Roles of orbital degree of freedom of Mn ions in phase transition as functi
ons of temperature and hole concentration in perovskite manganites are stud
ied. It is shown that the orbital order-disorder transition is of the first
order in the wide region of hole concentration, and the Neel temperature f
or the anisotropic spin ordering, such as the layer-type antiferromagnetic
one, is lower than the orbital ordering temperature due to the anisotropy i
n the orbital space. The calculated results of the temperature dependence o
f the spin and orbital order parameters explain a variety of the experiment
s observed in manganites.