†Dyseolemur pacificus (Omomyidae)
Dyseolemur pacificus ist eine Primatenart innerhalb der Familie Omomyidae, die ab dem Paläogen (Eozän) im Lutetium lebte, das vor rund 47,8 Millionen Jahren begann und bis vor 41,3 Millionen Jahren andauerte.
Daten zu den einzelnen Funden von Dyseolemur pacificus
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung | |
---|---|---|---|---|
Camp San Onofre | Lutetian zwischen 37.2 und 46.2 Millionen Jahren |
Santiago | Onofre Locality One; UCMP V-72088 | |
Kommentar z. Taxonomie | ||||
fauna is heavily dominated by small mammals: Lillegraven and Wilson 1975 late Uintan or Duchesnean |
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U.a. am Fundort ausgegraben: | Chumashius balchi |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|
Half Day Pocket | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Santiago | UCMP V-6885 |
Museum | |||
UCMP |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung | |
---|---|---|---|---|
Jeff's Discovery | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Santiago | SDSNH 3276 | |
Kommentar z. Stratigraphie | Kommentar z. Taxonomie | |||
reversed polarity: Prothero 2001 | SDSNH Locs. 3560 - 3564 also belong to this L.F., but all small mammals are present at 3276, and most of the large mammals appear to be present here as well | |||
U.a. am Fundort ausgegraben: | Walshina shifrae |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|
Laguna Riviera Quarry | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Santiago | LACM 68102, UCMP V-6839, RV-6830 |
Museum | |||
LACM |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|---|
Rancho del Oro | Oceanside | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Santiago | SDSNH 3431-3437, 3441, 3442, 3444-3446, 3449, 3451, 3461-3464, 3466, 3467 |
Kommentar z. Taxonomie | ||||
while the small mammals are listed separately for each locality, the large mammals are not does not include SDSNH 3438, 3439, and 3447, this is a lapsus: Walsh 1996b |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|
Cloud 9 (SDSNH 3273) | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Mission Valley | La Mesa, in part |
Kommentar z. Taxonomie | |||
not to be confused with the very broadly defined "Cloud 9 Fauna" of Walsh 1996b the Mission Valley Fm. has been dated at 42.18 Ma (Ar-Ar); the dated horizon is only clearly associated with two sites (SDSNH Locs. 3428 and 3539) but presumably applies well to the entire fauna; the date is corrected to 42.83 +/- 0.24 (AA on bentonite) by Walsh 1996b |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|
Eastview | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Pomerado | SDSNH 3493, 3755, 3757 |
Kommentar z. Taxonomie | |||
most of the material is from SDSNH 3755, but original list of Walsh 1991 pertained only to SDSNH 3493 SDSNH 3493 and 3755 are from the Lower Member, and SDSNH 3757 is actually from the overlying Miramar Sandstone; however, I cannot determine if the taxa listed are restricted to SDSNH 3757, or what else it might contain late Uintan |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|---|
Tapo Canyon (Upper) | "In a small exposure of red beds in a large canyon on the east side of the first canyon west of Tapo Canyon or 2.9 miles N. 39.5º E. of Santa Susana Bench Mark 961" (Brattstrom 1955) | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Sespe | CIT 180, 217 Tapo Canyon |
Museum | Kommentar z. Taxonomie | |||
CIT | appears to be at the level of LACM 5857 based on literal interpretation of scale in sections given by Kelly 1990 and Kelly et al. 1991 almost entirely from CIT 180, but some Kelly 1990 records may be from UCMP V-6103 or V-87155; CIT 217 of Golz and Lillegraven 1977, which yielded only "Artiodactyla indet." NISP 1324+ record of ? Hyaenodontidae indet. is omitted by Kelly 1990 "cf. Sespedectes sp." is omitted by Kelly 1990 not clear what "cf. Hemiacodon sp." is "Reithroparamyinae indet." is omitted by Kelly 1990 |
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U.a. am Fundort ausgegraben: | Craseops sylvestris |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|---|
Brea Canyon (Bed CS2) | "in the section between Alamos and Brea Canyons... on the north side of Simi Valley" (Brattstrom 1955) | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Sespe | CIT 207 |
Museum | Kommentar z. Taxonomie | |||
CIT | Brea Canyon (CIT 127, 202, 207) NISP: 94 artiodactyls (Golz 1976) 5+ others at CIT 127 (XXX%) 83+ others at CIT 202 (XXX%) 42+ others at CIT 207 (XXX%) total 210, split about 7/147/54 records of Kelly 1990 may come from UCMP V-72066 or LACM 5616, but 5616 is in CS 3 according to according to Kelly et al. 1991 |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|---|
Brea Canyon (Bed CS3) | "north side of Simi Valley... near the head of the canyon between Brea and Alamos Canyon" (Brattstrom 1955) | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Sespe | CIT 202; LACM 5616, 5660 |
Museum | Kommentar z. Taxonomie | |||
CIT | records of Kelly 1990 may derive from UCMP V-72065, LACM 5617, 5625, 5649 "? Apatemyidae indet." is omitted by Kelly 1990 "cf. Simidectes sp." is omitted by Kelly 1990 |
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U.a. am Fundort ausgegraben: | Macrotarsius roederi |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|
Brea Canyon (Bed SS5) | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Sespe | LACM 5863 |
Kommentar z. Stratigraphie | Museum | Kommentar z. Taxonomie | |
SS5 horizon | LACM | from "clay lens in SS5 horizon" |
Sammlung | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|
Strathern (Bed CS14) | Lutetian zwischen 37.2 und 46.2 Millionen Jahren |
Sespe | CIT 128 (in part), LACM 5636 |
Museum | |||
LACM |
Sammlung | Kommentar zum Fundort | Epoche, Alter | Geologie, Formation | Kommentar zur Sammlung |
---|---|---|---|---|
Cooper Center 02020 | OCPC 21791 was discovered in 1995 as a result of paleontological salvage operations during Eastern Transportation Corridor highway construction in Orange County, southern California (Lander, 2003). The type locality, OCPC 2038, is in the northern (ETC Windy Ridge) segment of State Route (SR) 241, about 8.2 km south of its intersection with SR 91 (Riverside Freeway) and north of its intersection with SR 261 in sec. 23, T.4S, R.8W (33 490 3400 N, 117 420 5200 W) in the northern Santa Ana Mountains, Orange County, California. | Lutetian zwischen 40.4 und 46.2 Millionen Jahren |
Sespe | badlands northwest of ETC Windy Ridge; OCPC 2020; OCPC loc. 2021; OCPC loc. 2024; Basal Orange County S/V fauna |
Literatur
D. J. Golz, J. A. Lillegraven 1977, Summary of known occurrences of terrestrial vertebrates from Eocene strata of southern California. Contributions to Geology, University of Wyoming. 15:1, p. 43 - 65T. S. Kelly, J. A. Lillegraven 1990, Biostratigraphy of Uintan and Duchesnean land mammal assemblages from the Middle Member of the Sespe Formation, Simi Valley, California. Contributions in Science, Natural History Museum of Los Angeles County. 419:1, p. 1 - 42
S. L. Walsh, J. A. Lillegraven 1991, Eocene mammal faunas of San Diego County. Pacific Section SEPM. 68:1, p. 161 - 178
T. S. Kelly, E. B. Lander, D. P. Whistler, M. A. Roder, R. E. Reynolds 1991, Preliminary Report on a Paleontologic Investigation of the Lower and Middle Members, Sespe Formation, Simi Valley Landfill, Ventura County, California. PaleoBios. 13:50, p. 1 - 13
D. T. Rasmussen, M. Shekelle, S. L. Walsh, B. O. Riney 1995, The dentition of Dyseolemur, and comments on the use of the anterior teeth in primate systematics. Journal of Human Evolution. 29:4, p. 301 - 320
J. Alroy, M. Shekelle, S. L. Walsh, B. O. Riney 2002, Synonymies and reidentifications of North American fossil mammals. . :4, p. - 320
D. P. Whistler, E. B. Lander, S. L. Walsh, B. O. Riney 2003, New Late Uintan to Early Hemingfordian Land Mammal Assemblages from the Undifferentiated Sespe and Vaqueros Formations, Orange County, and from the Sespe and Equivalent Marine Formations in Los Angeles, Santa Barbara, and Ventura Counties, Southern California. Bulletin of the American Museum of Natural History. 279:4, p. 231 - 268, DOI: 10.1206/0003-0090(2003)279<0231:C>2.0.CO;2