Ozarkodina is an extinct genus of conodonts in the family Spathognathodontidae.

Ozarkodina
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Conodonta
Order: Ozarkodinida
Family: Spathognathodontidae
Genus: Ozarkodina
Branson and Mehl 1933[1]
Species
  • Ozarkodina anika
  • Ozarkodina confluens
  • Ozarkodina derenjalensis
  • Ozarkodina eberleini
  • Ozarkodina hassi
  • Ozarkodina maroccanica
  • Ozarkodina snajdri
  • Ozarkodina soegina
  • Ozarkodina typica

Use in stratigraphy

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Ozarkodina snajdri forms a subdivision of the Pseudomonoclimacis latilobus graptolite zone in the Burgsvik beds Silurian formation in Sweden.[2] An Ozarkodina snajdri crispa zone has also been identified in the Wills Creek in Virginia.[3]

Ozarkodina derenjalensis is found in the Silurian of the Niur Formation in Iran.[4]

The Kellwasser event in the Devonian which saw the extinction of all Ozarkodina species is reported in the list of Global Boundary Stratotype Sections and Points.

References

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  1. ^ A study of Hinde's types of conodonts preserved in the British Museum. EB Branson and MG Mehl, University of Missouri Studies, 1933, 8:133–156, pages 165–167
  2. ^ Conodont-based revisions of the Late Ludfordian on Gotland, Sweden. Jeppsson L., GFF, December 2005, volume 127, issue 4, pages 273–282, doi:10.1080/11035890501274273 Retrieved 2007-08-10.
  3. ^ Harris, A.G., Stamm, N.R., Weary, D.J., Repetski, J.E., Stamm, R.G., and Parker, R.A., 1994, Conodont color alteration index (CAI) map and conodont-based age determinations for the Winchester 30' x 60' quadrangle and adjacent area, Virginia, West Virginia, and Maryland: U.S. Geological Survey Miscellaneous Field Studies Map, MF-2239, 40 p., 1 sheet, scale 1:100,000 [1]
  4. ^ A new early Silurian prioniodontid conodont with three P elements from Iran and associated species. Peep Männik, C. Giles Miller and Vachik Hairapetian, Acta Palaeontologica Polonica, 2015, volume 60, issue 3, pages 733–746, doi:10.4202/app.00003.2013
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