Rhizocorallium commune Schmid, 1876
publication ID |
https://doi.org/ 10.5281/zenodo.13190253 |
persistent identifier |
https://treatment.plazi.org/id/53058F04-FFDF-400E-FF41-F994FBA2F829 |
treatment provided by |
Felipe |
scientific name |
Rhizocorallium commune Schmid, 1876 |
status |
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Rhizocorallium commune Schmid, 1876
Material: several epichnial specimens on top of sandstone beds from the R 21 interval, but also positive hypichnia right below the mentioned level ( Fig. 5e View Fig ).
Description: U-shape horizontal-subhorizontal tonguelike structures of 6-8 cm long, with up to 1.5 cm individual tunnel diameter ( Fig. 5f View Fig ). Usually the tubes are covered by striae. The distance between the limbs of U is up to 2.5 cm. One specimen reveals protrusive spreiten ( Fig. 5g View Fig ).
Remarks: Rhizocorallium is considered a burrow of deposit – feeding polychaete worm or a dwelling burrows of filter feeders ( Knaust, 2013). According to Seilacher
(2007), Rhizocorallium is ethologically interpreted as fodinichnia but without a behavioral genealogy. Gingras et al. (2009) noted that it is the result of a complex ethology of relatively deep tier tracemakers that systematically feed both with suspension and accumulated sediment. The Rhizocorallium from the analyzed section shows horizontal spreiten which normally represent deposit feeding of the subsurface strip-mining type ( Bromley, 1996). While feeding, the animal builds up the burrow for housing. The presence of striae is a clue for some deposit consistency at bioturbation time. They are usually found in littoral to neritic environment, the specimens older than Cretaceous being described exclusively in shallow waters ( Knaust, 2013). Rarely, it can be found in the deep water, indicating increasing oxygenation and depth of the redox boundary in sediment ( Kotlarczyk & Uchman, 2012). According to Buatois & Mángano (2011), this ichnospecies characterizes lower shoreface to the lower offshore environment.
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Departamento de Geologia, Universidad de Chile |
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