Judahella dizluense
publication ID |
https://doi.org/ 10.5252/geodiversitas2020v42a21 |
publication LSID |
urn:lsid:zoobank.org:pub:7EC0E4FA-D538-4CE2-91B8-D7F549C32985 |
DOI |
https://doi.org/10.5281/zenodo.4488347 |
persistent identifier |
https://treatment.plazi.org/id/5A3887A8-FF9E-0E7B-0C72-FEF81EEE0C2D |
treatment provided by |
Felipe |
scientific name |
Judahella dizluense |
status |
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Judahella dizluense Kristan-Tollmann in Kristan- Tollmann, Tollmann & Hamedani, 1980 ( Fig. 7E, F View FIG )
Judahella (Judahella) dizluense Kristan-Tollmann in Kristan-Tollmann, Tollmann & Hamedani, 1980: 190, pl. 9, fig. 16. — Forel et al. 2019a: 35, fig. 18I.
Mostlerella dizluense – Kristan-Tollmann in Mette & Mohtat-Aghai 1999: 55, 56, pl. 6, figs 11, 12.
EXAMINED MATERIAL. — Four right valves, two left valves.
OCCURRENCE. — Rhaetian, Late Triassic, Bagerabad, Iran (Kristan- Tollmann et al. 1980); Rhaetian, Late Triassic, Tyrol, Austria (Mette & Mohtat-Aghai 1999); Tetraporobrachia haeckeli radiolarian Zone, Julian, Carnian, Late Triassic, Mersin Mélange, southern Turkey, Huğlu Tuffite (Forel et al. 2019a); Nicoraella ? budaensis conodont zone, late Julian-?earliest Tuvalian, Carnian, Late Triassic, samples BE17, 18, 21 ( Fig. 3 View FIG ), Belca section, ‘Raibl Beds’, Karavanke Mountains, Slovenia (this work).
DISCUSSION
Judahella dizluense occurs in samples BE17 to BE21, in which it is not abundant ( Fig. 3 View FIG ). Because of the preservation state of the material in Belca, the specimens were not measured. The present record is the second Carnian occurrence of this species.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
Kingdom |
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Phylum |
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Class |
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Order |
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SuperFamily |
Cypridoidea |
Family |
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Genus |
Judahella dizluense
Forel, Marie-Béatrice, Kolar-Jurkovšek, Tea & Jurkovšek, Bogdan 2020 |
Kristan-Tollmann 1999: 55, 56 |
Forel et al. 2019 2019: 35 |
Kristan-Tollmann, 1980 1980: 190 |