In this work, we analyse the sequence of bifurcated equilibria in two dimen
sional reduced magnetohydrodynamics. Diamagnetic effects are studied un der
the assumption of a constant equilibrium pressure gradient, not altered by
the formation of a magnetic island. The formation of an island when the sy
mmetric equilibrium becomes unstable is studied as a function of the tearin
g-mode stability parameter Delta' and of the diamagnetic frequency, by empl
oying fixed-point numerical technique and an initial-value code. At larger
values of Delta', a tangent bifurcation takes I,lace, above which no small-
island solutions exist. This bifurcation persists up to fairly large values
of the diamagnetic frequency (of the order of one-tenth of the Alfven freq
uency). The implications of this phenomenology for the intermittent MHD dyn
amics observed in tokamaks is discussed.