren |
Suffolk Pebble Beds | Kingston |
| Kommentar z. Stratigraphie | ||||
| assigned to the Platychoerops doubrei zone (Ypresian) based on presence of Pleisadapis aff. remensis | ||||
| U.a. am Fundort ausgegraben: | Cantius eppsi | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Carrière de Pourcy | Carrière de Pourcy, Marne dept, France | Ypresian zwischen 47.8 und 56 Millionen Jahren |
Lignites de Soissonais | Pourcy quarry |
| Kommentar z. Stratigraphie | ||||
| early Sparnacian: "NP10", MP7? (Smith & Smith, 2003) | ||||
| U.a. am Fundort ausgegraben: | Platychoerops daubrei | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Try (Marne) spoil heap | Try (Marne) | Ypresian zwischen 48.6 und 59.2 Millionen Jahren |
Marnes de Dormans | Marnes de Dormans; Platychoerops georgei type |
| Kommentar z. Stratigraphie | Museum | Kommentar z. Taxonomie | ||
| The unit is divisible into an upper part whose base is conglomeratic ("Conglomerat a Coryphodon") and a lower part with concretionary limestone and "Paludina" aspersa. The lower part may be equivalent to the Calcaire de Rilly, which overlies the Sables de Berru and like them belongs to the Sphaerochara edda charophyte zone (Riveline 1984 : 134). Except for the Coryphodon, it is not known in which level or levels the mammals occur, as they were found in quarry spoil (Louis et al. 1983). | MNHN | Some reworking | ||
| U.a. am Fundort ausgegraben: | Plesiadapis tricuspidens | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung | |
|---|---|---|---|---|
| Montchenot West | west of highway D951, Montchenot, near Reims, Marne | Thanetian zwischen 56 und 59.2 Millionen Jahren |
Les Monts-Martin; Mont-Chenot | |
| Kommentar z. Stratigraphie | Museum | Kommentar z. Taxonomie | ||
| Marnes de Montchenot | MNHN | The full taxonomic list for Montchenot West is not provided in Jehle et al. (2012) - only those taxa explicitly stated as coming from this locality (rather than Montchenot East or a combined Montchenot fauna) are listed. Almost all mammal specimens found at Montchenot are isolated teeth, mainly of micromammals. A maxillary with P3–M3 of a louisinine “condylarth” and a few other specimens with associated dental remains demonstrate the potential of these sites for delivering more complete fossil remains. More than 400 dental mammal specimens identifiable at least to genus level are currently available. Only few mammalian postcranial remains have been recovered up to now. | ||
| U.a. am Fundort ausgegraben: | Berruvius lasseroni | |||
Literatur
P. D. Gingerich 1976, Cranial Anatomy and Evolution of Early Tertiary Plesiadapidae (Mammalia, Primates). University of Michigan Papers on Paleontology. 15, p. 1 - 141J. J. Hooker 1994, A new species of Platychoerops (Plesiadapiformes, Mammalia) from the latest Palaeocene of the Paris, London and Belgian Basins. Geobios. 27:3, p. 343 - 352
M. Jehle, M. Godinot, D. Delsate, A. Phélizon, J.-L. Pellouin 2018, Evolution of plesiadapid mammals (Eutheria, Euarchonta, Plesiadapiformes) in Europe across the Paleocene/Eocene boundary: implications for phylogeny, biochronology and scenarios of dispersal. Palaeobiodiversity and Palaeoenvironments. :3, p. 1 - 59, DOI: 10.1007/s12549-018-0331-6