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† Wilkingia maxvillensis (Allorisma maxvillensis)

Wilkingia maxvillensis

Additional Functions

Grouping

Belong­ing to

Gaeabionta  ⇒ Domäne: Eukaryota  ⇒ Reich: Animalia  ⇒ Mittelreich: Eumetazoa  ⇒ Klade: Triploblastica  ⇒ Klade: Eutriploblastica  ⇒ Klade: Neotriploblastica  ⇒ Klade: Eucoelomata  ⇒ Superstamm: Eutrochozoa  ⇒ Stamm: Mollusca  ⇒ Klasse: Bivalvia  ⇒ Unterklasse: Heterodonta  ⇒ ohne Rang: Cardioni  ⇒ ohne Rang: Cardiidia  ⇒ Überfamilie: Grammysioidea  ⇒ Familie: Sanguinolitidae  ⇒ Unterfamilie: Undulomyinae  ⇒ Gattung: Wilkingia

Taxo­nomic seg­ment

Art

This mentioned taxonomy is an attempt to make an conclusive assignment from the different classifications of various scientists. Because the taxonomy may change due to the latest investigative methods and other findings, our map is a guide only.

Name from

Corre­spond­ing author (Name, Year)

Whitfield, 1882

Other languages

scientific

Wilkingia maxvillensis

Recombined

scientific

Allorisma maxvillensis

Whitfield, 1882
Ref.: R. P. Whitfield. 1882. Descriptions of new species of fossils from Ohio, with remarks on some of the geological formations in which they occur. Annals of the New York Academy of Sciences 2:193-244

Lebenszeitraum in Million Jahren (Ma)

Start age: 326.4 Ma - End age: 326.4 Ma
Phanerozoic
(Phanerozoikum)
Paleozoic
(Paläozoikum)
Carboniferous
(Karbon)
Mississippian
(Mississippium)
Serpukhovian
(Serpukhovium)
Visean
(Vise)
318.1
326.4
326.4
345.3

Additional data by PBDB, License: CC BY

Motility: facultatively mobile
Habit: deep infaunal
Diet:

suspension feeder

Compositon of the remains:

Aragonite

Reference- and Source indication, Literature

On the same taxonomic level (siblings) (Count: 22)

Taxonomic assignment (0)

References by PBDB, License: CC BY

  • R. D. Hoare, 2007 - Bivalve mollusks from the Maxville Limestone (Mississippian) in Ohio - The Ohio Journal of Science (107), 63-75 (journal article, English)
  • R. P. Whitfield, 1882 - Descriptions of new species of fossils from Ohio, with remarks on some of the geological formations in which they occur - Annals of the New York Academy of Sciences (2), 193-244 (journal article, English)