Cole Edwards
Appalachian State University, Boone, NC
Activity
2025
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WHEN ARE BRACHIOPODS OR CONODONTS MOST USEFUL FOR SR ISOTOPE STRATIGRAPHY OF PALEOZOIC SUCCESSIONS?
27 The Early Paleozoic of Eastern North AmericaFriday, 21 March 20258:00 AM - 10:00 AMAppalachian B
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LOCATION MATTERS, OR DOES IT? TESTING CARBON AND OXYGEN ISOTOPIC VARIABILITY FROM ORDOVICIAN CARBONATE LITHOLOGIES: IMPLICATIONS FOR DIAGENETIC OVERPRINTS OF PALEOENVIRONMENTAL RECONSTRUCTIONS
41 Biogeochemical Cycling of Elements at the Earth’s Surface Across Space and Time (Posters)Friday, 21 March 20251:00 PM - 5:00 PMShenandoah ABC
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STABLE CARBON ISOTOPE (Δ13CCARB AND Δ13CORG) EVIDENCE OF THE TOARCIAN OCEAN ANOXIC EVENT FROM CENTRAL ITALY: EVIDENCE FOR A GLOBALLY MIXED TETHYS SEA.
40 Co-evolution of Life and its Environment: From Biodiversification Events to Mass Extinction and Everything in Between (Posters)Friday, 21 March 20251:00 PM - 5:00 PMShenandoah ABC
2023
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EVOLUTION OF THE DEVONIAN EARTH SYSTEM THROUGH THE LENS OF GEOCHEMISTRY: FROM CARBON CYCLING AND ANOXIA TO PLATE TECTONICS
T80 The Early Paleozoic III: Radiations, Extinctions, and EnvironmentMonday, 16 October 20238:00 AM - 12:00 PM304 / 305
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CALCIUM ISOTOPIC CONSTRAINTS ON THE ORIGIN OF THE MID-DARRIWILIAN CARBON ISOTOPE EXCURSION (MDICE)
T58 The Early Paleozoic II: Radiations, Extinctions, and EnvironmentSunday, 15 October 20231:30 PM - 5:30 PM304 / 305
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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CARBON AND SULFUR ISOTOPES: PAIRING PROXIES FROM CARBONATE ROCKS TO CONSTRAIN THE TIMING OF ANOXIA DURING THE LATE DEVONIAN IN THE GREAT BASIN REGION, USA
T168 Dynamics of Earth’s Climate System and Biogeochemical Cycles in Deep Time (Posters)Tuesday, 11 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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STRONTIUM (87SR/86SR) AND LITHIUM (δ7LI) ISOTOPIC EVIDENCE FOR SHIFTS IN DEVONIAN WEATHERING PATTERNS: IMPLICATIONS FOR THE EXPANSION OF LAND PLANTS AND THE ONSET OF THE ACADIAN OROGENY
T80 Advances in Non-Traditional Stable Isotope Measurements and Utility as Proxies in Modern and Paleo-SettingsMonday, 10 October 20228:00 AM - 12:00 PM506
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USING PAIRED CARBON AND SULFUR ISOTOPES FROM CARBONATE ROCKS TO CONSTRAIN THE TIMING OF ANOXIA DURING THE LATE DEVONIAN IN THE GREAT BASIN REGION, USA: IMPLICATIONS FOR CHEMOSTRATIGRAPHIC CORRELATIONS
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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REVISITING A TREMADOCIAN (EARLY ORDOVICIAN) MASS EXTINCTION EVENT AND OCEAN ANOXIA: NEW INSIGHTS FROM TRACE METAL ABUNDANCES AND URANIUM ISOTOPE COMPOSITIONS OF CARBONATES FROM THE GREAT BASIN REGION, WESTERN USA
130 D13. Recent Advances in Paleoclimatology/PaleoceanographyTuesday, 12 October 20218:00 AM - 12:00 PMD137
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HOW ROBUST IS YOUR FAVORITE ANOXIA PROXY? LESSONS WE'RE LEARNING FROM THE LATE DEVONIAN
T144 Broken Paradigms: Shallow-Water Deposition of Organic-Rich Facies through Earth HistoryTuesday, 12 October 20218:00 AM - 12:00 PMB113/B114 (Hybrid Room)
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DID A TECTONIC UPLIFT AND BASALTIC WEATHERING ENHANCE NUTRIENT DELIVERY TO THE MIDDLE ORDOVICIAN OCEANS?
T141 The Evolution of Early Phanerozoic Oceans: A Geobiological PerspectiveTuesday, 12 October 20218:00 AM - 12:00 PME145
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IDENTIFYING THE CAUSES OF EARLY PALEOZOIC MASS EXTINCTIONS USING NEW CARBONATE GEOCHEMICAL PROXIES: LOCAL EVIDENCE OF MARINE ANOXIA USING I/CA RATIOS
T10 New Perspectives on Phanerozoic Mass Extinctions and Environmental Perturbations ISunday, 10 October 20218:00 AM - 12:00 PME143/E144
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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
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SEARCHING FOR THE LATE DEVONIAN KELLWASSER EVENT IN THE GREAT BASIN REGION, USA: WAS ANOXIA THE MAIN DRIVER OF THE LATE DEVONIAN MASS EXTINCTION?
T76 Co-Evolution of Earth’s Surface Environment and Eukaryotic Life from the Mid-Proterozoic to Early PaleozoicTuesday, 27 October 20201:30 PM - 5:30 PMMeeting Rooms
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WAS ANOXIA THE MAIN DRIVER OF THE LATE DEVONIAN MASS EXTINCTION? NEW INSIGHTS USING PAIRED STABLE CARBON AND SULFUR ISOTOPES
T76 Co-Evolution of Earth’s Surface Environment and Eukaryotic Life from the Mid-Proterozoic to Early PaleozoicTuesday, 27 October 20201:30 PM - 5:30 PMMeeting Rooms
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CHASING THE LATE DEVONIAN KELLWASSER EVENT IN THE GREAT BASIN REGION, USA: WAS ANOXIA THE MAIN DRIVER OF THE LATE DEVONIAN MASS EXTINCTION?
32 Chemostratigraphic, Biotic, and Sedimentologic Changes through Earth HistorySaturday, 21 March 20208:00 AM - 12:00 PMLake Audubon
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DOES FOOLS GOLD TELLS THE TRUTH ABOUT ANOXIA? RETHINKING THE CAUSE OF THE LATE DEVONIAN MASS EXTINCTION USING SULFUR ISOTOPES IN CARBONATES
50 Chemostratigraphic, Biotic, and Sedimentologic Changes through Earth History (Posters)Saturday, 21 March 20201:30 PM - 5:30 PMLake Anne
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SEARCHING FOR EVIDENCE OF LATE DEVONIAN LOCALIZED ANOXIA IN THE GREAT BASIN REGION (SOUTHERN NV, USA): RETHINKING CAUSES OF THE LATE DEVONIAN MASS EXTINCTION
50 Chemostratigraphic, Biotic, and Sedimentologic Changes through Earth History (Posters)Saturday, 21 March 20201:30 PM - 5:30 PMLake Anne
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
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COORDINATED BIOTIC AND ABIOTIC CHANGE DURING THE GREAT ORDOVICIAN BIODIVERSIFICATION EVENT: DARRIWILIAN ASSEMBLY OF EARLY PALEOZOIC BUILDING BLOCKS
T68 The Ordovician Earth: Integrated Perspectives on the Fossil and Rock RecordsSunday, 22 September 20191:30 PM - 5:30 PMRoom 228AB, North Building
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DID EARLY LAND PLANTS PRODUCE A STEPWISE-CHANGE IN ATMOSPHERIC OXYGEN DURING THE LATE ORDOVICIAN (SANDBIAN ~ 458 MA)?
T68 The Ordovician Earth: Integrated Perspectives on the Fossil and Rock RecordsSunday, 22 September 20191:30 PM - 5:30 PMRoom 228AB, North Building
2018
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WHERE IS THE LATE DEVONIAN ANOXIC KELLWASSER EVENT ACROSS THE FRASNIAN-FAMENNIAN BOUNDARY?: NEW INSIGHTS FROM THE GREAT BASIN REGION, USA
T234 Greenhouse to Icehouse Transition: Global Events of the Devonian, Carboniferous, and Early Permian IWednesday, 7 November 20188:00 AM - 12:00 PMRoom 140
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TESTING WHETHER LATE ORDOVICIAN CARBON ISOTOPE EXCURSIONS RECORD RAPID VARIATIONS IN THE GLOBAL CARBON CYCLE
18 D7. Stratigraphy, Sedimentation, and Diagenesis (Posters)Thursday, 12 April 20181:30 PM - 5:30 PMRoom 301 DE/Henley Concourse
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STRONTIUM ISOTOPE (87SR/86SR) STRATIGRAPHY OF LOWER DEVONIAN CARBONATE ROCKS FROM THE GREAT BASIN REGION: TESTING SR ISOTOPE METHODS USING CONODONT APATITE AND BULK CARBONATE
18 D7. Stratigraphy, Sedimentation, and Diagenesis (Posters)Thursday, 12 April 20181:30 PM - 5:30 PMRoom 301 DE/Henley Concourse
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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
2017
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δ13C, δ34S, AND I/CA EVIDENCE FOR ANOXIA AT AN EARLY ORDOVICIAN (TREMADOCIAN) MASS EXTINCTION
30 Clastics, Carbonates, and Soils (Posters)Friday, 31 March 20171:00 PM - 5:00 PMJames River Ballroom
2016
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NEODYMIUM (ND) AND STRONTIUM (SR) ISOTOPE EVIDENCE FOR WEATHERING OF ARC VOLCANICS DURING THE ORDOVICIAN GREENHOUSE-ICEHOUSE TRANSITION
T288 The Early Paleozoic World: Radiations, Extinctions, and Paleoenvironmental Change IIWednesday, 28 September 20168:00 AM - 12:00 PMMile High Ballroom 3C
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OXYGENATION AS A DRIVER OF THE GREAT ORDOVICIAN BIODIVERSIFICATION EVENT
T224 The Early Paleozoic World: Radiations, Extinctions, and Paleoenvironmental Change ITuesday, 27 September 20161:30 PM - 5:30 PMMile High Ballroom 3C