This will be an IN-PERSON meeting only. Three excellent talks will be presented:
ELI MOORE, U.S. Geological Survey: Subsurface Metaproteomics Reveals Diverse Active Microbial Metabolisms in the Antrim Shale
ROBERTA RUDNICK, University of California – Santa Barbara: Metapelites in the lower crust beneath the Potrillo Volcanic Field provide insights into the mysterious 1.4 Ga Picuris Orogeny
ADAM WALLACE, University of Delaware: Reassessment of the Roles of Ion Hydration and Dehydration on the Reactivity of the Calcite-Water Interface
Come at 7:30 PM to socialize and imbibe, the meeting begins at 8 PM, and ends by 10 PM.
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Parking is free on the campus, or on-street in the vicinity
This will be a special event, highlighting the work of early-career scientists. Ahead of the formal program, we will hold an informal gathering with food, beverages, and poster presentations by students, post-docs and other early-career workers. We welcome poster presentation contributions: please email Dan Doctor (dhdoctor@usgs.gov) if you have a poster to present!
Hors d’oeuvres and beverages will be served beginning at 6:30 p.m., during the poster presentations
***This will be a hybrid meeting***
If you wish to join the virtual Zoom webcast, please email geosocwash@gmail.com by Tuesday, April 23 for the information to join the webcast.
Formal program begins at 8:00 p.m, with the following speakers:
Emmanuel Codillo, Carnegie Earth and Planets Laboratory — Tracking carbon-rich magmas in the upper mantle using electrical conductivity
Vasilije Dobrosavljevic, Carnegie Earth and Planets Laboratory — Probing materials at Earth’s enigmatic core-mantle boundary landscape
Jennifer Kasbohm, Yale University/Carnegie Earth and Planets Laboratory — Calibrating timescales and measuring pCO2 to test the role of Columbia River Basalt volcanism in the Miocene Climate Optimum
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The GSW meeting at the Cosmos Club hosted three talks. A draft of the meeting minutes are available here. Please contact Michael Purucker with any suggestions, changes or corrections.
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High resolution (128x higher than typical weather models & 500x higher than climate models) enables detailed tracking of CO2 plumes from individual sources and reveals their interactions with other Earth systems.