Edwards established Aglaophyton for the plant formerly called Rhynia major after re-examining new and historical material; the profile preserves the paper's refusal to assign the genus to a living higher group.
claim:taxon:aglaophyton:taxonomyAglaophyton major is represented here by Edwards's re-examination of new and historical Rhynie-chert material, which established the genus and reconstructed its axes and conducting strand without assigning it to a living higher group.
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Edwards established Aglaophyton for the plant formerly called Rhynia major after re-examining new and historical material; the profile preserves the paper's refusal to assign the genus to a living higher group.
claim:taxon:aglaophyton:taxonomyThe profiled Aglaophyton major material is from the Rhynie Chert of Aberdeenshire, Scotland; this named deposit does not establish the genus's complete geographic distribution or centre of origin.
claim:taxon:aglaophyton:biogeographyThe Aglaophyton reconstruction includes extensive stands of decumbent axes with upright branches, but the fossil study did not measure carbon acquisition, population breadth or a genus-wide ecological guild.
claim:taxon:aglaophyton:ecologyAglaophyton major was reconstructed with decumbent axes, dichotomously branching upright axes and terminal sporangia; its three-zoned conducting strand lacks the differential wall thickenings used to diagnose tracheids.
claim:taxon:aglaophyton:morphologyThe displayed 412.8–410.2 Ma interval is the 411.5 ± 1.3 Ma U–Pb uncertainty window used for the represented Rhynie-chert material; it is not a global Aglaophyton first appearance, last appearance or lineage duration.
claim:taxon:aglaophyton:fossil-range