Aaglacrinus
Temporal range: Carboniferous[1]
Scientific classification
Kingdom:
Phylum:
Class:
Order:
Family:
Dendrocrinidae
Genus:
Aaglacrinus

G. D. Webster, 1981[2][3]
Species

See text

Synonyms

Aaglaocrinus[2][3]

Aaglacrinus is an extinct genus of crinoidea in the Cladia order.[4][5][6][7][8] It has been proposed that it was a stationary (attached) suspension feeder the hard parts of which were composed of magnesium calcite.[4][9]

Species

There are currently two species in this genus, both of which are under the name Aaglaocrinus:

  • Aaglaocrinus bowsheri (Webster & Kues, 2006)[10][11]
  • Aaglaocrinus sphaeri (Strimple 1949)[12][13][14]

References

  1. peters, shanan. "Sepkoski Online Results". strata.geology.wisc.edu. Retrieved 20 July 2018.
  2. 1 2 "Archived copy". Archived from the original on 2011-06-13. Retrieved 2010-03-24.{{cite web}}: CS1 maint: archived copy as title (link)
  3. 1 2 Analytics, Clarivate. "ION: Index to Organism Names". www.organismnames.com. Retrieved 20 July 2018.
  4. 1 2 "The Paleobiology Database". Archived from the original on 2010-03-06. Retrieved 2010-03-03.
  5. "Opinions from J. J. Sepkoski 2002". paleodb.org. Retrieved 2022-09-29.
  6. "The Paleobiology Database". Archived from the original on 2007-10-30. Retrieved 2010-03-24.
  7. New crinoids from the Naco Formation (middle Pennsylvanian) of Arizona and a revision of the family Cromyocrinidae. Journal of Paleontology, 55(6) 1981: 1176-1199. [Zoological Record Volume 118]
  8. "Namebank Record Detail". www.ubio.org. Retrieved 20 July 2018.
  9. Reference no: 9940
  10. Pennsylvanian crinoids of New Mexico. New Mexico Geology, 28(1), February 2006: 3-37. [Zoological Record Volume 143]
  11. Analytics, Clarivate. "ION: Index to Organism Names". www.organismnames.com. Retrieved 20 July 2018.
  12. "Namebank Record Detail". www.ubio.org. Retrieved 20 July 2018.
  13. "Namebank Record Detail". www.ubio.org. Retrieved 20 July 2018.
  14. "ION: Index to Organism Names". www.organismnames.com. Archived from the original on 20 July 2018. Retrieved 22 May 2022.


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