Isotope analysis of human dental calculus δ 13 CO 3 2− : Investigating a potential new proxy for sugar consumption-Reference-Cited by-同舟云学术

Isotope analysis of human dental calculus δ ¹³ CO ₃ ²⁻ : Investigating a potential new proxy for sugar consumption

Published:2022-03-25 Issue:11 Volume:36 Page:
ISSN:0951-4198
Container-title:Rapid Communications in Mass Spectrometry
language:en
Short-container-title:Rapid Comm Mass Spectrometry

Author:

Chidimuro Blessing¹²^ORCID,Mundorff Amy³^ORCID,Speller Camilla²⁴^ORCID,Radini Anita²^ORCID,Boudreault Noémie²,Lucas Mary²⁵,Holst Malin²⁶^ORCID,Lamb Angela⁷^ORCID,Collins Matthew²⁸⁹^ORCID,Alexander Michelle²^ORCID

Affiliation:

1. Department of Geography and Environmental Science University of Reading Reading UK

2. BioArCh, Department of Archaeology University of York York UK

3. Department of Anthropology University of Tennessee Knoxville Tennessee USA

4. Department of Anthropology University of British Columbia Vancouver BC Canada

5. Department of Archaeology Max Planck Institute for the Science of Human History Jena Germany

6. York Osteoarchaeology Ltd, Bishop Wilton York UK

7. National Environmental Isotope Facility, British Geological Survey Keyworth UK

8. Natural History Museum University of Copenhagen Denmark

9. Department of Archaeology University of Cambridge Cambridge UK

Funder

Arts and Humanities Research Council

University of York

University of Leicester

University of Tennessee

Publisher

Wiley

Subject

Organic Chemistry,Spectroscopy,Analytical Chemistry

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/rcm.9286

Reference93 articles.

1. Direct evidence of milk consumption from ancient human dental calculus

2. Proteomic evidence of dietary sources in ancient dental calculus

3. Dental calculus in the industrial age: Human dental calculus in the Post-Medieval period, a case study from industrial Manchester

4. Stable carbon and nitrogen isotopes of human dental calculus: a potentially new non-destructive proxy for paleodietary analysis

5. Paleodiet in northern Chile through the Holocene: extremely heavy δ15N values in dental calculus suggest a guano-derived signature?

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