Oxygen, strontium, and sulfur isotopes in modern deer bone from Virginia, USA: a model for geographic location in east coast North America
收藏DataCite Commons2026-05-13 更新2026-04-25 收录
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https://tandf.figshare.com/articles/dataset/Oxygen_strontium_and_sulfur_isotopes_in_modern_deer_bone_from_Virginia_USA_a_model_for_geographic_location_in_east_coast_North_America/30642661/1
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资源简介:
Understanding movements of animals and people in modern or historic contexts is hindered by limited animal tissue proxies to indicate regional origins. On North America’s east coast, stable oxygen and hydrogen isoscapes provide broad latitudinal proxies, but more nuanced geographical proxies are lacking. This study examines oxygen, strontium, and sulfur isotopes in deer bone bioapatite and collagen from Virginia, USA, which reflects grazing location, to create the first robust δ<sup>34</sup>S<sub>collagen</sub> distribution in this region, contribute new <sup>87</sup>Sr/<sup>86</sup>Sr<sub>bone</sub> data to a currently small regional dataset, consider δ<sup>18</sup>O<sub>bioapatite</sub> values on a more nuanced scale, determine which isotope systems best indicate particular regions, and especially consider the efficacy of δ<sup>34</sup>S<sub>collagen</sub> for geographic location. Random forest models show longitudinal trends in δ<sup>18</sup>O<sub>bioapatite</sub> and <sup>87</sup>Sr/<sup>86</sup>Sr<sub>bone</sub> data; δ<sup>34</sup>S<sub>collagen</sub> values were more variable across Virginia with unique values in specific areas. Model results suggest δ<sup>18</sup>O<sub>bioapatite</sub> values are most affected by geomorphic and meteorological controls, specifically altitude effects of the Appalachian Mountains, aridity, and mean annual temperature. The <sup>87</sup>Sr/<sup>86</sup>Sr<sub>bone</sub> ratios are controlled largely by underlying bedrock geology, allochthonous dust and sea spray deposition, and surface source mixing. The western coal-bearing formations of the Appalachian Plateau showed relatively low δ<sup>34</sup>S<sub>collagen</sub> values; the eastern Coastal Plains showed relatively high δ<sup>34</sup>S<sub>collagen</sub> resulting from dust and sea spray deposition. Modeled proxies for modern anthropogenic inputs of these elements (e.g. fossil fuels) notably were not strong controlling factors for these isotope systems; therefore, the models produced here are suitable for identification of geographic location using bone isotope values from modern, historic, or paleontological samples. Linear discriminant analysis suggests A multi-isotope approach using δ<sup>18</sup>O<sub>bioapatite</sub>, <sup>87</sup>Sr/<sup>86</sup>Sr<sub>bone</sub>, and δ<sup>34</sup>S<sub>collagen</sub> data provides a more nuanced geographic prediction than one isotope system alone in this region. The δ<sup>34</sup>S<sub>collagen</sub> values in particular are emerging as a potential new proxy to indicate broad east–west movements of animals and people.
提供机构:
Taylor & Francis
创建时间:
2025-11-17



