liik

Pinaceocladichnus onubensis Mayoral, 1988

Taksoni kirjeldused

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).

Mayoral, 1988

Diagnosis. Pinaceocladichnus nov. ichnogen. con sistemas de bifurcacion myu regulares. Presentan aberturas subovaladas a fusiformes situadas muy cerca de los tuneles correspondientes que conectan con camaras alargadas, cilindricas o en forma de saco. Se disponen paralelas a los tunels anteriores.[Pinaceocladichnus nov. ichnogen. with very regular branching systems. They present subovate to 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.]

Sünonüümika
1988     Pinaceocladichnus onubensis nov. ichnoesp. — Mayoral , lk. 18, joon. 6-9
2023     Pinaceocladichnus onubensis Mayoral, 1988 — Gaaloul et al. , lk. 671, joon. 8B, 12A
Valik taksonit käsitlevast teaduskirjandusest
Toom, U., Vinn, O., Hints, O. 2019. Ordovician and Silurian ichnofossils from carbonate facies in Estonia: A collection-based review. Palaeoworld 28, 1-2, 123-144. DOI:10.1016/j.palwor.2018.07.001
Mayoral, E. 1988. Pennatichnus nov. icnogen.; Pinaceocladichnus nov. icnogen. e Iramena. Huellas de bioerósion debidas a Bryozoa perforantes (Ctenostomata, Plioceno inferior) en la cuenca del Bajo Guadalquivir [Pennatichnus nov. icnogen; Pinaceocladichnus nov. icnogen. and Iramena. Bioerósion traces due to perforating Bryozoa (Ctenostomata, lower Pliocene) in the Lower Guadalquivir basin]. Revista Española de Paleontología 3, 13–23.
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Levik kirjandusandmetel