Just throwing a little historical context in here, but Gibbs was the first to publish regarding this idea (1902). In my opinion there really isn't anything fundamental encoded in Liouville's theorem, other than rules of calculus and n-dimensional divergence theorem. When we go a little further with the Hamiltonian we can start to extract some interesting information from it.
I've been enjoying studying this concept for a number of years now and here's my explanation of it. First there's a probability distribution that is a function of all of the position and momenta in a system (and is an explicit function of time),
$$\rho \equiv \rho(p_1, q_1, ..., p_n, q_n, t)$$
It's the probability of "finding" the state with the above state variables. It is also a true probability in the sense that integrating it over the limit of all states gives 1,
$$\int^{phase\ limits}... \int \rho\ dp_1 dq_1...dp_n dq_n dt = 1$$
Using the partial differential chain rule we can establish,
$$\frac{d\rho}{dt} = \frac{\partial \rho}{\partial t}\frac{dt}{dt}+\frac{\partial \rho}{\partial p_1}\frac{dp_1}{dt}+\frac{\partial \rho}{\partial q_1}\frac{dq_1}{dt}+ ...$$
If we assume the phase space is analogous to an incompressible fluid, we can use n-dimensional divergence theorem to arrive at the following (Gibbs showed this as well, but using older notation),
$$\frac{d\rho}{dt}=0$$
We get Liouville's Theorem,
$$\frac{\partial \rho}{\partial t}=-\sum^{n}_{i=1}\left( \frac{\partial \rho}{\partial p_i}\frac{dp_i}{dt}+\frac{\partial \rho}{\partial q_i}\frac{dq_i}{dt} \right)$$
Using Hamiltonian notation and rearranging slightly,
$$\frac{\partial \rho}{\partial t}=-\sum^{n}_{i=1}\left(\frac{\partial \rho}{\partial q_i}\frac{\partial H}{\partial p_i} -\frac{\partial \rho}{\partial p_i}\frac{\partial H}{\partial q_i} \right)$$
As per the interesting types of things you can do with Liouville's Theorem, we can actually derive the canonical ensemble using the condition of statistical equilibrium (the idea that the probability density function does not change with respect to time, considering all phase variables constant),
$$\frac{\partial \rho}{\partial t} = 0$$
And then we get,
$$-\sum^{n}_{i=1}\left(\frac{\partial \rho}{\partial q_i}\frac{\partial H}{\partial p_i} -\frac{\partial \rho}{\partial p_i}\frac{\partial H}{\partial q_i} \right)=0$$
A solution of this partial differential equation, is the following (this is easy to verify with kinetic/potential energy functions in Newtonian mechanics),
$$\rho=Ae^{-H/kT}=e^{F/kt}e^{-H/kT}=e^{(F-H)/kT} $$
From which falls out the thermodynamic identity.