We re-examine V. Gribov's theorem of 1960 according to which the total
cross-section cannot approach a finite non-zero limit with, at the same time, a
diffraction peak having a finite slope. We are very close to proving by an
explicit counter-example that elastic unitarity in the elastic region is an
essential ingredient of the proof. By analogy, we raise the question of the
saturation of the Froissart-Martin bound, for which no examples incorporating
elastic unitarity exist at the present time.Comment: 11 pages, 1 figures, latex with sproc.st