The equation you have written cannot be correct, even approximately, except in cases where rotation is unimportant.
If rotation of the gas is important, that rotation occurs around an axis. This breaks any spherical symmetry (and if it doesn't then rotation is unimportant), makes the problem at least two dimensional and an equation featuring a single spatial coordinate won't do.
To make further progress then the relevant expression for hydrostatic equilibrium depends on the rotation law of the gaseous object $\Omega({\bf r})$.
If the cloud rotates as a solid body, such that $\Omega$ is constant, then we can write.
$$ \frac{1}{\rho} \nabla P = -\nabla \Phi + \frac{1}{2} \nabla (\Omega^2 r^2\sin^2 \theta)\ ,$$
where $\nabla P$ is the local pressure gradient, $\Phi$ is the gravitational potential, and the second term on the right is the gradient of the centrifugal potential with $r \sin \theta$ representing the distance to the rotation axis at co-latitude $\theta$.
This can be rewritten by assuming a new combined potential
$$ \Psi = -\frac{GM_r}{r} - \frac{1}{2}\Omega^2 r^2\sin^2 \theta$$
so that
$$ \frac{1}{\rho} \nabla P = -\nabla \Psi $$
In general then, the pressure gradient is no longer in the radial direction, however the isobars are still equipotentials.
An alternative approximation is to consider "shellular rotation", where $\Omega$ is constant along isobars. In this case
$$ \frac{1}{\rho} \nabla P = -\nabla \Psi -r^2 \sin^2 \theta \nabla \Omega $$
Here, the surfaces of constant pressure are not equipotentials.
If all you are interested in is establishing whether rotation could alter the pressure gradient, then you just need to compare $GM/r^2$ with $\Omega^2 r$.