Resolved observations of millimetre-sized dust, tracing larger planetesimals,
have pinpointed the location of 26 Edgeworth-Kuiper belt analogs. We report
that a belt's distance R to its host star correlates with the star's
luminosity L⋆, following R∝L⋆0.19 with a low
intrinsic scatter of ∼17%. Remarkably, our Edgeworth-Kuiper belt in the
Solar System and the two CO snow lines imaged in protoplanetary disks lie close
to this R-L⋆ relation, suggestive of an intrinsic relationship
between protoplanetary disk structures and belt locations. To test the effect
of bias on the relation, we use a Monte Carlo approach and simulate
uncorrelated model populations of belts. We find that observational bias could
produce the slope and intercept of the R-L⋆ relation, but is unable
to reproduce its low scatter. We then repeat the simulation taking into account
the collisional evolution of belts, following the steady state model that fits
the belt population as observed through infrared excesses. This significantly
improves the fit by lowering the scatter of the simulated R-L⋆
relation; however, this scatter remains only marginally consistent with the one
observed. The inability of observational bias and collisional evolution alone
to reproduce the tight relationship between belt radius and stellar luminosity
could indicate that planetesimal belts form at preferential locations within
protoplanetary disks. The similar trend for CO snow line locations would then
indicate that the formation of planetesimals and/or planets in the outer
regions of planetary systems is linked to the volatility of their building
blocks, as postulated by planet formation models