Adelaide Research & Scholarship
Please use this identifier to cite or link to this item:
https://hdl.handle.net/2440/45094
| Citations | ||
| Scopus | Web of Science® | Altmetric |
|---|---|---|
|
?
|
?
|
|
| Type: | Journal article |
| Title: | Variations of the Eocene climate reflected in the isotopic composition of fossil resins from the Northwest Territories, Canada |
| Author: | Tappert, Ralf Wolfe, Alexander P. Muehlenbachs, Karl |
| Citation: | Geochimica et Cosmochimica Acta, 2007; 71(15, S1):A1004 |
| Part of: | Awards Ceremony Speeches and Abstracts of the 17th Annual V. M. Goldschmidt Conference Cologne, Germany August 2007 |
| Publisher: | Elsevier |
| Issue Date: | 2007 |
| ISSN: | 0016-7037 |
| School/Discipline: | School of Earth and Environmental Sciences : Geology and Geophysics |
| Statement of Responsibility: | R. Tappert, A. Wolfe and K. Muehlenbachs |
| Abstract: | Middle Eocene conifer resins have been analyzed for their C and H isotopic compositions, as well as spectral characteristics using FTIR. The resins were recovered from an unlithified peat sequence that forms part of the infill of the Giraffe kimberlite crater in the Lac de Gras field, Northwest Territories, Canada. Based on the presence of well-preserved macrofossils and FTIR spectra of fossil and modern resins, it is believed that the fossil resins were produced by Metasequoia glyptostroboides. |
| Rights: | Copyright © 2007 Published by Elsevier Ltd. |
| DOI: | 10.1016/j.gca.2007.06.027 |
| Appears in Collections: | Geology & Geophysics publications |
Files in This Item:
There are no files associated with this item.
Items in DSpace are protected by copyright, with all rights reserved, unless otherwise indicated.