Helicerina, Bronnimann and Masse, 1968
publication ID |
https://doi.org/ 10.4202/app.2009.0094 |
persistent identifier |
https://treatment.plazi.org/id/A2018795-2146-FFB2-FCEE-FCA090C9F96E |
treatment provided by |
Felipe |
scientific name |
Helicerina |
status |
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Helicerina ? isp. A aff. Helicerina siciliana Senowbari−Daryan, Schäfer , and Catalano 1979
Fig. 2C View Fig .
Material.— Four poorly preserved specimens of thin section CPBA−N ° 20675, 20676, Rahue creek ( Fig. 1 View Fig , 36 ° 01.762'S, 69 ° 59.393'W) GoogleMaps .
Description.—Microcoprolite with circular outline and a cross section of 900 µm in diameter. The specimen is characterised by one canal which lies in the symmetry plane. This canal can be compared with the canal developed in Helicerina siciliana Senowbari−Daryan, Schäfer , and Catalano, 1979. In contrast to Helicerina siciliana the canal in Helicerina ? isp. A is not clearly separated in distinct canals (in Helicerina siciliana : a dorsal diamond shaped and a ventral triangular shaped canal) but seems to form one “unit”.
Contrary to all other known Helicerina ichnospecies the canal shows no connection to the “outside of the coprolite” (terminology according to Senowbari−Daryan and Bernecker 2005). However, this connection is very thin and can be clossed. If additional findings will confirm the lack of connection, our specimen belongs to a new ichnogenus and −species.
Stratigraphic and geographic range.— Helicerina isp. A aff. Helicerina siciliana was recognised in levels corresponding to the Lissonia riveroi and Olcostephanus (Olcostephanus) atherstoni zones (early Valanginian) of the Vaca Muerta Formation.
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