38 Undergraduate Research I (Posters)

Saturday, 21 March 2020
8:00 AM - 12:00 PM
Grand Ballroom A–D


USING FORAMINIFERA TO CONSTRAIN GREENLAND ICE SHEET MELT DURING PAST PLEISTOCENE WARM PERIODS

Paper number: 38-16
Program: Theme Sessions
Time: 8:00 AM – 12:00 PM


Authors


Abstract

Greenland’s ice is melting at an alarming rate. While there is direct evidence for periods where the Greenland Ice Sheet was much smaller than today, the timing of Greenland Ice Sheet melt during ancient warm periods is still poorly constrained. Foraminifera, surface-dwelling marine plankton, provide a means of studying melt events which exceed modern seasonal variation. Foraminifera 𝛿18O reflects surface ocean water 𝛿18O, which would have decreased in the surface ocean near the coast as the Greenland Ice Sheet melted during ancient warm periods. We produce a record of planktic foraminifera 𝛿18O of south Greenland from the mid- to late-Pleistocene, which will help us understand the dynamics of how the Greenland Ice Sheet may melt in modern and future warm periods.

Geological Society of America Abstracts with Programs. Vol. 52, No. 2

doi: 10.1130/abs/2020SE-344566

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