| Literature DB >> 24204860 |
Shelly L Donohue1, Larisa R G DeSantis, Blaine W Schubert, Peter S Ungar.
Abstract
Dramatic environmental changes associated with global cooling since the late Miocene, and the onset of glacial-interglacial cycles in the Pleistocene served as a backdrop to the evolutionary radiation of modern bears (family Ursidae). These environmental changes likely prompted changes in food availability, and triggered dietary adaptations that served as motive forces in ursid evolution. Here, we assess correspondence of dental microwear textures of first and second lower molars with diet in extant ursids. We use the resulting baseline data to evaluate the hypothesis that the Pleistocene giant short-faced bear, Arctodus simus, was a bone consumer and hyper-scavenger at Rancho La Brea, California, USA. Significant variation along the tooth row is consistent with functional differentiation, with the second molar serving as a better dietary recorder than the first. Results evince significant variation among species: carnivorous and omnivorous ursids (Ursus maritimus, U. americanus) have significantly higher and more variable complexity (Asfc) than more herbivorous ones (Ailuropoda melanoleuca, Tremarctos ornatus, U. malayanus), and A. melanoleuca is differentiated from U. maritimus and U. americanus by significantly higher and more variable anisotropy (epLsar) values. Arctodus simus from Rancho La Brea exhibits wear attributes most comparable to its closest living relative (T. ornatus), which is inconsistent with hard-object (e.g., bone) consumption, and the hypothesis that short-faced bears were bone consuming hyper-scavengers across their range.Entities:
Mesh:
Year: 2013 PMID: 24204860 PMCID: PMC3813673 DOI: 10.1371/journal.pone.0077531
Source DB: PubMed Journal: PLoS One ISSN: 1932-6203 Impact factor: 3.240
Figure 1Phylogeny and dietary ecology of Ursidae including three-dimensional microwear photosimulations of analyzed taxa.
Phylogeny modified from Krause and colleagues [1] with an update to polar bear origination from Miller and co-authors [2]. The shaded bar highlights the rapid evolutionary radiation of bears, which correlates with climatic and environmental changes. Numbers indicate divergence dates in millions of years. Po, Pliocene; Ps, Pleistocene; H, Holocene. A–F are three-dimensional photosimulations of lower second molars taken at 100× magnification, length and width measurements of photosimulation F correspond to all. A. Ursus maritimus, NMNH 512117; B. Ursus americanus, UF 28436; C. Ursus malayanus, NMNH 151866; D. Tremarctos ornatus, NMNH 271418; E. Ailuropoda melanoleuca, NMNH 259028; F. Arctodus simus, LACMHC 1292.
Figure 2Depiction of ursid tooth facets analyzed for dental microwear.
Pictured: Ursus americanus (NMNH 198391), left mandible, buccal view, anterior is to the right. Shading indicates scanned regions. A. Second molar (m2) hypoconulid, mesial facet. B. First molar (m1) protoconid, buccal facet.
Descriptive statistics of dental microwear attributes used to differentiate diet in bears.
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| Species | Tooth |
| mean | SD | mean | SD | mean | SD |
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| m1 | 15 | 5.705 | 5.741 | 0.0040 | 0.0051 | 3520 | 5432 |
| m2 | 11 | 1.996 | 1.010 | 0.0039 | 0.0021 | 8230 | 5507 | |
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| m1 | 15 | 4.348 | 3.245 | 0.0013 | 0.0035 |
| 5248 |
| m2 | 11 | 4.172 | 2.288 | 0.0028 | 0.0009 |
| 4410 | |
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| m1 | 7 |
| 0.719 |
| 0.0012 | 11057 | 3309 |
| m2 | 6 |
| 2.519 |
| 0.0009 | 10639 | 3715 | |
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| m1 | 16 |
| 3.035 |
| 0.0025 |
| 4232 |
| m2 | 15 |
| 4.576 |
| 0.0011 |
| 4528 | |
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| m1 | 15 |
| 2.444 | 0.0020 | 0.0041 |
| 3812 |
| m2 | 16 |
| 3.640 | 0.0022 | 0.001 |
| 2136 | |
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| m1 | 15 | 3.350 | 1.962 | 0.0025 | 0.0008 |
| 2513 |
| m2 | 16 | 4.586 | 2.295 | 0.0022 | 0.0010 |
| 1753 | |
Indicates significant differences (P<0.05, Wilcoxon signed-rank test or paired Student’s t-test, where applicable) between m1 and m2 values;
denotes the extinct taxon; SD, standard deviation, n, number of individuals sampled; Asfc, area-scale fractal complexity; epLsar, anisotropy; Tfv, textural fill volume.
Pairwise differences for microwear attributes of extant ursid lower second molars (Dunn’s procedure).
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| −13.00 | −11.20 | − | − |
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| 1.80 | − | − | |
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| −15.17 | − | ||
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| −3.5 | |||
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| 8.91 | 15.98 |
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| 7.08 | 8.84 | 9.60 | |
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| 1.77 | 2.52 | ||
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| 0.75 | |||
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| −14.09 | −3.58 | −12.84 | − |
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| 10.52 | 1.25 | 0.62 | |
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| −9.27 | −9.90 | ||
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| −0.63 |
Significant values are noted in bold text (P<0.05) and represent analyses performed absent of the Bonferroni correction; Asfc, area-scale fractal complexity; epLsar, anisotropy; Tfv, textural fill volume.
Pairwise differences of variance between lower second molars of all extant and extinct bears.
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| 0.134 | 0.090 | − | − | −0.082 |
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| −0.044 | − | − | 0.051 | |
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| − | − | −0.008 | ||
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| −0.072 | − | |||
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| − | ||||
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| 0.056 | −0.056 | −0.111 | −0.012 | |
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| −0.112 | −0.167 | −0.067 | ||
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| −0.055 | 0.044 | |||
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| 0.100 |
Indicates significant (P<0.05) Fisher’s (LSD) tests;
indicates significant (P<0.05) Fisher’s (LSD) and Tukey's (HSD) tests; Asfc, area-scale fractal complexity; epLsar, anisotropy.
Denotes the extinct taxon. Data transformed for Levene’s test, X′ = |X – median(X)/median(X)|following Plavcan and Cope [51].
Figure 3Bivariate plot of complexity (Asfc) vs. anisotropy (epLsar) for lower second molars of ursids.
Polygons enclose data points.