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Megaloolithus maghrebiensis
Taxonomy
Megaloolithus maghrebiensis was named by Garcia et al. (2003). It is considered to be a form taxon. Its type specimen is ACH2-05, an egg, and it is a 3D body fossil. Its type locality is Achlouj 2 (ACH2), which is in a Maastrichtian terrestrial mudstone in the Irbzer Formation of Morocco.
Synonymy list
Year | Name and author |
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2003 | Megaloolithus maghrebiensis Garcia et al. p. 62 figs. 2d, 3 |
2003 | Megaloolithus maghrebiensis Vianey-Liaud and Garcia p. 173 |
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If no rank is listed, the taxon is considered an unranked clade in modern classifications. Ranks may be repeated or presented in the wrong order because authors working on different parts of the classification may disagree about how to rank taxa.
†Megaloolithus maghrebiensis Garcia et al. 2003
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Diagnosis
Reference | Diagnosis | |
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G. Garcia et al. 2003 | Megaloolithus irregularly compactituberculate. Eggshell thickness from 1.7 to 2.5 mm. Elongation ratio (HIW) of the units from 2.5 to 3.7. Fan-shaped units with arched growth lines in the mammillae throughout the shell units. Units are well separated (node diameters 0.5 to 1.3 mm). In the areas where the nodes are fused in short chains and flat, the units are not clearly defined and the horizontal growth lines continue from one to the other. Pore canals are straight or linked by oblique bridges, as in Megaloolithus siruguei. Pore canal diameters between 75 to 130 m. Large eisospherite (0.15 to 0.3 mm) per node. Size and shape of the egg unknown. |
Measurements
No measurements are available
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Source: infrao = infraorder | |||||
Reference: Marsh 1875 |
Age range: Late/Upper Maastrichtian or 70.60000 to 66.00000 Ma
Collections: one only
Time interval | Ma | Country or state | Original ID and collection number |
---|---|---|---|
Late/Upper Maastrichtian | Morocco (Fes-Boulmane) | Megaloolithus maghrebiensis (type locality: 206442) |