Uncharted permian to jurassic continental deposits in the far north of victoria land, east antarctica

• Published in: Journal of the Geological Society
• Main Authors: Bomfleur, Benjamin, Mörs, Thomas, Unverfärth, Jan, Liu, Feng, Läufer, Andreas, Castillo, Paula, Oh, Changhwan, Park, Tae-Yoon S., Woo, Jusun, Crispini, Laura
• Format: Article in Journal/Newspaper
• Language: unknown
• Published: Geological Society of London 2021
• Subjects: CENTRAL TRANSANTARCTIC MOUNTAINS; BRAIDED RIVER DEPOSIT; BEACON SUPERGROUP; TRIASSIC BOUNDARY; AGE CONSTRAINTS; ASSEMBLAGES; STRATIGRAPHY; GONDWANA; FOSSILS; GEOLOGY; East Antarctica; Victoria Land; Transantarctic Mountains; Rennick; Rennick Glacier; Section Peak; Van der Hoeven; Helliwell Hills; Antarc*; Antarctica
• Online Access: https://hdl.handle.net/10371/197852; https://doi.org/10.1144/jgs2020-062

© 2020 The Author(s). Published by The Geological Society of London. All rights reserved.The remote lower reaches of the Rennick Glacier in the far north of Victoria Land hold some of the least-explored outcrop areas of the Transantarctic basin system. Following recent international field-work efforts in the Helliwell Hills, we here provide a comprehensive emendation to the regional stratigraphy. Results of geological and palaeontological reconnaissance and of petrographic, geochemical and palynostratigraphic analyses reveal a stack of three previously unknown sedimentary units in the study area: the Lower Triassic Van der Hoeven Formation (new unit, 115+ m thick) consists mainly of quartzose sandstone and non-carbonaceous mudstone rich in continental trace fossils. The Middle to Upper Triassic Helliwell Formation (new unit, 235 m thick) consists of coal-bearing overbank deposits and volcaniclastic sandstone and yielded typical plant fossils of the Gondwanan Dicroidium flora together with plant-bearing silicified peat. The succession is capped by c. 14 m of the sandstone-dominated Section Peak Formation (uppermost Triassic–Lower Jurassic). Our results enable more detailed correlation of the Palaeozoic–Mesozoic successions throughout East Antarctica and into Tasmania. Of particular interest is one section that spans the end-Permian mass extinction interval, which promises to allow detailed reconstructions of high-latitude vegetation dynamics across this critical interval in Earth history. N 1