The recent classification of the onset of turbulence as a directed percolation (DP) phase transition has been applied to all major shear flows including pipe, channel, Couette and boundary layer flows. A cornerstone of the DP analogy is the memoryless (Markov) property of turbulent sites. We here show that for the classic case of channel flow, the growth of turbulent stripes is deterministic and that memorylessness breaks down. Consequently turbulence ages and the one to one mapping between turbulent patches and active DP-sites is not fulfilled. In addition, the interpretation of turbulence as a chaotic saddle with supertransient properties, the basis of recent theoretical progress, does not apply. The discrepancy between channel flow and the established transition model illustrates that seemingly minor geometrical differences between flows can give rise to instabilities and growth mechanisms that fundamentally alter the nature of the transition to turbulence.