†Vectipithex smithorum (Omomyidae)
Vectipithex smithorum ist eine Primatenart innerhalb der Familie Omomyidae, die ab dem Paläogen (Eozän) im Priabonium lebte, das vor rund 38 Millionen Jahren begann und bis vor 33,9 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 Vectipithex smithorum
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
|---|---|---|---|
| Headon Hill, Bembridge Limestone (marl 15), Isle of Wight | N. E. Headon Hill, west section | Priabonian zwischen 33.9 und 37.2 Millionen Jahren |
Bembridge Limestone |
| Kommentar z. Stratigraphie | Lithographie | ||
| This is Hooker's unit, and the numbered units begin above his "lower Bembridge Limestone" unit | This sequence is primarily marl/mudstone, while the rest of the formation is limestone. This bed is brown shelly marl |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
|---|---|---|---|
| Headon Hill, Bembridge Limestone (marl 18), Isle of Wight | N. E. Headon Hill, west section | Priabonian zwischen 33.9 und 37.2 Millionen Jahren |
Bembridge Limestone |
| Kommentar z. Stratigraphie | Lithographie | ||
| This is Hooker's unit, and the numbered units begin above his "lower Bembridge Limestone" unit | This sequence is primarily marl/mudstone, while the rest of the formation is limestone. This bed is brown shelly marl with organic mud seams. |
| Sammlung | Epoche, Alter | Geologie, Formation | ||
|---|---|---|---|---|
| How Ledge Limestone clay unit, Headon Hill | Priabonian zwischen 33.9 und 38 Millionen Jahren |
Headon Hill | ||
| Lithographie | ||||
| Lignitic clay | ||||
| U.a. am Fundort ausgegraben: | Pseudoloris parvulus | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | |
|---|---|---|---|---|
| Totland Bay, Lower Headon Beds, Isle of Wight | in the cliff at Totland Bay, 150-250 m north of the Pier | Priabonian zwischen 33.9 und 37.2 Millionen Jahren |
Lower Headon Beds | |
| Kommentar z. Stratigraphie | Lithographie | |||
| fauna comes from a grey-green clay with shell-fragments (approx. 8 cm thick) passing upwards into a lignitic clay. These laywers are overlain by a pale brown marly limestone with mollusc shells. | fauna comes from a grey-green clay with shell-fragments (approx. 8 cm thick) passing upwards into a lignitic clay. These laywers are overlain by a pale brown marly limestone with mollusc shells. | |||
| U.a. am Fundort ausgegraben: | Microchoerus erinaceus | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Hordle Cliff Mammal Beds | Hordle Cliff Locality, near Mildford-on-Sea (L/L), Hampshire, England | Priabonian zwischen 33.9 und 37.2 Millionen Jahren |
Headon Hill | Hordwell |
| Kommentar z. Stratigraphie | Kommentar z. Taxonomie | |||
| From the Rodent and Mammal Beds: "Mammal Bed" is considered to be ca. 0.75 my older than than the "Rodent Bed" at this locality. Unit corresponds to European Land Mammal Age Zone MP 17. | Cray, 1973 has a group of taxa that come from either the Mammal or Crocodile Bed including: Peratherium spp A and B, Scraeva woodi (n. gen., n. sp.), Opsiclaenodon major, Adapis magnus, Pseudoloris parvulus, Adelomys ? depereti, A. sp., ?Anchilophus sp., Plagiolophus annectens, P. minor, Cebochoerus sp., Choeropotamus depereti, Dacrytherium ovinum, Catodontherium sp., Haplobunodon lydekkeri, H. sp., Dichodon cervinum, Pseudamphimeryx hantonensis |
| Sammlung | Epoche, Alter | Geologie, Formation |
|---|---|---|
| Headon Hill HH3, Upper Headon Beds, Isle of Wight | Priabonian zwischen 33.9 und 37.2 Millionen Jahren |
Upper Headon Beds |
| Kommentar z. Stratigraphie | Lithographie | |
| This author considers the Upper Headon Beds to be a formation, HH3 refers to a locality within a unit ( 30 cm thick), situated immediately below a lignite band of variable thickness. HH3 is immediately below HH4 (1m) and approx. 14 m above HH2 | overall lithology is claystone with interbedded marl (some silty/sandy) and limestone, fossils come from a chocolate-brown laminated silty marl with many shell-fragments |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
|---|---|---|---|
| Headon Hill, lower Bembridge Limestone, Isle of Wight | Headon Hill, at a quarry that no longer exists, but was colledted by Keeping at the far end of the outcrop | Priabonian zwischen 33.9 und 37.2 Millionen Jahren |
Bembridge Limestone |
| Kommentar z. Stratigraphie | |||
| Hooker call this unit the White Limestone (lower Bembridge Limestone) |