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2 results for “Caulostrepsis”
Fig. 8. Caulostrepsis, a in In vivo and post-mortem bioerosion traces in solitary corals from the upper Pliocene deposits of Tunisia
Fig. 8. Caulostrepsis, a domichnion produced by polychates, in the skeleton of caryophylliid coral Ceratotrochus (Edwardsotrochus) duodecimcostatus Goldfuss, 1826), from the El Melah stream section, the upper part of the Argiles de Sidi Barka Formation (upper Pliocene) of Tunisia. A. Caulostrepsis cretacea (Voigt, 1971), INGUJ265P156. B. Caulostrepsis taeniola Clarke, 1908 and Pinaceocladichnus onubensis Mayoral, 1988 (Pn), INGUJ265P154. C. Caulostrepsis avipes Bromley and D'Alessandro, 1983, INGUJ265P176. D. A cluster of Caulostrepsis taeniola Clarke, 1908, INGUJ265P162. E–G. Caulostrepsis penicillus isp. nov. E. INGUJ265P158 holotype (a), and paratype (b). F. INGUJ265P174 paratype. G. INGUJ265P172, partial views (G1, G2).
Fig. 4. Bioerosion trace Caulostrepsis. A. Specimen DZP−18422 in Biotic interaction between spionid polychaetes and bouchardiid brachiopods: Paleoecological, taphonomic and evolutionary implications
Fig. 4. Bioerosion trace Caulostrepsis. A. Specimen DZP−18422, ventral valve of Bouchardia rosea showing the typical morphology of Caulostrepsis. Note the well−developed central ridge, and the straight morphology of the trace. B, C. Specimens DZP−18423 and 18424, respectively. Note that the galleries are roughly straight, and not enlarged at their distal extremities. The apertural groove (arrow) is well marked. D. Specimen DZP−18425, dorsal valve, showing multiple (arrows), straight traces. E, F. X−ray images of the specimens DZP−18426 and 18427, respectively. Note the straight morphology of unabraded tubes and the apertural groove (arrow) in the specimen DZP−18427. Scale bars 5 mm.
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