Dodecaactinella cf. cynodontota Bengtson and Runnegar, 1990
publication ID |
https://doi.org/ 10.5281/zenodo.13285795 |
persistent identifier |
https://treatment.plazi.org/id/A07B87A4-D738-2812-FF97-6D8280EEFA1A |
treatment provided by |
Felipe |
scientific name |
Dodecaactinella cf. cynodontota Bengtson and Runnegar, 1990 |
status |
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Dodecaactinella cf. cynodontota Bengtson and Runnegar, 1990 in Bengtson et al. 1990
Fig. 5A, B.
Material.—Three phosphatic replacements of calcitic spicules from etching residues of limestone erratic boulder Me32. Figured specimens, ZPAL Pf. V/35 S23, 26 .
Description.—Triacts, with rays branching dichotomously (Fig. 5A) or trichotomously (Fig. 5B).
Remarks.—These specimens resemble the Early Cambrian type material from the Ajax Limestone at the Mount Scott Range, South Australia ( Bengtson et al. 1990), but their subsidiary rays are stright more like the triactine−based spicules from the early Middle Cambrian Tindall Limestone of the Daly Basin, Northern Territory, Australia ( Kruse 1990), and their surfaces are corroded and rough as a result of the phosphatic replacement.
Occurrence.—Allochthonous Early Cambrian (Botomian) boulders (Me32), King George Island, Antarctica.
ZPAL |
Zoological Institute of Paleobiology, Polish Academy of Sciences |
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