Calede et al.—Ecomorphology of Leptarctus oregonensis
carnassial/10^(0.5906*Log (body mass)+1.9842))*100. The regression was run in R 3.3.1 (R Development Core Team, 2015) using RStudio 1.0.143 (RStudio, 2015). Although our formulas differ (they are dataset dependent), the BFQs we calculated are very similar to those calculated byWroe et al. (2005). We also investigated the proportions of the teeth of
Leptarctus oregonensis and their possible link with diet by expanding upon a previous analysis by Popowics (2003). We undertook a principal component analysis (PCA) and a cano- nical variate analysis (CVA) of five ratios of tooth measure- ments that describe the shape of the P4 and M1 of small carnivorans.We used the data from Popowics (2003) and newly collected data for extant small carnivores (Table 2) measuring the P4 and M1 following the guidelines of Popowics (2003). The PCA and CVA were run in R 3.3.1 (R Development Core Team, 2015) using RStudio 1.0.143 (RStudio, 2015), the package vegan 2.4-3 (Oksanen et al., 2015), and biostats (McGarigal, 2015). We used a broken-stick distribution to determine the PCA axes whose eigenvalues were larger than expected by chance and only displayed those.
Repositories and institutional abbreviations.—Types, figured, and other specimens examined in this study are deposited in the following institutions: American Museum of Natural History (AMNH), New York City, USA; Frick Collection of the American Museum of NaturalHistory (F:AM),New York City,USA;Natural History Museum of Los Angeles County (LACM), Los Angeles, USA; University of California Museum of Paleontology (UCMP), Berkeley, USA; University of Florida (UF), Gainesville, USA; University of Oregon Museum of Natural and Cultural History (UOMNH), Eugene, USA; University of Washington Burke Museum of Natural History and Culture (UWBM), Seattle, USA.
Systematic paleontology
Nomenclature abbreviations.—P4LB, length of P4; P4W, width of P4; P4PM, length of basin of P4; PRBL, length of shearing blade of P4; M1BL, length of shearing surface of M1; M1LL, length of M1; M1W, width of M1.
Class Mammalia Linnaeus, 1758 Order Carnivora Bowdich, 1821 Family Mustelidae Fischer, 1817 Genus Leptarctus Leidy, 1856
Type species.—Leptarctus primus Leidy, 1856, by original designation
Leptarctus oregonensis Stock, 1930 Figures 1.1–6.1
1924 Leptarctus primus Matthew, p. 139, figs. 37, 38.
1930 Leptarctus oregonensis Stock, Pl. I, fig. 1a, b, text- figures 1, 2.
293
1957 Leptarctus oregonensis; Olsen, p. 2, fig. 2A. 1998 Leptarctus oregonensis; Baskin, p. 158. 2001a Leptarctus primus (part); Lim and Martin, p. 636. 2001 Leptarctus primus (part); Lim, Martin, and Wilson, p. 1044, fig. 1.
2002 Leptarctus primus (part); Lim and Martin, p. 271, fig. 2B.
2005 Leptarctus oregonensis; Baskin, p. 431. 2009 Leptarctus oregonensis; Korth and Baskin, p. 29.
Holotype.—Partial maxilla with the left P4–M1, the right P4, a partial zygomatic arch, and a cranial fragment including part of the lateral temporal crest (LACM (CIT) 206) from LACM CIT 113: exposures of Mascall deposits north of the east fork of the John Day River, ~ 2.4 km NW of Dayville, Oregon (Stock, 1930).
Diagnosis.—Smaller than L. ancipidens, L. mummorum Korth and Baskin, 2009, L. neimenguensis Zhai, 1964, L. primus, L. webbi Baskin, 2005, L. wortmani, and L. kansaensis Lim and Martin, 2001a; rostrum proportionately shorter than in L. wortmani and L. mummorum; skull proportionately narrower, more rectangular in posterior view than that of L. mummorum; postorbital processes not as strong as those of L. mummorum; infraorbital foramen proportionately larger than in L. wortmani; optic foramen directed anterodorsally to the sphenorbital fissure unlike L. mummorum; parasagittal crests do not converge, unlike L. mummorum; post-glenoid foramen larger and located more laterally than in L. mummorum; parietals not as inflated as in L. primus; projections of the tympanic projection do not overlap, unlike in L. primus; tympanic projections present, unlike in L. webbi, and aligned with external auditory meatus, unlike in L. primus; hypocone of P4 smaller than in L. primus and L. ancipidens; metacone blade of P4 longer than in L. primus; tympanic projections do not extend posteriorly to edge of paroccipital process, unlike L. kansaensis; parastyle of P4 not as strong as in L. ancipidens;M1 roughly square, unlike L. ancipidens; no distinct metastyle adjoining the posterior border of the metacone on M1 unlike in L. neimenguensis; tympanic projection double (with a central foramen) unlike L. mummorum, L. wortmani,and L. supremus; paracone of P4 smaller and more acute than in L. desuii and L. martini; meta- cone of P4 longer and more blade-like than in L. desuii and L. martini; parastyle of M1 longer and more-blade like than in L. martini; P4 not wider than long, unlike in L. progressus.
Occurrence.—Early Barstovian of the Mascall Formation of Oregon; early Barstovian of the Olcott Formation of Nebraska.
Description.—UOMNH F-35458 is a nearly complete skull. The rostrum—the only cranial material represented by the type specimen—ismissing, broken anteriorly to P3. The upper canines and incisors are also absent. The P4 and M1 are preserved.
Figure 1. Skull of Leptarctus oregonensis, UOMNH F-35458: (1) dorsal view; (2) ventral view. Abbreviations: aud, auditory bulla; bac, basioccipital; euc, Eustachian canal; fr, frontal; fov, foramen ovale; glsq, glenoid fossa of the squamosal; iof, infraorbital foramen; ju, jugal; lam, lambdoidal crest; mas, mastoid process; max, maxilla; occ, occipital condyles; pal, palatine; par, parietals; poc, paroccipital process; pop, postorbital process; psag, parasagittal crest; pte, pterygoid flange; sq, squamosal; tym, tympanic projections. Scale bar is 1 cm.
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