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Activity

2013

• MULTIPLE PALEOCENE AND EARLY EOCENE HYPERTHERMALS RECORDED IN THE TERRESTRIAL WILLWOOD FORMATION, NORTHERN BIGHORN BASIN, WYOMING
  381 Back to the Future: Eocene–Early Oligocene Climatic Response to Geological Processes and Implications for the Future Earth
  Wednesday, 30 October 2013

  1:00 PM - 5:00 PM

  Mile High Ballroom 4AB

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2005

• ESTIMATING PCO2 ACROSS THE PETM USING CARBON ISOTOPE RATIOS OF PALEOSOL CARBONATES AND ORGANIC MATTER FROM THE BIGHORN BASIN, WYOMING
  T186 Causes and Effects of the Paleocene-Eocene Thermal Maximum and Other Paleogene Hyperthermal Events II
  Tuesday, 18 October 2005

  1:30 PM - 5:30 PM
• FORENSIC GEOLOCATION USING ENVIRONMENTAL ISOTOPES
  61 Archaeological Geology
  Monday, 17 October 2005

  8:00 AM - 12:00 PM
• THE WATER CYCLE OF THE PETM: EVIDENCE IN HAND AND THE DATA WE WOULD LIKE TO HAVE
  T117 Causes and Effects of the Paleocene-Eocene Thermal Maximum and Other Paleogene Hyperthermal Events I
  Monday, 17 October 2005

  1:30 PM - 5:30 PM
• KEYNOTE: SOILS, WATER, AND TERRESTRIAL-MARINE CONNECTIVITY THROUGH THE PALEOCENE-EOCENE THERMAL MAXIMUM
  14 Soil Organic Matter: Cycling, Transport, and Ocean-Climate Interaction
  Tuesday, 9 August 2005

  9:00 AM - 12:00 PM

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2004

• WHAT IS ISOTOPE SEASONALITY?
  T13 Stable Isotopes in Fossils and Paleosols: Records of Late Cenozoic Environmental Change
  Sunday, 7 November 2004

  8:00 AM - 12:00 PM