Three major bilaterian clades first appear in the Early Cambrian fossil rec
ord: Deuterostomia, Lophotrochozoa, and Ecdysozoa. The taxa placed in Ecdys
ozoa are characterized by a moulting habit, unknown in the other major clad
es. The origin and consequences of moulting are of fundamental importance t
o the history of the ecdysozoan clade, chiefly because moulting precludes m
otile ectodermal cilia. Moulting may have originated as an adaptation to pe
rmit the enlargement, during growth, of secreted cuticular spines, flanges,
and other structures used as ancillary locomotory devices. A combination o
f phylogenetic and fossil evidence suggests that the early members of these
clades were small vermiform paracoelomates that likely lacked indirect-dev
eloping planktotrophic larvae. Thus, the evolution of planktotrophic larvae
may have been independently achieved at least three times within Bilateria
. The nonmoulting clades evolved larvae that swim and feed via ciliated tuf
ts and bands, presumably intercalating these forms within their early devel
opmental systems. Within Ecdysozoa, feeding larvae lacked ciliary feeding t
racts and evolved by modification of early instars, employing limbs or seta
e to generate feeding currents. The setting aside during larval life of cel
ls that give rise to adult features is probably an adaptation associated wi
th metamorphosis.