D/H in beetle chitin from the late-glacial Lismore site in eastern Canada: supplementary note

Authors

  • Randall F. Miller Steinhammer Palaeontology Laboratory, Natural Sciences Division, New Brunswick Museum, Saint John NB

DOI:

https://doi.org/10.4138/2120

Abstract

D/H (Deuterium-Hydrogen) analysis of chitin from a late-glacial site in eastern Canada demonstrates promising results and lends support to other evidence for the Killarney Oscillation. RÉSUMÉ L'analyse du rapport D/H (Dentérium-Hydrogène) de chitine provenant d'un site tardi-glaciaire dans l'Est du Canada démontre des résultats prometteurs et vient appuyer d'autres données pour l'oscillation de Killarney. [Traduit par la rédaction]

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Published

1994-03-01

How to Cite

Miller, R. F. (1994). D/H in beetle chitin from the late-glacial Lismore site in eastern Canada: supplementary note. Atlantic Geoscience, 30(1). https://doi.org/10.4138/2120

Issue

Vol. 30 No. 1 (1994)

Section

Articles

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