Emiluvia prisca Tekin, 2020

Tekin, Kagan, Krystyn, Leopold, Okuyucu, Cengiz, Bedi, Yavuz & Sayit, Kaan, 2020, Late Triassic to Early Jurassic radiolarian, conodont and ammonite assemblages from the Tavuscayiri block, Mersin Mélange, southern Turkey: Time constraints for the T / J boundary and sedimentary evolution of the southern margin of the northern Neotethys, Geodiversitas 42 (27), pp. 493-537 : 508

publication ID

https://doi.org/ 10.5252/geodiversitas2020v42a27

publication LSID

urn:lsid:zoobank.org:pub:1A437774-B5BE-49F2-8DEF-D46F2790484A

DOI

https://doi.org/10.5281/zenodo.4494950

persistent identifier

https://treatment.plazi.org/id/7DE81B35-1355-426F-89AC-1AA538F91A9C

taxon LSID

lsid:zoobank.org:act:7DE81B35-1355-426F-89AC-1AA538F91A9C

treatment provided by

Felipe

scientific name

Emiluvia prisca Tekin
status

sp. nov.

Emiluvia prisca Tekin , n. sp.

( Fig. 6 View FIG W-Y)

urn:lsid:zoobank.org:act:7DE81B35-1355-426F-89AC-1AA538F91A9C

HOLOTYPE. — Sample Orbuk-46, HU.JMB.0111 ( Fig. 6W View FIG ).

PARATYPES. — HU.JMB.0112 ( Fig. 6X View FIG ), HU.JMB.0113 ( Fig. 6Y View FIG ).

TYPE LOCALITY. — Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey.

ETYMOLOGY. — From the Latin: Prisca: former, ancient, old-fashioned, due to its old occurrence.

OCCURRENCE. — Lower Jurassic, middle Lower Pliensbachianupper Pliensbachian, Orbuklukeli section, Mersin Mélange, NW of Mersin city, southern Turkey.

DIMENSIONS (based on three specimens, in µm). — Diameter of test: 92-100 (holotype: 100, average: 97.3); Length of spines: 110- 130 (holotype: 130, average: 118.6).

DESCRIPTION

Test large, sphaerical to subsphaerical with four spines situated at corners. Very large nodes present at pore frame vertices on the outer layer of cortical shell. Four nodes visible per row. Inner layer of pore frames polygonal (mainly triangular). Spines longer than the diameter of cortical shell and mainly equal, tapering distally, terminated with very sharp end. They are tricarinate with relatively wide ridges and wide grooves.

REMARKS

This species can be differentiated from Emiluvia tuberis ( Carter et al. 1998: 41-42, pl. 5, figs 9, 10, 19) by having a sphaerical to subsphaerical cortical shell with large nodes at pore frame vertices.

Kingdom

Chromista

Phylum

Radiozoa

Class

Polycystina

Order

Spumellaria

Family

Emiluviidae

Genus

Emiluvia

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