These ferns have creeping rhizomes. The compound eaves fork multiple times, with the final leaf lobes ending in a pinnate arrangement. The sori are found at the bottom of the leaves and are made of a few sporangia. They are not covered by an indusium (protective covering). The sori occur in a unique chamber in the laminar pits - a feature found only in this genus.
Fossil record
Gleichenia dicarpa leaves
The fossil record indicates that this genus had emerged by the late Jurassic period, although it was far more common in the early Cretaceous period. There is some evidence that it may have emerged even earlier - in the upper Triassic period. There are, however, multiple genera in the fossil record that show a similar leaf branching pattern to Gleichenia, which can make it difficult to determine the exact identity of a specimen that does not have adequately preserved fruiting bodies.
Fossils have been found in across a wide geographic range including:
The Pariwar formation in India (Jurassic-Cretaceous boundary)
12"Genus Gleichenia". PlantNET - New South Wales Flora Online. Royal Botanic Gardens & Domain Trust, Sydney Australia. Retrieved 2009-01-26.
↑Pryer, K. M., E. Schuettpelz, P. G. Wolf, H. Schneider, A. R. Smith, and R. Cranfill (2004). Phylogeny and Evolution of Ferns (Monilophytes) with a Focus on the Early Leptosporangiate Divergences. American Journal of Botany 91 (10): 1582–98.
↑Levyns, M.R. (1966). A Guide to the Flora of the Cape Peninsula (2nd Reviseded.). Juta & Company, Limited. OCLC621340.
↑Bose, M.N.; Kumaran, K.P.N.; Baneiji, J. (1982). "Pachypteris haburensisn. sp. and other plant fossils from the Pariwar Formation". Palaeobotanist. 30 (1): 1–11.