Frank Peters said:
should cause a density gradient
Questions to be asked are:
1, Why should that be so?
2. Can a hydrostatic equation be set up to confirm?
3. What does a profile of graph of a density vs height look like? Pressure vs height? temperature vs height?
4 Will assumptions need to be made about the fluid? If so, which assumptions?
5. Will changing assumptions lead to a different profile?
6. How are other variables in the state of the fluid affected by the assumptions?
Of course that is pretty much what you are asking in the first place, so really nothing new.
But, rather than trying to explain it to yourself, how would you explain into another person, perhaps younger and learning, keen in mathematics and science, Sometimes easier to see the problem by stepping back a little.
By the way, for an incompressible fluid, such as water, we assume that density does not vary with pressure. The graph of density vs distance under the surface of a lake is linear, a vertical straight line, and that of P vs h is also linear, with P increasing with depth.