We report experimental results for heat-transport measurements by turbulent Rayleigh-B'enard convection in a cylindrical sample of aspect ratio $\Gamma \equiv D/L = 1.00D = 1.12L = 1.12$ m the height). They are for the Rayleigh-number range $4\times10^{11} \alt \Ra \alt 2\times10^{14}$ and for Prandtl numbers \Pra\ between 0.79 and 0.86. For we find $\Nu = N_0 \Ra^{\gamma_{eff}}\gamma_{eff} = 0.321 \pm 0.002N_0 = 0.0776$, consistent with classical turbulent Rayleigh-B'enard convection in a system with laminar boundary layers below the top and above the bottom plate and with the prediction of Grossmann and Lohse. For the data rise above the classical-state power-law and show greater scatter. In analogy to similar behavior observed for $\Gamma = 0.50$, we interpret this observation as the onset of the transition to the ultimate state. Within our resolution this onset occurs at nearly the same value of as it does for . This differs from an earlier estimate by Roche {\it et al.} which yielded a transition at $\Ra_U \simeq 1.3\times 10^{11} \Gamma^{-2.5\pm 0.5}\Gamma\Ra^*_1$ would suggest that the boundary-layer shear transition is induced by fluctuations on a scale less than the sample dimensions rather than by a global -dependent flow mode. Within the resolution of the measurements the heat transport above is equal for the two values, suggesting a universal aspect of the ultimate-state transition and properties. The enhanced scatter of \Nu\ in the transition region, which exceeds the experimental resolution, indicates an intrinsic irreproducibility of the state of the system.

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