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Polysporangiophyte

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34-417: Polysporangiophytes , also called polysporangiates or formally Polysporangiophyta , are plants in which the spore-bearing generation ( sporophyte ) has branching stems (axes) that bear sporangia . The name literally means 'many sporangia plant'. The clade includes all land plants ( embryophytes ) except for the bryophytes (liverworts, mosses and hornworts) whose sporophytes are normally unbranched, even if

68-563: A Canadian geologist and paleobotanist, was the first to discover and describe a megafossil of a polysporangiophyte. In 1859 he published a reconstruction of a Devonian plant, collected as a fossil from the Gaspé region of Canada, which he named Psilophyton princeps . The reconstruction shows horizontal and upright stem-like structures; no leaves or roots are present. The upright stems or axes branch dichotomously and have pairs of spore-forming organs ( sporangia ) attached to them. Cross-sections of

102-568: A few exceptional cases occur. While the definition is independent of the presence of vascular tissue , all living polysporangiophytes also have vascular tissue, i.e., are vascular plants or tracheophytes. Extinct polysporangiophytes are known that have no vascular tissue and so are not tracheophytes. Paleobotanists distinguish between micro- and megafossils. Microfossils are primarily spores , either single or in groups. Megafossils are preserved parts of plants large enough to show structure, such as stem cross-sections or branching patterns. Dawson ,

136-558: A monophyletic clade, but some genera previously included in the group fell outside this clade (e.g., Hicklingia , Nothia ). The trimerophytes were paraphyletic stem groups to both the crown group ferns and the crown group seed plants . Many researchers have urged caution in the classification of early polysporangiophytes. Taylor et al. note that basal groups of early land plants are inherently difficult to characterize since they share many characters with all later-evolving groups (i.e., have multiple plesiomorphies ). In discussing

170-489: A much simpler fashion than those of true vascular plants, the eutracheophytes. If the cladogram above is correct it has implications for the evolution of land plants. The earliest diverging polysporangiophytes in the cladogram are the Horneophytopsida , a clade at the 'protracheophyte' grade that is sister to all other polysporangiophytes. They had essentially an isomorphic alternation of generations (meaning that

204-528: A natural group named stomatophytes . The evolutionary history of plants is far from settled. Sporophyte Too Many Requests If you report this error to the Wikimedia System Administrators, please include the details below. Request from 172.68.168.226 via cp1108 cp1108, Varnish XID 248396794 Upstream caches: cp1108 int Error: 429, Too Many Requests at Thu, 28 Nov 2024 11:00:15 GMT Whisk fern Psilotum

238-575: A polysporangiophyte, have been dated to the succeeding Wenlock epoch ( 433 to 427 million years ago ). The concept of the polysporangiophytes, more formally called Polysporangiophyta, was first published in 1997 by Kenrick and Crane. (The taxobox at the right represents their view of the classification of the polysporangiophytes.) The defining feature of the clade is that the sporophyte branches and bears multiple sporangia. This distinguishes polysporangiophytes from liverworts , mosses and hornworts , which have unbranched sporophytes each with

272-431: A rhyniophyte. Boyce has shown that the sporophytes of some Cooksonia species and allies ('cooksonioids') had stems that were too narrow to have supported sufficient photosynthetic activity for them to be independent of their gametophytes – inconsistent with their position in the cladogram. Because the stomata in mosses , hornworts and polysporangiophytes are viewed as homologous, it has been suggested they belong in

306-433: A simple vascular cylinder, homosporous and terminal eusporangia and a lack of roots. Unfortunately, no fossils of psilophytes are known to exist. A careful study of the morphology and anatomy suggests that whisk ferns are not closely related to rhyniophytes, and that the ancestral features present in living psilophytes represent a reduction from a more typical modern fern plant. Significant differences between Psilotum and

340-477: A simplified cladogram for the polysporangiophytes (which they call polysporangiates), based on a number of figures in Kenrick and Crane (1997). Their cladogram is reproduced below (with some branches collapsed into 'basal groups' to reduce the size of the diagram). Their analysis is not accepted by other researchers; for example Rothwell and Nixon say that the broadly defined fern group (moniliforms or monilophytes)

374-508: A single sporangium. Polysporangiophytes may or may not have vascular tissue – those that do are vascular plants or tracheophytes. Prior to that, most of the early polysporangiophytes had been placed in a single order , Psilophytales, in the class Psilophyta, established in 1917 by Kidston and Lang. The living Psilotaceae , the whisk-ferns, were sometimes added to the class, which was then usually called Psilopsida. As additional fossils were discovered and described, it became apparent that

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408-467: A slightly different characterization of the early diverging polysporangiophytes: †'Protracheophytes' †Paratracheophytes Eutracheophytes The paraphyletic protracheophytes, such as Aglaophyton , have water-conducting vessels like those of mosses, i.e., without cells containing thickened cell walls. The paratracheophytes, a name intended to replace Rhyniaceae or Rhyniopsida, have 'S-type' water-conducting cells, i.e., cells whose walls are thickened but in

442-502: A thick lignified wall at maturity that provides mechanical strength. Unlike plants at the bryophyte grade, their sporophytes were branched. According to the cladogram, the genus Rhynia illustrates two steps in the evolution of modern vascular plants. Plants have vascular tissue, albeit significantly simpler than modern vascular plants. Their gametophytes are distinctly smaller than their sporophytes (but have vascular tissue, unlike almost all modern vascular plants). The remainder of

476-423: Is a genus of fern -like vascular plants . It is one of two genera in the family Psilotaceae commonly known as whisk ferns , the other being Tmesipteris . Plants in these two genera were once thought to be descended from the earliest surviving vascular plants , but more recent phylogenies place them as basal ferns, as a sister group to Ophioglossales . They lack true roots and leaves are very reduced,

510-649: Is consistent with Kenrick and Crane's cladistic analysis and subsequent research, though Cantino et al. have published a Phylocode classification. Banks' three groups continue to be used for convenience. A major cladistic study of land plants was published in 1997 by Kenrick and Crane; this both established the concept of the polysporangiophytes and presented a view of their phylogeny . Since 1997 there have been continual advances in understanding plant evolution, using RNA and DNA genome sequences and chemical analyses of fossils (e.g., Taylor et al. 2006), resulting in revisions to this phylogeny. In 2004, Crane et al. published

544-1269: Is not monophyletic. †  Horneophytopsida  ( Caia , Horneophyton , Tortilicaulis ) †  Aglaophyton †  Rhyniaceae  ( Huvenia , Rhynia , Stockmansella ) † basal groups ( Aberlemnia caledonica [= Cooksonia caledonica ], Cooksonia pertoni ) Cooksonia  cambrensis, Renalia , Sartilmania , Uskiella , Yunia †  Hicklingia Adoketophyton , Discalis , Distichophytum (= Rebuchia ), Gumuia , Huia , Zosterophyllum  myretonianum , Z. llanoveranum, Z. fertile Zosterophyllum divaricatum , Tarella , Oricilla , Gosslingia , Hsua , Thrinkophyton , Protobarinophyton , Barinophyton  obscurum , B. citrulliforme , Sawdonia , Deheubarthia , Konioria , Anisophyton , Serrulacaulis , Crenaticaulis Nothia , Zosterophyllum  deciduum extant and extinct members †  Eophyllophyton † basal groups ( Psilophyton  crenulatum, Ps. dawsonii ) moniliforms (ferns; extant and extinct members) † basal groups ( Pertica , Tetraxylopteris ) spermatophytes (seed plants; extant and extinct members) More recently, Gerrienne and Gonez have suggested

578-582: Is unusual in that it branches dichotomously, lives underground and possesses vascular tissue. The nutrition of the gametophyte appears to be myco-heterotrophic , assisted by endophytic fungi . The genus Psilotum was first formally described in 1801 by Olof Swartz and the description was published in Journal für die Botanik (Schrader) . The name of the genus is from the Ancient Greek word psilos meaning "bare", "smooth" or "bald" referring to

612-778: The Rhynie chert – a fine-grained sedimentary rock found near the village of Rhynie, Aberdeenshire , now dated to the Pragian of the Lower Devonian (around 411 to 408 million years ago ). The fossils were better-preserved than Dawson's, and showed clearly that these early land plants did indeed consist of generally naked vertical stems arising from similar horizontal structures. The vertical stems were dichotomously branched with some branches ending in sporangia. Since these discoveries, similar megafossils have been discovered in rocks of Silurian to mid-Devonian age throughout

646-746: The 'protracheophytes' diverging earlier than the lycophytes; however, lycophytes were present in the Ludfordian stage of the Silurian around 430 to 420 million years ago , long before the 'protracheophytes' found in the Rhynie chert , dated to the Pragian stage of the Devonian around 410  million years ago . However, it has been suggested that the poorly preserved Eohostimella , found in deposits of Early Silurian age (Llandovery, around 440 to 430 million years ago ), may be

680-963: The Psilophyta were not a homogeneous group of plants. In 1975, Banks expanded on his earlier 1968 proposal that split it into three groups at the rank of subdivision. These groups have since been treated at the ranks of division, class and order. A variety of names have been used, which the table below summarizes. For Banks, rhyniophytes comprised simple leafless plants with terminal sporangia (e.g., Cooksonia , Rhynia ) with centrarch xylem ; zosterophylls comprised plants with lateral sporangia that split distally (away from their attachment) to release their spores, and had exarch strands of xylem (e.g., Gosslingia ). Trimerophytes comprised plants with large clusters of downwards curving terminal sporangia that split along their length to release their spores and had centrarch xylem strands (e.g., Psilophyton ). Research by Kenrick and Crane that established

714-461: The U.S., P. nudum is found from Florida to Texas, and P. complanatum in Hawaii. Psilotum superficially resembles certain extinct early vascular plants, such as the rhyniophytes and the trimerophyte genus Psilophyton . The unusual features of Psilotum that suggest an affinity with early vascular plants include dichotomously branching sporophytes, aerial stems arising from horizontal rhizomes,

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748-603: The cladogram derived from Kenrick and Crane's studies and its implications for the evolution of land plants have been questioned by others. A 2008 review by Gensel notes that recently discovered fossil spores suggest that tracheophytes were present earlier than previously thought; perhaps earlier than supposed stem group members. Spore diversity suggests that there were many plant groups, of which no other remains are known. Some early plants may have had heteromorphic alternation of generations, with later acquisition of isomorphic gametophytes in certain lineages. The cladogram above shows

782-540: The classification of the trimerophytes, Berry and Fairon-Demaret say that reaching a meaningful classification requires "a breakthrough in knowledge and understanding rather than simply a reinterpretation of the existing data and the surrounding mythology". Kenrick and Crane's cladograms have been questioned – see the Evolution section below. As of February 2011, there appears to be no complete Linnean (i.e., rank-based) classification for early polysporangiophytes that

816-514: The fusion of three sporangia and which produce the spores . When mature, the synangia release yellow to whitish spores which develop into a gametophyte less than 2 mm (0.08 in) long. The gametophyte lives underground as a mycoheterotroph, tapping into mycorrhizal networks to access carbon and other nutrients. When the gametophyte is mature, it is monoicous , producing both egg and sperm cells. The sperm cells swim using several flagella and when they reach an egg cell, unite with it to form

850-731: The lack of the usual plant organs, and the seeming lack of leaves. There are two species, Psilotum nudum and Psilotum complanatum , with a hybrid between them known, Psilotum × intermedium W. H. Wagner . The distribution of Psilotum is tropical and subtropical, in the New World , Asia , and the Pacific , with a few isolated populations in south-west Europe. The highest latitudes known are in South Carolina , Cádiz province in Spain , and southern Japan for P. nudum . In

884-405: The leaves effectively grow from the base). The euphyllophytes are by far the largest group of vascular plants, in terms of both individuals and species. Euphyllophytes have large 'true' leaves (megaphylls), which develop through marginal or apical meristems (i.e., the leaves effectively grow from the sides or the apex). ( Horsetails have secondarily reduced megaphylls resembling microphylls.) Both

918-467: The polysporangiophytes concluded that none of Banks' three groups were monophyletic . The rhyniophytes included "protracheophytes", which were precursors to vascular plants (e.g., Horneophyton , Aglaophyton ); basal tracheophytes (e.g., Stockmansella , Rhynia gwynne-vaughanii ); and plants allied to the lineages that led to the living club-mosses and allies as well as ferns and seed plants (e.g., Cooksonia species). The zosterophylls did contain

952-414: The polysporangiophytes divide into two lineages, a deep phylogenetic split that occurred in the early to mid Devonian, around 400 million years ago. Both lineages have developed leaves, but of different kinds. The lycophytes, which make up less than 1% of the species of living vascular plants, have small leaves ( microphylls or more specifically lycophylls), which develop from an intercalary meristem (i.e.,

986-468: The rhyniophytes and trimerophytes are that the development of its vascular strand is exarch , while it is centrarch in rhyniophytes and trimerophytes. The sporangia of Psilotum are trilocular synangia resulting from the fusion of three adjacent sporangia, and these are borne laterally on the axes. In the rhyniophytes and trimerophytes the sporangia were single and in a terminal position on branches. Molecular evidence strongly confirms that Psilotum

1020-420: The sporophytes and gametophytes were equally free living), which might suggest that both the gametophyte-dominant life style of bryophytes and the sporophyte-dominant life style of vascular plants evolved from this isomorphic condition. They were leafless and did not have true vascular tissues. In particular, they did not have tracheids : elongated cells that help transport water and mineral salts, and that develop

1054-645: The stems being the organs containing photosynthetic and conducting tissue. There are only two species in Psilotum and a hybrid between the two. They differ from those in Tmesipteris in having stems with many branches and a synangium with three lobes rather than two. Whisk ferns in the genus Psilotum lack true roots but are anchored by creeping rhizomes . The stems have many branches with paired enations , which look like small leaves but have no vascular tissue . Above these enations there are synangia formed by

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1088-404: The upright axes showed that vascular tissue was present. He later described other specimens. Dawson's discoveries initially had little scientific impact; Taylor et al. speculate that this was because his reconstruction looked very unusual and the fossil was older than was expected. From 1917 onwards, Robert Kidston and William H. Lang published a series of papers describing fossil plants from

1122-568: The world, including Arctic Canada, the eastern US, Wales, the Rhineland of Germany, Kazakhstan, Xinjiang and Yunnan in China, and Australia. As of 2019, Eohostimella , dated to the Llandovery epoch ( 444 to 433 million years ago ), is one of the earliest fossils that has been identified as a polysporangiophyte. Fossils assigned to the genus Cooksonia , which is more certainly

1156-403: The young sporophyte . A mature sporophyte may grow to a height of 30 cm (10 in) or more but has no apparent leaves. The stem has a core of thick-walled protostele in its centre surrounded by an endodermis which regulates the flow of water and nutrients. The surface of the stem is covered with stomata which allow gas exchange with the surroundings. The gametophyte of Psilotum

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