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Bison antiquus

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Journal Article

Late Pleistocene northward-dispersing Bison antiquus from the Bighill Creek Formation, Gallelli Gravel Pit, Alberta, Canada, and the fate of Bison occidentalis Available to Purchase

Michael C. Wilson, Leonard V. Hills, Beth Shapiro
Published: 27 August 2008
Canadian Journal of Earth Sciences (2008) 45 (7): 827–859.
DOI: https://doi.org/10.1139/E08-027
... of Beringia. Two partial crania, dated to 11 290 and 10 100 14 C years BP, are referred to the southern species Bison antiquus Leidy, indicating northward movement from the midcontinent as ice retreat opened a corridor between Laurentide and Cordilleran ice. Their large size suggests a dispersal phenotype...
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View PDF for article title, Late Pleistocene northward-dispersing <span class="search-highlight">Bison</span> <span class="search-highlight">antiquus</span> from the Bighill Creek Formation, Gallelli Gravel Pit, Alberta, Canada, and the fate of <span class="search-highlight">Bison</span> occidentalis
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Journal Article

A combined mesowear analysis of Mexican Bison antiquus shows a generalist diet with geographical variation Available to Purchase

Roberto Díaz-Sibaja, Eduardo Jiménez-Hidalgo, Javier Ponce-Saavedra, María Luisa García-Zepeda
Published: 01 November 2018
Journal of Paleontology (2018) 92 (6): 1130–1139.
DOI: https://doi.org/10.1017/jpa.2018.19
...Roberto Díaz-Sibaja; Eduardo Jiménez-Hidalgo; Javier Ponce-Saavedra; María Luisa García-Zepeda Abstract Bison antiquus Leidy, 1852 was one of the largest and most widely distributed megafaunal species during the Late Pleistocene in North America, giving rise to the modern plains bison in the middle...
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View PDF for article title, A combined mesowear analysis of Mexican <span class="search-highlight">Bison</span> <span class="search-highlight">antiquus</span> shows a generalist diet with geographical variation
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Figure 5. Bison section, Archuleta Creek. Bison antiquus bones date to 10,190 14C yr B.P. Buried soils suggest that three episodes of incision occurred between 10,190 and 7210 14C yr B.P.

Figure 5. Bison section, Archuleta Creek. Bison antiquus bones date to 10... Available to Purchase

Published: 01 November 2007
Figure 5. Bison section, Archuleta Creek. Bison antiquus bones date to 10,190 14 C yr B.P. Buried soils suggest that three episodes of incision occurred between 10,190 and 7210 14 C yr B.P.
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Summary of mean mesowear patterns of the fossil Bison antiquus of this st... Available to Purchase

Published: 01 November 2018
Table 1. Summary of mean mesowear patterns of the fossil Bison antiquus of this study. %high=percentage of high cusps; %low=percentage of low cusps; %sharp=percentage of sharp cusps; %round=percentage of rounded cusps; mesial=mesial enamel band score; distal=distal enamel band score; j-junction
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Fig. 6. The larger Bison antiquus cranial fragment, including right horn ... Available to Purchase

Published: 27 August 2008
Fig. 6. The larger Bison antiquus cranial fragment, including right horn core, from Gallelli Pit, UCG 4066. (1) anterior view, (2) posterior view, (3) dorsal view, (4) ventral view.
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Fig. 7. The smaller Bison antiquus cranium from Gallelli Pit, UCG 6125. (... Available to Purchase

Published: 27 August 2008
Fig. 7. The smaller Bison antiquus cranium from Gallelli Pit, UCG 6125. (Above), dorsal view; (below), posterior (occipital) view.
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Fig. 11. Right metacarpal (anterior view) of Bison antiquus from Gallelli... Available to Purchase

Published: 27 August 2008
Fig. 11. Right metacarpal (anterior view) of Bison antiquus from Gallelli Pit (UCA 74.33.2).
Journal Article

Late Pleistocene Camelops from the Gallelli Pit, Calgary, Alberta: morphology and geologic setting Free

Michael Wilson, C. S. Churcher
Published: 01 May 1978
Canadian Journal of Earth Sciences (1978) 15 (5): 729–740.
DOI: https://doi.org/10.1139/e78-080
... of the camel humerus suggest some revisions in our views concerning morphologic variation in the species: the species was probably more plastic than has been accepted to date. Associated Bison bison antiquus and Equus conversidens from the same gravels (Gallelli and Galvin Pits) are briefly described...
Add to Citation Manager for Late Pleistocene Camelops from the Gallelli Pit, Calgary, Alberta: morphology and geologic setting
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Summary of results: (1) hierarchical cluster diagram of mesowear signatures of our samples plus 27 extant model species with known diet; (2) mesowear univariate scores of 50 extant model species with known dietary preferences against Bison antiquus samples from previous studies; (3) mesowear III scores of extant model species and our samples; (4) canonical plot of the discriminant analysis combining extended mesowear univariate signatures with mesowear III signatures. Color code: red=grazers; orange=nonstrict grazers; green=mixed feeders; blue=browsers. AA=Alces alces (Linnaeus, 1758); ab=Alcelaphus buselaphus; BaBC=Bison antiquus from Blackwater Draw, Clovis Pit, Curry County, New Mexico; BaBD=B. antiquus from Blackwater Draw, Dry Cave, and Dark Canyon Cave, New Mexico, and Lubbock Lake and Scharbauer Ranch, Texas (Barrón-Ortíz, 2016); BaFQ=B. antiquus from Folsom Quarry, New Mexico (Rivals et al., 2007b); BaIP=B. antiquus from Ingleside, San Patricio County; BaLC=B. antiquus from La Cinta-Portalitos; BaLP=B. antiquus from La Piedad-Santa Ana; BaPV=B. antiquus from Plainview Quarry, Hale County, Texas (Rivals and Semprebon, 2012); BaVV=B. antiquus from Viko Vijin; Cc=Cervus canadensis (Erxleben, 1777); cs=Ceratotherium simum (Burchell, 1817); Cs=Capricornis sumatraensis (Bechstein, 1799); ct=Connochaetes taurinus; DB=Diceros bicornis (Linnaeus, 1758); dl=Damaliscus lunatus (Burchell, 1824); DS=Dicerorhinus sumatrensis (Fischer, 1814); eg=Equus grevyi; Et=Eudorcas thomsonii (Günther, 1884); eq=Equus quagga Boddaert, 1785; GC=Giraffa camelopardalis (Linnaeus, 1758); he=Hippotragus equinus (Desmarest, 1804); hn=H. niger (Harris, 1838); ke=Kobus ellipsiprymnus; Me=Aepyceros melampus (Lichtenstein, 1812); Ng=Nanger granti (Brooke, 1872); OH=Odocoileus hemionus (Rafinesque, 1817); OJ=Okapia johnstoni (Sclater, 1901); Om=Ovibos moschatus (Zimmermann, 1780); OV=Odocoileus virginianus (Zimmermann, 1780); PBb=plains bison, B. bison; rr=Redunca redunca (Pallas, 1767); RS=Rhinoceros sondaicus (Desmarest, 1822); To=Taurotragus oryx (Pallas, 1766); Ts=Tragelaphus scriptus (Pallas, 1766); WBb=wood bison, B. bison.

Summary of results: ( 1 ) hierarchical cluster diagram of mesowear signatur... Available to Purchase

Published: 01 November 2018
Figure 4. Summary of results: ( 1 ) hierarchical cluster diagram of mesowear signatures of our samples plus 27 extant model species with known diet; ( 2 ) mesowear univariate scores of 50 extant model species with known dietary preferences against Bison antiquus samples from previous studies
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Fig. 14. Left metatarsal: anterior (left) and posterior (right) views of ... Available to Purchase

Published: 27 August 2008
Fig. 14. Left metatarsal: anterior (left) and posterior (right) views of Bison antiquus from Gallelli Pit (UCA 74.33.1).
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Fig. 12. Right femur: anterior (left), medial (middle), and posterior (ri... Available to Purchase

Published: 27 August 2008
Fig. 12. Right femur: anterior (left), medial (middle), and posterior (right)views of Bison antiquus from Gallelli Pit (UCA 74.33.5).
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Fig. 13. Right tibia: lateral (left), anterior (middle), and medial (righ... Available to Purchase

Published: 27 August 2008
Fig. 13. Right tibia: lateral (left), anterior (middle), and medial (right) views of Bison antiquus from Gallelli Pit (UCA 74.33.6).
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Prevalence of enamel hypoplasia in the equid and bison samples studied. Bf Ef = Equus “ferus,” Bluefish Caves; AB Ef = E. “ferus,” Alberta; AB Bp = Bison sp., Alberta; SW Ec = “Equus conversidens,” American Southwest; SW Ef = E. “ferus,” American Southwest; SW Ba = Bison antiquus, American Southwest. Time interval abbreviations: Pre-LGM = preglacial; LGM = full-glacial; Post-LGM = postglacial.

Prevalence of enamel hypoplasia in the equid and bison samples studied. Bf ... Available to Purchase

Published: 03 June 2019
 =  Bison antiquus , American Southwest. Time interval abbreviations: Pre-LGM = preglacial; LGM = full-glacial; Post-LGM = postglacial.
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Mean number of hypoplastic events per affected specimen in the equid and bison samples studied. Bf Ef = Equus “ferus,” Bluefish Caves; AB Ef = E. “ferus,” Alberta; AB Bp = Bison sp., Alberta; SW Ec = “Equus conversidens,” American Southwest; SW Ef = E. “ferus,” American Southwest; SW Ba = Bison antiquus, American Southwest. Time interval abbreviations: Pre-LGM = preglacial; LGM = full-glacial; Post-LGM = postglacial.

Mean number of hypoplastic events per affected specimen in the equid and bi... Available to Purchase

Published: 03 June 2019
Southwest; SW Ba =  Bison antiquus , American Southwest. Time interval abbreviations: Pre-LGM = preglacial; LGM = full-glacial; Post-LGM = postglacial.
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Fig. 10. Proximal end of right humerus, anterior (left) and medial (right... Available to Purchase

Published: 27 August 2008
Fig. 10. Proximal end of right humerus, anterior (left) and medial (right) views, of Bison antiquus from Gallelli Pit (UCA 74.33.3). Difference in apparent length results from slight rotation in photography.
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Temporal distribution of the late Pleistocene equid and bison samples studi... Available to Purchase

Published: 03 June 2019
Southwest Equus “ ferus ” Equus “ ferus ” Bison sp. Equus “ ferus ” “ Equus conversidens ” Bison antiquus Post-LGM X X X X X X LGM X* X X Pre-LGM X X X
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Fig. 9. Right lateral view of 5th thoracic vertebra (left), and right lat... Available to Purchase

Published: 27 August 2008
Fig. 9. Right lateral view of 5th thoracic vertebra (left), and right lateral and posterior views of 7th cervical vertebra (middle and right) of Bison antiquus from Gallelli Pit (grouped as UCA 74.33.7). Note asymmetry of C7 postzygapophyses.
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Average mesowear score for the late Pleistocene bison and equid samples studied and extant ungulate species reported in Kaiser et al. (2013). Each data point is the average for a species sample. Abbreviations: LB = leaf browsers; MF = mixed feeders; G = grazers; Pre-LGM = preglacial; LGM = full-glacial; Post-LGM = postglacial; BaS = Bison antiquus (American Southwest); BpA = Bison sp. (Alberta); EcS = “Equus conversidens” (American Southwest); EfA = Equus “ferus” (Alberta); EfB = E. “ferus” (Bluefish Caves, Yukon); EfS = E. “ferus” (American Southwest).

Average mesowear score for the late Pleistocene bison and equid samples stu... Available to Purchase

Published: 03 June 2019
; LGM = full-glacial; Post-LGM = postglacial; BaS =  Bison antiquus (American Southwest); BpA =  Bison sp. (Alberta); EcS = “ Equus conversidens ” (American Southwest); EfA =  Equus “ ferus ” (Alberta); EfB =  E. “ ferus ” (Bluefish Caves, Yukon); EfS =  E. “ ferus ” (American Southwest).
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Results of Kruskal-Wallis tests used to evaluate the hypotheses of the coev... Available to Purchase

Published: 03 June 2019
. conversidens ” Postglacial 14 1.309 0.4851 E. “ ferus ” 10 Bison antiquus 8
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Results of NP-MANOVA tests (10,000 replications and using the Mahalanobis d... Available to Purchase

Published: 03 June 2019
” Full-glacial 6 1.713 0.0496 E. “ ferus ” 12 “ E. conversidens ” Postglacial 13 0.8747 0.6263 E. “ ferus ” 10 Bison antiquus 9