Unequal vascular cambium growth of a small Archaeopteris branch with Callixylon zalesskyi-type wood from the Late Devonian (early Frasnian) of New York demonstrates that reaction wood is a basal lignophyte growth response, rather than a derived feature of more recent seed plants. Archaeopteris reaction wood shows the same anatomical signatures of compression wood, opposite wood, and side wood as occur in modern conifer gymnosperms. Cambial growth is markedly asymmetric with one side having far more secondary xylem cells than the other. Secondary phloem production, however, is the same. Tracheids on the side with more production are smaller, with some intercellular spaces, and have thicker secondary walls that are often rounded (some detached from primary walls). Pits of tracheids with the thickest secondary walls lack obvious pit borders, which suggests a thick S2 but no S3 wall layer, and have abundant helical cavities or splits (checks) on their tangential and radial walls. Tracheids on the opposite side, where many fewer cells are produced, are larger in XS, lack intercellular spaces, have thinner secondary walls that are always attached to the primary wall, have fully bordered pits (complete S2 and S3 layers), and have solid unchecked walls when seen in LS surface view. Rays on both sides of the axis are of similar widths and have ray tracheids. Rays on the side with more growth are curved, although this may result from compression. Secondary growth mechanisms thus appear to be substantially the same for all lignophytes, from Devonian progymnosperms to conifers and angiosperm trees of today.

Key words: Archaeopteris, Devonian, progymnosperm, reaction wood