Isityumzi Explained

Isityumzi mlomomde is fossil lungfish described from fragmentary remains including one complete parasphenoid, tooth plates fragments and scales from the Late Devonian Sarcopterygians (lobe finned fishes).[1] It represents the only record of Late Devonian lungfish remains from western Gondwana.

This novel species was described through an international collaboration from the world renowned Waterloo Farm lagerstätte in the former Grahamstown (Makhanda) of the Eastern Cape province, South Africa. The type material for this genus was excavated from a layer of black metashale located in a predominantly arenaceous Witpoort Formation corresponding to the Famennian age.

Lungfish are believed to have solely originated from tropical to warm temperate regions, however, evidence from the Isityumzi mlomomde adds a bigger circle of information to the current perception as evidence from these now suggests that lungfishes originated from the high palaeolatitude fauna located at 70° latitude and possibly further south.[2] [3] This was the position of now Waterloo Farm lagerstätte in what was once Gondwana landmass.

Isityumzi mlomomde is further believed to have coexisted with the tetrapods of the Famennian in an estuarine ecosystem environment as seen through the Waterloo Farm lagerstätte's geological lens.[4] [5] [6]

Description

To date, two parasphenoid bones have been found in Waterloo Farm, one partial and the other (latest) complete. The current description is mainly based on the complete specimen found with other fragments, as the incomplete one has already been described previously.[7]

The parasphenoid of the Isityumzi mlomomde is thin and flat, not fused with the pterygoids but shows a clear area for overlap by these bones. The size difference across the widest point between the holotype and the partial parasphenoid is 16mm, with the former being smaller. The anterior part is wide, with almost half the entire length of the total specimen. The parasphenoid has a distinctly broad rhombic anterior portion (corpus) and a narrow posterior shaft. The shaft is slender with parallel sides that taper to a single point posteriorly. The lateral angle between the stalk and the corpus is 30°. A long median ridge runs anteroposteriorly carrying a broad channel across the length of the stalk but it is unclear whether or not this lies on the dorsal or ventral surface. The overall appearance of the bones resembles those of Oervigia.

Etymology

The genus name Isityumzi is derived from the IsiXhosa language meaning 'device for crushing'. The species epithet mlomomde is also an IsiXhosa name meaning 'long mouthed'.

Notes and References

  1. Gess. Robert W.. Clement. Alice M.. 2019-12-04. A high latitude Devonian lungfish, from the Famennian of South Africa . PeerJ . en . 7 . e8073 . 10.7717/peerj.8073 . 2167-8359 . 6898985 . 31824758 . free .
  2. Torsvik. Trond H.. Cocks. L. Robin M.. 2011. The Palaeozoic palaeogeography of central Gondwana. Geological Society, London, Special Publications. 357. 1. 137–166. 10.1144/sp357.8. 2011GSLSP.357..137T . 131031948 . 0305-8719.
  3. Torsvik. Trond H.. Cocks. L. Robin M.. 2013. Gondwana from top to base in space and time . Gondwana Research. en. 24. 3–4. 999–1030. 10.1016/j.gr.2013.06.012. 2013GondR..24..999T .
  4. Friedman. Matt. Daeschler. Edward B.. Late Devonian (Famennian) Lungfishes from the Catskill Formation of Pennsylvania, USA . 2006. Palaeontology . en . 49 . 6 . 1167–1183 . 10.1111/j.1475-4983.2006.00594.x . 2006Palgy..49.1167F . 0031-0239. free.
  5. Lebedev. O. A. 2004. A new tetrapod Jakubsonia livnensis from the Early Famennian (Devonian) of Russia and palaeoecological remarks on the Late Devonian tetrapod habitats. Acta Universitatis Latviensis. 679. 79–98. dspace.lu.lv.
  6. Thomson; Panchen. KS; AL. 1980. The ecology of Devonian lobe-finned fishes. In The terrestrial environment and the origin of land vertebrates. Academic Press London. 15. 187–222.
  7. Anderson; Gess; Hiller. M.E; R.W; N. 1994. The first Bothriolepsis-associated Devonian fish fauna from Africa. South African Journal of Science. 90. 397.