Triassic Kykloxylon wood (Umkomasiaceae, Gymnospermopsida) from Skinner Ridge, northern Victoria Land, East Antarctica

International audience During the ␣rst Korea Antarctic Geological Expedition (KAGEX I, 2013/2014), fossil wood was collected from the Triassic ␣uvial deposits of the Beacon Supergroup at Skinner Ridge in northern Victoria Land, Antarctica. The material is coali␣ed and partially silici␣ed; most speci...

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Bibliographic Details
Published in:Review of Palaeobotany and Palynology
Main Authors: Oh, Changhwan, Park, Tae-Yoon, Woo, Jusun, Bomfleur, Benjamin, Philippe, Marc, Decombeix, Anne-Laure, Kim, Young-Hwan G., Lee, Jong Ik
Other Authors: Division of Polar Earth-System Sciences, Korea Polar Research Institute (KOPRI), Forschungsstelle für Paläobotanik, Westfälische Wilhelms-Universität Münster (WWU), Department of Palaeobotany, Swedish Museum of Natural History, Laboratoire d'Ecologie des Hydrosystèmes Naturels et Anthropisés (LEHNA), Université Claude Bernard Lyon 1 (UCBL), Université de Lyon-Université de Lyon-École Nationale des Travaux Publics de l'État (ENTPE)-Centre National de la Recherche Scientifique (CNRS), Botanique et Modélisation de l'Architecture des Plantes et des Végétations (UMR AMAP), Centre National de la Recherche Scientifique (CNRS)-Université de Montpellier (UM)-Institut National de la Recherche Agronomique (INRA)-Centre de Coopération Internationale en Recherche Agronomique pour le Développement (Cirad)-Institut de Recherche pour le Développement (IRD France-Sud ), Polar Science, University of Science and Technology
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2016
Subjects:
Online Access:https://hal-sde.archives-ouvertes.fr/hal-01369185
https://doi.org/10.1016/j.revpalbo.2016.07.006
Description
Summary:International audience During the ␣rst Korea Antarctic Geological Expedition (KAGEX I, 2013/2014), fossil wood was collected from the Triassic ␣uvial deposits of the Beacon Supergroup at Skinner Ridge in northern Victoria Land, Antarctica. The material is coali␣ed and partially silici␣ed; most specimens are slightly compressed due to burial compaction. In spite of this imperfect preservation, anatomical features of both the xylem and the pith could be observed in some specimens. The xylem displays prominent growth rings and usually araucarioid or somewhat mixed- type radial pitting with some abnormal rings partly composed of parenchymatous tissues. Some specimens also have a wood cylinder that is divided radially by parenchymatous zones. These anatomical features indicate a systematic af␣nity with Kykloxylon Mey.-Berth., T.N.Taylor et Ed.L.Taylor, a characteristic wood type of the Umkomaciaceae, which ␣ourished throughout Gondwana during the Triassic. The Kykloxylon specimens in this study represent the only wood fossil taxon in the Triassic of Victoria Land, except for a dubious report of Antarcticoxylon Seward in 1914. This may indicate a low diversity of Triassic wood fossils in this area, as in other parts of Antarctica. On the contrary, diverse other gymnosperm organs are known to occur in the Triassic of Antarctica. This low diversity of wood taxa compared to the various plant organs in the Triassic of Antarctica is remarkable. We hypothesize three major reasons for this: 1) the overall structural uniformity of gymnosperm wood compared to other vegetative and especially reproductive organ diversity; 2) the overwhelming dominance of corystosperm plants, with a minor component of voltzialean conifers in the canopy-forming forest vegetation during the Triassic in Antarctica; and 3) the very few systematic studies of fossil wood compared to other plant macrofossils.