Matthew T. Hurtgen
Harvard Univ, Cambridge, MA
Activity
2005
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SULFUR CYCLING IN THE AFTERMATH OF A NEOPROTEROZOIC SNOWBALL GLACIATION: EVIDENCE FOR A SYN-GLACIAL SULFIDIC DEEP OCEAN?
45 Marine Anoxia over Geologic Time—Where, When, Why, and Cause and Effect Relationships to the Evolving Biosphere IIIThursday, 11 August 20059:00 AM - 12:00 PM
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OCEAN HYPERSTRATIFICATION FOLLOWING THE MARINOAN (NEOPROTEROZOIC) GLACIATION
45 Marine Anoxia over Geologic Time—Where, When, Why, and Cause and Effect Relationships to the Evolving Biosphere IIIThursday, 11 August 20059:00 AM - 12:00 PM
2004
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NEOPROTEROZOIC S ISOTOPES, THE EVOLUTION OF MICROBIAL S SPECIES AND THE BURIAL EFFICIENCY OF SULFIDE AS SEDIMENTARY PYRITE
T205 Ocean Chemistry through the Precambrian and Paleozoic IWednesday, 10 November 20048:00 AM - 12:00 PM
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GEOCHEMICAL EVIDENCE FOR A STRATIFIED OCEAN AFTER A NEOPROTEROZOIC (MARINOAN) SNOWBALL GLACIATION
T156 Ocean Chemistry through the Precambrian and Paleozoic (Posters)Tuesday, 9 November 20048:00 AM - 12:00 PM