Recently, the existence of a pointlike pertuber PX with 1 m ♂ m X 2.4 m ⊕ (the symbol " ♂ " denotes Mars) supposedly moving at 65 − 80 AU along a moderately inclined orbit has been hypothesized in order to explain certain features of the midplane of the Kuiper Belt Objects (KBOs). We preliminarily selected two possible scenarios for such a PX, and numerically simulated its effect on the Earth-Saturn range ρ (t) by varying some of its orbital parameters over a certain time span; then, we compared our results with some existing actual range residuals. By assuming m X = 1 m ♂ and a circular orbit, such a putative new member of our Solar System would nominally perturb ρ (t) by a few km over ∆t = 12 yr (2004 − 2016). However, the Cassini spaceraft accurately measured ρ (t) to the level of σ ρ ≃ 100 m. Nonetheless, such a scenario should not be considered as necessarily ruled out since the Cassini data were reduced so far without explicitly modeling any PX. Indeed, a NASA JPL team recently demonstrated that an extra-signature as large as 4 km affecting the Kronian range would be almost completely absorbed in fitting incomplete dynamical models, i.e. without PX itself, to such simulated data, thus not showing up in the standard post-fit range residuals. Larger anomalous signatures would instead occur for m X > 1 m ♂ . Their nominal amplitude could be as large as 50 − 150 km for m X = 2.4 m ⊕ , thus making less plausible their existence.