A theory for non-linear rheology of molten polymer layers between soli
d surfaces in the Rouse regime is discussed. It is shown that the effe
ct of finite extensibility of polymer chains leads to I;he characteris
tic 1/3 power law for the shear stress vs. shear velocity in the regim
e of high velocities. It is also shown that bridging polymer fragments
connecting the two surfaces play an important role for the rheology i
f the effective monomer friction in the immediate vicinity of the surf
aces is much higher than far from the surfaces. In particular we predi
ct that shear stress is decreasing with shear velocity u in a limited
range between u(1) and u(min). This effect results in a possibility of
stick-slip periodical dynamics of the layer under a constant imposed
velocity.