Osprioneides kampto Beuck et Wisshak, 2008
| ID | 12324 |
|---|---|
| Fossil group | Bioerosional trace fossils |
| Taxon | Osprioneides kampto |
| Author | Beuck et Wisshak, 2008 |
| Reference | Beuck et al., 2008a |
| Parent taxon | Osprioneides |
| FAD | Sandbian |
| LAD | Sheinwoodian |
Type specimens
| Type | No | Type locality | Type horizon | Remarks | Reference | ||||
|---|---|---|---|---|---|---|---|---|---|
| holotype | Naturhistoriska Riksmuseet, Stockholm | NRM−Cn 69062 | Hallshuk, Gotland | Wenlock | within the stromatoporoid Densastroma pexisum | Beuck et al., 2008a |
Description(s)
Beuck et al., 2008a:
Diagnosis. Large, straight to irregularly bent, unlined boring of variable length entering the substrate perpendicular to subparallel; cross−section oval; roughly constant oval diameter; terminus tapered to rounded.
Description. From a single oval aperture, the unbranched borings are sharply incised in the dense host skeleton, showing no deflections of the host growth increments, and are filled with a micritic matrix (Figs. 3, 4). The borings enter the substrate in a perpendicular to subparallel manner and follow primarily a straight course but may as well slightly curve or undulate. Individual traces measure up to 120 mm in length with an oval cross−section of averaging 7 (min. 5) × 13 (max. 17) mm in diameter, with a max/min ratio in excess of 2/1. Individual borings have a tapered to rounded terminus. Due to the high−abundance of traces within the sample analysed, borings occasionally truncate each other, occasionally resembling a branching pattern. Neither scratch marks nor any internal lining were observed. An idealised schematic drawing of the trace is given in Fig. 8.
Specimens with images (24)