Abstract

Chen, K., Stilwell, J.D. & Mays, C., 12.3.2015. Palaeoenvironmental reconstruction of Livingston Island, Antarctic Peninsula in the Early Cretaceous: interpretations from the Walker Bay erratics. Alcheringa 39, 000–000. ISSN 0311-551Fossiliferous, volcaniclastic sandstone erratics, containing abundant plant fragments, palynomorphs and a possible insect wing, were extracted from the previously unstudied Walker Bay moraine, Livingston Island (ca 62°36ʹS, 60°42ʹW). These samples provide new insights into high southern latitude ecosystems of the South Shetland Islands region during the Early Cretaceous greenhouse interval. The palynofloral assemblage, in particular the co-occurrence of Ischyosporites punctatus, Concavissimisporites penolaensis and Reticulatisporites pudens, suggests that deposition could have occurred between the early Aptian and mid-Albian (ca 125–109 Ma), but was most likely early to mid-Albian (ca 112–109 Ma). The high relative abundance of the pteridophyte taxon, Cyathidites and associated fungal disaster taxa, together with significant quantities of volcaniclastic material, indicates a volcanically perturbed post-eruption riparian environment. Petrologic evidence suggests that the volcanic sediments were deposited rapidly in the above-mentioned fluvial setting. Comparisons to geological studies conducted on Livingston Island reveal an affinity of the Walker Bay erratics to the Byers Group; the unique palynofloral assemblage and petrological features of the erratics suggesting that the volcanogenic lithic sandstone facies may represent a previously undescribed unit of the upper Cerro Negro Formation.Kevin Chen [kevin.chen@monash.edu], Jeffrey D. Stilwell* [jeffrey.stilwell@monash.edu] & Chris Mays [chris.mays@monash.edu], School of Earth, Atmosphere and Environment, Faculty of Science, Monash University, Vic 3800, Australia. *Also affiliated with Australian Museum, 6 College Street, Sydney, NSW 2000, Australia.

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