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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.
Naturhistoriska riksmuseet, Enheten för paleobiologi.ORCID-id: 0000-0001-6723-239X
Korea Polar Research Institute.
Vise andre og tillknytning
2020 (engelsk)Inngår i: Papers in Palaeontology, ISSN 2056-2799, E-ISSN 2056-2802, Vol. 6, s. 1-29Artikkel i tidsskrift (Fagfellevurdert) 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.

sted, utgiver, år, opplag, sider
London, 2020. Vol. 6, s. 1-29
Emneord [en]
fossil woods, Eocene, Antarctica, growth-ring analysis, rainfall gradient, palaeoclimate
HSV kategori
Forskningsprogram
Ekosystem och arthistoria; Den föränderliga jorden
Identifikatorer
URN: urn:nbn:se:nrm:diva-3833DOI: 10.1002/spp2.1256OAI: oai:DiVA.org:nrm-3833DiVA, id: diva2:1502341
Forskningsfinansiär
Swedish Research Council, 2014–5234
Merknad

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)

Tilgjengelig fra: 2020-11-01 Laget: 2020-11-19 Sist oppdatert: 2025-09-12bibliografisk kontrollert

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