The homology of larval-feeding modes has been a major element in recent dis
cussions about animal phylogeny. 'Downstream-feeding' is one of the two mai
n larval-feeding modes, and is usually equated to an opposed-band system in
volving ciliary bands called the prototroch and metatroch. Larval-feeding i
n Spiralia is reviewed here and the homology hypothesis of downstream larva
l-feeding is expanded, encompassing any feeding involving the prototroch. I
t is often argued that the presence of planktotrophic larvae using downstre
am-feeding is plesiomorphic among spiralian animals, and that there is a bi
as in transformations, such that feeding larvae tend to be lost rather than
gained. These hypotheses are assessed in relation to the Spiralia, Trochoz
oa and particularly polychaete annelids. Cladistic parsimony analyses are p
erformed based on datasets of Rouse & Fauchald (1997) and Rouse (1999), wit
h an additional character based on downstream larval-feeding. Methods adopt
ed to assess the possibility of a bias in transformations towards loss of d
ownstream larval-feeding include: expanded primary homology arguments, char
acter transformations favouring reversals and polymorphic terminals coded a
s having downstream larval-feeding. These measures all tend to favour the p
ossibility that downstream larval-feeding will be plesiomorphic, and tends
to be lost rather than gained. Nevertheless, all analyses show that downstr
eam larval-feeding is not plesiomorphic, and appears to have evolved multip
le times. The results support a conclusion that the prototroch has become a
ssociated with feeding a number of times. Hypotheses of metazoan phylogeny
that are predicated on the assumption that downstream-feeding larvae are pl
esiomorphic (e.g. Peterson et al. 1997) should be re-assessed.