Avetoichnus Uchman & Rattazzi, 2011

Anistoroae, Anca & Miclăuș, Crina, 2015, The Cruziana Ichnofacies In The Lower Member Of The Bisericani Formation (Eastern Carpathians, Romania), Acta Palaeontologica Romaniae 11 (2), pp. 9-23 : 17-18

publication ID

https://doi.org/ 10.5281/zenodo.13190253

persistent identifier

https://treatment.plazi.org/id/53058F04-FFD0-4000-FF41-F8BCFDF6FDA4

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Felipe

scientific name

Avetoichnus Uchman & Rattazzi, 2011
status

 

Ichnogenus Avetoichnus Uchman & Rattazzi, 2011 Avetoichnus luisae Uchman & Rattazzi, 2011

Material: around 50 endichnia specimens in two levels of whitish-gray mudstone from the levels R 7 to R 17.

Description: dark-colored horizontal to slightly curved zip-like trace fossils. Specimens are up to 45 mm long and over 3 mm wide and appear as two rows of dots arranged along a central axis. Zip-like shape is the result of a “beheaded” helical spiral, each whorl of the spiral being preserved as a pair of dots ( Fig. 5h View Fig ).

Remarks: the ethology of the ichnospecies is debatable. According to Uchman & Rattazzi (2011), this complex trace fossil is an agrichnion of a non-graphoglyptide tracemaker which stashed the nutrients rich sediment in its central tubular axis for starting a bacteria farm. It was described as populating deep marine environment, but based on its co-occurrence especially with Rhizocorallium it seems that this species is rather a crossfacies one and its ethology may be more complicated than the original proposed one ( Anistoroae & MiclăuȘ, 2014).

Aside from the described ichnotaxa, many other trace fossils occur in the logged sedimentary succession, but systematic feeding traces of graphogliptides lack. They are generally three-dimensional, horizontal, and subhorizontal, some of them being in co-occurrence, while others are isolated. The plan-parallel or ripple cross laminated coarser beds are dominated by hypichnia, rare epichnia, while endichnia are well developed in the “background” laminated mudstone beds.

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Departamento de Geologia, Universidad de Chile

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