The 'antithetic theory' on the origin of the alternation of generation
s requires the interpolation of a multicellular sporophytic stage in e
arly land plants and the evolution of a gametophyte-sporophyte junctio
n, i.e., a true 'embryophytic' organization. Such gametophyte-sporophy
te junctions, omnipresent in modern archegoniate]and plants, have neve
r been found in fossil plants. It is postulated that the longitudinal
section through the base of an aerial axis (stem) and the basal corm o
f the Lower Devonian plant Horneophyton lignieri, published by Taylor
& Taylor (1993), might indicate such a fossilized gametophyte-sporophy
te junction.