Colosteidae

Colosteidae is a family of stegocephalians (stem-group tetrapods) that lived in the Carboniferous period.^[1] They possessed a variety of characteristics from different tetrapod or stem-tetrapod groups, which made them historically difficult to classify. They are now considered to be part of a lineage intermediate between the earliest Devonian terrestrial vertebrates (such as Ichthyostega), and the different groups ancestral to all modern tetrapods, such as temnospondyls (probably ancestral to modern amphibians) and reptiliomorphs (ancestral to amniotes such as mammals, reptiles, and birds).

Colosteidae Temporal range: Carboniferous (Viséan–late Moscovian) PreꞒ Ꞓ O S D C P T J K Pg N
Life restoration and size comparation of three members of Colosteidae
Scientific classification
Domain:	Eukaryota
Kingdom:	Animalia
Phylum:	Chordata
Clade:	Sarcopterygii
Clade:	Tetrapodomorpha
Clade:	Stegocephali
Family:	†Colosteidae Cope, 1875
Type genus
†Colosteus Cope, 1871
Genera
†Colosteus †Deltaherpeton †Greererpeton †Pholidogaster

Description

Colosteids had elongated bodies, with an estimated 40 vertebrae, not including the tail. The skull is relatively flat and composed of many separate bones, like that of other stegocephalians. Colosteids lacked otic notches at the back of the head, unlike temnospondyls and other "labyrinthodonts". However, they did possess large mandibular and palatal fangs (on the lower jaw and the roof of the mouth), in addition to smaller marginal teeth (at the edge of the mouth), like "labyrinthodonts". The skull was overlaid with wide sensory grooves known as lateral lines, which extended from rear edge of the skull to the tip of the snout. Most aquatic stegocephalians have their lateral lines dip, unbroken, under the nostrils once they reach the tip of the snout, or alternately disconnect into separate grooves separated by the nostrils. However, colosteids evolved a unique alternative; their lateral lines droop below the nostrils so far that they contact the marginal teeth, so that the edge of the skull is responsible for subdividing the grooves, rather than the nostrils.^[1]

The mandibular fangs were larger than the palatal ones, though those on the palate were still large. Colosteids were unique compared to most stegocephalians in the fact that a pair of palatal fangs were present on the premaxillary bones at the tip of the snout. In conjunction with the forward position of these fangs, the dentary bones of the lower jaw developed a notch on either side near the symphysis (chin). The symphysis itself is formed by a rough area of bone on the left and right dentaries. This rough patch is formed by a complex system of ridges, which have been described as "brassicate" (textured like a cauliflower).^[2] Only Megalocephalus is known to share this brassicate patch with colosteids. The mandibles were also unique in the fact that they possessed a single elongated hole along their inner surface, known as an exomeckelian foramen (or a meckelian fenestra). Earlier stegocephalians like Ichthyostega possessed a subtle slit in the mandible, while most later groups had a series of smaller, well-defined holes.^[1]

Relationships

The analysis below was conducted by Swartz in 2012, showing the relationship of colosteids with other tetrapodomorphs.^[3]

Elpistostegalia	Panderichthys Stegocephalia Elpistostege Tiktaalik Elginerpeton Ventastega Acanthostega Ichthyostega Whatcheeriidae Colosteidae Crassigyrinus Baphetidae Crown group Tetrapoda

References

1. John R. Bolt & R. Eric Lombard (2010). "Deltaherpeton hiemstrae, a New Colosteid Tetrapod from the Mississippian of Iowa". Journal of Paleontology. 84 (6): 1135–1151. doi:10.1666/10-020.1. S2CID 83774501.
2. Lombard, R. Eric; Bolt, John R. (September 2001). "The mandible of the primitive tetrapod Greererpeton, and the early evolution of the tetrapod lower jaw". Journal of Paleontology. 75 (5): 1016–1042. doi:10.1017/S0022336000039913. ISSN 1937-2337. JSTOR 1307064. S2CID 232347256.
3. Swartz, B. (2012). "A marine stem-tetrapod from the Devonian of Western North America". PLOS ONE. 7 (3): e33683. doi:10.1371/journal.pone.0033683. PMC 3308997. PMID 22448265.

External links

• "Tetrapoda: Carboniferous Forms. Colosteidae". Palaeos. Archived from the original on October 6, 2022.
• "Museum of Geology & Natural History: Selected Fossils". West Virginia: Geological & Economic Survey. Archived from the original on October 10, 2023.