Abstract
We report the excavation and analysis of a Chiroptera-dominated bonebed from Bat Cave, Edmonson County, Kentucky. Paleontological materials recovered in 1999 offered new insight into formation processes of the bonebed. Stratigraphic and geochronological information indicate a long, episodic history of the deposit spanning much of the Holocene. The vertebrate assemblage is dominated by Myotis spp. Although initially believed to represent a single, catastrophic kill event due to historic flooding, our results suggest that the Bat Cave bonebed was formed by a minimum of eleven accumulation events that took place between approximately 2200 and 10,800 cal BP.
Original language | English (US) |
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Pages (from-to) | 91-98 |
Number of pages | 8 |
Journal | Journal of Cave and Karst Studies |
Volume | 77 |
Issue number | 2 |
DOIs | |
State | Published - Aug 1 2015 |
All Science Journal Classification (ASJC) codes
- Earth-Surface Processes