Wednesday, 17 December 2014
Andrei Kurbatov1, Nelia W Dunbar2, Nels Anton Iverson3, Christopher C Gerbi1, Martin G Yates1, Donna Kalteyer1 and William C. McIntosh2, (1)University of Maine, Orono, ME, United States, (2)New Mexico Institute of Mining and Technology, Socorro, NM, United States, (3)New Mexico Tech, Palouse, WA, United States
Modern paleoclimate research is heavily dependent on establishing accurate timing related to rapid shifts in Earth’s climate system. The ability to correlate these events at local, and ideally at the intercontinental scales, allows assessment, for example, of phasing or changes in atmospheric circulation. Tephra-producing volcanic eruptions are geologically instantaneous events that are largely independent of climate. We have developed a tephrochronological framework for paleoclimate research in Antarctic in a user friendly, freely accessible online Antarctic tephra (AntT) database (http://cci.um.maine.edu/AntT/).

Information about volcanic events, including physical and geochemical characteristics of volcanic products collected from multiple data sources, are integrated into the AntT database.
The AntT project establishes a new centralized data repository for Antarctic tephrochronology, which is needed for precise correlation of records between Antarctic ice cores (e.g. WAIS Divide, RICE, Talos Dome, ITASE) and global paleoclimate archives. The AntT will help climatologists, paleoclimatologists, atmospheric chemists, geochemists, climate modelers synchronize paleoclimate archives using volcanic products that establishing timing of climate events in different geographic areas, climate-forcing mechanisms, natural threshold levels in the climate system. All these disciplines will benefit from accurate reconstructions of the temporal and spatial distribution of past rapid climate change events in continental, atmospheric, marine and polar realms. Research is funded by NSF grants: ANT-1142007 and 1142069.