†Macaca florentina (Cercopithecidae)
Macaca florentina 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
Die Funddaten, die Systematik sowie die unten folgende Literatursammlung stammen aus der Paleobiology Database, Lizenz
Daten zu den einzelnen Funden von Macaca florentina
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung |
|---|---|---|---|
| Hohensulzen bei Worms | near Worms | Calabrian zwischen 0.78 und 2.59 Millionen Jahren |
Hohensülzen |
| Kommentar z. Stratigraphie | |||
| Latest Lower Pleistocene, but Feijfar et al (1997) say Biharian (= earliest Middle Pleistocene). |
| Sammlung | Kommentar zum Fundort | Epoche, Alter |
|---|---|---|
| Sandalja 1, bei Pula | Co-ordinates based on the town of Pula, the site is nearby. | Calabrian zwischen 0.78 und 2.59 Millionen Jahren |
| Kommentar z. Stratigraphie | ||
| Early Pleistocene. |
| Sammlung | Kommentar zum Fundort | Epoche, Alter |
|---|---|---|
| Pietrafitta, Perugia | Co-ordinates based on the Nestore River, near Perugia. The site is a lignite mine to the south of Lake Trasimento, in the Tavernelle Basin. | Calabrian zwischen 0.78 und 2.59 Millionen Jahren |
| Kommentar z. Stratigraphie | Kommentar z. Taxonomie | |
| Early Pleistocene, Early Biharian, Farneta faunal unit, Latest Villafranchian. There are three separate lignite mine workings, but the levels are thought to be the roughly the same date based on the macro- and micromammalian remains. | The dominance of arvicolids nay suggest an environment chracaterised locally by open areas with a cold climate. This hypothesis is further strengthened by the presence of the giant deer Megaceroides obscurus. Mimomys savini has been reported previously, but this is thought to have been the mis-identification of a large Mimomys chalinei upper M1. |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | ||
|---|---|---|---|---|
| Senèze, Domeyrat | Co-ordinates based on the village of Senèze | - zwischen 0.01 und 5.33 Millionen Jahren |
||
| Kommentar z. Stratigraphie | ||||
| This site has been dated to the Late Pliocene or Early Pleistocene by many different authors. There is a suggestion in this paper that there may be a mix of faunas from both time periods at this site, particularly based on the presence of Hippopotamus. Villafranchian according to Martin (1971) | ||||
| U.a. am Fundort ausgegraben: | Dolichopithecus arvernensis | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung |
|---|---|---|---|
| La grotte de l'Escale bed G, Saint-Esteve-Janson, Bouches du Rhone. | Near the village of Saint-Esteve-Janson, found during the building of the canal EDF in 1960. | Middle Pleistocene zwischen 0.13 und 0.78 Millionen Jahren |
L'Escale |
| Kommentar z. Stratigraphie | Lithographie | Kommentar z. Taxonomie | |
| Middle Pleistocene (Biharian), roughly 0.8-0.7Ma. There are a number of beds within the cave - from A (lowermost)-L (topmost), not all of which contain fauna. Each faunal level has been entered separately. | Fauna comes from bed G, which consists of deteriorated (altere) fallen rocks of a reddish colour, lacustrine limestones, travertines with seeds of Celtis and stalagmite floors. Total thickness between 1.5-3 metres. | Fauna indicative of a temperate environment - macrofauna indicates warm and dry conditions, the cold environment rodents in level H have disappeared and seeds of Celtis are very abundant. |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung |
|---|---|---|---|
| La grotte de l'Escale lower bed B, Saint-Esteve-Janson, Bouches du Rhone. | Near the village of Saint-Esteve-Janson, found during the building of the canal EDF in 1960. | Middle Pleistocene zwischen 0.13 und 0.78 Millionen Jahren |
L'Escale |
| Kommentar z. Stratigraphie | Lithographie | Kommentar z. Taxonomie | |
| Middle Pleistocene (Biharian), roughly 0.8-0.7Ma. There are a number of beds within the cave - from A (lowermost)-L (topmost), not all of which contain fauna. Each faunal level has been entered separately. | Fauna comes from the lower part of bed B. Bed is described as a whole - it contains deteriorated (altere) browny-reddish fallen rocks, with reddish clayey silts. The whole bed is 1-2 metres thick. | Fauna of lower bed B is indicative of a temperate and humid/wet environment. |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung | |
|---|---|---|---|---|
| Tourkovounia 3-5 | Co-ordinates based on Athens. | Piacenzian zwischen 2.59 und 3.2 Millionen Jahren |
TRV; Tourkobounia 3-5 | |
| Kommentar z. Stratigraphie | ||||
| Uncertain age but thought to be Early Villanyian, Middle Villafranchian, MNQ17, Pliocene. | ||||
| U.a. am Fundort ausgegraben: | Macaca sylvanus | |||
Literatur
E. Heintz, C. Guerin, R. Martin, F. Prat 1974, Principaux gisements villafranchiens de France: Listes fauniques et biostratigraphie. Memoires du Bureau de Recherches Geologiques et Minieres . 78:1, p. 169 - 182N. Symeonidis, C. Guerin, H. Zapfe 1976, Primatezahne (Cercopithecidae) aus einer Plistozanen Spaltenfullung im Steinbruch Tourkobounja, Athen. Annales geologiques des pays helleniques. 28:1, p. 207 - 214
M. Malez, C. Guerin, H. Zapfe 1986, Die quataren Vertebraten-Faunen in der SFR Jugoslawien. Quatarpalaontologie. 6:1, p. 101 - 117
E. Bonifay, C. Guerin, H. Zapfe 1991, Les Premieres industries du Sud-Est de la France et du Massif-Central. Les Premiers Europeens. Edition du comite des Travaux Historiques et Scientifiques (CTHS). :1, p. 63 - 80
S. Gentili, L. Abbazzi, F. Masini, P. Ambrosetti, P. Argenti, D. Torre 1996, Voles from the Early Pleistocene of Pietrafitta (central Italy, Perugia). Acta Zoologica Cracovensia. 39:1, p. 185 - 199
W. von Koenigswald, W.-D. Heinrich, F. Masini, P. Ambrosetti, P. Argenti, D. Torre 1999, Mittelpleistozane Saugetierfaunen aus Mitteleuropa - der Versuch einer biostratigraphischen Zuordnung. Kaupia. 9:1, p. 53 - 112