Pinaceocladichnus onubensis Mayoral, 1988
| ID | 15809 |
|---|---|
| Fossil group | Bioerosional trace fossils |
| Taxon | Pinaceocladichnus onubensis |
| Author | Mayoral, 1988 |
| Reference | Mayoral, 1988 |
| Parent taxon | Pinaceocladichnus |
| FAD | Dapingian |
| LAD | Recent |
Type specimens
| Type | No | Type locality | Type horizon | Remarks | Reference | ||||
|---|---|---|---|---|---|---|---|---|---|
| holotype | Sevilla University | MO1/5B/01-02 | Moguer (Huelva) | Pliocene | Arenas de Huelva | Mayoral, 1988 |
Description(s)
Gaaloul et al., 2023:
Diagnosis.—Pinaceocladichnus with very regular bifurcation systems. They present sub-oval or fusiform openings located very close to the corresponding tunnels that connect with elongated, cylindrical or sac-shaped chambers. They are arranged parallel to the previous tunnels (translated from Mayoral 1988).
Stratigraphic and geographic range.—Ordovician (Estonia; Toom et al. 2019) to the Recent (worlwide).
Specimens with images (4)
