AnimaliaNot EvaluatedacceptedspeciesAccepted
Parabolbinella coeni

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

Export occurrence data

Darwin Core Archive (ZIP)

CLASSIFICATION

Taxonomic Classification Tree

MULTIMEDIA

Media Files(1)

FIGURE 4. Height / length diagram for Evlanella peranensis Maillet n. sp .. The trendline equation (y) is indicated.

Imageimage/png© Maillet, Sebastien;Milhau, Bruno;Vreulx, Michel;Posada, Luis-Carlos Sánchez DeMaillet, Sebastien;Milhau, Bruno;Vreulx, Michel;Posada, Luis-Carlos Sánchez De

IMAGES

Gallery(1)

See Gallery

Occurrences with images

Source Information

Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications

checklist

This dataset contains the digitized treatments in Plazi based on the original journal article 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

Abstract

Asturian ostracods of the Givetian carbonate Candás Formation are documented for the first time from the Peran-Perlora and Carranques reference sections. More than 1,200 specimens were extracted from 44 samples by means of the hot acetolysis method. In all, 75 taxa are described herein, of which 21 are formally described and one, Evlanella peranensis Maillet n. sp., is new. All the taxa are marine benthic and belong to the Eifelian Mega-Assemblage. The assemblages recognized are representative of semi-restricted to shallow open-marine palaeoenvironments above the storm wave base. The stratigraphical distribution of the taxa shows a strong faunal renewal in the top of the Candás Formation. Long-ranging taxa found at the base of the formation, of which many are known from the base of the Middle Devonian, disappear within the base of the member C and are replaced above, around the Middle/Upper Givetian boundary, by more cosmopolitan taxa characteristic of the Frasnian. The lower half of the member C is also characterized both by unstable environments and occurrence of some short-ranging opportunistic ostracod taxa. This renewal within shallow water ostracod communities is probably a consequence of the global Taghanic Biocrisis, leading world-widely to extinctions in several faunal groups. Faunal affinities with Givetian ostracod taxa reported in other areas of the world reflect the commonly accepted palaeogeographical patterns. Close relations between the Cantabrian Zone (NW-Spain), the Armorican Massif (W- France), the Mouthoumet Massif (S-France) and North Africa (Morocco and Algeria) suggest a narrow oceanic space between the western European terranes and the northern Gondwanan margin that involves an advanced phase of closure of the Medio-European Ocean.

Key words: Middle Devonian, new species, faunal renewal, systematic, Taghanic Biocrisis

Maillet S, Milhau B, Vreulx M, Posada L S D, plazi (2016). Givetian ostracods of the Candás Formation (Asturias, North-western Spain): taxonomy, stratigraphy, palaeoecology, relationship to global events and palaeogeographical implications. Plazi.org taxonomic treatments database. Checklist dataset https://doi.org/10.11646/zootaxa.4068.1.1 accessed via GBIF.org on 2026-06-18.

CC0Published 12/31/2016View dataset
GBIF Usage Key
127639208
Dataset Key
b9c1e3a3-e591-4b34-9f30-d6d88a230673
Origin
source
Taxon ID
03B94C39E8424B7BFF22FEDEFBE9F9DD.taxon
Last Crawled
6/11/2026
Last Interpreted
6/11/2026