Cosmochlaina

Cosmochlaina
Cosmochlaina
Temporal range: Late Silurian to Early Devonian
Cuticle of Cosmochlaina, retrieved from the Burgsvik beds by acid maceration. Cells about 12 μm in diameter.
Scientific classification e
Kingdom: Plantae (?)
Phylum: Nematophyta
Class: Nematophytina
Order: Nematophytales
Family: Nematothalaceae
Strother 1993
Genus: Cosmochlaina
Edwards 1986
Species
  • C. verruculosus
(May be a typo, in Taylor 1988)
  • C. verrucosa (Type)
  • C. maculata
  • C. physema
  • C. Versiformis
(All defined by Edwards 1986)

Cosmochlaina (from Greek: kosmos=ornament; xlaina=wrapper/cloak) is a form genus of nematophyte – an early (Siluran – Devonian) plant known only from fossil cuticles,[1] often found in association with tubular structures.[2] Where Nematothallus is sometimes used to relate only to tube-like structures, Cosmochlaina refers to the cuticle fragments. The form genus was put forwards by Dianne Edwards, and is diagnosed by inwards-pointing flanges and randomly oriented pseudo-cellular units.[3] Projections on the outer surface are always present, and sometimes also appear on the inner surface; however, the surface of the cuticle itself is always smooth.[3] The holes in the cuticle are often covered by round flaps, loosely attached along a side.[3]

It has been suggested that the pores of Cosmochlaina represent broken-off rhizoids, on the basis that rotting and acid treatment of extant liverworts produces a similar perforated texture.[4] However, the status of this form genus in any one kingdom is not secure; members could, for example, represent arthropod cuticle.[5] Alternatively, different species may in fact represent different parts of the same organism.[3]

See also

References

  1. ^ Kenrick, P.; Crane, P.R. (1997). "The origin and early evolution of plants on land". Nature 389 (6646): 33–39. Bibcode 1997Natur.389...33K. doi:10.1038/37918. 
  2. ^ Gensel, P.G.; Johnson, N.G.; Strother, P.K. (1990). "Early Land Plant Debris (Hooker's" Waifs and Strays"?)". PALAIOS 5 (6): 520–547. doi:10.2307/3514860. JSTOR 3514860. 
  3. ^ a b c d Edwards, D. (1986). "Dispersed cuticles of putative non-vascular plants from the Lower Devonian of Britain". Botanical journal of the Linnean Society 93 (3): 259–275. doi:10.1111/j.1095-8339.1982.tb01025.x. 
  4. ^ Graham, L.E.; Wilcox, L.W.; Cook, M.E.; Gensel, P.G. (2004). "Resistant tissues of modern marchantioid liverworts resemble enigmatic Early Paleozoic microfossils". Proceedings of the National Academy of Sciences 101 (30): 11025–11029. Bibcode 2004PNAS..10111025G. doi:10.1073/pnas.0400484101. PMC 503736. PMID 15263095. http://www.pubmedcentral.nih.gov/articlerender.fcgi?tool=pmcentrez&artid=503736. 
  5. ^ Taylor, T.N. (1988). "The Origin of Land Plants: Some Answers, More Questions". Taxon 37 (4): 805–833. doi:10.2307/1222087. JSTOR 1222087. 

Wikimedia Foundation. 2010.

Игры ⚽ Поможем написать курсовую

Look at other dictionaries:

  • Нематофитовые водоросли — ? † Нематофитовые водоросли …   Википедия

  • Nematothallus — Temporal range: Ludfordian–Downtonian …   Wikipedia

  • Nematophyta — Temporal range: Cambrian–410[1] …   Wikipedia

  • Charophyta — Scientific classification Domain …   Wikipedia

  • Fossil wood — petrified softwood Fossil wood is wood that is preserved in the fossil record. Over time the wood will usually be the part of a plant that is best preserved (and most easily found). Fossil wood may or may not be petrified. The study of fossil… …   Wikipedia

  • Chaetocladus — Temporal range: Middle Ordovician Devonian[1] The holotype of Chaetocladus plumula (USNM 41 137, from LoDuca 1997) …   Wikipedia

  • Ornatifilum — Temporal range: Late Silurian (Wenlock) Early Devonian (Lochkovian)[1] An Ornatifilum like fossil, identical to those described by Sherwood Pike and Gray  …   Wikipedia

Share the article and excerpts

Direct link
Do a right-click on the link above
and select “Copy Link”