“…The two structural forms of free ferrihydrite often studied are the smaller, less-ordered two-line (2L) ferrihydrite and the larger, more-ordered six-line (6L) ferrihydrite, where the number of lines refers to the number of X-ray diffraction maxima [25, 26]. When the iron content per ferritin protein cage is lower, the ferritin mineral resembles 2L ferrihydrite; as the iron content per cage increases, the mineral resembles 6L ferrihydrite [27, 28]. We compared free 2L and 6L ferrihydrite with 2L and 6L ferrihydrite inside ferritin cages for three reasons: (1) structurally distinct, microscale to macroscale iron (oxyhydr)oxide minerals have in the past influenced bacterial iron bioavailability [17, 29–31] and dissolution rates in the presence of siderophores [32]; (2) aggregation of free ferrihydrite [15–17] is faster with 2L ferrihydrite than with 6L ferrihydrite (unpublished observations); (3) ferritin protein cages, which control both mineral synthesis and dissolution [23, 24, 33], may be degraded in diseased tissue [34, 35], exposing the ferrihydrite core (hemosiderin).…”