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Donovaniconus oklahomensis

Cephalopoda - Donovaniconida - Donovaniconidae

Taxonomy
Donovaniconus oklahomensis was named by Doguzhaeva et al. (2002). It is not a trace fossil. Its type locality is Deep Fork River bridge, Okmulgee [Wewoka Shale], which is in a Desmoinesian marine shale in the Wewoka Shale Formation of Oklahoma. It is the type species of Donovaniconus.

Synonymy list
YearName and author
2002Donovaniconus oklahomensis Doguzhaeva et al.
2003Donovaniconus oklahomensis Doguzhaeva et al. p. 72

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RankNameAuthor
kingdomAnimalia()
—Bilateria
—EubilateriaAx 1987
—Protostomia
—Spiralia
superphylumLophotrochozoa
phylumMollusca
RankNameAuthor
classCephalopodaCuvier 1797
subclassColeoideaBather 1888
superorderBelemnoidaGray 1849
orderDonovaniconidaDoguzhaeva et al. 2002
familyDonovaniconidaeDoguzhaeva et al. 2002
genusDonovaniconusDoguzhaeva et al 2002
speciesoklahomensisDoguzhaeva et al. 2002

If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.

†Donovaniconus oklahomensis Doguzhaeva et al. 2002
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Diagnosis
No diagnoses are available
Measurements
No measurements are available
Composition: aragonitec
Environment: marinec
Locomotion: fast-movingc
Life habit: nektonicc
Diet: carnivorec
Vision: well-developedc
Created: 2004-02-28 11:51:48
Modified: 2023-08-18 17:28:37
Source: c = class
Reference: Kiessling 2004

Age range: Desmoinesian or 312.80000 to 306.00000 Ma

Collections: one only


Time interval Ma Country or state Original ID and collection number
Desmoinesian312.8 - 306.0USA (Oklahoma) Donovaniconus oklahomensis (type locality: 84451)