The introduction and rapid spread of Drosophila subobscura in the New-World
two decades ago provide an opportunity to determine the predictability and
rate of evolution of a geographic cline. In ancestral Old World population
s, wing length increases clinally with latitude, in North American populati
ons, no wing length cline was detected one decade after the introduction. A
fter two decades, however, a cline has evolved and largely converged on the
ancestral cline. The rate of morphological evolution on a continental scal
e is very fast, relative even to rates measured within local populations. N
evertheless, different wing sections dominate the New versus Old World clin
es. Thus, the evolution of geographic variation in wing length has been pre
dictable, but the means by which the cline is achieved is contingent.