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Annals of Botany 88: 33-54, 2001
© 2001 Annals of Botany Company

A Fossil Wood Flora from King George Island: Ecological Implications for an Antarctic Eocene Vegetation

Imogen Poole+, Richard J. Hunt and David J. Cantrill

Wood Anatomy Section, National Herbarium of the Netherlands Utrecht University branch, P.O. Box 80102, 3585, CS, Utrecht, The Netherlands School of Earth Sciences, University of Leeds, Leeds, LS2 9JT, UK British Antarctic Survey, Natural Environmental Research Council, Madingley Road, High Cross, Cambridge, CB3 0ET, UK

Received: 11 December 2000 ; Returned for revision: 12 February 2001 . Accepted: 16 March 2001

Early Tertiary sediments of the Antarctic Peninsula region continue to yield a rich assemblage of well-preserved fossil dicotyledonous angiosperm wood. The wood flora under consideration is from the Collins Glacier region on Fildes Peninsula, King George Island and is derived from tuffaceous sediments of the Middle Unit of the Fildes Formation. These deposits accumulated in a volcanic setting adjacent to a basic-intermediate stratocone. The fossil assemblage provides further evidence for the existence of cool temperate forests, similar in composition to those found today in New Zealand, Australia and, in particular, southern South America. This paper describes two conifer and five angiosperm morphotypes, four of which are new additions to the Antarctica palaeoflora records. Cupressinoxylon Goeppert, which is the dominant conifer in terms of numbers, and Podocarpoxylon Gothan represent the conifers. The angiosperm component includes two species ofNothofagoxylon and two previously undescribed wood morphotypes that exhibit greatest anatomical similarity to woods ofLuma A. Gray (Myrtaceae) and Eucryphia Cav. (Cunoniaceae). These morphotypes are described and assigned to the organ genera Myrceugenelloxylon Nishida, and Weinmannioxylon Petriella, respectively. A model based on the extant cool temperate Valdivian rainforests is proposed and ecological reconstructions based on palaeobotanical and geological evidence suggest that changes in the palaeovegetation reflect natural dynamics following volcanic disturbances.Copyright 2001 Annals of Botany Company

Fossil wood, Antarctica, Myrtaceae, Eucryphia, Nothofagaceae, Eocene, Valdivia, Tertiary


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