[Papers in Palaeontology, Vol. 6, Part 1, 2020, pp. 1–29] NEW FOSSIL WOODS FROM LOWER CENOZOIC VOLCANO-SEDIMENTARY ROCKS OF THE FILDES PENINSULA, KING GEORGE ISLAND, AND THE IMPLICATIONS FOR THE TRANS-ANTARCTIC PENINSULA EOCENE CLIMATIC GRADIENT by CHANGHWAN OH1 , MARC PHILIPPE2 , STEPHEN MCLOUGHLIN3 , JUSUN WOO4,MARCELOLEPPE5 ,TERESATORRES6, TAE-YOON S. PARK4 and HAN-GU CHOI7 1Department of Earth & Environmental Sciences, Chungbuk National University, Cheongju 28644, Korea;
[email protected] 2Universite Lyon 1 & CNRS, UMR 5023, 7 rue Dubois, F69622 Villeurbanne, France;
[email protected] 3Department of Palaeobiology, Swedish Museum of Natural History, Box 50007, S-104 05 Stockholm, Sweden;
[email protected] 4Division of Polar Earth-System Sciences, Korea Polar Research Institute, Incheon 21990, Korea;
[email protected],
[email protected] 5Instituto Antartico Chileno (INACH), Plaza Munoz~ Gamero 1055 Punta Arenas, Chile;
[email protected] 6Facultad de Ciencias Agronomicas Casilla 1004, Universidad Chile, Santiago, Chile;
[email protected] 7Division of Polar Life Sciences, Korea Polar Research Institute, Incheon 21990, Korea;
[email protected] Typescript received 14 August 2018; accepted in revised form 22 November 2018 Abstract: Ten embedded fossil logs sampled in situ from assemblages from Seymour Island, on the western and east- the middle Eocene volcano-sedimentary rocks close to Suf- ern sides of the Antarctic Peninsula respectively, are inter- field Point in the Fildes Peninsula, King George Island, preted to result from environmental and climatic gradients Antarctica, are assigned to Protopodocarpoxylon araucarioides across the Peninsula Orogen during the early Palaeogene. In Schultze-Motel ex Vogellehner, Phyllocladoxylon antarcticum particular, a precipitation gradient inferred across the Penin- Gothan, Agathoxylon antarcticum (Poole & Cantrill) Pujana sula at that time might have been induced by a rain-shadow et al., A.