  The formation mechanisms of the ice giants Uranus and Neptune, and the origin
of their elemental and isotopic compositions, have long been debated. The
density of solids in the outer protosolar nebula is too low to explain their
formation, and spectroscopic observations show that both planets are highly
enriched in carbon, very poor in nitrogen, and the ices from which they
originally formed might had deuterium-to-hydrogen ratios lower than the
predicted cometary value, unexplained properties observed in no other planets.
Here we show that all these properties can be explained naturally if Uranus and
Neptune both formed at the carbon monoxide iceline. Due to the diffusive
redistribution of vapors, this outer region of the protosolar nebula
intrinsically has enough surface density to form both planets from carbon-rich
solids but nitrogen-depleted gas, in abundances consistent with their observed
values. Water rich interiors originating mostly from transformed CO ices
reconcile the D/H value of Uranus and Neptune's building blocks with the
cometary value. Finally, Our scenario generalizes a well known hypothesis that
Jupiter formed on an iceline (water snowline) for the two ice giants, and might
be a first step towards generalizing this mechanism for other giant planets.
