Gymnosperm woods from the Cretaceous (mid-Aptian) Cerro Negro Formation, Byers Peninsula, Livingston Island, Antarctica: the arborescent vegetation of a volcanic arc
Silicified gymnosperm trunks usually more than 30 cm in diameter and several metres in length occur abundantly in the lower part of the mid-AptianCerroNegroFormation, which crops out on ByersPeninsula, LivingstonIsland, northern Antarctic Peninsula. These fossil woods are found within silicic ignimb...
| Published in: | Cretaceous Research |
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| Main Authors: | , |
| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
Academic Press
2001
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| Subjects: | |
| Online Access: | http://nora.nerc.ac.uk/id/eprint/18591/ http://www.sciencedirect.com/science/article/pii/S0195667101902599 |
| Summary: | Silicified gymnosperm trunks usually more than 30 cm in diameter and several metres in length occur abundantly in the lower part of the mid-AptianCerroNegroFormation, which crops out on ByersPeninsula, LivingstonIsland, northern Antarctic Peninsula. These fossil woods are found within silicic ignimbrites, tuffs and lapilli-tuffs interpreted as the product of hot pyroclastic flows, and in silicic and andesitic conglomerates interpreted as fluvially-reworked volcanic sediments. A detailed quantitative study of the wood taxonomy has revealed the presence of three form genera, Araucarioxylon,Podocarpoxylon , and Sahnioxylon. The former two genera represent the conifer families Araucariaceae and Podocarpaceae respectively and the latter probably belongs to the extinct gymnosperm order Bennettitales. These wood genera represent the remains of the arborescentvegetation, which grew on the margins of an active pyroclastic volcanic cone near the edge of the mid-Cretaceous Antarctic Circle (palaeolatitude 62°S). |
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