2017
DOI: 10.1080/10420940.2016.1270209
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Canid Coprolites from the Late Pleistocene of Hidalgo, Central Mexico: Importance for the Carnivore Record of North America

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Cited by 15 publications
(12 citation statements)
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“…However, in contrast to the bear-dog, or unidentified canids in other studies (e.g. Bravo-Cuevas et al 2017), the Skara Brae dog faeces contain fewer identifiable remains, most being too finely fragmented to permit the recognition of anatomical and taxonomical provenance. Bone inclusions from Skara Brae were also tightly condensed, often with only a small amount of coprolite matrix between the pieces of trabecular bone.…”
Section: Discussionmentioning
confidence: 75%
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“…However, in contrast to the bear-dog, or unidentified canids in other studies (e.g. Bravo-Cuevas et al 2017), the Skara Brae dog faeces contain fewer identifiable remains, most being too finely fragmented to permit the recognition of anatomical and taxonomical provenance. Bone inclusions from Skara Brae were also tightly condensed, often with only a small amount of coprolite matrix between the pieces of trabecular bone.…”
Section: Discussionmentioning
confidence: 75%
“…The presence of micromammal remains provides evidence of other processes taking place at the site. Orkney vole remains from Skara Brae coprolites are much smaller than the North American pocket gophers (Pappogeomys/ Cratogeomys) in canid coprolites studied by Bravo-Cuevas et al (2017), but show a similar level of preservation, with fragments being easily identifiable anatomically and in many cases also taxonomically. Previous research on the Skara Brae micromammal assemblages found significant concentrations of rodents within the site centre (Trench I) and periphery (Trench II), possibly related to human occupation (Romaniuk et al 2016).…”
Section: Discussionmentioning
confidence: 91%
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“…Larger camel and dromedary are very drought-tolerant, whereas the smaller vicuña is quite waterdependent. Some Camelops δ 18 O values overlap with Bison, Equus, and Mammuthus compositions, suggesting substantial consumption of free-standing waters, but commonly, slightly higher Camelops tooth enamel δ 18 O values suggest a greater droughttolerance (see data from Connin et al, 1998;Higgins and MacFadden, 2009;Kohn and McKay, 2012;Perez-Crespo et al, 2012;Kita et al, 2014;Trayler et al, 2015;Bravo-Cuevas et al, 2017). Creek locality, Nevada, and 12 fossil tufas from units D1, E0, E1b, and E2 (Table 5).…”
Section: Specimens and Research Areamentioning
confidence: 99%