THE GREAT GULLY GROUP: A TIME-STRATIGRAPHIC FRAMEWORK FOR LATE QUATERNARY EVENTS IN THE CENTRAL FINGER LAKES OF NEW YORK STATE
Identification of laterally continuous and distinct lithologic units observed from 16 exposures has allowed us to develop a comprehensive type section and confidently assign formal names at the formation and member level lithostratigraphic hierarchy. Newly collected continuous wire-line cores, 50 meters in depth, substantiate continuity and expand the stratigraphic and spatial range of preserved deposits.
Lithostratigraphic units are comprised of alternating packages of diamicton and fluvial\lacustrine facies. The fortuitous abundance of subtill organics provides a metric to establish a robust, internally consistent radiocarbon chronology and assess paleoenvironmental conditions. Strata older than the limits of radiocarbon are constrained by optically stimulated luminescence dating. Together the combined geochronology and lithostratigraphic information provide a unique basis for a chronostratigraphic record of glacial and non-glacial phases in the Finger Lakes spanning Marine Isotope Stages (MIS) 1-5 and possibly beyond.