Polygnathus

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Polygnathus
Conodonts.jpg
10–11. Polygnathus sp.
detail
10–14. Conodonts from the basal 20 cm of the Loyalhanna Limestone Member of the Mauch Chunk Formation, Keystone quarry, Pa. (93RS–79a), and Westernport, Md. (93RS–67). Note the highly abraded and reworked aeolian forms.
10. Polygnathus sp., Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, 93RS–79a, X140.
11. Polygnathus sp., Pa element, upper view, reworked Late Devonian to Early Mississippian morphotype, 93RS–67, X140.
Scientific classification OOjs UI icon edit-ltr.svg
Domain: Eukaryota
Kingdom: Animalia
Phylum: Chordata
Class: Conodonta
Order: Ozarkodinida
Family: Polygnathidae
Genus: Polygnathus
Hinde 1879
Species and subspecies

See text

Polygnathus is an extinct genus of conodonts.

Species

Use in stratigraphy

The Tournaisian, the oldest age of the Mississippian (also known as Lower Carboniferous), contains eight conodont biozones, one of which is defined by a Polygnathus species:

Contents

See also

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References

  1. Lower Devonian Subspecies of the Conodont Polygnathus linguiformis Hinde from Southeastern Australia. G. M. Philip and J. H. Jackson, Journal of Paleontology, Vol. 41, No. 5 (Sep., 1967), pages 1262-1266 (Stable URL retrieved 1 May 2016)