A cladistic analysis places the Onychophora between Polychaeta and Art
hropoda. The 'Uniramia' concept is not supported. No justification was
found for either onychophoran family to be considered ancestral. A cl
adogram of fossil genera indicates the common ancestor to have long on
copods, armoured plates and an annulated body. Later forms show adapta
tions to life in reduced spaces. Physiological data suggest that the O
nychophora became adapted to land via the littoral zone, before the La
te Ordovician. Adhesive glands evolved for defence on land. Peripatops
idae and Peripatidae were distinct by the late Triassic. The occurrenc
e of onychophorans probably dates from post-Pliocene in New Guinea and
southern Australia, and post-Early Cretaceous in Chile, the southern
half of Southeast Asia, Mesoamerica and the Caribbean. After the Early
Cretaceous, the peripatids of tropical Africa lost terrestrial contac
t with those of South America. A new biogeographic technique, formaliz
ed here under the name retrovicariance, indicates that the Peripatidae
of Equatorial Africa and the Neotropics are sister-groups. Typical in
breeding adaptations found in some onychophorans include: female-biase
d sex ratios; gregarious development; relatively constant time of deve
lopment and number of offspring in each clutch; male polygamy and shor
ter life span; frequent sibmating in the microhabitat of development,
and sperm storage by females, so that a single insemination fertilizes
all ova.