Conchodontus, Mitrellataxis and Fungulodus are phosphatic microfossils from
the Late Devonian of China and North America, alternatively interpreted as
conodont elements or fish scales. The histology and microornament of these
sclerites have been studied in an attempt to resolve their affinity, and t
o determine characters for distinguishing between conodont elements and the
ichthyoliths of other lower vertebrates. The histology of all three genera
is directly comparable to conodont elements, dispelling the notion that co
nodonts are histologically indistinguishable from the teeth and scales of o
ther vertebrates. Microornament is found not to be useful in discriminating
between high-level taxonomic groupings. White matter and thickness of pris
mless enamel are suggested as apomorphies of the Conodonta.