AnimaliaNot EvaluatedacceptedspeciesAccepted
Refrathella struvei

Refrathella struvei

Becker, 1967

GBIF:127639192

0year

ABOUT

Descriptions(4)

Description. Medium-sized elongated and equivalve carapace, sub-rectangular outline in lateral view, arrowhead-shaped in dorsal view. Hmax at 1 / 3 anterior; Lmax at 1 / 3 dorsal; Wmax in the postero-ventral part (at ridge extremity). Straight hinge line and dorsal margin. Adductorial sulcus slightly anterior to mid-dorsal. Slightly convex ventral margin, posteriorly oblique. Well rounded and regularly convex anterior margin, forming an angle of about 120 ° with the dorsal margin. Slightly rounded posterior margin, more arched in its ventral part, forming an angle of about 120 ° with the dorsal margin. Anterior part of the carapace higher than the posterior one. Surface with very large reticles, except along the free margins of the carapace. Smooth and flattened free margins. Marked ridge in the ventral half of each valve, formed by two lines of large reticles. Ridge long of 5 / 6 of Lmax beginning at the anterior margin and becoming more prominent in its posterior part, thus forming lateral robust wings in dorsal view.
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
cf. 1967 Refrathella struvei nov. sp.; Becker: pl. I, figs. 1 – 9. cf. 2013 Refrathella struvei Becker; Maillet: 62, pl. VI, figs. 14 – 15. 2013 Refrathella sp. B., cf. R. struvei Becker; Maillet: 63, pl. VI, fig. 17. cf. 2013 Refrathella struvei Becker; Casier in Casier & Préat: 488, pl. II, fig. 15, pl. III, fig. 1.
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. A Refrathella characterized by a larger carapace than R. struvei Becker, 1967 and a carina with thick ridges on each valve. Occurrence. Middle Givetian (Candás Fm, mbs A, B and C), Asturias (Peran-Perlora section).
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. 8 specimens (5 V, 3 F).
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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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 2026-06-17.

CC0Published 12/31/2016View dataset
GBIF Usage Key
127639192
Dataset Key
b9c1e3a3-e591-4b34-9f30-d6d88a230673
Origin
source
Taxon ID
03B94C39E8594B60FF22FF63FB1CFC7B.taxon
Last Crawled
6/11/2026
Last Interpreted
6/11/2026