Tyrrhenocythere pezinokensis ( Jiříček, 1985 )

Pipík, Radovan, 2007, Phylogeny, palaeoecology, and invasion of non-marine waters by the late Miocene hemicytherid ostracod Tyrrhenocythere from Lake Pannon, Acta Palaeontologica Polonica 52 (2), pp. 351-368 : 356-358

publication ID

https://doi.org/ 10.5281/zenodo.13741768

persistent identifier

https://treatment.plazi.org/id/03F00B19-FFA6-FFCA-F16B-CA0CC2ACFB16

treatment provided by

Felipe

scientific name

Tyrrhenocythere pezinokensis ( Jiříček, 1985 )
status

 

Tyrrhenocythere pezinokensis ( Jiříček, 1985)

Figs. 4A–F, 5G View Fig 1 View Fig , G 2 View Fig , J, 6F View Fig .

1985 Hemicytheria pezinokensis sp. nov.; Jiříček 1985: 405, pl. 56: 10–12.

1998 Tyrrhenocythere pezinokensis ( Jiříček, 1985) ; Pipík 1998: pl. 2: 5, 6.

Remark.—The original description is incomplete, hence a description of the hinge, muscle scars and marginal zone is given based on the material collected in Pezinok clay pit, the layer 36+37A.

Material.— 30 adult valves, 1 juvenile.

Description.—Muscle scars: a vertical row of six scars (the second and the third of the “standard” row of four each divided in two), with three additional anterior scars ( Fig. 5G View Fig 1 View Fig ).

Hinge (amphidont): The hinge ( Fig. 5G View Fig 2 View Fig , J) of the LV is composed of a rhomboidal anterior socket; a square tooth that continues into a smooth bar; a posterior socket with an elongate opening toward the interior; a tiny tooth in the middle of the posterior socket. The hinge of the RV has a strong, elongated tooth divided into two lobes; a socket that passes into a slightly curved, smooth groove; a posterior elongated, kidney−shaped tooth composed of 3 tiny elements.

Marginal zone: inner lamella large, with a series of parallel striae; inner margin parallel with outer margin; 5 fully developed brush−like marginal pore canals (MPC); 6 to 8 MPC on ADM ( Fig. 6F View Fig ); AVM are separate or incompletely fused; simple MPC on VM; large zone of fusion; drop−like space between the “brushes” on AM; irregular, sinusoidal line of concrescence on AM.

Stratigraphical and geographical range.—The species, first described by Jiříček (1985: 405) from the Pannonian clay deposits in Pezinok, is still known only from its type locality.

Kingdom

Animalia

Phylum

Arthropoda

Class

Ostracoda

Order

Podocopida

Family

Hemicytheridae

Genus

Tyrrhenocythere

Loc

Tyrrhenocythere pezinokensis ( Jiříček, 1985 )

Pipík, Radovan 2007
2007
Loc

Hemicytheria pezinokensis

Jiricek, R. 1985: 405
1985
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