“…The closest living relative of these plants is the diminutive Isoetes , which is a member of the cormose group of isoetaleans that have a much reduced, compact base rather than a more extensive stigmarian system (Bierhorst, 1971; Larsén & Rydin, 2016). Present fossil evidence suggests that isoetaleans with contrasting stigmarian and cormose rooting systems co‐occurred in the Devonian (e.g., Chitaley & Pigg, 1996; Wang et al, 2003; Cressler & Pfefferkorn, 2005; Prestianni & Gess, 2014; Hetherington et al, 2016, 2019; Xu & Wang, 2016; Stein et al, 2020). Given the evidence for pervasive heterochrony as a force shaping the gross morphology of these plants (Bateman & DiMichele, 1991; Pigg, 1992; Bateman, 1994), we increasingly suspect that forms with reduced rhizomorphic rooting systems may represent multiple origins from stigmarian ancestors.…”