†Nannodectes lynasi (Plesiadapidae)
Nannodectes lynasi ist eine Primatenart innerhalb der Familie Plesiadapidae, die ab dem Paläogen (Paläozän) im Danium lebte, das vor rund 66 Millionen Jahren begann und bis vor 61,6 Millionen Jahren andauerte.
Daten zu den einzelnen Funden von Nannodectes lynasi
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
---|---|---|---|
RAM locality V200510 | "Grand Canyon area" | - zwischen 56.8 und 61.7 Millionen Jahren |
Goler |
Kommentar z. Stratigraphie | |||
Lofgren et al. 2014: The mammalian fauna from member 4a and the lower part of member 4b is collectively referred to as the Goler Assemblage. the Goler Assemblage is probably middle Tiffanian (Ti3–Ti4a), although a Ti5a age is also possible. |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
---|---|---|---|
RAM locality V200706 | "Grand Canyon area" | - zwischen 56.8 und 61.7 Millionen Jahren |
Goler |
Kommentar z. Stratigraphie | |||
Lofgren et al. 2014: The mammalian fauna from member 4a and the lower part of member 4b is collectively referred to as the Goler Assemblage. the Goler Assemblage is probably middle Tiffanian (Ti3–Ti4a), although a Ti5a age is also possible. |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
---|---|---|---|
RAM locality V200804 | "Grand Canyon area" | - zwischen 56.8 und 61.7 Millionen Jahren |
Goler |
Kommentar z. Stratigraphie | |||
Lofgren et al. 2014: The mammalian fauna from member 4a and the lower part of member 4b is collectively referred to as the Goler Assemblage. the Goler Assemblage is probably middle Tiffanian (Ti3–Ti4a), although a Ti5a age is also possible. |
Sammlung | Epoche, Alter | Geologie, Formation | ||
---|---|---|---|---|
Edentulous Jaw Site, locality V98012 | - zwischen 56.8 und 61.7 Millionen Jahren |
Goler | ||
Kommentar z. Stratigraphie | Lithographie | |||
Ti2–Ti3 Lofgren et al. 2014: The mammalian fauna from member 4a and the lower part of member 4b is collectively referred to as the Goler Assemblage. the Goler Assemblage is probably middle Tiffanian (Ti3–Ti4a), although a Ti5a age is also possible. | Sandstone and siltstone | |||
U.a. am Fundort ausgegraben: | Ignacius frugivorus |
Sammlung | Epoche, Alter | Geologie, Formation | ||
---|---|---|---|---|
Primate Gulch, RAM locality V200202 | - zwischen 56.8 und 61.7 Millionen Jahren |
Goler | ||
Kommentar z. Stratigraphie | Lithographie | |||
Ti4 Lofgren et al. 2014: The mammalian fauna from member 4a and the lower part of member 4b is collectively referred to as the Goler Assemblage. the Goler Assemblage is probably middle Tiffanian (Ti3–Ti4a), although a Ti5a age is also possible. | Red-brown conglomerate and sandstone | |||
U.a. am Fundort ausgegraben: | Plesiadapis churchilli |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung | |
---|---|---|---|---|
Laudate | - zwischen 56.8 und 61.7 Millionen Jahren |
Goler | Laudate Discovery Site; UCMP V-5252 (= UCMP V-5502, RAM V94014), UCMP V-5870 (= RAM V94133) | |
Kommentar z. Stratigraphie | Lithographie | Museum | Kommentar z. Taxonomie | |
believed to be Puercan or Torrejonian by McKenna et al., but "definitely Tiffanian" according to McKenna and Lofgren 2003 from "near the base of information member 4b (formerly Tgsu)" Lofgren et al. 2014: The mammalian fauna from member 4a and the lower part of member 4b is collectively referred to as the Goler Assemblage. the Goler Assemblage is probably middle Tiffanian (Ti3–Ti4a), although a Ti5a age is also possible. | formation is "non-marine and then marine" going up section, and consists of "Almost 4 km of conglomerates, feldspathic sandstones, and drab or variegated mudstones" | UCMP | material of Lofgren et al. 1999 is from "Laudate" but these authors do include Black Mountain in the fauna | |
U.a. am Fundort ausgegraben: | Paromomys depressidens |