Rowan Whittle
British Antarctic Survey, Cambridge
Activity
2024
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QUANTIFYING EXTINCTION, ENVIRONMENT, AND ECOLOGICAL CHANGE ACROSS THE CRETACEOUS-PALEOGENE BOUNDARY ON SEYMOUR ISLAND, ANTARCTICA
T89 The Cretaceous-Paleogene (K-Pg) Boundary Interval: From Large-scale Geological Events to Mass Extinction MechanismsMonday, 23 September 20248:00 AM - 12:00 PM204C
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THE K-PG MASS EXTINCTION DID NOT PERMANENTLY RESTRUCTURE MARINE ECOSYSTEMS
T138 Life on the Boundary: Cretaceous/Paleogene Environments, Ecology, and Extinction Dynamics in AntarcticaMonday, 23 September 20241:30 PM - 5:30 PM204C
2020
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THE EVOLUTION OF BENTHIC ECOLOGY IN THE CENOZOIC OF ANTARCTICA
T114 Polar Paleobiology and Paleoenvironmental ProxiesWednesday, 28 October 202010:00 AM - 12:00 PMMeeting Rooms
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PALEOBIOGEOGRAPHY OF ANTARCTIC MOLLUSC BIVALVES AND THE ENVIRONMENTAL CHANGES AFTER THE CENOZOIC COOLING
T114 Polar Paleobiology and Paleoenvironmental ProxiesWednesday, 28 October 202010:00 AM - 12:00 PMMeeting Rooms
2019
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NATURE AND TIMING OF BIOTIC RECOVERY IN ANTARCTIC BENTHIC MARINE ECOSYSTEMS FOLLOWING THE CRETACEOUS–PALEOGENE MASS EXTINCTION
T247 Volcanism, Impacts, and Phanerozoic Mass Extinctions: Discovering a Common Cause and Planning for the 6th Mass Extinction IWednesday, 25 September 20198:00 AM - 12:00 PMRoom 227ABC, North Building
2018
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GLOBALLY DISCORDANT ISOCRINIDA (CRINOIDEA) MIGRATION CONFIRMS ASYNCHRONOUS MARINE MESOZOIC REVOLUTION
T136 Echinoderm Paleobiology II: In Honor of the Career of James SprinkleMonday, 5 November 20181:30 PM - 5:30 PMRoom 142
2015
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NO SAFER IN THE SOUTH: A SHALLOW MARINE MOLLUSCAN RECORD OF THE CRETACEOUS-PALEOGENE (K-PG) MASS EXTINCTION EVENT IN ANTARCTICA
T68 Mass Extinction Causality: Records of Anoxia, Acidification, and Global Warming during Earth's Greatest Crises IISunday, 1 November 20151:30 PM - 5:30 PMRoom 310