Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet

The primary biomaterial used for stable isotope analysis to study diet in prehistoric and protohistoric populations is bone collagen, and requires destructive analysis and hence may dissuade museum curators from allowing access to this material. This study has investigated the use of dental calculus...

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Main Author: Simon Poulson
Format: Dataset
Language:unknown
Published: Arctic Data Center 2017
Subjects:
Online Access:https://doi.org/10.18739/A29P2W73Z
id dataone:doi:10.18739/A29P2W73Z
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spelling dataone:doi:10.18739/A29P2W73Z 2024-06-03T18:46:42+00:00 Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet Simon Poulson Greenland Iceland Colombia Belize Palau Peru Portugal United Kingdom Mexico ENVELOPE(-56.0,-20.0,77.0,60.0) BEGINDATE: 2014-08-01T00:00:00Z ENDDATE: 2017-07-31T00:00:00Z 2017-12-12T00:00:00Z https://doi.org/10.18739/A29P2W73Z unknown Arctic Data Center dental calculus diet stable isotopes carbon nitrogen Dataset 2017 dataone:urn:node:ARCTIC https://doi.org/10.18739/A29P2W73Z 2024-06-03T18:18:20Z The primary biomaterial used for stable isotope analysis to study diet in prehistoric and protohistoric populations is bone collagen, and requires destructive analysis and hence may dissuade museum curators from allowing access to this material. This study has investigated the use of dental calculus as an alternative to bone collagen, as it is a secondary or "add-on" biomaterial, which may ease access to required material for analysis. The goals of this research have been to determine whether stable isotope analysis of dental calculus can be used as an alternative to bone collagen, and whether the isotopic composition of dental calculus is a reliable indicator of the isotopic composition of diet. This study has performed stable isotope (d13C, d15N) and elemental analysis (weight% C, weight% N) of dental calculus for a number of opportunistically-sampled locations, including Greenland, Iceland and other non-Arctic locations. The majority of analyses have been performed using bulk dental calculus, but the organic carbon fraction (i.e. removal of the carbonate fraction by treatment with acid) has also been analyzed when sufficient material is available. Results of elemental analysis demonstrate that the atomic C/N ratio of dental calculus is a key indicator of possible post-depositional chemical alteration, as noted and proposed by previous researchers. For dental calculus samples that pass the C/N quality control criterion, results of stable isotope analysis indicate that the isotopic composition of dental calculus shows good correlation with the isotopic composition of bone collagen for the same populations, and hence that the isotopic composition of dental calculus shows promise as an alternate biomaterial to bone collagen as an indicator of diet history when bone collagen material may be unavailable. Dataset Arctic Greenland Iceland Arctic Data Center (via DataONE) Arctic Greenland ENVELOPE(-56.0,-20.0,77.0,60.0)
institution Open Polar
collection Arctic Data Center (via DataONE)
op_collection_id dataone:urn:node:ARCTIC
language unknown
topic dental calculus
diet
stable isotopes
carbon
nitrogen
spellingShingle dental calculus
diet
stable isotopes
carbon
nitrogen
Simon Poulson
Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet
topic_facet dental calculus
diet
stable isotopes
carbon
nitrogen
description The primary biomaterial used for stable isotope analysis to study diet in prehistoric and protohistoric populations is bone collagen, and requires destructive analysis and hence may dissuade museum curators from allowing access to this material. This study has investigated the use of dental calculus as an alternative to bone collagen, as it is a secondary or "add-on" biomaterial, which may ease access to required material for analysis. The goals of this research have been to determine whether stable isotope analysis of dental calculus can be used as an alternative to bone collagen, and whether the isotopic composition of dental calculus is a reliable indicator of the isotopic composition of diet. This study has performed stable isotope (d13C, d15N) and elemental analysis (weight% C, weight% N) of dental calculus for a number of opportunistically-sampled locations, including Greenland, Iceland and other non-Arctic locations. The majority of analyses have been performed using bulk dental calculus, but the organic carbon fraction (i.e. removal of the carbonate fraction by treatment with acid) has also been analyzed when sufficient material is available. Results of elemental analysis demonstrate that the atomic C/N ratio of dental calculus is a key indicator of possible post-depositional chemical alteration, as noted and proposed by previous researchers. For dental calculus samples that pass the C/N quality control criterion, results of stable isotope analysis indicate that the isotopic composition of dental calculus shows good correlation with the isotopic composition of bone collagen for the same populations, and hence that the isotopic composition of dental calculus shows promise as an alternate biomaterial to bone collagen as an indicator of diet history when bone collagen material may be unavailable.
format Dataset
author Simon Poulson
author_facet Simon Poulson
author_sort Simon Poulson
title Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet
title_short Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet
title_full Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet
title_fullStr Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet
title_full_unstemmed Testing Stable Isotopes of Human Dental Calculus as a Nondestructive Proxy for Paleodiet
title_sort testing stable isotopes of human dental calculus as a nondestructive proxy for paleodiet
publisher Arctic Data Center
publishDate 2017
url https://doi.org/10.18739/A29P2W73Z
op_coverage Greenland
Iceland
Colombia
Belize
Palau
Peru
Portugal
United Kingdom
Mexico
ENVELOPE(-56.0,-20.0,77.0,60.0)
BEGINDATE: 2014-08-01T00:00:00Z ENDDATE: 2017-07-31T00:00:00Z
long_lat ENVELOPE(-56.0,-20.0,77.0,60.0)
geographic Arctic
Greenland
geographic_facet Arctic
Greenland
genre Arctic
Greenland
Iceland
genre_facet Arctic
Greenland
Iceland
op_doi https://doi.org/10.18739/A29P2W73Z
_version_ 1800869913489833984