Sineruga insolita, Perrier, 2012

Perrier, Vincent, 2012, An atypical Silurian myodocope ostracod from the Armorican Massif, France, Acta Palaeontologica Polonica 57 (2), pp. 363-373 : 365-368

publication ID

https://doi.org/ 10.4202/app.2010.0006

persistent identifier

https://treatment.plazi.org/id/03E78B44-FFC6-2B70-FCDE-8627D8B1F862

treatment provided by

Felipe

scientific name

Sineruga insolita
status

gen. et sp. nov.

Sineruga insolita View in CoL gen. et sp. nov.

Figs. 2–5 View Fig View Fig View Fig View Fig , 7I, J, N.

Etymology: From Latin insolita , unusual.

Type material: Holotype: FSL 710900 View Materials ( Figs. 2F View Fig , 3A View Fig ) right valve preserved in 3D (L = 2.91 mm; H = 1.75 mm) . Paratype: FSL 710893 View Materials ( Fig. 2A View Fig ) left valve preserved in 3D (L = 3.19 mm; H = 1.96 mm) .

Type locality: Les Chevrolières , St. Denis−d’Orques, Sarthe, France (Loc. 1) .

Type horizon: Highly deformed siltstone and mudstone beds containing numerous partly pyritized nodules; Le Val Formation ; uppermost Ludlow to lower Pridoli .

Referred material.—Hundreds of valves from four localities in France. 3D preserved specimens: the largest and the smallest specimens (respectively FSL 710630, Fig. 2A, L View Fig = 3.20 mm, H = 2.03 mm and FSL 710897, Fig. 2A, L View Fig = 1.33 mm, H = 0.87 mm) come from Loc. 1. Flattened specimens: the largest specimen (FSL 710533, Fig; 4A, L = 3.96 mm; H = 2.60 mm) comes from Loc. 3, the smallest (FSL 710924, Fig; 4B, L = 1.11 mm; H = 0.70 mm) from Loc. 4.

Diagnosis.— Entomozoidae with reniform outline, rounded to square anterior margin, rounded ventral margin, slightly pointed posterior margin and straight dorsal margin. Anterior half of valves less prominent than posterior. Dorsal connection centred above sulcus. Sinusoidal adductorial sulcus with simple elliptical muscle spot. Ventral and posterodorsal tubercle often present. Valves completely smooth.

Measurements.—See scatterplots diagrams ( Fig. 6 View Fig ). Length to height ratios (L:H) were calculated for 39 specimens from four localities. Five to six ontogenetic stages are probably represented ( Fig. 6 View Fig ).

Description.—Symmetrical reniform valves. Maximum valve length (L) across the posterior tubercle; maximum valve height (H) at approximatively mid−length (ventral tubercle) and maximum width across the centre of the posterior half of the carapace. The lateral outline tapers anteriorly. Valves divided by a subcentral sulcus; anterior part less prominent than posterior part (respectively 1/3 and 2/3 of valve area). Straight dorsal margin showing the dorsal connection (more than half of valve length) centred above the sulcus and the muscle spot. Anterodorsal part of the carapace flattened, rounded to square without rostrum or rostral incisures. Ventral margin perfectly rounded. Posterior margin slightly pointed (tubercle) or rounded when tubercle absent. The entire lateral surface is more or less deeply (deeper in the dorsal part) incised by a narrow sinusoidal sulcus. This sulcus originates in a triangular area (centre of the dorsal connection) and extends from dorsal to ventral margins. The sulcus is concave frontward in the dorsal part, and backward in the ventral part. The sulcus broadens in the muscle spot region, which is located at the inflection point of the sulcus. The muscle spot consists of a single reniform scar. Two small tubercles are often present; they are situated posterodorsally and ventrally. External surface of the valve completely smooth.

http://dx.doi.org/10.4202/app.2010.0006 http://dx.doi.org/10.4202/app.2010.0006

Remarks.— Sineruga insolita gen. et sp. nov. is difficult to place within a previously described group of Palaeozoic myodocopid ostracods. Sineruga definitely belongs neither to the cypridinids (no rostrum, but a sulcus and a straight dorsal margin; compare Fig. 7L and N) nor to the bolbozoids (no rostrum and no bulb, but simple muscle scar and straight dorsal margin; compare Fig. 7K and N). Nevertheless, Sineruga shares several characteristics with Silurian and Devonian entomozoids. For example, S. insolita gen. et sp. nov. shares several morphological features with Richteria migrans (middle Ludlow, Fig. 7G, H; see Perrier et al. 2007), such as a bean−shaped outline, a straight dorsal connection, and a well−developed adductorial sulcus (compare Fig. 7M and N). However, Sineruga bears two tubercles and a small frontal projection. These characters are absent in Richteria , which displays the typical entomozoid ribbed ornament and an “eye tubercle”. In some features, Sineruga is also close to the Devonian Rhomboentomozoidae Franklinella lysogorensis from Givetian/Frasnian boundary interval ( Olempska 2002). Both the Silurian and the Devonian species display a straight dorsal connection with a small anterodorsal projection and two tubercles situated posteriorly and ventrally. However, Franklinella has a ribbed ornament and a nearly circular outline very different from the elongated bean shape of S. insolita gen. et sp. nov.

The biggest problem with the entomozoid assignment is that Sineruga lacks the typical external ribbed ornament characteristic of the entomozoaceans (see Gooday 1983). However, when Barrande (1872) described the first known entomozoid “ Entomis migrans ” (now known as Richteria migrans ), he included in this genus three smooth species that clearly belong to the entomozoaceans (see details in Perrier et al. 2007). Their carapaces are smooth, bean shaped with a more or less developed adductorial sulcus, and one species bears an anterior tubercle. Other smooth species were described as Entomis by Canavari (1900; Ludlow, Sardinia). Within these new Canavari (1900) forms, Perrier et al. (2007) suggested that six of these non−ribbed taxa should be included in the entomozoaceans (see also Gnoli et al. 2009). Among the smooth forms described by Barrande (1872) and Canavari (1900) several poorly preserved specimens may have lost their external ornament. However, some specimens clearly show an unornamented carapace.

The carapace of Sineruga insolita gen. et sp. nov. also resembles that of Colymbosathon ecplecticos (Wenlock of England; Siveter et al. 2003) in its general outline and shares with this species the possession of a deep dorsal sulcus. However, S. insolita gen. et sp. nov. has a much longer S−shaped adductorial sulcus that reaches the anteroventral margin, two tubercles located both ventrally and posteriorly ( Colymbosathon has only an eye tubercle), and a less prominently developed anterior lobe. C. ecplecticos was described with its soft parts and placed within the Cylindroleberididae (Myodocopa) . In the absence of preserved soft parts the author cannot be precise with the assignment of S. insolita , however its general outline shows many similarities with Richteria migrans and herein, S. insolita is placed within the Entomozoidae where it possibly deserves its own subfamily. Perrier et al. (2007) showed that R. migrans has a very similar valve outline and lobal/sulcal morphology to that of C. ecplecticos . Moreover, these two taxa lack a rostrum and a rostral incisure. These authors suggested that entomozoaceans may have had strong affinities with myodocopes and perhaps Cylindroleberididae . The same suggestion can be made for Sineruga gen. nov. Stratigraphic and geographic range.—Silurian (late Wenlock to early Pridoli Series), Armorican Massif ( France).

Kingdom

Animalia

Phylum

Arthropoda

Class

Ostracoda

Family

Entomozoidae

Genus

Sineruga

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