Close-by planets may excite various kinds of oscillations in their host stars
through their time-varying tidal potential. Magnetostrophic oscillations with a
frequency much smaller than the stellar rotation frequency have recently been
proposed to account for the spin-orbit commensurability observed in several
planet-hosting stars. In principle, they can be resonantly excited in an
isolated slender magnetic flux tube by a Fourier component of the time-varying
tidal potential with a very low frequency in the reference frame rotating with
the host. However, due to the weakness of such high-order tidal components, a
mechanism is required to lock the oscillations in phase with the forcing for
long time intervals ( years) in order to allow the oscillation
amplitude to grow. We propose that the locking mechanism is an autoresonance
produced by the non-linear dependence of the oscillation frequency on its
amplitude. We suggest that the angular momentum loss rate is remarkably reduced
in hosts entering autoresonance that contributes to maintain those systems in
that regime for a long time. We apply our model to a sample of ten systems
showing spin-orbit commensurability and estimate the maximum drifts of the
relevant tidal potential frequencies that allow them to enter the autoresonant
regime. Such drifts are compared with the expected drifts owing to the tidal
evolution of the planetary orbits and the stellar angular momentum loss in the
magnetized winds finding that autoresonance is a viable mechanism in eight
systems, at least in our idealized model. The duration of the autoresonant
regime and the associated spin-orbit commensurability may be comparable with
the main-sequence lifetimes of the host stars, indicating that gyrochronology
may not be applicable to those hosts.