It is shown that if the Al-26 inventory of the early solar system, tak
en as (Al-26/Al-27).= 5 x 10(-5), is a result of injection of fresh de
bris from a Type II supernova (SNII), then Fe-60/Fe-56 would have to b
e between 3 x 10(-7) and 1 x 10(-5). This inferred correlation of Al-2
6 and Fe-60 is based on the observation that both nuclei are produced
dominantly in the O/Ne zone and that for SNII ejecta Al-26/Fe-60 is be
tween 0.6 and 23. A similar correlation applies to Ca-41, Cl-36, O-16,
and O-18, which are also produced in the same zone or in nearby regio
ns. The supernova trigger hypothesis may be tested by determination of
Ni-60 excesses correlated with Fe in samples where Al-26 was demonstr
ated to be present. From available experimental data, it appears that
the observed abundance of 60Fe is too low to be compatible with a supe
rnova trigger that injected the Al-26 into the protosolar nebula. The
same is true for Mn-53, a short-lived nucleus produced in the outer ed
ge of the Ni core.