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Sampling and Pretreatment of Tooth Enamel Carbonate for Stable Carbon and Oxygen Isotope Analysis
Published on: August 15, 2018
Magnesium stable isotope ecology using mammal tooth enamel
Jeremy E Martin1, Derek Vance2, Vincent Balter3
1Bristol Isotope Group, School of Earth Sciences, University of Bristol, Bristol BS8 1RJ, United Kingdom; UMR 5276 CNRS, Laboratoire de Géologie de Lyon: Terre, Planètes, et Environnement, École Normale Supérieure de Lyon et Université Lyon 1, 69364 Lyon, France; and jeremy.martin@ens-lyon.fr.
Stable magnesium isotopes (δ(26)Mg) in tooth enamel can reveal ancient diets. This study shows δ(26)Mg values increase with trophic level, distinguishing herbivores from omnivores when combined with barium/calcium ratios.
Area of Science:
- Paleoecology
- Geochemistry
- Isotope analysis
Background:
- Traditional paleodietary proxies like carbon isotopes (δ(13)C) have limitations.
- Nontraditional stable isotopes offer new avenues for reconstructing complex diets.
Purpose of the Study:
- To investigate the utility of stable magnesium isotopes (δ(26)Mg) as a paleodietary proxy.
- To assess the relationship between δ(26)Mg in tooth enamel and an animal's trophic level.
Main Methods:
- Analysis of tooth enamel, vegetation, and feces from 11 extant African mammal species.
- Measurement of δ(26)Mg, δ(13)C, Sr/Ca, and Ba/Ca ratios.
Main Results:
- Tooth enamel δ(26)Mg values increase from herbivores to omnivores/faunivores.
- A potential mechanism for this enrichment is increased δ(26)Mg in muscle tissue.
- δ(26)Mg combined with Ba/Ca ratios can differentiate herbivores from omnivores.
Conclusions:
- Stable magnesium isotopes show promise for paleodietary reconstruction, particularly for distinguishing feeding strategies.
- Multiproxy approaches incorporating δ(26)Mg can refine our understanding of ancient trophic ecology.
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