Aviv Bachan
Stanford University, Stanford, CA
Activity
2016
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A MODEL FOR THE DECREASE IN AMPLITUDE OF CARBON ISOTOPE EXCURSIONS THROUGHOUT THE PHANEROZOIC
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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THE OXYGEN MINIMUM ZONE AS A KEY CONTROL ON EXCURSIONS, RECOVERY, AND ENVIRONMENTAL CHANGE FOLLOWING THE END-PERMIAN EXTINCTION
T183 Excursions, Extinctions, and Environmental Change: New Advances in Geochemical Tools Linked to Critical Intervals of Environmental and Biotic Change in Earth HistoryTuesday, 27 September 20168:00 AM - 12:00 PMRoom 404
2015
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THE ROLE OF OCEAN ANOXIA IN MODULATING EARTH SYSTEM RECOVERY FOLLOWING MASS EXTINCTION EVENTS
T68 Mass Extinction Causality: Records of Anoxia, Acidification, and Global Warming during Earth's Greatest Crises IISunday, 1 November 20151:30 PM - 5:30 PMRoom 310
2011
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COUPLED ORGANIC AND CARBONATE δ13C RECORDS OF THE LATE TRIASSIC AND EARLY JURASSIC IN NORTHERN ITALY: IMPLICATIONS FOR CARBON CYCLING DURING THE AFTERMATH OF THE END-TRIASSIC MASS EXTINCTION
T55 Multidisciplinary Approaches to Studying the Causes and Consequences of Mass Extinction: Geochemistry, Paleoecology, and Paleoenvironments IISunday, 9 October 20111:30 PM - 5:30 PMRoom 200H-J
2010
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CARBON CYCLE DYNAMICS AND ENVIRONMENTAL CHANGE AT THE TRIASSIC-JURASSIC BOUNDARY
T47 Links between Mesozoic Climate and Biodiversity (Posters)Sunday, 31 October 20108:00 AM - 6:00 PMHall D