†Altiatlasius koulchii
Altiatlasius koulchii ist eine Primatenart, 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 Altiatlasius koulchii
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
|---|---|---|---|
| Adrar Mgorn 1 | coordinate based on Adrar Mkorn ridge | Thanetian zwischen 56 und 59.2 Millionen Jahren |
Jbel Guersif |
| Kommentar z. Stratigraphie | Lithographie | Museum | Kommentar z. Taxonomie |
| "Shark teeth indicate that the age is Thanetian" (Gingerich, 1990). Lithostratigraphy is from Augé & Rage (2006) and Dragastan & Herbig (2007, Micropaleontology 53(1-2), 1-72). (TL) " [...] a magnetostratigraphic study has suggested an Upper or Uppermost Thanetian age for Adrar Mgorn 1 (Gheerbrant et al., 1998)" (Augé & Rage, 2006). | "hard calcareous matrix" (Gingerich, 1990). According to Tawadros (2012, Geology of North Africa, Taylor & Francis) and Dragastan & Herbig (2007, Micropaleontology 53(1-2), 1-72), the Jbel Guersif Formation consists of at least one shallowing-upward sequence of shallow marine, white to pale rose bioclastic limestones. Augé & Rage (2006) speak of "dolomitic limestones". Thus the original lithology entry >>calcareous "siliciclastic"<< was altered (TL). | MNHN | "Twenty-three mammalian species are represented" (Gingerich, 1990) |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
|---|---|---|---|
| Adrar Mgorn 1 | coordinate based on Adrar Mkorn ridge | Thanetian zwischen 56 und 59.2 Millionen Jahren |
Jbel Guersif |
| Kommentar z. Stratigraphie | Lithographie | Museum | Kommentar z. Taxonomie |
| "Shark teeth indicate that the age is Thanetian" (Gingerich, 1990). Lithostratigraphy is from Augé & Rage (2006) and Dragastan & Herbig (2007, Micropaleontology 53(1-2), 1-72). (TL) " [...] a magnetostratigraphic study has suggested an Upper or Uppermost Thanetian age for Adrar Mgorn 1 (Gheerbrant et al., 1998)" (Augé & Rage, 2006). | "hard calcareous matrix" (Gingerich, 1990). According to Tawadros (2012, Geology of North Africa, Taylor & Francis) and Dragastan & Herbig (2007, Micropaleontology 53(1-2), 1-72), the Jbel Guersif Formation consists of at least one shallowing-upward sequence of shallow marine, white to pale rose bioclastic limestones. Augé & Rage (2006) speak of "dolomitic limestones". Thus the original lithology entry >>calcareous "siliciclastic"<< was altered (TL). | MNHN | "Twenty-three mammalian species are represented" (Gingerich, 1990) |
Literatur
P. D. Gingerich 1990, African dawn for primates. Nature. 346, p. 411E. Gheerbrant, J. Sudre, S. Sen, C. Abrial, B. Marandat, B. Sigé, M. Vianey-Liaud 1998, Nouvelles données sur les mammifères du Thanétien et de l'Yprésien du bassin d'Ouarzazate (Maroc) et leur contexte stratigraphique. Palaeovertebrata. 27:3-4, p. 155 - 202