Jc. Regier et Jw. Shultz, Molecular phylogeny of arthropods and the significance of the Cambrian "explosion" for molecular systematics, AM ZOOLOG, 38(6), 1998, pp. 918-928
Accurate phylogenetic reconstruction requires character systems that have e
volved fast enough to have kept pace with cladogenesis but slowly enough to
have conveyed the resulting phylogenetic signal to the present. Because st
ratigraphic evidence suggests that basal arthropod lineages arose rapidly d
uring an ancient (Cambrian) phylogenetic radiation, the discovery of molecu
lar sequences capable of resolving arthropod phylogeny may be a significant
challenge for molecular systematists. This challenge is exemplified by our
attempt to resolve arthropod phylogeny using the amino acid sequence of el
ongation factor-1 alpha (EF-1 alpha). Our fossil- based assessment of evolu
tionary rates indicates that EF-1 alpha should be capable of resolving Camb
rian-age divergences. However, phylogenetic analysis using EF-1 alpha fails
to establish relationships among most higher-level groups, although it doe
s recover more recently derived clades, Here we propose two models to expla
in this incongruity, The Rapid Radiation Model maintains that fossil-based
estimates of arthropod diversification are essentially accurate and that di
versification occurred so rapidly during the Cambrian that few phylogenetic
ally significant changes occurred in the slowly evolving EF-1 alpha sequenc
e, The Enhanced Preservation Model maintains that fossil-based estimates of
Cambrian-age divergences reflect enhanced preservation of pre-existing lin
eages and that arthropod diversification occurred before the Cambrian, This
model attributes lack of resolution to degradation of phylogenetic signal
within EF-1 alpha, by subsequent evolution. Current evidence is more consis
tent with the Enhanced Preservation Model, which implies that fossil-based
methods can be very misleading when attempting to gauge the phylogenetic in
formation content of molecular sequences for Cambrian- and Pre-cambrian age
divergences.