Potential hybrid fossil crinoids, Eretmocrinus magnificus x Eretmocrin
us praegravis, are identified from the Lower Mississippian Fort Payne
Formation of south-central Kentucky. These are the first fossil hybrid
crinoids identified, and one of very few examples of hybrids recogniz
ed in the fossil record. Eretmocrinus magnificus x E. praegravis speci
mens have shapes and calyx plate sculpturing that are morphologically
intermediate between well-defined, distinct parent species. Suspected
hybrids occur at localities where parent species co-occur and where th
e parent species are the most abundant; the hybrids occur at what may
have been the distributional margins of the parent species; and the mi
xture of characters on suspected hybrids seems to be morphogenetically
partitioned. Parent species are derived from separate lineages within
Eretmocrinus, and hybridization is the most probable explanation for
these morphologically intermediate specimens. This example highlights
the need to consider hybridization as a potential interpretation of in
termediate morphologies among fossils and raises questions concerning
the impact of hybridization for our interpretation of the fossil recor
d and the role of hybridization in the evolutionary process.