Jump to content
 







Main menu
   


Navigation  



Main page
Contents
Current events
Random article
About Wikipedia
Contact us
Donate
 




Contribute  



Help
Learn to edit
Community portal
Recent changes
Upload file
 








Search  

































Create account

Log in
 









Create account
 Log in
 




Pages for logged out editors learn more  



Contributions
Talk
 



















Contents

   



(Top)
 


1 Anatomy  





2 Taxonomy  





3 List of genera  





4 References  





5 External links  





6 Taxonomy  





7 Gallery  














Edrioasteroidea






Azərbaycanca
Català
Čeština
Deutsch
Español
Français
Italiano

Português
Русский
Svenska

 

Edit links
 









Article
Talk
 

















Read
Edit
View history
 








Tools
   


Actions  



Read
Edit
View history
 




General  



What links here
Related changes
Upload file
Special pages
Permanent link
Page information
Cite this page
Get shortened URL
Download QR code
Wikidata item
 




Print/export  



Download as PDF
Printable version
 




In other projects  



Wikimedia Commons
Wikispecies
 
















Appearance
   

 






From Wikipedia, the free encyclopedia
 

(Redirected from Edrioasteroid)

Edrioasteroids
Temporal range: Middle Cambrian–Early Permian

O

S

D

C

P

T

J

K

Pg

N


Possible Ediacaran occurrence
Streptaster vorticellatus (13 mm across) from the Upper Ordovician of Kentucky, USA
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Echinodermata
Subphylum: Crinozoa
Class: Edrioasteroidea
Billings 1858
Genera

See text

Edrioasteroidea is an extinct classofechinoderms. The living animal would have resembled a pentamerously symmetrical disc or cushion. They were obligate encrusters and attached themselves to inorganic or biologic hard substrates (frequently hardgroundsorbrachiopods).[1] A 507 million years old species, Totiglobus spencensis, is actually the first known echinoderm adapted to live on a hard surface after the soft microbial mats that covered the seafloor were destroyed in the Cambrian substrate revolution.[2]

The oldest undisputed fossils of Edrioasteroidea are known from Cambrian (Stage 3, about 515-520 Ma ago) of Laurentia and are among the oldest known fossils of echinoderms. Some authors propose that an enigmatic Ediacaran (about 600 Ma) organism Arkarua is also an edrioasteroid, but this interpretation did not gain wide acceptance.[3] Last edrioasteroids are known from Permian (Late Kungurian, about 270-280 Ma).[4]

Anatomy[edit]

The body plan for this class was simple: a main body (theca), composed of many small plates, with a peripheral rim for attachment, and (in some species) a pedunculate zone for extension and retraction. Circling and sometimes attached to the body was a peripheral rim of plates. The main feature consisted of five arms, or ambulacra, in the body wall radiating outwards from the central mouth. The ambulacra grew either curved or straight. When curved, they may all turn in the same direction or else one or two on the right side will curve opposite the others. The ambulacra are built of underlying floor plates that form the food groove and protective cover plates that roof the food groove. The anus was under the mouth region and was made of small triangular plates to form a cone-shaped area. The bottom surface of the theca is unplated.

Edrioasteroid species are distinguished by differences in the ambulacral curvature, the relationships of the cover plates, and ornamentation. The mode of life was sessile; they were often attached via a stalk made of small plates to a hard object such as a carbonate hardground or shell. Several examples of epibiotic attachment have also been noted.

In the discocystinids, the area between the body and peripheral rim could be extended and retracted; in so doing the two were separated. The peripheral rim became the base of the stalk which was attached to a surface. Underneath the body was a recumbent zone, which was about 12 millimetres (0.47 in) wide in the genus Giganticlavus, followed by the pedunculate zone attached to the peripheral rim of 12 millimetres (0.47 in).[5]

Taxonomy[edit]

List of genera[edit]

A very incomplete list of some genera.

References[edit]

  • ^ Zamora S.; Lefebvre B.; Álvaro J. J.; et al. (2013). "Chapter 13. Cambrian echinoderm diversity and palaeobiogeography". Geological Society, London, Memoirs. 38: 157–171. doi:10.1144/M38.13.
  • ^ Sumrall C. D. (2009). "First Definite Record of Permian Edrioasteroids: Neoisorophusella maslennikovi n. sp. from the Kungurian of Northeast Russia". Journal of Paleontology. 83 (6): 990–993. doi:10.1666/09-063.1.
  • ^ Sumrall 1996
  • External links[edit]

    All accessed on March 8, 2008.

    Taxonomy[edit]

    Gallery[edit]


    Retrieved from "https://en.wikipedia.org/w/index.php?title=Edrioasteroidea&oldid=1225150370"

    Categories: 
    Edrioasteroidea
    Cambrian first appearances
    Permian extinctions
    Hidden categories: 
    Articles with short description
    Short description is different from Wikidata
    Articles with 'species' microformats
    Webarchive template wayback links
    Commons category link from Wikidata
     



    This page was last edited on 22 May 2024, at 17:35 (UTC).

    Text is available under the Creative Commons Attribution-ShareAlike License 4.0; additional terms may apply. By using this site, you agree to the Terms of Use and Privacy Policy. Wikipedia® is a registered trademark of the Wikimedia Foundation, Inc., a non-profit organization.



    Privacy policy

    About Wikipedia

    Disclaimers

    Contact Wikipedia

    Code of Conduct

    Developers

    Statistics

    Cookie statement

    Mobile view



    Wikimedia Foundation
    Powered by MediaWiki