Donald J. DePaolo
University of California, Berkeley, Berkeley, CA
Activity
2019
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IMPLICATIONS OF CARBONATE MINERAL SURFACE DYNAMICS FOR STUDIES OF PAST OCEANS AND CLIMATES
T138 Effects of Mineral-Water Interface Complexity on Geochemical Processes: A Session in Honor of Mineralogical Society of America Awardee for 2018, Laura Nielsen LammersMonday, 23 September 20191:30 PM - 5:30 PMRoom 229B, North Building
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MN INCORPORATION INTO CALCITE: INFLUENCE OF INTERFACIAL DYNAMICS ON TRACE ELEMENT PARTITIONING, CALCIUM ISOTOPE FRACTIONATION, AND GROWTH KINETICS
T138 Effects of Mineral-Water Interface Complexity on Geochemical Processes: A Session in Honor of Mineralogical Society of America Awardee for 2018, Laura Nielsen LammersMonday, 23 September 20191:30 PM - 5:30 PMRoom 229B, North Building
2016
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QUANTIFYING AQUEOUS URANIUM MOBILITY FROM IN SITU RECOVERY MINING SITES USING ISOTOPE-CONTRAINED REACTIVE TRANSPORT MODELS
T309 In-Situ Technologies for Energy Resource Extraction: The Role of WaterWednesday, 28 September 20161:30 PM - 5:30 PMRoom 501
2014
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TESTING TECTONIC MODELS USING TIME-VARYING CRUSTAL THICKNESS VARIATIONS ACROSS SOUTHERN TIBET
T181 Exploring the Development of the Himalayan-Karakorum- Tibet Orogenic System from the Mantle to Mountain PeaksTuesday, 21 October 20148:00 AM - 12:00 PM119/120
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A CALCIUM ISOTOPE EXCURSION ASSOCIATED WITH THE END-TRIASSIC MASS EXTINCTION: IMPLICATIONS FOR OCEAN ACIDIFICATION AND CARBON CYCLE DYNAMICS
T108 Major Evolutionary Events of the Early Mesozoic— Paleontology and Paleoecology from the Middle Triassic to the Late JurassicMonday, 20 October 20148:00 AM - 12:00 PM220
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THE END-PERMIAN MASS EXTINCTION AND ITS AFTERMATH: INSIGHTS FROM NON-TRADITIONAL ISOTOPE SYSTEM
63 Mass Extinctions: Volcanism, Impacts, and Catastrophic Environmental ChangesSunday, 19 October 20141:00 PM - 5:00 PMBallroom A
2013
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CONSTRAINING THE CAUSE OF THE END-GUADALUPIAN EXTINCTION WITH COUPLED RECORDS OF CARBON AND CALCIUM ISOTOPES
303 Recent Advances in Paleoclimatology/PaleooceanographyWednesday, 30 October 20138:00 AM - 12:00 PMRoom 605
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RADIOGENIC INGROWTH OF 40CA FROM DECAY OF 40K PROVIDES A POWERFUL TRACER FOR UNDERSTANDING THE ORIGINS OF FELSIC MAGMAS
T26 Illuminating Felsic Origins: Using Novel Multiple-Method Approaches to Investigate the Birth of Silicic MagmasSunday, 27 October 20138:00 AM - 12:00 PMRoom 205
2011
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A CALCIUM ISOTOPE TEST OF END-PERMIAN OCEAN ACIDIFICATION USING BIOGENIC APATITE
T153 Permian-Triassic Changes and Extinction Event: New Insights from Sedimentary, Geochemical, and Paleobiological Records and Modeling Approaches ITuesday, 11 October 20118:00 AM - 12:00 PMRoom 200FG
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CONSTRAINTS ON OCEAN BIOGEOCHEMISTRY DURING THE END-GUADALUPIAN BIOTIC CRISIS FROM STABLE CALCIUM ISOTOPES
T153 Permian-Triassic Changes and Extinction Event: New Insights from Sedimentary, Geochemical, and Paleobiological Records and Modeling Approaches ITuesday, 11 October 20118:00 AM - 12:00 PMRoom 200FG
2010
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NANOSCALE CONTROL OF GEOLOGIC CO2: A DOE ENERGY FRONTIER RESEARCH CENTER
T137 Geochemistry of Geologic Sequestration of CO2: Understanding Gas-Water-Mineral Interactions over Wide Temporal and Spatial Ranges IIMonday, 1 November 20101:30 PM - 5:30 PMRoom 205
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USING NATURAL ISOTOPIC TRACERS TO UNRAVEL THE HYDROLOGY OF THE HANFORD 300 AREA AND ITS IMPACT ON URANIUM MOBILITY AT THE SITE
T9 Advances in Understanding Aquifer Heterogeneity and Multi-Scale Flow and Transport in Porous and Fractured MediaSunday, 31 October 20108:00 AM - 12:00 PMRoom 612
2009
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GROWTH AND EVOLUTION OF THE ISLAND OF HAWAII: PERSPECTIVES FROM HSDP DEEP DRILLING
6 The Evolution of Basaltic Landscapes: Time and the River and Lava FlowingSunday, 18 October 20098:00 AM - 12:00 PMPortland Ballroom 254
2008
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A Calcium Isotope Record across the Permian-Triassic Boundary from An Isolated Carbonate Platform in South China
314 Paleoclimatology/PaleoceanographyWednesday, 8 October 20081:30 PM - 5:30 PM
2007
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LATTICE BOLTZMANN SIMULATION OF OXYGEN- AND HYDROGEN-ISOTOPE FRACTIONATIONS DURING SNOW CRYSTAL FORMATION
1 GeochemistrySunday, 28 October 20078:00 AM - 12:00 PM