Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants
The Promontory caves (Utah) and Franktown Cave (Colorado) contain high-fidelity records of short-term occupations by groups with material culture connections to the Subarctic/Northern Plains. This research uses Promontory and Franktown bison dung, hair, hide, and bone collagen to establish local bas...
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ftzenodo:oai:zenodo.org:4341326 2024-09-15T18:38:04+00:00 Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants Metcalfe, Jessica Ives, John Shirazi, Sabrina Gilmore, Kevin Hallson, Jennifer Brock, Fiona Clark, Bonnie Shapiro, Beth 2021-07-23 https://doi.org/10.7291/D18Q23 unknown Zenodo https://zenodo.org/communities/dryad https://doi.org/10.7291/D18Q23 oai:zenodo.org:4341326 info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode info:eu-repo/semantics/other 2021 ftzenodo https://doi.org/10.7291/D18Q23 2024-07-25T15:45:02Z The Promontory caves (Utah) and Franktown Cave (Colorado) contain high-fidelity records of short-term occupations by groups with material culture connections to the Subarctic/Northern Plains. This research uses Promontory and Franktown bison dung, hair, hide, and bone collagen to establish local baseline carbon isotopic variability and identify leather from a distant source. The ankle wrap of one Promontory Cave 1 moccasin had a δ 13 C value that indicates a substantial C 4 component to the animal's diet, unlike the C 3 diets inferred from 171 other Promontory and northern Utah bison samples. We draw on a unique combination of multi-tissue isotopic analysis, carbon isoscapes, ancient DNA (species and sex identification), tissue turnover rates, archaeological contexts, and bison ecology to show that the high δ 13 C value was not likely a result of local plant consumption, bison mobility, or trade. Rather, the bison hide was likely acquired via long-distance travel to/from an area of abundant C 4 grasses far to the south or east. Expansive landscape knowledge gained through long-distance associations would have allowed Promontory caves inhabitants to make well-informed decisions about directions and routes of movement for a territorial shift, which seems to have occurred in the late thirteenth century. We have uploaded alignments (.bam files) of these shotgun data to bison (Bison bison; NCBI GCA_000754665), cattle (Bos taurus; NCBI Btau_4.6.1), bighorn sheep (Ovis canadensis; NCBI CP011912.1), and two-toed sloth (Choloepus hoffmanni; NCBI5KN174222.1) genomes. We have not supplied raw shotgun data because there is a chance that ancient human DNA could be examined from these Moccasin samples and we do not have permission to study this DNA. Other/Unknown Material Subarctic Bison bison bison Zenodo |
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The Promontory caves (Utah) and Franktown Cave (Colorado) contain high-fidelity records of short-term occupations by groups with material culture connections to the Subarctic/Northern Plains. This research uses Promontory and Franktown bison dung, hair, hide, and bone collagen to establish local baseline carbon isotopic variability and identify leather from a distant source. The ankle wrap of one Promontory Cave 1 moccasin had a δ 13 C value that indicates a substantial C 4 component to the animal's diet, unlike the C 3 diets inferred from 171 other Promontory and northern Utah bison samples. We draw on a unique combination of multi-tissue isotopic analysis, carbon isoscapes, ancient DNA (species and sex identification), tissue turnover rates, archaeological contexts, and bison ecology to show that the high δ 13 C value was not likely a result of local plant consumption, bison mobility, or trade. Rather, the bison hide was likely acquired via long-distance travel to/from an area of abundant C 4 grasses far to the south or east. Expansive landscape knowledge gained through long-distance associations would have allowed Promontory caves inhabitants to make well-informed decisions about directions and routes of movement for a territorial shift, which seems to have occurred in the late thirteenth century. We have uploaded alignments (.bam files) of these shotgun data to bison (Bison bison; NCBI GCA_000754665), cattle (Bos taurus; NCBI Btau_4.6.1), bighorn sheep (Ovis canadensis; NCBI CP011912.1), and two-toed sloth (Choloepus hoffmanni; NCBI5KN174222.1) genomes. We have not supplied raw shotgun data because there is a chance that ancient human DNA could be examined from these Moccasin samples and we do not have permission to study this DNA. |
format |
Other/Unknown Material |
author |
Metcalfe, Jessica Ives, John Shirazi, Sabrina Gilmore, Kevin Hallson, Jennifer Brock, Fiona Clark, Bonnie Shapiro, Beth |
spellingShingle |
Metcalfe, Jessica Ives, John Shirazi, Sabrina Gilmore, Kevin Hallson, Jennifer Brock, Fiona Clark, Bonnie Shapiro, Beth Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants |
author_facet |
Metcalfe, Jessica Ives, John Shirazi, Sabrina Gilmore, Kevin Hallson, Jennifer Brock, Fiona Clark, Bonnie Shapiro, Beth |
author_sort |
Metcalfe, Jessica |
title |
Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants |
title_short |
Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants |
title_full |
Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants |
title_fullStr |
Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants |
title_full_unstemmed |
Isotopic evidence for long-distance connections of the AD thirteenth century Promontory caves occupants |
title_sort |
isotopic evidence for long-distance connections of the ad thirteenth century promontory caves occupants |
publisher |
Zenodo |
publishDate |
2021 |
url |
https://doi.org/10.7291/D18Q23 |
genre |
Subarctic Bison bison bison |
genre_facet |
Subarctic Bison bison bison |
op_relation |
https://zenodo.org/communities/dryad https://doi.org/10.7291/D18Q23 oai:zenodo.org:4341326 |
op_rights |
info:eu-repo/semantics/openAccess Creative Commons Zero v1.0 Universal https://creativecommons.org/publicdomain/zero/1.0/legalcode |
op_doi |
https://doi.org/10.7291/D18Q23 |
_version_ |
1810482399961677824 |