A late Eocene (Chadronian) mammalian fauna from the White River Formation in Kings Canyon, northern Colorado

2012 ◽  
Vol 47 (2) ◽  
pp. 113-132
Author(s):  
K. J. Lloyd ◽  
J. J. Eberle
2016 ◽  
Vol 3 (10) ◽  
pp. 160518 ◽  
Author(s):  
Susumu Tomiya ◽  
Zhijie Jack Tseng

The Middle to Late Eocene sediments of Texas have yielded a wealth of fossil material that offers a rare window on a diverse and highly endemic mammalian fauna from that time in the southern part of North America. These faunal data are particularly significant because the narrative of mammalian evolution in the Paleogene of North America has traditionally been dominated by taxa that are known from higher latitudes, primarily in the Rocky Mountain and northern Great Plains regions. Here we report on the affinities of two peculiar carnivoraforms from the Chambers Tuff of Trans-Pecos, Texas, that were first described 30 years ago as Miacis cognitus and M. australis . Re-examination of previously described specimens and their inclusion in a cladistic analysis revealed the two taxa to be diminutive basal amphicyonids; as such, they are assigned to new genera Gustafsonia and Angelarctocyon , respectively. These two taxa fill in some of the morphological gaps between the earliest-known amphicyonid genus, Daphoenus , and other Middle-Eocene carnivoraforms, and lend additional support for a basal caniform position of the beardogs outside the Canoidea. The amphicyonid lineage had evidently given rise to at least five rather distinct forms by the end of the Middle Eocene. Their precise geographical origin remains uncertain, but it is plausible that southern North America served as an important stage for a very early phase of amphicyonid radiation.


1940 ◽  
Vol 28 (4) ◽  
pp. 363 ◽  
Author(s):  
William Berryman Scott ◽  
Glenn Lowell Jepsen
Keyword(s):  

1937 ◽  
Vol 28 (2) ◽  
pp. 155 ◽  
Author(s):  
William Berryman Scott ◽  
Glenn Lowell Jepsen ◽  
Albert Elmer Wood
Keyword(s):  

2020 ◽  
Vol 297 (2) ◽  
pp. 205-215 ◽  
Author(s):  
Gerald Mayr ◽  
Thomas Perner

We describe a new species of the Accipitridae (hawks, eagles, and allies) from the late Eocene of North America. ? Palaeoplancus dammanni n. sp. is based on a nearly complete tarsometatarsus from the Chadronian of Wyoming (USA) and is the fifth accipitrid species from the White River Group. If correctly assigned to the taxon Palaeoplancus, the new species is likely to be a stem group representative of the Accipitridae, and together with "Buteo "antecursor it is among the earliest New World records of the Accipitridae. Some of the diagnostic features of ? P. dammanni indicate a strong development of muscles controlling the hallux and second toe, which are likely to have been correlated with a particular — albeit unknown — foraging behavior or prey type.


2019 ◽  
Vol 132 (1-2) ◽  
pp. 373-388 ◽  
Author(s):  
Diana Sahy ◽  
Joe Hiess ◽  
Anne U. Fischer ◽  
Daniel J. Condon ◽  
Dennis O. Terry ◽  
...  

AbstractAn accurate and precise geomagnetic polarity time scale is crucial to the development of a chronologic framework in which to test paleoclimatic and paleoenvironmental interpretations of marine and terrestrial records of the Eocene–Oligocene transition (EOT). The magnetic polarity patterns of relatively continuous marine and terrestrial records of the EOT have been dated using both radio-isotopic techniques and astronomical tuning, both of which can achieve a precision approaching ±30 k.y. for much of the Paleogene. However, the age of magnetic reversals between chrons C12n and C16n.2n has proved difficult to calibrate, with discrepancies of up to 250 k.y. between radio-isotopically dated and astronomically tuned marine successions, rising to 600 k.y. for comparisons with the 206Pb/238U-dated terrestrial record of the White River Group in North America. In this study, we reevaluate the magnetic polarity pattern of the Flagstaff Rim and Toadstool Geologic Park records of the White River Group (C12n–C16n.2n). Our interpretation of the Flagstaff Rim polarity record differs significantly from earlier studies, identifying a previously unreported normal polarity zone correlated to C15n, which eliminates discrepancies between the WRG and the 206Pb/238U-dated marine record of the Rupelian Global Stratotype Section and Point in the Italian Umbria-Marche basin. However, residual discrepancies persist between U-Pb–dated and astronomically tuned records of the EOT even when stratigraphic and systematic uncertainties associated with each locality and dating method are taken into account, which suggests that the uncertainties associated with astronomically tuned records of the EOT may have been underestimated.


1994 ◽  
Vol 31 (8) ◽  
pp. 1335-1341 ◽  
Author(s):  
John E. Storer

The Kealey Springs West (KSW) local fauna from the Cypress Hills Formation (Eocene to Miocene), Saskatchewan, is probably latest Chadronian in age, and is the northernmost assemblage representing a time near the Eocene–Oligocene boundary in North America. Presence of Pseudocylindrodon neglectus is strong evidence that the assemblage is Chadronian. Herpetotherium valens, Protosciurus, Namatomys cf. N. lloydi, and Centimanomys also suggest a Chadronian age. The assemblage contains Adjidaumo maximus and Palaeolagus cf. P. hemirhizis, species that have been cited as characteristic of the early part of the Orellan Land Mammal Age (early Oligocene), and the typically Orellan Heliscomys hatcheri and Eumys elegans. Several other tara in the KSW assemblage are known from both the Chadronian (late Eocene) and Orellan.


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