liik
Pseudopolydorites radwanskii Głazek, Marcinowski et Wierzbowski, 1971
Tüüpeksemplari andmed
holotüüp: Department of Geology, University of Warsaw ; Not pointed out; Sudół vana karjäär; Cenomani lade
Reference:
Głazek, J., Marcinowski, R. Wierzbowski, A. 1971. Lower Cenomanian trace fossils and transgressive deposits in the Cracow Upland. pp. 433–448.
Taksoni kirjeldused
Głazek et al., 1971
Diagnosis. - Tubular, U-shapeded borings, probalblly left by polychaetes, round in section and about 6 to 8 mm in diameter. The limbs of the U~shaped loop are usually 3 to 15 cm long, thIis length being sometimes shortened as a result of abrasiono (Fig.3c). The space between the limbs aboult 1.2 cm to 1.8 cm wide camposed of an original, non-reworked, solid rock. Boring openings on the surface round, without a funnel-like depression. In the near-opernng part, the limbs display a characteristic defllection of their trace in relation to the deeper parts of the boring.
Sünonüümika
Valik taksonit käsitlevast teaduskirjandusest
Głazek, J., Marcinowski, R. Wierzbowski, A. 1971. Lower Cenomanian trace fossils and transgressive deposits in the Cracow Upland. Acta Geologica Polonica 21, 3, 433–448.
Klassifikatsioon
| organismirühm | Biota |
| ihnorühm | Ichnofossils |
| Bioerosional trace fossils | |
| sugukond | Osteichnidae |
| perekond | Pseudopolydorites |
| liik | radwanskii |
Levik kirjandusandmetel
- Głazek et al., 1971 Sudół vana karjäär Cenomani lade