“…Reduced mobility has been demonstrated for most of the principal constituents of the core, such as ions, 15,16 pyridine-2,6-dicarboxylic acid (dipicolinic acid, DPA), 14,17 proteins, 18 and IM lipids, 5 but the mobility of core water has remained controversial. Early on, it was observed that virtually all spore water exchanges with external water within minutes, 19,20 implying that core water is in a liquid, rather than a glassy, state. This led to what may be termed the "gel scenario" of the core as a matrix of immobilized macromolecules (as well as DPA and chelated divalent metal ions) permeated by mobile or, at least, liquid water.…”