Cubiculum inornatus Xing et al., 2015

Hedeny, Magdy El, Mohesn, Sara, Tantawy, Abdel-aziz, El-Sabbagh, Ahmed, AbdelGawad, Mohamed & El-Kheir, Gebely Abu, 2023, Bioerosion traces on the Campanian turtle remains: New data from the lagoonal deposits of the Quseir Formation, Kharga Oasis, Egypt, Palaeontologia Electronica (a 40) 26 (3), pp. 1-21 : 7-8

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https://doi.org/ 10.26879/1315

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scientific name

Cubiculum inornatus Xing et al., 2015
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Cubiculum inornatus Xing et al., 2015

( Figure 3D, F View FIGURE 3 )

Material. Four ellipsoidal chambers on a carapace remain (NVP006).

Description. Discrete, ellipsoidal borings in bone with marked concavity of flanks and bottom and marked constriction of walls in the upper area. Boring boundaries, wall and bottom are sharp and smooth. No bioglyphs or fillings were observed.

Discussion. In the present assemblage, C. inornatus is associated with other trace fossils; C. ornatus and Osteocallis mandibulus . Cubiculum inornatus resembles C. ornatus but is differentiated by having tapering ends and the absence of bioglyphs in their walls. Cubiculum levis Pirrone et al. (2014, p. 253 , figure 3) differs from our specimens in having interior bowl-shaped morphology and a marked constriction of walls in the upper area.

Producer. Indeterminate osteophagous insect (Xing et al., 2015; Paes Neto et al., 2016).

Stratigraphic and geographic distribution. Campanian of the Qarn Ganah, Kharga Oasis (this study). Cubiculum inornatus was recorded from the Middle Triassic of Brazil ( Paes Neto et al., 2016) to Lower‒Middle Jurassic of China and South Africa (Xing et al., 2015). The present determination greatly expands the stratigraphic range of C. inornatus to the Upper Cretaceous (Campanian).

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