The Devono-Carboniferous chondrichthyan Stethacanthus is best known for its
striking 'spine-brush' complex. Here we provide the first detailed descrip
tion of the neurocranium, using several well-preserved specimens from Bears
den, Scotland (Serpukhovian; Pendleian El). Significant features include an
otico-occipital region of about the same length as the ethmosphenoid divis
ion; short but distinct lateral otic processes; a short; broad endolymphati
c fossa; a persistent otico-occipital fissure; Y-shaped basicranial canals
indicating origin of the lateral aortae anterior to the occipital level; an
d minimal suborbital shelves limited to small, ethmoidally located outgrowt
hs. Using placoderm, osteichthyan and acanthodian neurocrania for outgroup
comparison, PAUP analysis of a matrix of 23 neurocranial characters produce
d the following branching sequence: (Helodus (Stethacanthus, Cobelodus (Tam
iobatis (Xenacanthus (Cladodus wildungensis (Tristychius, Hybodus)))))). Th
e location of Cladoselache in this analysis is uncertain and probably resul
ts from missing data and a morphologically restricted character set. Plesio
morphic conditions for chondrichthyan braincases are found to include the p
resence of a persistent otico-occipital fissure, projection of the median d
orsal aorta anterior to the occipital level, and absence of suborbital shel
ves. These results may have important implications with regard to primitive
gnathostome interrelationships, and especially the phylogenetic position o
f placoderms.