†Pseudoloris crusafonti (Omomyidae)
Pseudoloris crusafonti ist eine Primatenart innerhalb der Familie Omomyidae, die ab dem Paläogen (Eozän) im Bartonium lebte, das vor rund 41,3 Millionen Jahren begann und bis vor 38 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 Pseudoloris crusafonti
| Sammlung | Epoche, Alter | Geologie, Formation | ||
|---|---|---|---|---|
| Grisolles | Bartonian zwischen 38 und 41.3 Millionen Jahren |
Calcaire de Saint-Ouen | ||
| Kommentar z. Stratigraphie | ||||
| European Mammal Zone ('Niveau Repère') based on rodents. A stratified locality. The fossiliferous level is 3 to 4 cm thick and is located 4.5 m above a level of green marls (Mortefontaine Formation); about the same level than Robiac | ||||
| U.a. am Fundort ausgegraben: | Necrolemur zitteli | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | |
|---|---|---|---|---|
| Creechbarrow Hill | on Creechbarrow Hill, Nat. Grid System 922 824 | Bartonian zwischen 38 und 41.3 Millionen Jahren |
Creechbarrow Limestone | |
| Kommentar z. Stratigraphie | Lithographie | |||
| This is the only known outcrop of the Creechbarrow Limestone, ranges in thickness from 0-16 m and lies above unnamed sands and clays "Chreechbarrow Hill is dated to mammal Paleogene Reference Level MP16 and the lautricense-siderolithicum Zone, by comparison with continental European faunas" (Benton et al., 2005) | in general it's a buff marl containing variable sized limestone clasts, the limestone (sensu stricto) is a cream coloured, mottled with buff, soft to hard, massive micritic limestone with drusy sparite, scattered angular to subangular quartz grains up to 1mm in diameter, oncoliths often containing [molluscs and vertebrate remains]. Hard limestone in recent excavations was mainly encountered in the basal rubbly soid layer (A). buff marl: a buff calcareous silty clay with abundant angular to subangular quartz grains up to 1 m m in diameter and containing limestone clasts. It also contains oncoliths often containing [mollusc] and vertebrate remains and derived silicified Cretacous bryozoans. | |||
| U.a. am Fundort ausgegraben: | Vectipithex quaylei | |||
Literatur
P. Louis, J. Sudre 1975, Nouvelles donnees sur les primates de l'Eocene superieur europeen. Colloque international CNRS, Problemes actuels de paleontologie - evolution des vertebres. :218, p. 805 - 828J. J. Hooker, J. Sudre 1977, The Creechbarrow Limestone - its biota and correlation. Tertiary Research. 1:4, p. 139 - 145