This research focuses on simulating crack propagation in fluid-saturated porous materials undergoing large deformations. A two-scale numerical model is used, with the micro-scale governing fluid flow through the deformable porous material, and the macro-scale using finite elements coupled to the local momentum and mass balances from the micro-scale. Micro-cracks are modeled using cohesive zone laws, where the traction decreases with crack opening. The resulting equations are nonlinear and solved iteratively using Newton-Raphson and Crank-Nicholson schemes. The goal is to extend the approach to fully capture large material deformations with small crack openings, using hyperelastic constitutive models.