†Paromomys depressidens (Paromomyidae)
Paromomys depressidens ist eine Primatenart innerhalb der Familie Paromomyidae, die ab dem Paläogen (Paläozän) im Danium lebte, das vor rund 66 Millionen Jahren begann und bis vor 61,6 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 Paromomys depressidens
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Dragon Canyon | "western half of section 8, T. 19 S., R. 6 E." according to Gazin 1939 coordinate based on township and range | Danian zwischen 61.7 und 63.3 Millionen Jahren |
North Horn | Gazin's Locality 2; OMNH V799; UALP 76111, 76112, 7776 |
| Kommentar z. Stratigraphie | Kommentar z. Taxonomie | |||
| close to the top of a normal magnetic polarity zone interpreted as C28n, but there is no tie point in the section: see Lucas et al. 1997 | firmly correlated with Wagonroad Upper Horizon, which was included in the list of Tomida and Butler 1980; paleomagnetic data strongly support a correlation between the two horizons descriptions of Robison 1986 do not incorporate the collections reported by Tomida and Butler and Tomida 1982 "Oxyclaenus pearcei" is not discussed by Robison 1986 and I assume it is only present at Wagonroad Upper Horizon Haploconus "inopinatus" is not discussed by Robison 1986 and I assume it is only present at Wagonroad Upper Horizon |
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| U.a. am Fundort ausgegraben: | Draconodus apertus | |||
| Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung | |
|---|---|---|---|---|
| Kimbetoh Arroyo (Middle) | Danian zwischen 61.7 und 63.3 Millionen Jahren |
Nacimiento | UALP 7784, 77113, 77114 | |
| Kommentar z. Stratigraphie | Kommentar z. Taxonomie | |||
| three UALP localities are separated stratigraphically by five meters: Tomida 1981 near the top of the local section in a normal paleomag interval that is is probably chron 27n but could be chron 28n | called "Upper Kimbetoh" by Tomida 1981 identical to list 12 of Williamson 1996 some records may be from an equivalent level in Betonnie- Tsosie Arroyo list probably omits some multis |
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| U.a. am Fundort ausgegraben: | Palaechthon woodi | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Swain Quarry | SE 1/4 NE 1/4 sec 3 T15N R92W, Washakie Basin | Danian zwischen 61.7 und 63.3 Millionen Jahren |
Fort Union | CM loc 217 |
| Kommentar z. Taxonomie | ||||
| there are seven other localities in the same section, but none of the material is described Mesodma pygmaea, i.e. sp. P, not listed, but mentioned by Krause 1977 | ||||
| U.a. am Fundort ausgegraben: | Paromomys maturus | |||
| Sammlung | Epoche, Alter | Geologie, Formation | ||
|---|---|---|---|---|
| Cedar Mountain (UW V-82040) | Danian zwischen 61.7 und 63.3 Millionen Jahren |
Fort Union | ||
| Museum | ||||
| UW | ||||
| U.a. am Fundort ausgegraben: | Paromomys maturus | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | |
|---|---|---|---|---|
| Gidley Quarry | Crazy Mountain Basin | Danian zwischen 61.7 und 63.3 Millionen Jahren |
Fort Union | |
| Kommentar z. Stratigraphie | Kommentar z. Taxonomie | |||
| said by Buckley 1993 to be in the same (unidentified) reversed polarity chron as Silberling Quarry, i.e., possibly C27r | many of the types were described by Simpson 1935d Simpson 1935d lists the type of "Chriacus pusillus" from "Gidley or Silberling Quarries" - no other specimens are listed but the type's catalogue number is close to that of other types from Gidley Quarry; however, this record is omitted by Simpson 1937a and later authors |
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| U.a. am Fundort ausgegraben: | Palaechthon alticuspis | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung | |
|---|---|---|---|---|
| Rock Bench Quarry | Bighorn Basin | Danian zwischen 61.7 und 63.3 Millionen Jahren |
Locality No. 6 | |
| Kommentar z. Stratigraphie | Kommentar z. Taxonomie | |||
| in a stratigraphically isolated reversed polarity zone interpreted as chron 27r: Butler et al. 1987 | >I have used Van Valen's 1978 list of condylarths because Rose gives no reason for ignoring it meter level follows Butler et al. 1981 above two records presumably include "Tricentes cf. punitor" and "cf. Chriacus sp." |
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| U.a. am Fundort ausgegraben: | Plesiolestes problematicus | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Cochrane 2 | 0.5 km E of Cochrane, Bow River in SE 1/4 sec 1 T26 R4 W5 "fossils occur intermittently along about 30 m of strike" (Fox 2011) | - zwischen 56.8 und 61.7 Millionen Jahren |
Paskapoo | Cochrane 11; Cochrane II |
| Kommentar z. Stratigraphie | Lithographie | Kommentar z. Taxonomie | ||
| reassigned from the Porcupine Hills Formation to the Paskapoo Formation by Fox (2011) fossils are from "within an interval ranging from a few centimeters to a meter or so in thickness" (Fox 2011) | "poorly bedded grayishgreen siltstones, rich in broken bivalve and gastropod shells that are accompanied by bits of coalified wood and occasional wellrounded pebbles" (Fox 2011) | same as the list given by Fox 1990a | ||
| U.a. am Fundort ausgegraben: | Torrejonia sirokyi | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation |
|---|---|---|---|
| Rock Springs Uplift (UW V-77014) | east flank Rock Springs Uplift | - zwischen 56.8 und 61.7 Millionen Jahren |
Fort Union |
| Museum | Kommentar z. Taxonomie | ||
| UW | Torrejonian according to Winterfeld but probably early Tiffanian: Thewissen 1990 |
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Kommentar zur Sammlung | |
|---|---|---|---|---|
| Love Quarry | Togwotee Pass, Wind River Basin | - zwischen 56.8 und 61.7 Millionen Jahren |
Love's Locality L-14 | |
| Lithographie | Museum | Kommentar z. Taxonomie | ||
| "limestone-pellet conglomerate" | USGS | unit underlying Lower Variegated Sequence Gunnell 1994 lists Ptilodus sp. "C"; not clear if this replaces P. fractus |
||
| U.a. am Fundort ausgegraben: | Zanycteris paleocenus | |||
| Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
|---|---|---|---|---|
| Shotgun | NE 1/4 SE 1/4 sec 31 T6N R3W, northern Wind River Basin: MacIntyre 1966 | - zwischen 56.8 und 61.7 Millionen Jahren |
Fort Union | UW V-60014, V-60016; Keefer Hill; Twin Buttes; Jenkins Mountain; New Anthill |
| Kommentar z. Taxonomie | ||||
| this is NOT West Side of Shotgun Butte (see), which is the uppermost of three fossiliferous horizons; the fauna of the lowest horizon is not discussed by Gunnell apart from the plesiadapiforms, Gunnell's list is mostly repeated from ancient sources without modification Gunnell lists Eudaemonema cuspidata from "Shotgun fauna, Keefer Hill" but omits this from his faunal list | ||||
| U.a. am Fundort ausgegraben: | Nannodectes intermedius | |||
| 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: | Plesiadapis anceps | |||
| Sammlung | Epoche, Alter | Geologie, Formation | ||
|---|---|---|---|---|
| UCM locality 2011056 | - zwischen 56.8 und 61.7 Millionen Jahren |
Fort Union | ||
| Kommentar z. Stratigraphie | Lithographie | |||
| approximately 85 meters stratigraphically above base of Overland Member | sandstone consists of coarse-grained sandstone with pieces of quartz, feldspar granules, and chert pebbles | |||
| U.a. am Fundort ausgegraben: | Nannodectes intermedius | |||
Literatur
M. C. McKenna 1980, Late Cretaceous and Early Tertiary vertebrate paleontological reconnaissance, Togwotee Pass area, northwestern Wyoming. Aspects of Vertebrate History: Essays in Honor of Edwin Harris Colbert, L. L. Jacobs (ed.), Museum of Northern Arizona Press. , p. 323 - 343J. K. Rigby, Jr. 1980, Swain Quarry of the Fort Union Formation, Middle Paleocene (Torrejonian), Carbon County, Wyoming: geologic setting and mammalian fauna. Evolutionary Monographs. 3, p. 1 - 178
K. D. Rose 1981, The Clarkforkian Land-Mammal Age and Mammalian Faunal Composition Across the Paleocene-Eocene Boundary. University of Michigan Papers on Paleontology. 26, p. 1 - 197
G. F. Winterfeld 1982, Mammalian paleontology of the Fort Union Formation (Paleocene), eastern Rock Springs Uplift, Sweetwater County, Wyoming. Contributions to Geology, University of Wyoming. 21:1, p. 73 - 112
J. E. Hartman 1986, Paleontology and biostratigraphy of lower part of Polecat Bench Formation, southern Bighorn Basin, Wyoming. Contributions to Geology, University of Wyoming. 24:1, p. 11 - 63
G. F. Gunnell 1989, Evolutionary History of Microsyopoidea (Mammalia, ?Primates) and the Relationship Between Plesiadapiformes and Primates. University of Michigan Papers on Paleontology. 27:1, p. 1 - 157
D. L. Lofgren, J. G. Honey, M. C. McKenna, R. L. Zondervan, E. E. Smith 2008, Paleocene primates from the Goler Formation of the Mojave Desert in California. Natural History Museum of Los Angeles County Science Series. 41:1, p. 11 - 28
E. K. Halverson, J. J. Eberle, M. C. McKenna, R. L. Zondervan, E. E. Smith 2018, A new middle Paleocene (early Tiffanian) mammalian fauna from the Overland Member of the Fort Union Formation, Great Divide Basin, Wyoming, U.S.A. . Rocky Mountain Geology. 53:2, p. 75 - 111, DOI: 10.24872/rmgjournal.53.2.75