A specific crystalline order, involving the Fibonacci series, had unti
l now only been observed in plants (phyllotaxis). Here, these patterns
are obtained both in a physics laboratory experiment and in a numeric
al simulation. They arise from self-organization in an iterative proce
ss. They are selected depending on only one parameter describing the s
uccessive appearance of new elements, and on initial conditions. The o
rdering is explained as due to the system's trend to avoid rational (p
eriodic) organization, thus leading to a convergence towards the golde
n mean.