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]
^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
^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.
^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]
^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