We present a cladistic analysis of the Cirripedia Thoracica using morp
hological characters and the Acrothoracica and Ascothoracida as outgro
ups. The list of characters comprised 32 shell and soft body features.
The operational taxonomic units (OTUs) comprised 26 well-studied foss
il and extant taxa, principally genera, since uncertainty about monoph
yly exists for most higher ranking taxonomic units. Parsimony analyses
using PAUP 3.1.1 and Hennig86 produced 189 trees of assured minimal l
ength. We also examined character evolution in the consensus trees usi
ng MacClade and Clados. The monophyly of the Balanomorpha and the Verr
ucomorpha sensu stricto is confirmed, and all trees featured a sister
group relationship between the 'living fossil' Neoverruca and the Brac
hylepadomorpha. In the consensus trees the sequential progression of '
pedunculate' sister groups up to a node containing Neolepas also confo
rms to current views, but certain well-established taxa based solely o
n plesiomorphies stand out as paraphyletic, such as Pedunculata (=Lepa
domorpha); Eolepadinae, Scalpellomorpha and Chthamaloidea. The 189 tre
es differed principally in the position of shell-less pedunculates, Ne
overruca, the scalpelloid Capitulum, and the interrelationships within
the Balanomorpha, although the 50% majority rule consensus tree almos
t fully resolved the latter. A monophyletic Sessilia comprising both V
errucomorpha and Balanomorpha appeared among the shortest trees, but n
ot in the consensus. A tree with a monophyletic Verrucomorpha includin
g Neoverruca had a tree length two steps longer than the consensus tre
es. Deletion of all extinct OTUs produced a radically different tree,
which highlights the importance of fossils in estimating cirripede phy
logeny. Mapping of our character set onto a manually constructed clado
gram reflecting the most recent scenario of cirripede evolution result
ed in a tree length five steps longer than any of our shortest trees.
Our analysis reveals that several key questions in cirripede phylogeny
remain unsolved, notably the position of shell-less forms and the tra
nsition from 'pedunculate' to 'sessile' barnacles. The inclusion of mo
re fossil species at this point in our understanding of cirripede phyl
ogeny will only result in even greater levels of uncertainty. When con
structing the character list we also identified numerous uncertainties
in the homology of traits commonly used in discussing cirripede evolu
tion. Our study highlights larval ultrastructure, detailed studies of
early ontogeny, and molecular data as the most promising areas for fut
ure research. (C) 1995 The Linnean Society of London