The Tarphycerida were the first of the coiled cephalopods, found in marine sediments from the Lower Ordovician (middle and upper Canad) to the Middle Devonian. Some, such as Aphetoceras and Estonioceras, are loosely coiled and gyroconic; others, such as Campbelloceras, Tarphyceras, and Trocholites, are tightly coiled, but evolute with all whorls showing. The body chamber of tarphycerids is typically long and tubular,[1] as much as half the length of the containing whorl in most, greater than in the Silurian Ophidioceratidae. The Tarphycerida evolved from the elongated, compressed, exogastric Bassleroceratidae, probably Bassleroceras, around the end of the Gasconadian through forms like Aphetoceras. Close coiling developed rather quickly, and both gyroconic and evolute forms are found in the early middle Canadian.

Temporal range: Lower Ordovician–Devonian
Estonioceras, found at Mt. Kinnekulle, Sweden.png
Estonioceras, found at Mt. Kinnekulle, Sweden
A coiled cephalopods imprint from Dane county, Wisconsin.jpg
A Trocholites imprint from Mount Horeb, Wisconsin
Scientific classification e
Kingdom: Animalia
Phylum: Mollusca
Class: Cephalopoda
Subclass: Nautiloidea
Order: TarphyceridaFlower, 1950 Tarphycerids tend to uncoil in the late mature stage of their growth, indicating they settled into a benthic lifestyle as they became older. Younger, wholly coiled forms were probably more active, nektobenthic, certainly more maneuverable. Composition and taxonomyEdit

The Tarphycerida comprise three phylogenetically related groups of families. They are: the tarphyceratid group consisting of the Estonioceratidae, Tarphyceratidae, Trocholitidae, and Ophidioceratidae; the barradeoceratid group, derived from Centrotarphyceras, consisting of the Barrandeoceratidae, Bickmoritidae, Nephriticeratidae, and Uranoceratidae; and the plectoceratid group, derived from Campbelloceras, consisting of the Plectoceratidae, Lechritrochoceratidae, and Apsidoceratidae.[2]

The tarphyceratids comprise the Tarphycerida of the Treatise on Invertebrate Paleontology Part K [1] to which Flower added the ancestral Bassleroceratidae. The Estonioceratidae, Tarphyceratidae, and Trocholitidae are primitive forms characterized by siphuncles with thick-walled connecting rings. The Ophidioceratidae are derived offshoots.

The barrandeoceratid and plectoceratid families were once combined in the Barrandeocerida,[3] determined[2] to be invalid due to having multiple ancestors in the Tarphyceriatidae and therefore abandoned. The common characteristic of these forms is the thin-walled connecting rings in their siphuncles.

A recent classification[4] divides the Tarphycerida into suborders Tarphycerina and Barrandeocerina, which were previously defined as separate orders.

Broader relationshipsEdit

Tarphycerids are more closely related to the diverse Oncocerida, through the ancestral Bassleroceratidae in the Lower Ordovician, than to the other nautiloid orders. The Oncocerida, in turn, gave rise to the Nautilida which include the recent Nautilus and Allonautilus. This puts the Tarphycerida in the broad group that includes the nautilids. It makes them also separate from the groups that include the Discosorida, Actinocerida, Endocerida, and Orthocerida, and from the superficially similar Ammonoidea.[5][6]

Tarphycerid biologyEdit

The tarphycerid animal must have been rather elongated, like squid, although no close relationship is implied. Either that or it was able to retreat deep into its portable lair. As for whatever arms or tentacles they may have had, no indication has been found. They probably went through two stages, first a younger more active and swimming stage with simple coiled shells, followed by a less active, bottom-dwelling stage with shells that diverge during which they mated and produced, probably a single litter of young, like the modern but unrelated coleoids.


  1. ^ a b Furnish and Glenister 1964; Nautiloidea - Tarphycerida; In the Treatise on Invertebrate Paleontology Vol K; Teichert and Moore, (eds) GSA and U of Kansas Press 1964
  2. ^ a b Flower R.H. 1984, Bodeiceras A New Mohawkian Oxycone, with revision of the Older Barrandeocerida and Discussion of the Status of the Order; Journal of Paleontology V 58, no.6, pp1372–1379, Nov 1984
  3. ^ Sweet W. 1964; Nautiloidea - Barrandeocerida; In the Treatise on Invertebrate Paleontology Vol K; Teichert and Moore, (eds) GSA and U of Kansas Press 1964
  4. ^ Teichert, C 1988; Main Features of Cephalopod Evolution, Ch 2 in The Mollusca, Vol 12 Paleontology and Neontology of Cephalopods, M.R. Clarke and E.R Trueman Eds.
  5. ^ Teichert, C and Moore, R.C 1964; Classification and Stratigraphic Distribution; Treatise on Invertebrate Paleontology Vol K; Teichert and Moore, (eds) GSA and U of Kansas Press 1964
  6. ^ Wade, M, 1988; Nautiloids and their descendants: cephalopod classification in 1986; New Mexico Bureau of Mines and Mineral Resources Memoir 44, Oct 1988.

Further readingEdit

  • Flower R.H. 1988; Progress and Changing Concepts in Cephalopod and Particularly Nautiloid Phylogeny and Distribution, in Cephalopods – Present and Past pp 17–24, Wiedmann & Kullman (Eds), Stuttgart.