Agoniatitida

Extinct order of molluscs From Wikipedia, the free encyclopedia

Agoniatitida, also known as the Anarcestida, is the ancestral order within the cephalopod subclass Ammonoidea originating from bactritoid nautiloids, that lived in what would become Africa, Asia, Australia, Europe, and North America during the Devonian from about the lower boundary of Zlichovian stage (corresponding to late Pragian, after 409.1 mya) into Taghanic event during upper middle Givetian (between 385 and 384 mya), existing for approximately 25 million years.

Phylum:Mollusca
Subclass:Ammonoidea
Order:Agoniatitida
Ruzhencev, 1957
Quick facts Scientific classification, Suborders ...
Agoniatitida
Temporal range: 409 – 384 Ma Late Pragian – Middle Givetian
An image showing the siphuncle (which could be agoniatitid), the tube which connects the current living shell to the previous ones. They have been dead for many years as we have found fossils.
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Mollusca
Class: Cephalopoda
Subclass: Ammonoidea
Order: Agoniatitida
Ruzhencev, 1957
Suborders
  • Agoniatitina
  • Anarcestina
  • Auguritina
  • Gephuroceratina
  • Gephurocerina
  • Pharciceratina
  • Timanocerina
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Taxonomic nomenclature

The Order Agoniatitida, named by Ruzhencev, 1957,[1] is a subjective synonym for the Order Anarcestida, named by Miller and Furnish, 1954.[2] Accordingly, the name Anarcerstida is based on the family Anarcestidae (ex Anarcestinae) of Steinmann 1890. That of Agoniatiida is based on the family Agnoniatidae of Holzapfel, 1899.

Saunders, Work, and Nikolaeva, 1999,[3] refer to the Anarcestida, with Agoniatina a suborder, maintaining the priority as found in the Treatise. Shevyrev, 2006[4] on the other hand follows Ruzhencev, 1957 and used Agonititida.

Morphology

Agoniatitids are primitive ammonoids with a ventral retrochoanitic siphuncle (septal necks point to the rear) reflective of their nautiloid ancestors and goniatitic sutures with a variable number of lobes. Shells vary from discoidal to globular. Coiling may be loose with whorls barely touching or tight with a dorsal impression.[2]

Fossil distribution

Fossils are restricted to strata of the Zlichovian (Late Pragian/Early Emsian) to late middle Givetian epochs.

Sources

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