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Rahman et al., 2015

Miocene Clypeaster from Valencia (E Spain): Insights into the taphonomy and ichnology of bioeroded echinoids using X-ray micro-tomography

Rahman, I. A., Belaústegui, Z., Zamora, S., Nebelsick, J. H., Domènech, R., Martinell, J.
JournalPalaeogeography, Palaeoclimatology, Palaeoecology
Typearticle in journal


Taphonomic analysis and X-ray micro-tomography (.CT) were applied to Clypeaster specimens from the Miocene of Fuente del Jarro (Valencia, Spain). This enabled the identification of various preservational features, including encrustation, bioerosion, abrasion and post-depositional cracking. Approximately 15% of the studied
specimens were affected by encrusters and/or borers. Of particular interest was a single intensely-bored specimen preserving numerous cross-cutting bioerosion structures. These structures exhibit a distinctivemorphology consisting of clavate or flask-shaped chambers with a circular to oval cross-section, a narrowneck region near the figure-of-eight-shaped aperture and a chimney extending outside the Clypeaster test. The excellent preservation and characteristic morphology, as revealed by the CT scan, coupled with the observation that (in some cases) articulated bivalve shells are still present within the chambers, allows for the identification of the tracemaker as the boring bivalve Rocellaria, reaffirming these tube-dwelling animals as borers, burrowers and crypt-builders. The trace fossils described herein are semi-endoskeletal dwellings, representing a combination of bioerosion through the plates of the echinoids, bioturbation in the form of burrowing into the sediment infill of the Clypeaster specimen and carbonate secretion resulting in a crypt. The morphologies of the different dwellings are influenced by the limited available space within the echinoid tests. This study confirms the importance of the relatively stable and thick Clypeaster shells as benthic islands in Cenozoic sandy littoral settings. The high degree of multiple colonizations, as well as the uniformorientation of the burrows, suggests a long-termstable position of this secondary substrate at or near the sediment surface.

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