Christopher T. Conwell
The Ohio State University, Columbus, OH
Activity
2022
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ND ISOTOPIC EVIDENCE FOR ENHANCED MAFIC WEATHERING LEADING TO ORDOVICIAN COOLING
T227 Do Carbon Sources or Sinks Drive the Phanerozoic Carbon Cycle?: Understanding Geobiologic Forcings and FeedbacksWednesday, 12 October 20228:00 AM - 12:00 PM506
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LITHOFACIES AND ND ISOTOPE STRATIGRAPHY OF THE KNOX UNCONFORMITY IN THE CENTRAL APPALACHIAN BASIN
T241 Cambrian–Ordovician Faunas and Events (Posters): A Session in Honor of John F. Taylor and John E. RepetskiWednesday, 12 October 20229:00 AM - 1:00 PMExhibit Hall F
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FACTORS AFFECTING 87SR/86SR SIGNAL PRESERVATION IN CONODONT APATITE: A LONG-RANGING DATA COMPILATION AND A CASE STUDY FROM THE ORDOVICIAN OF BALTOSCANDIA
T198 Radiogenic Isotopes as Tracers of Geologic Processes: Dates, Rates, and Proxies (Posters)Tuesday, 11 October 20222:00 PM - 6:00 PMExhibit Hall F
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LITHOFACIES AND ND ISOTOPE STRATIGRAPHY OF THE KNOX UNCONFORMITY IN THE CENTRAL APPALACHIAN BASIN
35 Correlating the Ordovician: Honoring the Career and Contributions of Stig M. Bergström (Posters)Friday, 8 April 20228:00 AM - 12:00 PMJunior Ballroom B
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CORRELATING MIDDLE–LATE ORDOVICIAN CARBONATE STRATA ACROSS THE IAPETUS USING STRONTIUM ISOTOPES (87SR/86SR) CALIBRATED TO CONODONT BIOSTRATIGRAPHY
10 Correlating the Ordovician: Honoring the Career and Contributions of Stig M. BergströmThursday, 7 April 20221:30 PM - 5:30 PMNorth Meeting Room 203/204
2021
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PAIRED MIDDLE–LATE ORDOVICIAN CONTINENTAL WEATHERING (87SR/86SR AND ΕND(T)) AND PALEOTEMPERATURE (δ18O) PROXY MEASUREMENTS LINK ENHANCED MAFIC WEATHERING TO GLOBAL COOLING
T8 Evolution of Earth’s Surface: Honoring Xiao-Ming Liu, Recipient of the 2021 Mineralogy, Geochemistry, Petrology, and Volcanology Division’s Early Geological Career AwardSunday, 10 October 20218:00 AM - 12:00 PMPortland Ballroom 252 (Hybrid Room)
2020
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GLOBAL COOLING LINKED TO BASALTIC WEATHERING DURING THE ORDOVICIAN GREENHOUSE–ICEHOUSE TRANSITION
T179 The Ordovician Earth: New Insights to Environmental and Biotic Responses in the Fossil and Rock Record IThursday, 29 October 202010:00 AM - 12:00 PMMeeting Rooms
2019
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DID TACONIC OROGENESIS ENHANCE MAFIC WEATHERING RATES IN THE MIDDLE–LATE ORDOVICIAN? A TEST USING SEAWATER STRONTIUM AND NEODYMIUM ISOTOPES
T169 Chemostratigraphy: Physical and Temporal ApplicationsTuesday, 24 September 20198:00 AM - 12:00 PMRoom 224B, North Building
2018
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TACONIC WEATHERING AND ORDOVICIAN COOLING: TESTING THE LINK USING PAIRED SR AND ND ISOTOPES, ANTELOPE VALLEY, CENTRAL NV
T11 New Developments in Geochemical Proxies for Paleoceanographic ResearchSunday, 4 November 20188:00 AM - 12:00 PMRoom 140
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ASSESSING CRITICAL DRIVERS OF THE ORDOVICIAN GREENHOUSE-ICEHOUSE TRANSITION WITH PAIRED STRONTIUM AND NEODYMIUM ISOTOPE STRATIGRAPHY
4 Evolution of the Taconic Foreland: Insights into Active Margins and Global Climate ChangeSunday, 18 March 20188:00 AM - 12:00 PMDiamond Ballroom II