Thomas H.G. Ezard
University of Southampton, Southampton
Activity
2022
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A TRANSITION TO AUTOMATED PHENOTYPIC METHODS
T262 Integrative Perspectives on Morphological Change: Shaping Our Understanding of the Fossil RecordWednesday, 12 October 20221:30 PM - 5:30 PMMile High Ballroom 3C
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DO BIOTIC CONTROLS BUFFER AGAINST CLIMATE-DRIVEN EXTINCTION THREATS?
T192 Conservation Paleobiology: Lessons from the Past, Guidance for the Future IITuesday, 11 October 20221:30 PM - 5:30 PMMile High Ballroom 4A
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LASER ABLATION MASS SPECTROMETRY BLAST THROUGH DETECTION IN R
T118 Insights from Microfossils and Their Modern Analogs: From Traditional and Emerging Approaches to Critical Re-EvaluationsMonday, 10 October 20221:30 PM - 5:30 PM506
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INFERRING SPECIATION AND POST-SPECIATION DIVERGENCE BY DEPTH PARAPATRY
T49 New Advances in GeobiologySunday, 9 October 20221:30 PM - 5:30 PMMile High Ballroom 2C
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IS POROSITY A FUNCTIONAL TRAIT IN PLANKTIC FORAMINIFERA?
T48 Exploring the Mechanisms of Morphologic Change IISunday, 9 October 20221:30 PM - 5:30 PMMile High Ballroom 4A
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WHEN IN ONTOGENY DO SPECIES DIFFERENCES EMERGE? A CASE STUDY OF A FOSSIL PLANKTONIC FORAMINIFERA LINEAGE
T12 Exploring the Mechanisms of Morphologic Change ISunday, 9 October 20228:00 AM - 12:00 PMMile High Ballroom 4A
2020
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DOES DEVELOPMENTAL PLASTICITY INFLUENCE SPECIATION? USING HIGH-RESOLUTION CT SCANNING TO QUANTIFY ONTOGENETIC TRAJECTORIES IN PLANKTONIC FORAMINIFERA BEFORE, DURING AND AFTER SPECIATION
T180 Linking Biological Questions to Paleontological Data: Statistical Models, Technological Advancements and Conceptual Improvements IThursday, 29 October 202010:00 AM - 12:00 PMMeeting Rooms
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UNDERSTANDING DIACHRONEITY: PALAEOENVIRONMENTAL CONTROLS ON DISPERSAL OF PLANKTONIC FORAMINIFERA IN THE HIGH-LATITUDE PLIO-PLEISTOCENE OCEANS
T114 Polar Paleobiology and Paleoenvironmental ProxiesWednesday, 28 October 202010:00 AM - 12:00 PMMeeting Rooms
2018
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DOES DEVELOPMENTAL PLASTICITY INFLUENCE SPECIATION? USING HIGH-RESOLUTION CT SCANNING TO QUANTIFY ONTOGENETIC TRAJECTORIES IN PLANKTONIC FORAMINIFERA BEFORE, DURING AND AFTER SPECIATION
T236 Applications of 3D Printing and Other 3D Methods to Experimental PaleontologyWednesday, 7 November 20188:00 AM - 12:00 PMRoom 142
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THE ADAPTIVE POWER OF DEVELOPMENTAL PLASTICITY
199 D23. Paleontology, Evolution and DevelopmentTuesday, 6 November 20181:30 PM - 5:30 PMRoom 141
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USING STATISTICAL CLUSTERING TECHNIQUES TO DETERMINE THE FIRST OCCURRENCE DATUM OF THE PLANKTONIC FORAMINIFER ORBULINOIDES BECKMANNI AND THE BASE OF PLANKTONIC FORAMINIFERAL BIOZONE E12
T187 Integrated Biostratigraphy (Posters)Tuesday, 6 November 20189:00 AM - 6:30 PMHalls J-K
2017
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EVOLUTIONARY RESPONSE OF THE PLANKTIC FORAMINIFER ORBULINOIDES BECKMANNI TO CLIMATIC CHANGE DURING THE MIDDLE EOCENE CLIMATIC OPTIMUM (MECO)
T268 Cenozoic Paleoclimates and Ecosystems (Posters)Tuesday, 24 October 20179:00 AM - 6:30 PMHalls 4EF
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VARIATION ACROSS SPACE DOES NOT PREDICT EVOLUTIONARY CHANGE THROUGH TIME
T10 Biodiversity Dynamics in the Face of Environmental Change: Integrating Paleontological and Neontological Approaches to Macroevolution ISunday, 22 October 20178:00 AM - 12:00 PMRoom 608
2016
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CAN SHARED EVOLUTIONARY HISTORY HELP PALEOCEANOGRAPHERS TO UNLOCK THE "BLACK-BOX" OF PLANKTONIC FORAMINIFERAL VITAL-EFFECTS?
T104 Microfossil Proxies in Earth HistoryMonday, 26 September 20168:00 AM - 12:00 PMRoom 505
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BIOGEOGRAPHIC RANGE SHIFTS IN THREE SPECIES OF PLANKTONIC FORAMINIFERA DURING THE INTENSIFICATION OF NORTHERN HEMISPHERE GLACIATION
T104 Microfossil Proxies in Earth HistoryMonday, 26 September 20168:00 AM - 12:00 PMRoom 505
2015
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GEOLOGICAL AND CLIMATIC CHANGE DEFINE ECOLOGICAL LIMITS TO SPECIES DIVERSITY
T97 Biotic Interactions and Their Influence on Long-Term Evolution IMonday, 2 November 20158:00 AM - 12:00 PMRoom 314
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DISENTANGLING SYNERGISTIC CLIMATE DRIVERS ON THE ANAGENETIC EVOLUTION OF PLANKTONIC FORAMINIFERA
T18 Co-Evolution of Life and Planet: Broad–Scale Controls on Biodiversity ISunday, 1 November 20158:00 AM - 12:00 PMRoom 314