Epibionts on specimens of Flexicalymene (Late Ordovician, Cincinnati A
rch region, U.S.A.) that were encrusted while alive show an apparent p
reference for attachment along the relatively elevated sagittal axis o
f the exoskeleton (glabella, axial rings of thorax and pygidium) or th
e medial portion of the cephalic doublure. This site-specificity suppo
rts an interpretation of a semi-infaunal habit for this trilobite and
may indicate a commensal relationship between the epizoan and host (e.
g., epizoan bryozoans exploiting the trilobite exoskeleton as a hard s
ubstrate and perhaps benefitting from feeding currents generated by th
e trilobite). Epizoans are found only on larger individuals of this tr
ilobite, suggesting a terminal molt stage for Flexicalymene. Although
the number of previously reported encrusted trilobites is small, a sur
vey of the literature suggests the following hypotheses concerning the
relationships between trilobite life habit and susceptibility to epiz
oan colonization: 1) infaunal (burrow dwelling) trilobites were genera
lly free of epizoans; 2) a small proportion of shallow-burrowing (semi
-infaunal or ''ploughing'') trilobites were suitable hosts for epizoan
s, but the epizoans preferentially colonized the elevated or anterior
portions of the exoskeleton; 3) epifaunal (and some pelagic?) trilobit
es were more susceptible to encrustation.