R. Lund et Ed. Grogan, RELATIONSHIPS OF THE CHIMAERIFORMES AND THE BASAL RADIATION OF THE CHONDRICHTHYES, Reviews in fish biology and fisheries, 7(1), 1997, pp. 65-123
The origin and early evolution of the cartilaginous fishes (Chondricht
hyes) has been the subject of considerably more debate than of data. T
he two modern groups, Chimaeriformes and Elasmobranchii, differ so rad
ically in morphology that in the past they have often been considered
unrelated - descended from some remote and unknown common ancestor. Th
e current consensus promotes the Chimaeriformes and Elasmobranchii as
sister taxa of the Class Chondrichthyes which are linked by an assembl
age of Palaeozoic fossil taxa, but no taxonomic or phylogenetic scheme
has been accepted for the Class. Of the two groups, the Chimaeriforme
s is the less understood. The few species of Chimaeriformes existing t
oday are enigmatic, principally deeper-water fish that are not readily
accessible for study. In the past the fossil record of both groups ha
s been relatively scanty, primarily due to the poor potential for skel
etal fossilization, and so has provided little useful input into funda
mental discussions of vertebrate diversification. However, these situa
tions are changing. Chimaerids are increasingly becoming the subject o
f renewed biological and limited fisheries interests. Regarding extinc
t chondrichthyans, the last 30 or so years have entailed discoveries o
f new fossils that illuminate our view of Palaeozoic life and are elic
iting dramatic changes in our understanding of these early fishes, the
ir relations, and the origins of jawed conditions. Morphological exami
nation of fossil chondrichthyans indicates that the plesiomorphous sta
te of the gnathostome suspensorium is autodiastylic and that complex l
abial cartilages are primitive and likely to have been critical to the
mechanical architecture of the first jaws. Analysis of cranial morpho
logy, cranial proportions, the phyletic and developmental history of c
alcified tissues, and postcranial data including the evolution of the
prepelvic tenaculum are now feasible. Cumulatively, when the results o
f these analyses are subject to cladistical evaluation, the result is
one predominant cladogram supporting two monophyletic subclasses: the
Elasmobranchii and the Euchondrocephali. The latter subclass contains
a monophyletic group of holocephalans including the Cochliodontomorpha
, and within this taxon, the restricted Chimaeriformes. Alternative cl
adograms of the non-holocephalan Euchondrocephali are dependent upon w
hether whole-body or cranial characters alone are employed in the anal
ysis, or the additive or non-additive treatment of characters. Otherwi
se, only the discovery and description of additional members of this d
iverse assemblage are expected to alter these patterns of associations
.