G.J. Harrington
Smithsonian Institution, Washington, DC
Activity
2022
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BIOSTRATIGRAPHICALLY SIGNIFICANT PALYNOFLORAS FROM THE PALEOCENE–EOCENE BOUNDARY OF THE USA
273 D24. Paleontology: Recent Advances in Phylogeny, Morphological Patterns, Biogeography, and Biostratigraphy (Posters)Wednesday, 12 October 20222:00 PM - 6:00 PMExhibit Hall F
2021
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REWORKED POLLEN REDUCES APPARENT FLORAL CHANGE DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM
130 D13. Recent Advances in Paleoclimatology/PaleoceanographyTuesday, 12 October 20218:00 AM - 12:00 PMD137
2020
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EVIDENCE FOR ABRUPT PALYNOFLORAL CHANGE IN CONTINENTAL SETTINGS DURING THE PALEOCENE-EOCENE THERMAL MAXIMUM
T243 Climatic and Biotic Processes through the Paleozoic, Mesozoic, and Cenozoic as Reconstructed from Microfossil RecordsFriday, 30 October 202010:00 AM - 2:00 PMMeeting Rooms
2011
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PLANT INTERCHANGE BETWEEN EUROPE AND NORTH AMERICA ACROSS THE PALEOCENE/EOCENE TRANSITION
173 Paleontology (Posters) III: Biogeography, Biostratigraphy, and TaphonomyTuesday, 11 October 20119:00 AM - 6:00 PMHall C
2006
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NORTH AMERICAN PARATROPICAL FLORAL EXTINCTION IN THE LATE PALEOCENE-EARLY EOCENE
154 Paleontology/Paleobotany VI: Ancient Terrestrial EcosystemsTuesday, 24 October 20061:30 PM - 5:30 PM
2005
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ENHANCED CONTINENTAL WEATHERING AND PEDOGENESIS ACROSS THE PALEOCENE/EOCENE BOUNDARY IN THE U.S. WESTERN INTERIOR (NORTH DAKOTA)
T117 Causes and Effects of the Paleocene-Eocene Thermal Maximum and Other Paleogene Hyperthermal Events IMonday, 17 October 20051:30 PM - 5:30 PM