Fig. 2: Distributions of 40K–40Ar system ages, measured by the K–Ar and 40Ar–39Ar methods.
From: An early giant planet instability recorded in asteroidal meteorites

Time is reported as both age (Ma, lower x axis) and time after Solar System formation (Myrss, upper x axis). Histograms reflect the summed distributions of ages from each dataset. K–Ar age density has a broad, shallow maximum at ~4,200 Ma, that gradually decays to low probability densities with minor local maxima extending to the present day. 40Ar–39Ar age density monotonically decreases from a sharp peak (>2× the height of the K–Ar peak) shortly after the age of the Solar System (dashed line), with minor local peaks between ~4,200 Ma and 3,600 Ma. By 3,500 Ma, the distribution converges on near-nil probability density until an approximately symmetric local maximum within the last 2,000 Ma. As these <2,000 Ma ages (shaded) are not associated with GPM (see text), we exclude them from our analyses. If we recalculate the 40Ar–39Ar age distribution with lower precision (σ = 6%) to mimic the K–Ar system, the early peak is more broad and shallow but the maximum remains >4,300 Ma.