We consider a granular gas under the action of gravity, fluidized by a vibrating base. We show that a horizontal temperature gradient, here induced by limiting dissipative lateral walls (DLW), leads always to a granular thermal convection (DLW-TC) that is essentially different from ordinary bulk-buoyancy-driven convection (BBD-TC). In an experiment where BBD-TC is inhibited, by reducing gravity with an inclined plane, we always observe a DLW-TC cell next to each lateral wall. Such a cell squeezes towards the nearest wall as the gravity and/or the number of grains increase. Molecular dynamics simulations reproduce the experimental results and indicate that at large gravity or number of grains the DLW-TC is barely detectable.Shaken granular media escape most of the laws of equilibrium thermodynamics and statistical mechanics [1], ranging from slow plastic flows [2] to fast gas-like dynamics [3][4][5]. In the wide granular phenomenology [6], an ubiquitous pattern is the convective cell. Notwithstanding its widespread occurrence, many different mechanisms lead to granular convection, and their relevance depends on the granular state under scrutiny.At high packing fraction and low fluidization, "dense convection" is observed [7][8][9][10]. A convincing explanation of dense convection comes from the asymmetric tangential friction at the lateral walls that results in a net downward shear force [11][12][13]. Dense granular convection can also involve more complex mechanisms, including the formation of unstable heaps at the free surface [14].In highly fluidized states (granular gases), the only known theoretical mechanism is bulk buoyancy-driven thermal convection (BBD-TC), first observed in simulations [15,16]. In analogy to molecular liquids [17,18], it originates from the buoyancy force associated to temperature/density gradients that, because of the intrinsic bulk inelasticity, emerge spontaneously [19], even with an open or reflecting top boundary [20]. BBD-TC is an instability of the hydrostatic state which requires a combination of parameters (including inelasticity, gravity and dimensions) to overcome a certain threshold [21,22]. A further confirmation that BBD-TC is essentially a "bulk" effect comes from simulations [15] and theory [21,22] where lateral walls are not required to observe it. Convective circulation in granular gases has been seen also in experiments, where lateral walls are always inelastic [23][24][25][26], and successive simulations with elastic [27] and also inelastic walls [28].The role of lateral walls in dilute granular convection has not been fully understood yet. Some of the mentioned studies recognize that lateral walls influence the observations. For instance, a downward flow velocity is always observed near lateral walls, perhaps because of a reduced buoyancy originated from enhanced dissipation [15,23,28]. However, quite contrasting results emerge in simulations and experiments concerning the necessity of dissipation at the lateral walls. In some simulations convection is strong even w...