Palynological Evidence from Seymour Island, Antarctic Peninsula
Palaeogeography, Palaeoclimatology, Palaeoecology 408 (2014) 26–47 Contents lists available at ScienceDirect Palaeogeography, Palaeoclimatology, Palaeoecology journal homepage: www.elsevier.com/locate/palaeo Latest Cretaceous–earliest Paleogene vegetation and climate change at the high southern latitudes: palynological evidence from Seymour Island, Antarctic Peninsula Vanessa C. Bowman a,⁎, Jane E. Francis a,RosemaryA.Askinb, James B. Riding c, Graeme T. Swindles d a British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 0ET, UK b Jackson, WY, USA c British Geological Survey, Environmental Science Centre, Keyworth, Nottingham NG12 5GG, UK d School of Geography, University of Leeds, Leeds LS2 9JT, UK article info abstract Article history: Fluctuations in Late Cretaceous climate were already influencing biotic change prior to the environmental up- Received 21 January 2014 heaval at the Cretaceous–Paleogene (K–Pg) boundary, but their general nature, magnitude and timing remain Received in revised form 29 April 2014 controversial. A high-resolution dataset on terrestrially-derived palynomorphs is presented from the high south- Accepted 30 April 2014 ern palaeolatitudes that unlocks details of small-scale climate variability throughout this period of significant Available online 9 May 2014 global change. Specifically, this is a quantitative spore and pollen analysis of an expanded uppermost Cretaceous to lowermost Paleogene (Maastrichtian–earliest Danian) shallow marine sedimentary succession from Seymour Keywords: Late Cretaceous Island, off the northeastern tip of the Antarctic Peninsula, then (as now) located at ~65°S. Using nearest living rel- Paleogene atives the first detailed vegetation, habitat and climate reconstruction is presented for the emergent volcanic arc Pollen at this time. On the coastal lowlands, a cool to warm temperate rainforest is envisaged growing in a riverine land- Palaeoclimate scape, with both wet (river margin, pond) and relatively dry (interfluve, canopy gap) habitats.
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