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Variation in collagen stable nitrogen values in black-tailed jackrabbits ( Lepus californicus) in relation to small-scale differences in climate, soil, and topography

Longstanding observations about the relationship between increasing aridity and 15N enrichment in mammalian collagen values have led to an interest in their use as a paleoclimatic marker. Here we report on variability in collagen nitrogen values from five modern and two archaeological samples of bla...

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Bibliographic Details
Published in:Journal of archaeological science 2011-07, Vol.38 (7), p.1417-1429
Main Authors: Ugan, Andrew, Coltrain, Joan
Format: Article
Language:English
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Summary:Longstanding observations about the relationship between increasing aridity and 15N enrichment in mammalian collagen values have led to an interest in their use as a paleoclimatic marker. Here we report on variability in collagen nitrogen values from five modern and two archaeological samples of black-tailed jackrabbits ( Lepus californicus) from the eastern Great Basin of the United States (N = 178 individuals). Nitrogen δ 15N values were highly variable within all samples. Modern samples showed significant differences despite similarities in average annual precipitation and temperature. Archaeological samples were indistinguishable from each other or from modern samples taken from the same area despite independent evidence for differences in precipitation for the two prehistoric periods considered. Differences between modern samples were most strongly associated with soil characteristics. We discuss these results in light of their relationship with topography and vegetation and highlight their implications for archaeological applications of stable nitrogen analyses in several contexts. ► New stable nitrogen data for modern and ancient hares from the eastern Great Basin. ► Complementary data for other prehistoric game animals and modern vegetation. ► Hare δ 15N values highly enriched and highly variable within and between regions. ► Differences in δ 15N values tied to topography, soil, and plant inputs.
ISSN:0305-4403
1095-9238
DOI:10.1016/j.jas.2011.01.015