Mazzonicebus almendrae (Homunculidae)



Mazzonicebus almendrae ist eine Primatenart innerhalb der Familie Homunculidae, die ab dem Neogen (Miozän) im Aquitanium lebte, das vor rund 23 Millionen Jahren begann und bis vor 20,4 Millionen Jahren andauerte.

Fundorte

Systematik

Daten zu den einzelnen Funden von Mazzonicebus almendrae
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation
Gran Barranca - southern cliff of lake Colhué Huapí Southern cliff of Lake Colhué Huapí Busker, et al. 2019: Gran Barranca is placed near Lake Colhue Huapi (southeastern Chubut Province, Madden et al., 2010) Burdigalian
zwischen 17.5 und 21 Millionen Jahren
Sarmiento
Kommentar z. Stratigraphie Museum
Busker, et al. 2019: Colhuehuapian SALMA (early Miocene) (Flynn and Swisher, 1995; Simpson, 1940; Vucetich et al., 2010b). Novo et al 2018: The Colhue-Huapi Member of the Sarmiento Formation is, early Miocene (Burdigalian Age) (see Simpson 1964; Madden & Scarano 2010 and references therein), approximately 20.0-20.2 Ma (Ré et al. 2010). MLP,MNHN
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation
La Estrella La Estrella locality is named like that due to its proximity (around 3 km in west-east direction) to the homonymous ranch, located in the western part of the Meseta del Canquel, central Chubut Province, Argentina. It's a new primate locality at about 75 km N-NW of the Colhue-Huapi lake. S 44835’36.6000; W 698 5’47.90'' Burdigalian
zwischen 17.5 und 21 Millionen Jahren
Sarmiento
Kommentar z. Stratigraphie Lithographie Museum
It consists of an isolated outcrop of the Sarmiento Formation. The fossil-bearing bed is around 15 m below a flow basalt, herein correlated with the uppermost flow basalt recorded in the Scarritt Pocket section. Relative age younger than Deseadan and not older than Colhuehuepian. The authors correlate the La Estrella section with the lower Colhue-Huapi Member. The section is 18 m thick and characterized by a monotonous succession of mostly massive, fine tuffs (Figure 2). The lowermost 6 m are pinkish gray in color, and contain floated medium size mammal remains. The upper part displays whitish and light greenish grey tuffs, and displays insect pupation chambers (Fictovichnus sp.) and small-sized mammal remains in place, including the material herein reported. This and other outcrops fill small depressions or directly lie above the basaltic plateau conforming the Meseta del Canquel, and are close to the classical vertebrate locality “Scarritt Pocket”, located at approximately 25 km to the east (Marshall, Cifelli, Drake, & Curtis, 1986) (Figure 1). The fossil-bearing bed is around 15 m below a flow basalt, herein correlated with the uppermost flow basalt recorded in the Scarritt Pocket section. MEF
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation
Gran Barranca - southern cliff of lake Colhué Huapí Southern cliff of Lake Colhué Huapí Busker, et al. 2019: Gran Barranca is placed near Lake Colhue Huapi (southeastern Chubut Province, Madden et al., 2010) Burdigalian
zwischen 17.5 und 21 Millionen Jahren
Sarmiento
Kommentar z. Stratigraphie Museum
Busker, et al. 2019: Colhuehuapian SALMA (early Miocene) (Flynn and Swisher, 1995; Simpson, 1940; Vucetich et al., 2010b). Novo et al 2018: The Colhue-Huapi Member of the Sarmiento Formation is, early Miocene (Burdigalian Age) (see Simpson 1964; Madden & Scarano 2010 and references therein), approximately 20.0-20.2 Ma (Ré et al. 2010). MLP,MNHN

Literatur

R. F. Kay 2010, A new primate from the early Miocene of Gran Barranca, Chubut Province, Argentina: paleoecological implications. The Paleontology of Gran Barranca: Evolution and Environmental Change through the Middle Cenozoic of Patagonia. , p. 220 - 239
N. M. Novo, M. F. Tejedor, M. E. Pérez, J. M. Krause 2017, New primate locality from the early Miocene of Patagonia, Argentina. American Journal of Physical Anthropology. 164, p. 861 - 867, DOI: 10.1002/ajpa.23309
N. M. Novo, M. F. Tejedor, L. R. González-Ruiz 2018, Previously unknown fossil platyrrhines (Primates) of Patagonia from the Tournouër collection at the Muséum national d'Histoire naturelle, Paris. Geodiversitas. 40:22, p. 529 - 535, DOI: 10.5252/geodiversitas2018v40a22