description Kay Behrensmeyer Overview
A. Kay Behrensmeyer is an American paleontologist and taphonomist at the Smithsonian National Museum of Natural History. She is recognized for her pioneering research in vertebrate taphonomy, particularly her long-term bone weathering and ecological studies in Amboseli National Park, Kenya, initiated in 1975. Her extensive fieldwork in East African fossil sites, such as the Koobi Fora formation, has significantly advanced the understanding of paleoecology and hominid environments.
She caters to researchers in paleontology and paleoecology.
help Kay Behrensmeyer FAQ
Where does Kay Behrensmeyer conduct her long-term paleontological field research?
Behrensmeyer is best known for her decades-long field studies in Amboseli National Park, Kenya. There she has systematically tracked how animal bones weather, scatter, and become buried in natural environments over time, generating data crucial to interpreting the fossil record.
What is the Behrensmeyer bone weathering scale and why is it important?
Behrensmeyer developed a classification system that categorizes progressive bone deterioration into stages based on surface cracking, splitting, and splintering of skeletal remains exposed to the elements. This scale remains a standard tool used by paleontologists and archaeologists worldwide to estimate how long bones have been surface-exposed before burial.
What institution is Kay Behrensmeyer affiliated with?
Behrensmeyer holds a position as a research paleontologist and curator at the Smithsonian Institution's National Museum of Natural History in Washington, D.C. She works within the museum's Department of Paleobiology, where she has been a leading figure for decades.
What exactly is vertebrate taphonomy, the field Behrensmeyer helped pioneer?
Vertebrate taphonomy is the study of everything that happens to animal remains between death and fossilization—including decay, transport by rivers, scavenger disturbance, and burial. Behrensmeyer's research established many of the foundational principles that allow scientists to determine whether fossil bone assemblages faithfully represent original animal communities or have been distorted by post-mortem processes.
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