AnimaliaNot EvaluatedacceptedspeciesAccepted

Parabolbinella coeni
Casier, 2011
GBIF:127639208
0year

ABOUT
Descriptions(6)
1983 a Falsipollex sp. Groos, 1969; Milhau: 351. 1985 Falsipollex? sp.; Coen: pl. I, fig. 5. 1988 Falsipollex? sp. 3 G; Milhau: 486, pl. 55, fig. 10. 1990 Parabolbinella? sp.; Casier in Casier & Préat: pl. 1, fig. 8.
Maillet, Sebastien, Milhau, Bruno, Vreulx, Michel, Posada, Luis-Carlos Sánchez De (2016): Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications. Zootaxa 4068 (1): 1-78, DOI: 10.11646/zootaxa.4068.1.1
2013 b Parabolbinella coeni Casier; Maillet et al.: figs. 7 M – N. 2013 Parabolbinella coeni Casier; Casier in Casier & Préat: 487, pl. II, fig. 4.
Maillet, Sebastien, Milhau, Bruno, Vreulx, Michel, Posada, Luis-Carlos Sánchez De (2016): Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications. Zootaxa 4068 (1): 1-78, DOI: 10.11646/zootaxa.4068.1.1
Description. Large preplete, bilobate and equivalve carapace. Hmax at 2 / 5 anterior; Lmax at 1 / 3 dorsal; Wmax corresponding to the anterior lobe (L 2). Straight hinge line and dorsal margin. Anterior cardinal angle of about 130 °. Posterior cardinal angle of about 95 ° with a possible spine pointing upwards (not preserved). Anterior margin more rounded than the posterior one. Anterior part of the carapace higher than the posterior one. Ventral margin regularly convex. Well-rounded and large posterior lobe (L 3), reaching the dorsal margin in lateral view. Smaller anterior lobe (L 2), located more ventrally and slightly elliptic with a major axis perpendicular to the dorsal margin. Marked adductorial sulcus. Tecnomorphic carapaces with two adventral spines on each valve. Surface papillose.
Maillet, Sebastien, Milhau, Bruno, Vreulx, Michel, Posada, Luis-Carlos Sánchez De (2016): Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications. Zootaxa 4068 (1): 1-78, DOI: 10.11646/zootaxa.4068.1.1
Diagnosis. Casier in Casier et al. (2011 a, p. 77).
Maillet, Sebastien, Milhau, Bruno, Vreulx, Michel, Posada, Luis-Carlos Sánchez De (2016): Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications. Zootaxa 4068 (1): 1-78, DOI: 10.11646/zootaxa.4068.1.1
Discussion. Our specimens show all the features of P. coeni, with a large and well rounded posterior lobe, a possible spine at the postero-dorsal angle and a papillose surface. Only tecnomorphic specimens have been collected, exhibiting two adventral robust spines, one antero-ventral and the other medio-ventral. Occurrence. Lower to Middle Givetian (Hanonet, Trois-Fontaines, Terres d’Haurs, Mont d’Haurs, Névremont Fms, and Fromelennes Fm, Flohimont and Moulin Boreux Mbs), Ardenne (Flohimont, Cul d’Houille, Mont d’Haurs, Aisemont, Resteigne, Couvin, Hotton, Glageon and Aisne section); Middle Givetian (Candás Fm), Asturias (Peran-Perlora section); Givetian, Boulonnais; Middle Devonian, Ruhr.
Maillet, Sebastien, Milhau, Bruno, Vreulx, Michel, Posada, Luis-Carlos Sánchez De (2016): Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications. Zootaxa 4068 (1): 1-78, DOI: 10.11646/zootaxa.4068.1.1
Material. 2 specimens (1 C, 1 V).
Maillet, Sebastien, Milhau, Bruno, Vreulx, Michel, Posada, Luis-Carlos Sánchez De (2016): Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications. Zootaxa 4068 (1): 1-78, DOI: 10.11646/zootaxa.4068.1.1
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