Reticulariopsis talenti Lenz & Johnson, 1985
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https://doi.org/ 10.5281/zenodo.5375016 |
persistent identifier |
https://treatment.plazi.org/id/03A0162A-E952-FFBF-D8C1-FC6C7ABC1B94 |
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Marcus |
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Reticulariopsis talenti Lenz & Johnson, 1985 |
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Reticulariopsis talenti Lenz & Johnson, 1985 ( Figs 24 View FIG B-F; 25)
Reticulariopsis talenti Lenz & Johnson, 1985: 91 , pl. 15, figs 1-11.
Reticulariopsis ? sp. – Lenz & Johnson 1985: 91, pl. 15, figs 12-16.
MATERIAL EXAMINED. — Four isolated shells, mainly embeded in the rock matrix, from loc. 21581, Komsomolets Island ( Männik et al. 2002: fig. 1); Severnaya Zemlya or Pod”emnaya formations.
REMARKS
Small specimens (L = 5.1-5.5 mm, W = 6.3-6.9 mm, T = 3.7-4.0 mm) are characterised by ventribiconvex as well as biconvex shells with poorly developed sinus and fold. Serially sectioned internal structure shows small triangular teeth support- ed by short anteriorly divergent dental plates. Dental sockets are longitudinal and narrow. Crural plates are wide, triangular, jointed near the bottom of the shell. Crura are thin, fluently merging with primary lamellae of spiralia. The coils of spiralia are directed laterally and comprise four whorls. No ctenophoridium is found ( Fig. 25 View FIG ). Shells of similar size, with laterally ovate outline, are characteristic of Reticulariopsis ? sp. ( Lenz & Johnson 1985: 91). In the Garra Formation (Wellington area in New South Wales, Australia), this type of shells occurs 4 m below R. talenti . There is no evidence of its co-occurrence together with R. talenti also from Severnaya Zemlya. Smaller size, acute apical angle, weakly developed sinus and fold are reliable criteria for discriminating R. talenti from Reticulariopsis ? warreni Perry, 1984 described from the Delorme Formation, Mackenzie District of the Yukon ( Perry 1984: 121, pl. 41, figs 29-46).
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Reticulariopsis talenti Lenz & Johnson, 1985
Modzalevskaya, Tatiana L. 2003 |
Reticulariopsis talenti
LENZ A. C. & JOHNSON B. D. 1985: 91 |
Reticulariopsis
LENZ A. C. & JOHNSON B. D. 1985: 91 |