Danubea

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 : 514

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.4497973

persistent identifier

https://treatment.plazi.org/id/03F387D7-FFE1-FFB8-FBE3-9AE7FAEF826C

treatment provided by

Felipe

scientific name

Danubea
status

 

Danubea sp. A

( Fig. 9I View FIG )

OCCURRENCE. — Lower Jurassic, lower Sinemurian of the Mersin Mélange, NW of Mersin city, southern Turkey.

DESCRIPTION

Test large with inflated cortical shell and two polar spines. Cortical shell sphaerical with triangular and tetragonal pore frames. Small nodes present at pore frame vertices. Spines unequal in length, needle-like, circular in transversal section and tapering gradually to the distal end.

REMARKS

This specimen differs from Danubea howardi Whalen & Carter in Carter et al. (1998: 40-41 , pl. 5, figs 2-4, 14, 18) by having an ellipsoidal test in the direction of polar spines and needle-like spines instead of tricarinate ones.

GBIF Dataset (for parent article) Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF