Jy. Sire et Fj. Meunier, SUPERFICIAL ORNAMENTATION AND STRUCTURE O F THE OSSEOUS DERMAL PLATESIN SOME ARMORED SILURIFORMS (LORICARIIDAE, CALLICHTHYIDAE, DORADIDAE), Annales des sciences naturelles. Zoologie et biologie animale, 14(3), 1993, pp. 101-123
The present study is devoted to the superficial ornamentation, the str
ucture and the mineralization of the postcranial osseous dermal plates
(scutes) in various species representative of three families of armou
red Siluriformes (Callichthyidae, Loricariidae and Doradidae). In Call
ichthyidae and Loricariidae, the scute surface shows numerous odontode
s but they lack in Doradidae the scutes of which are characterized by
a large central osseous spine. The odontodes are conical true teeth ;
they have various species specific shapes but they show the same organ
ization : dentin, covered by an hypermineralized substance (enamel or
enameloid), surrounding a central pulpar cavity which communicates wit
h the vascular network of the scute. The odontodes are always attached
to the scute surface by a ligament. The base of the latter remains ea
sily visible after the fall of the odontodes and looks like a crown (p
edestal) the center of which is occupied by the opening of a vascular
canal. The scute surface, examined with the scanning electron microsco
pe, is ornamentated with small anchoring bundles. In toto micrographs
show that the scutes always have a well-developed vacular network whic
h is the largest in the loricariid Liposarcus disjunctivus. Althouth t
he scutes have various shapes their structure is relatively homogeneou
s when examined on microradiographs of ground sections and on semi-thi
n sections. A scute is mainly constituted by an osseous cellular plate
composed of woven bone in the central region and surrounded by parall
el-fibered bone. This plate is covered by a layer of hyaloine, more or
less developed following the species. Hyaloine is a well-mineralized
tissue which is not bone. Its thin organic matrix is striated by lines
of arrested growth. The structure of the scutes is compared to that o
f the ganoid and elasmoid scales and the evolutionary problems raised
by the existence of the scutes are discussed.