The point Ji and others seem to agree with is that the observed, basally branched structures in the fossils fit well with Prum's evolutionary model of a down-like branching pattern evolving BEFORE the pinnate branching pattern. Fuzzy natal down is just a limited sub-class of down-like feathers. Those on the new dromaeosaurs and troodon are different, and seem very un-down-like to our (my) modern, natal-down-conditioned sensibilites. But they are still called "down-like" for the reasons I just mentioned.