Sawdonia

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Sawdonia
Scientific classification Red Pencil Icon.png
Kingdom: Plantae
Clade: Tracheophytes
Clade: Lycophytes
Plesion: Zosterophylls
Genus: Sawdonia
Hueber (1971)
Species
  • Sawdonia ornata
  • Sawdonia acanthotheca

Sawdonia is an extinct genus of early vascular plants, known from the Upper Silurian to the Lower Carboniferous ( 430 to 320 million years ago). Sawdonia is best recognized by the large number of spikes (enations) covering the plant. These are vascular plants that do not have vascular systems in their enations. The first species of this genus (Sawdonia ornata) was described in 1859 by Sir J. William Dawson and, was originally attributed to the genus Psilophyton . He named this plant Psilophyton princeps. In 1971 Francis Hueber proposed a new genus for this species due to its "Divergent technical characters from the generic description for Psilophyton." [1] The holotype used for description is Dawson Collection Number 48, pro parte, Museum Specimen Number 3243. (See Dawson 1871, Plate IX, fig 101.) Sir J. William Dawson Collection, Peter Redpath Museum, McGill University, Montreal, Quebec, Canada. [1]

Contents

Morphology

These plants are described by Hueber as having monopodially branched stems, that are unridged, spinous and circinately tipped. The sporangia are described as round in abaxial view, and oval in lateral view. These sporangia are formed laterally and singular on short stalks. The sporangium split along convex margins into equal valves in a trilete fashion. The spines are tapered and pointed lower on the plant but form loose spikes at end of the plant. The xylem are just one solid strand. The epidermal cells have cuticular papillae. There are stomata located on the on stem but not on spine surfaces. [1]

Sawdonia is defined by Francis Hueber in his 1971 paper as follows:

  1. Having stems up to 5 mm in diameter without measuring the spikes
  2. Multi cellular spines measuring 0.5-1.8 mm at the base, reaching 0.5-3.9mm long, with a density range of 4 to 45 per cm of stem
  3. Sporangia: 3-3.5 mm in diameter, with stalks 0.5-0.75 mm long and 1-1.25 mm wide
  4. A present Vascular strand
  5. Spores: round to sub-triangular, 54-64 um, trilete simple structure
  6. An oval xylem strand when viewed in cross section .074x0.34 mm in diameter
  7. Trachieds that have a helical scalariform
  8. Stomata 39-72 um long, 17-34 um wide, with parallel elongation in regards to the axis of the stem, with a thickened outer wall of guard cells [1]
Sawdonia ornata Cosmocaixa.JPG
Sawdonia ornata.jpg
Sawdonia ornata fossils from Gaspé, Quebec

Taxonomy

Classification

There is agreement that Sawdonia was a zosterophyll – a group of plants on the line of evolution leading to the modern lycopodiopsids. In their 1997 cladistic study, Kenrick and Crane placed Sawdonia in the family Sawdoniaceae, order Sawdoniales. [2] An alternative view places the genus in the family Gosslingiaceae, order Gosslingiales. [3]

Species

Range

Sawdonia had an extremely broad range, with many specimens found in Canada (Battery Point Formation), [7] Venezuela (Campo Chico Formation), [8] England and Scotland (Strathmore Group). [9] There have even been a species that has been found across China, that might fall under the Sawdonia genus.

Related Research Articles

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The lycophytes, when broadly circumscribed, are a vascular plant (tracheophyte) subgroup of the kingdom Plantae. They are sometimes placed in a division Lycopodiophyta or Lycophyta or in a subdivision Lycopodiophytina. They are one of the oldest lineages of extant (living) vascular plants; the group contains extinct plants that have been dated from the Silurian. Lycophytes were some of the dominating plant species of the Carboniferous period, and included tree-like species, although extant lycophytes are relatively small plants.

<span class="mw-page-title-main">Zosterophyll</span> Group of extinct land plants that first appeared in the Silurian period

The zosterophylls are a group of extinct land plants that first appeared in the Silurian period. The taxon was first established by Banks in 1968 as the subdivision Zosterophyllophytina; they have since also been treated as the division Zosterophyllophyta or Zosterophyta and the class or plesion Zosterophyllopsida or Zosteropsida. They were among the first vascular plants in the fossil record, and had a world-wide distribution. They were probably stem-group lycophytes, forming a sister group to the ancestors of the living lycophytes. By the late Silurian a diverse assemblage of species existed, examples of which have been found fossilised in what is now Bathurst Island in Arctic Canada.

<i>Baragwanathia</i> Extinct genus of spore-bearing plants

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<i>Drepanophycus</i> Extinct genus of spore-bearing plants

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<i>Asteroxylon</i> Extinct genus of spore-bearing plants

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<span class="mw-page-title-main">Drepanophycales</span> Extinct order of spore-bearing plants

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<i>Psilophyton</i> Genus of fossil plants

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. 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 and is thought to be part of the group from within which the modern ferns and seed plants evolved.

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<span class="mw-page-title-main">Sawdoniales</span> Extinct order of spore-bearing plants

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Renalia is a genus of extinct vascular plants from the Early Devonian. It was first described in 1976 from compressed fossils in the Battery Point Formation. It is difficult to reconstruct the original form of the complete plant, but it appears to have consisted of leafless branching stems whose side branches had sporangia at their tips. It is regarded as an early relative of the lycophytes.

<i>Adoketophyton</i> Extinct genus of spore-bearing plants

Adoketophyton is a genus of extinct vascular plants of the Early Devonian. The plant was first described in 1977 based on fossil specimens from the Posongchong Formation, Wenshan district, Yunnan, China. These were originally named Zosterophyllum subverticillatum; later the species was transferred to a new genus as Adoketophyton subverticillatum. One cladistic analysis suggested that it is a lycophyte, related to the zosterophylls. Other researchers regard its placement within the vascular plants as uncertain.

Discalis is a genus of extinct vascular plants of the Early Devonian. The name is derived from the Greek δίσκος, referring to the disc-shaped sporangia. The genus was first described by Hao in 1989 based on fossil specimens from the Posongchong Formation, Wenshan district, Yunnan, China.

Distichophytum is a genus of extinct vascular plants of the Late Silurian (Ludfordian) to Early Devonian (Emsian), around 426 to 393 million years ago. The genus has a tangled taxonomic history, also being known as Bucheria and Rebuchia.

<i>Nothia <span style="font-style:normal;">(plant)</span></i> Extinct genus of spore-bearing plants

Nothia was a genus of Early Devonian vascular plants whose fossils were found in the Rhynie chert in Scotland. It had branching horizontal underground stems (rhizomes) and leafless aerial stems (axes) bearing lateral and terminal spore-forming organs (sporangia). Its aerial stems were covered with small 'bumps' (emergences), each bearing a stoma. It is one of the best described early land plants. Its classification remains uncertain, although it has been treated as a zosterophyll. There is one species, N. aphylla.

<i>Ventarura</i> Extinct genus of spore-bearing plants

Ventarura is a genus of extinct vascular plants of the Early Devonian. Fossils were found in the Windyfield chert, Rhynie, Scotland. Some features, such as bivalved sporangia borne laterally and the anatomy of the xylem, relate this genus to the zosterophylls. Other features are unclear due to poor preservation.

Trichopherophyton is a genus of extinct vascular plants of the Early Devonian. Fossils were found in the Rhynie chert, Scotland. The remains are very fragmentary, but the plant appears to be related to the zosterophylls.

Demersatheca is a genus of extinct vascular plants of the Early Devonian. Fossils were first found in the Posongchong Formation of eastern Yunnan, China. The plant had smooth leafless stems at least 1 mm in diameter, but only regions which bore spore-forming organs or sporangia are well-known. Sporangia were borne in 'spikes' or strobili, at least 40 mm long; one had 32 sporangia. Sporangia were arranged in four rows, two sporangia being opposite to one another on the stem with the next two being at right angles. Each sporangium consisted of two 'valves' which opened at the top to release their spores. A particular feature of Demersatheca which distinguishes it from other zosterophylls is that the stalk-less sporangia were sunken into the stem of the spike, so that the outer valve was flush with the surface.

References

  1. 1 2 3 4 Hueber, Francis M (1971). "Sawdonia Ornata: A New Name for Psilophyton princeps var. Ornatum". Taxon. 20 (4): 641–2. doi:10.2307/1218284. JSTOR   1218284.
  2. Kenrick, Paul, and Peter R. Crane. The Origin and Early Diversification of Land Plants: a Cladistic Study. Smithsonian Inst. Press, 1997.[ page needed ]
  3. Hao, Shougang & Xue, Jinzhuang (2013), The early Devonian Posongchong flora of Yunnan: a contribution to an understanding of the evolution and early diversification of vascular plants, Beijing: Science Press, Table 4.3, p. 53, ISBN   978-7-03-036616-0
  4. Gensel, Patricia G; Berry, Christopher M (2016). "Sporangial Morphology of the Early Devonian Zosterophyll Sawdonia ornata from the Type Locality (Gaspé)" (PDF). International Journal of Plant Sciences. 177 (7): 618–32. doi:10.1086/687301. S2CID   51541053.
  5. Gensel, Patricia G; Andrews, Henry N; Forbes, William H (1975). "A New Species of Sawdonia with Notes on the Origin of Microphylls and Lateral Sporangia". Botanical Gazette. 136 (1): 50–62. doi:10.1086/336782. S2CID   84204867.
  6. Xu, Hong-He (2011). "Re-examination of specimens attributed to Sawdonia curstipa Wang and Hao (zosterophyll) from the Middle Devonian of Xinjiang, China". Palaeoworld. 20 (4): 357–61. doi:10.1016/j.palwor.2011.06.003.
  7. Gensel, Patricia G.; Berry, Christopher M. (2016-09-01). "Sporangial Morphology of the Early Devonian Zosterophyll Sawdonia ornata from the Type Locality (Gaspé)". International Journal of Plant Sciences. 177 (7): 618–632. doi:10.1086/687301. ISSN   1058-5893. S2CID   51541053.
  8. Berry, Christopher M.; Gensel, Patricia G. (2019-07-01). "Late Mid Devonian Sawdonia (Zosterophyllopsida) from Venezuela". International Journal of Plant Sciences. 180 (6): 540–557. doi:10.1086/702940. ISSN   1058-5893. S2CID   155145366.
  9. Rayner, R. J. (1983). "New observations on Sawdonia ornata from Scotland". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 74 (2): 79–93. doi:10.1017/S026359330001018X. ISSN   1473-7116. S2CID   130271616.