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Partially pyritised Holocene Banksia cones from Tianjara Plateau, New South Wales
Citation
Gibson, JAE and Jordan, GJ and Gibson, DL, Partially pyritised Holocene Banksia cones from Tianjara Plateau, New South Wales, Proceedings of the Linnean Society of New South Wales, 114, (3) pp. 171-177. ISSN 1839-7263 (1994) [Refereed Article]
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Copyright Statement
Licenced under Creative Commons Attribution-NonCommercial-ShareAlike 3.0 Unported (CC BY-NC-SA 3.0) http://creativecommons.org/licenses/by-nc-sa/3.0/
Official URL: http://www.biodiversitylibrary.org/page/34926317#p...
Abstract
Partially mineralised Banksia ericifolia L.f. cones collected from the Tianjara Plateau, New South Wales are described. The fossils have an outer layer of pyrite covering a charcoal interior. The cones were burnt prior to burial. Adsorbed organic material was subsequently oxidised under anaerobic conditions. Pyrite was formed by the precipitation of sulphide, produced by the concomitant reduction of sulphate, and ferrous ions. Carbon dating of material from the inside of one sample gave a conventional radiocarbon age of 6130 ± 80 BP.
Item Details
Item Type: | Refereed Article |
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Keywords: | taphonomy, diagenesis, fossilisation |
Research Division: | Earth Sciences |
Research Group: | Geology |
Research Field: | Palaeontology (incl. palynology) |
Objective Division: | Expanding Knowledge |
Objective Group: | Expanding knowledge |
Objective Field: | Expanding knowledge in the environmental sciences |
UTAS Author: | Gibson, JAE (Dr John Gibson) |
UTAS Author: | Jordan, GJ (Professor Greg Jordan) |
ID Code: | 88900 |
Year Published: | 1994 |
Deposited By: | Plant Science |
Deposited On: | 2014-02-19 |
Last Modified: | 2014-07-01 |
Downloads: | 193 View Download Statistics |
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