T122 New Perspectives on Phanerozoic Mass Extinctions and Environmental Perturbations (Posters)
Monday, 11 October 2021
2:30 PM - 6:30 PM
Exhibit Hall A
A COMPREHENSIVE EXAMINATION OF ABSOLUTE AND RELATIVE MICROFOSSIL ABUNDANCE DURING THE LATE DEVONIAN KELLWASSER EVENTS IN THE APPALACHIAN BASIN
Paper number: T122-2
Program: Technical Sessions
Time: 2:30 PM – 6:30 PM
Authors
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Ashlyn OhWilliams College, Williamstown, MA
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Kate PippengerWilliams College, Williamstown, MA
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Phoebe CohenWilliams College, Williamstown, MA
Abstract
We examine trends between the Upper and Lower Kellwasser events and between proximal and distal areas of the Basin. We also interrogate the hypothesis that certain taxa of organic-walled microfossils may be “disaster taxa” that flourished during extinction events and may be related to algal blooms that could have contributed to low-oxygen conditions. In addition, preliminary results show that acanthomorphs and non-acritarch microfossils are more abundant in proximal and presumably shallower locations. This microfossil analysis, taken together with other geochemical and paleontological proxies, including Hg, total organic carbon, and microfossil morphology, provides a complex picture of ecology during the End-Devonian extinction events in the Appalachian Basin.
Geological Society of America Abstracts with Programs. Vol. 53, No. 6
doi: 10.1130/abs/2021AM-369779
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