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New fossil woods from the early Cenozoic volcano-sedimentary rocks in the Fildes Peninsula, King George Island, and implications for the trans-Antarctic Peninsula Eocene climatic gradient
Chungbuk National University, South Korea.ORCID iD: 0000-0002-7820-0163
Universite Lyon.
Swedish Museum of Natural History, Department of Paleobiology.ORCID iD: 0000-0001-6723-239X
Korea Polar Research Institute.
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2020 (English)In: Papers in Palaeontology, ISSN 2056-2799, E-ISSN 2056-2802, Vol. 6, p. 1-29Article in journal (Refereed) Published
Abstract [en]

Ten embedded fossil logs sampled in situ from the middle Eocene volcano-sedimentary rocks close to Suffield Point in the Fildes Peninsula, King George Island,Antarctica, are assigned to Protopodocarpoxylon araucarioides Schultze-Motel ex Vogellehner, Phyllocladoxylon antarcticum Gothan, Agathoxylon antarcticum (Poole & Cantrill) Pujana et al., A. pseudoparenchymatosum (Gothan) Pujana et al. andan unidentified angiosperm wood. Differences in the taxonomic representation and growth-ring characters of the Eocene woods on King George Island and coeval assemblages from Seymour Island, on the western and eastern sides of the Antarctic Peninsula respectively, are interpreted to result from environmental and climatic gradients across the Peninsula Orogen during the early Palaeogene. In particular, a precipitation gradient inferred across the Peninsula at that time might have been induced by a rain-shadow effect.

Place, publisher, year, edition, pages
London, 2020. Vol. 6, p. 1-29
Keywords [en]
fossil woods, Eocene, Antarctica, growth-ring analysis, rainfall gradient, palaeoclimate
National Category
Other Earth Sciences
Research subject
Ecosystems and species history; The changing Earth
Identifiers
URN: urn:nbn:se:nrm:diva-3833DOI: 10.1002/spp2.1256OAI: oai:DiVA.org:nrm-3833DiVA, id: diva2:1502341
Funder
Swedish Research Council, 2014–5234
Note

This research is a part of the project ‘Long-Term Ecological Researches on King George Island to Predict Ecosystem Responses to Climate Change (PE15020)’ funded by the Korea Polar Research Institute, KOREA. Also funded by National Science Foundation (project #1636625)

Available from: 2020-11-01 Created: 2020-11-19 Last updated: 2025-02-07Bibliographically approved

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Oh, ChanghwanMcLoughlin, StephenLeppe, MarceloPark, Tae-Yoon
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