Computations of fluid drift turbulence treating ions and electrons on
equal footing, including both temperatures, are conducted in a model t
oroidal geometry. The resulting 'ion mixing mode' turbulence bears fea
tures of both electron drift-Alfven and ion temperature gradient turbu
lence, and nonlinear sensitivity to the relative strengths of the dens
ity and temperature gradients provides a possible route to the bifurca
tion needed for the L-H transition.