Temporal range: Devonian
|Reconstruction of Psilophyton forbesii; scale bar = 5 cm|
Dawson (1859) emend. Hueber & H.P.Banks (1967)
Psilophyton is a genus of extinct vascular plants. Described in 1859, it was one of the first fossil plants to be found which was of Devonian age (about ). Specimens have been found in northern Maine, USA; Gaspé Bay, Quebec and New Brunswick, Canada; the Czech Republic; and Yunnan, China. Plants lacked leaves or true roots; spore-forming organs or sporangia were borne on the ends of branched clusters. It is significantly more complex than some other plants of comparable age (e.g. Rhynia) and is thought to be part of the group from within which the modern ferns and seed plants evolved.
Almost all the species of Psilophyton have been found in rocks of Emsian age (around ). One exception is P. krauselii, from the Czech Republic, which is younger, being from the upper part of the Middle Devonian (around ).
Psilophyton dawsonii is the best-known species. Compressed and mineralized specimens have been found in several locations, particularly in calcareous pebbles on the Gaspé Peninsula, Quebec, Canada. Plants consisted of bare stems (axes) ending in blunt tips. Lower down they repeatedly branched dichotomously; higher up they bore sporangium-bearing 'units' in two rows on opposite sides of the stems. These units branched, also dichotomously, before terminating in sporangia, so that there were clusters of up to 128 paired, downward curved sporangia, oval in shape and about 5 mm long. Spores were released through a longitudinal slit. The first two branching points of the fertile units appear to have consisted of two closely spaced dichotomous branches in which the middle branch did not develop. The trilete spores were between 40 and 75 µm in diameter.
The internal structure of the stems of P. dawsonii was considerably more complex than that of other plants of a similar age, e.g. Rhynia. A central strand of xylem occupied up to a third of the diameter of the stem. In the lower parts of main stems it was circular, enlarging before it divided prior to dichotomous branching. Higher up it became elliptical in cross-section, corresponding to the two rows of fertile branching units. Within the branches of these units, the strand was more-or-less rectangular. The conducting elements of the xylem, the tracheids, were of the so-called 'P-type' in which the walls were strengthened by ladder-like (scalariform) bars with circular openings between them. The tissue around the central strand was multi-layered with open spaces below the stomata.
P. princeps, the first-discovered species, differed from P. dawsonii in having spines on the stems and larger sporangia. P. forbesii is the largest known species of Psilophyton. Reconstructions suggest a height of around 60 cm. Its stems were bare of spines but marked by longitudinal striations. Compared to P. dawsonii, both P. princeps and P. forbesii had a greater distinction between main stems and side branches, which may be considered an 'advanced' feature.
P. crenulatum was found in New Brunswick, Canada, also in rocks of Emsian age. Its branches bore spines up to 6 mm long which divided into two or three projections at their tips. It has resemblances to specimens of Aarabia, found in Morocco.
P. dapsile was found in Maine, USA. It appears to have been considerably smaller than the previous species, perhaps 30 cm tall, with smooth dichotomously branching stems, and sporangia only 2 mm long. Kasper et al. suggested that the smaller species P. dapsile and P. krauselii, which had mainly dichotomous branches, were the more 'primitive' members of the genus.
P. primitivum was found in Yunnan, China, in the Posongchong Formation, which is of Pragian (Siegenian) age (around ). All other species have been found in North America and Europe, which formed part of the continent of Laurussia in the Devonian. The name reflects a belief that the species is 'primitive', with considerable dichotomous branching and a loose, less tightly branched habit. As with all species of Psilophyton, pairs of sporangia were created by dichotomously branching fertile units, although in P. primitivum there were relatively few per unit (4–8) and they were somewhat loosely clustered. Similarities with P. microspinum and P. parvulum were suggested.
Leafless, dichotomously branching fossils bearing spines and possessing vascular tissue from the Devonian of Gaspé Peninsula, Canada, were thought by Dawson in 1859 to resemble the modern whiskfern, Psilotum. Accordingly, he named his new genus Psilophyton, the type species being P. princeps. Unfortunately, it later turned out that his description and subsequent reconstruction was based on fragments of three different unrelated plants, which caused confusion for many years. The sporangia were from Psilophyton, but some aerial stems were from what is now Sawdonia, and the rhizomes were from Taeniocrada.
In 1871, Dawson described specimens which had strong spines as P. princeps var. ornatum. He considered that groups of paired terminal sporangia found with these were part of the same plant, although no actual connection was found. Much later, in 1967, it was shown that fossils called "Psilophyton princeps" had two very different patterns of xylem development: from the centre outwards (centrarch) in P. princeps and from the outside inwards (exarch) in P. princeps var. ornatum. Hueber and Banks selected new specimens as the type for the species P. princeps, and Hueber later transferred P. princeps var. ornatum to a new genus as Sawdonia ornata. Only P. princeps had paired terminal sporangia; those of S. ornata were borne on the sides of the stems. Later additions of species to the genus have been based on the description by Hueber and Banks.
Dawson named another specimen Psilophyton robustius. On the grounds that this had side branches which divided into three as well as dividing into two, in 1956 Hopping moved it to a new genus Trimerophyton.
At first most of the early polysporangiophytes (land plants other than liverworts, mosses and hornworts) were placed in a single class, Psilophyta, established in 1917 by Kidston and Lang. As additional fossils were discovered and described, it became apparent that the Psilophyta were not a homogeneous group of plants. In 1968, Banks proposed splitting it into three groups, one of which was the subdivision Trimerophytina, informally called the trimerophytes. Psilophyton was a prominent member of this group. The distinction between main stems and strongly branched lateral stems evident in species such as P. forbesii has been considered to be one of the key steps towards the evolution of the leaves of euphyllophytes (modern members of which are the ferns and seed plants), based on the theory that such leaves evolved through 'webbing' of flattened lateral branching systems.
In 2004, Crane et al. published a simplified cladogram for the polysporangiophytes, based on a number of figures in Kenrick and Crane (1997). Part of their cladogram is reproduced below (with some branches collapsed into 'basal groups' to reduce the size of the diagram). It shows two of the better-known species of Psilophyton as early-diverging members of the euphyllophytes.
- Dawson, J.W. (1859), "On fossil plants from the Devonian rocks of Canada", Q. J. Geol. Soc. London 15: 477–488, doi:10.1144/gsl.jgs.1859.015.01-02.57, cited in Gerrienne 1995
- Hueber, F.M. & Banks, H.P. (1967), "Psilophyton princeps: the search for organic connection", Taxon 16 (81-85), JSTOR 1216887 , cited in Banks 1975
- Schweitzer, Hans-Joachim & Rebske, Christine (1988), Die basalen Organe von Psilophyton burnotense (Gilkinet) Kräusel & Weyland, Bonn: Paläobotanische Abteilung des Institutes für Paläontologie der Universität Bonn, OCLC 258188031
- Gensel, Patricia G. (1979), "Two Psilophyton species from the Lower Devonian of Eastern Canada with a discussion of morphological variation within the genus", Palaeontographica Abteilung B 168 (4-6): 81–99, cited in Edwards, D. (2003), "Xylem in early tracheophytes", Plant, Cell and Environment 26 (1): 57–72, doi:10.1046/j.1365-3040.2003.00878.x
- Trant, C.A. & Gensel, P.G. (1985), "Branching in Psilophyton : a new species from the Lower Devonian of New Brunswick, Canada", American Journal of Botany 72 (8): 1256–1273, doi:10.2307/2443406, cited in Gerrienne 1995
- Doran, J.B. (1980), "A new species of Psilophyton from the Lower Devonian of Northern New Brunswick, Canada", Canadian Journal of Botany 58: 2241– 2262, doi:10.1139/b80-259, cited in Gerrienne 1995
- Kasper, A.E.; Andrews, H.N. & Forbes, W.H. (1974), "New fertile species of Psilophyton from the Devonian of Maine", Am. J. Bot. 61: 339–359, doi:10.2307/2441802, cited in Banks 1980
- Banks, H.P.; Leclercq, S. & Hueber, F.M. (1975), "Anatomy and morphology of Psilophyton dawsonii, sp. n. from the Late Lower Devonian of Quebec (Gaspé) and Ontario, Canada", Palaeontogr. Am. 8: 75–127, cited in Banks 1980
- Andrews, H.N.; Kasper, A.E. & Mencher, E. (1968), "Psilophyton forbesii, a new Devonian plant from northern Maine", Bulletin of the Torrey Botanical Club 95: 1–11, cited in Gerrienne 1995
- Gerrienne, P. (1997), "The fossil plants from the Lower Devonian of Marchin (northern margin of Dinant Synclinorium, Belgium). V. Psilophyton genseliae sp. nov., with hypotheses on the origin of Trimerophytina", Review of Palaeobotany and Palynology 98 (3-4): 303–324, doi:10.1016/S0034-6667(97)00010-9
- Obrhel, J. (1959), "Neue Pflanzenfunde in den Srbsko-Schichten (Mitteldevon)", Vestn. Ustred. Ustavu Geol. (in German) 34: 384–388, cited in Gerrienne 1995
- Gerrienne, P. (1995), "Les fossiles végétaux du Dévonien inférieur de Marchin (bord nord du Synclinorium de Dinant, Belgique). III. Psilophyton parvulum nov. sp.", Geobios (in French) 28 (2): 131–144, doi:10.1016/S0016-6995(95)80220-7
- Hao, S.-G. & Gensel, P.G. (1998), "Some new plant finds from the Posongchong Formation of Yunnan, and consideration of a phytogeographic similarity between South China and Australia during the Early Devonian", Science China Earth Sciences 41 (1): 1–13, doi:10.1007/bf02932414
- Zdebska, D. (1986), "Psilophyton szaferi sp. nov. from the Lower Devonian of the Holy Cross Mountains, Poland", Acta Soc. Bot. Pol. 55: 315–324, doi:10.5586/asbp.1986.030, cited in Gerrienne 1995
- Banks, Harlan P. (1980), "The role of Psilophyton in the evolution of vascular plants", Review of Palaeobotany and Palynology 29: 165–176, doi:10.1016/0034-6667(80)90056-1
- Taylor, T.N.; Taylor, E.L. & Krings, M. (2009), Paleobotany, The Biology and Evolution of Fossil Plants (2nd ed.), Amsterdam; Boston: Academic Press, ISBN 978-0-12-373972-8, pp. 259–261
- Olmstead, R. (1998), "Review: How the Land Turned Green", Science 280 (5362): 393, Bibcode:1998Sci...280..393., doi:10.1126/science.280.5362.393, JSTOR 2895164
- Banks, H.P. (1975), "Reclassification of Psilophyta", Taxon 24: 401–413, doi:10.2307/1219491
- Crane, P.R.; Herendeen, P. & Friis, E.M. (2004), "Fossils and plant phylogeny", American Journal of Botany 91 (10): 1683–99, doi:10.3732/ajb.91.10.1683, PMID 21652317
- Banks, H.P. (1968), "The early history of land plants", in Drake, E.T., Evolution and Environment: A Symposium Presented on the Occasion of the 100th Anniversary of the Foundation of Peabody Museum of Natural History at Yale University, New Haven, Conn.: Yale University Press, pp. 73–107, cited in Banks 1975
- Beerling, D.J. & Fleming, A.J. (2007), "Zimmermann's telome theory of megaphyll leaf evolution: a molecular and cellular critique", Current Opinion in Plant Biology 10 (1): 4–12, doi:10.1016/j.pbi.2006.11.006, PMID 17141552