Very interesting article, but as a layman what I must have missed? is why are the orange tubercules are so very orange, it's an unusual colour. From a little experience years ago looking at rust (what an exciting job

) in non marine environments I'd associate chloride with producing particularly dark rust and almost black crustiness on corroding rebar, so why is that stuff very orange, could it be iron-3 chloride being formed there?
Not quite the same rust oysters, but I'd be surprised if things didn't share some mechanism. It also made me think about rust staining. In my lazy ignorance I've always seen ochreous staining and thought "iron" or something yellower/more orangey and thought "must be some sulphur too", but thinking about it, the orangeyer stuff might be fecl3 as often or more than sulphury gunk in the mix I mean slate and mudstones for example are previously marine after all? also I wonder if that is as solution inside an oyster as it would have a slightly foul acidic smell and be slightly murky brown -- which fits the description. If so it should have a pH of 2 but then again so do a lot of other things including mixtures or goodness knows what with chlorine sulphur iron hanging about. I wonder if testing the pH will tell us anything or just confuse us more
This is ripe for a PhD/MSc or something? Surely someone somewhere must need an idea for research and can look into this for us?