T241 The Cretaceous–Paleogene Boundary: From Impact Cratering Processes to Mass Extinction Mechanisms

Wednesday, 13 October 2021
1:30 PM - 5:30 PM
D139/D140


CRETACEOUS-PALEOGENE BOUNDARY SEDIMENTOLOGY: IMPACT EVIDENCE FROM SOUTH CAROLINA

Paper number: T241-16
Program: Technical Sessions
Time: 5:15 PM – 5:30 PM


Authors


Abstract

The Cretaceous-Paleogene (KPg) boundary is one of the most intensely studied stratigraphic sections from Earth history. Even so, the stratigraphic sections marking the boundary in South Carolina remain largely unexamined. Petrographic thin sections were made from samples collected directly below, from, and above the KPg boundary in exposed strata in South Carolina and in a well-studied locality from North Dakota. Thin sections were examined via standard and polarized light microscopy for the primary mineralogical indicators of the boundary, including impact microspherules and shocked quartz. Glass microspherules were observed in the boundary sediments from both South Carolina and North Dakota. Shocked quartz was observed in only the boundary sediments from South Carolina. Neither microspherules or shocked quartz grains were identified in sediments from below or above the KPg boundary clay layer. Although our sample size is small, the confirmation of a KPg boundary site near Columbia, South Carolina is significant, as it provides potential for further research and educational opportunities.

Geological Society of America Abstracts with Programs. Vol. 53, No. 6

doi: 10.1130/abs/2021AM-368268

© Copyright 2021 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.