Toragnostus

Toragnostus; Temporal range: late Middle Cambrian PreꞒ Ꞓ O S D C P T J K Pg N
	Toragnostus bituberculatus from specimen from Andrarum, Skåne, Sweden
Scientific classification
Kingdom:	Animalia
Phylum:	Arthropoda
Class:	Trilobita
Order:	Agnostida
Suborder:	Agnostina
Superfamily:	Agnostoidea
Family:	incertae sedis
Genus:	Toragnostus; Robison, 1988
Species
	T. bituberculatus (Angelin, 1851) synonyms Agnostus bituberculatus, Phalagnostus bituberculatus, Phoidagnostus bituberculatus[1]; T. placidus Buchholz, 1997 (tentatively assigned);

Toragnostus is a genus of trilobites restricted to the late Middle Cambrian. Its remains have been found in the United States, Greenland, Denmark, China, Sweden, the Russian Federation, and Kazakhstan. Its headshield and tailshield are almost completely effaced and it has two thorax segments.

Distribution

T. bituberculatus occurs in the late Middle Cambrian of the United States (Hillard Peak area, Alaska)[1] Greenland (Lejopyge laevigata-zone, Holm Dal Formation, West Peary-land), Denmark, China (Hunan), Sweden (Jincella brachymetopa-zone, Andrarum, Skåne), the Russian Federation (C. oriens and A. henrici-zones, Siberian Platform, and Bennett Island), and Kazakhstan (Mayan, Tian Shan Range).[2]

Description

Like all Agnostida, Toragnostus is diminutive, with the headshield (or cephalon) and tailshield (or pygidium) of approximately the same size (or isopygous) and outline. Like all Agnostina, Toragnostus has only two thorax segments. The cephalon and pygidium are almost completely effaced, lacking a cephalic border and with wide pygidial border. The cephalon is strongly convex. The central raised area of the cephalon (or glabella) is outlined at the rear, narrow and tapering forward. It carries an elongated median node, clearly in the front half of the cephalon. The pygidial axis (or rhachis) is very broad, with the frontal lobe (M1) defined by a furrow crossing the axis. There is a weak elongated node on the rhachis.[3]

gollark: How thoriated.

gollark: Only infinite? Weak.

gollark: (They are highly recursive)

gollark: Yep, definitely an inverted containment simulation.

gollark: As predicted, yes.

References

Palmer, A.R. (1967). Trilobites of East-Cental Alaska. Geological Survey Professional Paper. Retrieved 22 May 2013.
Whittington, H. B. et al. Part O, Treatise on Invertebrate Paleontology. Revised, Volume 1 – Trilobita – Introduction, Order Agnostida, Order Redlichiida. 1997
Robison, R.A. (1988). "Stratigraphy and Palaentology of the Holm Dal Formation (late Middle Cambrian), Central North Greenland". Meddelser om Gronland, Geoscience (20). Retrieved 22 May 2013.

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[Palmer-1] Palmer, A.R. (1967). Trilobites of East-Cental Alaska. Geological Survey Professional Paper. Retrieved 22 May 2013.

[Treatise-2] Whittington, H. B. et al. Part O, Treatise on Invertebrate Paleontology. Revised, Volume 1 – Trilobita – Introduction, Order Agnostida, Order Redlichiida. 1997

[Robison-3] Robison, R.A. (1988). "Stratigraphy and Palaentology of the Holm Dal Formation (late Middle Cambrian), Central North Greenland". Meddelser om Gronland, Geoscience (20). Retrieved 22 May 2013.