Microsyops knightensis (Microsyopidae)



Microsyops knightensis ist eine Primatenart innerhalb der Familie Microsyopidae, die ab dem Paläogen (Eozän) im Ypresium lebte, das vor rund 56 Millionen Jahren begann und bis vor 47,8 Millionen Jahren andauerte.

Systematik

Daten zu den einzelnen Funden von Microsyops knightensis
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation Kommentar zur Sammlung
Huerfano VI "Exposures in Garcia Canyon and Apodaca Gulch Sec. 33 and Sec. 34, T26S, R69W and in Sec. 3, 4, 5, T27S, R69W." Ypresian
zwischen 50.3 und 55.8 Millionen Jahren
Huerfano Garcia Canyon; Apodaca Gulch; UCM locality 77040
Kommentar z. Stratigraphie Kommentar z. Taxonomie
"Huerfano facies" Lostcabinian "Most of Wortman's collection of 1897 came from here and probably from unit 13 of measured section; unit 13 has consistently produced good specimens and matches the description of the best bone-bearing layer given by Wortman to Osborn. Granger and Olsen also made good collections here."
U.a. am Fundort ausgegraben: Microsyops scottianus
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation Kommentar zur Sammlung
La Barge on the Green River between La Barge and Big Piney Ypresian
zwischen 50.3 und 55.8 Millionen Jahren
Wasatch 12 mi north of Big Piney; Tulsa
Kommentar z. Stratigraphie Kommentar z. Taxonomie
said to be from the "Knight Mbr." (= LaBarge) said to underlie the Tipton Shale (=Fontenelle), therefore clearly within the La Barge Mbr. sensu Krishtalka et al. 1987
apparently includes material referred to by Szalay 1969a as "Muddy Creek locality, 12 miles north of Big Piney... Sublette Co."
Lostcabinian
U.a. am Fundort ausgegraben: Cantius nunienus
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation Kommentar zur Sammlung
South Pass (Lostcabinian) no details given Ypresian
zwischen 50.3 und 55.8 Millionen Jahren
Wasatch The Pinnacles
Kommentar z. Stratigraphie Lithographie
Clyde et al. 2001 took paleomagnetic samples through this part of the section but they were too poorly preserved to analyze "thick brown paper shales"
U.a. am Fundort ausgegraben: Notharctus venticolus
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation Kommentar zur Sammlung
South Pass (Gardnerbuttean) although South Pass is within Fremont Co., some localities also may be in Sublette and/or Sweetwater counties Ypresian
zwischen 46.2 und 50.3 Millionen Jahren
Wasatch Honeycomb Buttes
Kommentar z. Stratigraphie Lithographie
spans upper chron C24n and lower chron C23r: Clyde et al. 2001 ""thick brown paper shales interbedded with relatively pure carbonate, trona, and gypsum beds"
U.a. am Fundort ausgegraben: Microsyops scottianus
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation
MP-67 Quad = Sleepers Ranch, Township = 50N, Range = 99W, Section = 9 Ypresian
zwischen 50.3 und 55.8 Millionen Jahren
Willwood
Kommentar z. Stratigraphie Museum
Wa-7 UMMP
U.a. am Fundort ausgegraben: Absarokius abbotti
Sammlung Kommentar zum Fundort Epoche, Alter Geologie, Formation Kommentar zur Sammlung
Big Piney 3 S 32 T 32 N R 111 W Ypresian
zwischen 50.3 und 55.8 Millionen Jahren
Wasatch UCMP V-77064
Kommentar z. Stratigraphie Museum Kommentar z. Taxonomie
"35 m below the contact of the Wasatch Formation with the Scheggs Bed of the Tipton Shale Member of the Green River Formation" and now assigned to the main body of the Wasatch Formation per Smith and Holroyd 2003. UCMP,USNM this is almost due N of Big Piney and west of the New Fork- Big Sandy area; Gazin's La Barge localities are S of Big Piney, except some about 12 mi due N on Muddy Creek that are referred to as "Red Buttes" or "Muddy Creek" elsewhere in the literature This locality previously referred to Knight Mbr. or LaBarge Mbr. but these rocks placed in main body of Wasatch Fm. by Roehler 1992.
U.a. am Fundort ausgegraben: Absarokius abbotti
Sammlung Epoche, Alter Geologie, Formation
UM FB-16 Ypresian
zwischen 50.3 und 55.8 Millionen Jahren
Wasatch
U.a. am Fundort ausgegraben: Microsyops latidens

Literatur

W. C. Clyde 1997, Stratigraphy and mammalian paleontology of the McCullough Peaks, northern Bighorn Basin, Wyoming: Implications for biochronology, basin development, and community reorganization across the Paleocene-Eocene boundary. PhD Thesis, University of Michigan. , p.
G. F. Gunnell, W. S. Bartels 2001, Basin margins, biodiversity, evolutionary innovation, and the origin of new taxa. Eocene biodiversity: unusual occurrences and rarely sampled habitats (G. F. Gunnell, ed.). , p. 403 - 432
J. Alroy, W. S. Bartels 2002, Synonymies and reidentifications of North American fossil mammals. . , p. - 432
K. T. Smith, P. A. Holroyd 2003, Rare taxa, biostratigraphy, and the Wasatchian-Bridgerian boundary in North America. Geological Society of America Special Paper. 369, p. 501 - 511
G. F. Gunnell, J.-P. Zonneveld, W. S. Bartels 2016, Stratigraphy, mammalian paleontology, paleoecology, and age correlation of the Wasatch Formation, Fossil Butte National Monument, Wyoming\r\n. Journal of Paleontology. 90:5, p. 981 - 1011, DOI: 10.1017/jpa.2016.100