Michael undersells the following point a bit in the post but, in person, he has been making it for years:, i.e. that pumice provenance actually matters a great deal and can account for different observed performance of "pumice" in different parts of the US.
There are noticeable differences in pumice even within the northwestern US, for example between Oregon pumice and Idaho pumice (Hess mine). Japanese pumice is very different looking from the Oregon stuff as Michael has mentioned. The Hess mine stuff has a non-trivial quantity of obsidian in it and looks quite different (much whiter) when totally dry. When I tried the Hess mine stuff 5 years ago, Michael warned me that I might not like it as much as the local stuff.
I think we do ourselves a (mild) disservice when we treat pumice as a monolith (pun intended I guess), but given that many obtain it in a way that obscures the source (especially if shipped instead of picked up at a local aggregate supplier), I think it makes some sense we haven't been able to wrap our heads around it yet.
Even lava/scoria has some similar provenance issues. For example, the previously-discussed unwanted (boron I think?) toxicities in some (but not all) Oregon-collected lava. Meanwhile, other lava causes no issues for growers. I have similar results as
@Ruddigger in that my (non-Oregon-sourced AFAIK) lava holds a lot of water and is impressively hefty when wet (which I like, because it also seems to hold lots of air), but the stuff collected from the cinder cone in the Cascades (a common directly-collected source of lava for people around here) seems to hold less water than my out-of-state sourced stuff. They look noticeably different from one another but are both undeniably and clearly scoria. Unfortunately, I don't know where my out-of-state stuff came as it was ordered online. But there are differences.
Side note,
@Cadillactaste mentioned surface roots above. Something that is common teaching within Hagedorn's sphere of influence (students / apprentices) -- top dressing goes on damn near everything,
including conifers. IMO, top dressing (not just the precise way in which it is done, but also the lack of fear of top dressing) and specific watering practices (do it like the teacher says or the warranty is void) are a huge influence over the observed performance of any soil used by this group of people. I'll just say for
@Ruddigger 's benefit that I have found some really nice short-fiber moss that will reliably (albeit slowly) colonize scoria. Going back to pumice (and adding the possible confounding factors of pumice provenance), whenever people on the west coast (esp central valley and SW regions) report extremely rapid top-drying of pumice, I always wonder what their top dressing practices are, if any. Michael teaches multiple top dressing techniques -- not just moss, but as
@Cadillactaste mentions, also shohin-sized akadama/pumice.