Poraspididae, Kiaer, 1932
publication ID |
https://doi.org/ 10.5252/g2013n3a3 |
DOI |
https://doi.org/10.5281/zenodo.5463523 |
persistent identifier |
https://treatment.plazi.org/id/493F87AA-FF94-6223-6B43-FA00FD29FD3F |
treatment provided by |
Marcus |
scientific name |
Poraspididae |
status |
|
Poraspididae gen. et sp. indet.
( Fig. 6G, H View FIG )
MATERIAL. — Specimens GIT 580-4, 6 and 7 of the Institute of Geology, Tallinn University of Technology, Estonia: fragments of a flank scale ( GIT 580-4) and of undetermined plates ( GIT 580-6 and 7).
LOCALITY AND STRATIGRAPHIC HORIZON. — Locality (sample) 73, Tonnel’nyj Brook, south of De Long Strait , Chukotka ; Lower Member (1) of Enmakaj Formation, Lochkovian .
DESCRIPTION ħis material is represented by three small fragmentary remains of dermal bony elements. ħe specimen GIT 580-4 ( Fig. 6G View FIG ) is from a flank scale of a poraspidid heterostracan similar to the scales figured, for example, by Blieck (1982: pl. VIII: 2, 4: Poraspis rostrata Kiaer &Heintz, 1935 ). It bears six flat dentine ridges per mm as in various Poraspis Kiaer,1930 species from the Lochkovian of Spitsbergen ( Blieck& Heintz 1983: table 1). ħe specimen GIT 580-7 ( Fig. 6H View FIG ) has more vaulted (convex) and wider(2/mm) dentine ridges.It probably also comes from a poraspidid plate.
GIT |
Institute of Geology at Tallinn University of Technology |
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