Arabosteus variabilis, Olive & Goujet & Lelièvre & Janjou, 2011

Olive, Sébastien, Goujet, Daniel, Lelièvre, Hervé & Janjou, Dominique, 2011, A new Placoderm fish (Acanthothoraci) from the Early Devonian Jauf Formation (Saudi Arabia), Geodiversitas 33 (3), pp. 393-409 : 398-408

publication ID

https://doi.org/ 10.5252/g2011n3a1

persistent identifier

https://treatment.plazi.org/id/B53A87BD-FFB9-6A5C-BD86-24C9F02BFE70

treatment provided by

Marcus

scientific name

Arabosteus variabilis
status

sp. nov.

Arabosteus variabilis n. sp. ( Figs 2-8 View FIG View FIG View FIG View FIG View FIG View FIG View FIG )

Acanthothoraci gen. and sp. indet. – Lelièvre et al. 1994: figs 2.8, 2.9; 1999: figs 4, 5.

HOLOTYPE. — MNHN.F.1992-6-132 ( Figs 3A, B View FIG ; 5 View FIG ; 6 View FIG ).

OTHER MATERIAL EXAMINED. — Skull material: MNHN.F.1992-6-133 ( Fig. 3C, D View FIG ); 134 ( Fig. 2A, B View FIG ); 135 ( Fig. 2C, D View FIG ); 136 ( Fig. 8 View FIG ); 137 ( Fig. 4B View FIG ); 138 ( Fig. 4A View FIG ); 139 ( Figs 4C View FIG ; 7 View FIG ).

Several other separate elements have been recognized among the material, namely two possible synarcual ossifications, and two partial post-branchial parts of the body armour (partial IL and AL plates). They may be assigned to the same taxon according to their characteristic ornamentation. In the same sample, numerous isolated scales with the same ornamentation, have been isolated by acid etching.

ETYMOLOGY. — variabilis in reference to the variable skull roof pattern present on this taxon.

TYPE LOCALITY. — Al Huj section, Al Qalibah area, Saudi Arabia .

TYPE HORIZON. — Qasr Limestone Member of the Jauf Formation.

DIAGNOSIS. — A small taxon of which the skull measures about 40 mm in length. Dermal skull roof covered with non-stellate elongate oval tubercles.Very long nuchal plate tapering to the front and meeting the preorbital plates. Supraorbital sensory line grooves extending posteriorly onto the nuchal plate. Presence of a supernumerary plate named posterior central, on several specimens, between the central and the medial paranuchal plates. Absence of the central sensory line.

REMARKS

All the characters of the previous diagnosis, except the size, distinguish Arabosteus variabilis n. gen., n. sp. from all other acanthothoracids.

In the Jauf Formation, another placoderm has been described: Nefudina qalibahensis Lelièvre, Janvier, Janjou & Halawani, 1995 . It is assigned to the rhenanids and differs considerably from A. variabilis n. gen., n. sp. by the size of the skull, the endocranium organization and its older stratigraphical position (Hammamiyat Member, Early Emsian).

DESCRIPTION

Skull roof

The studied material of Arabosteus variabilis n. gen., n. sp. includes eight partially preserved skulls with maximum length about 40 mm and maximum width about 30 mm. Two specimens consist of an almost complete dermal skull roof ( MNHN.F.1992-6-132 [ Fig. 3A, B View FIG ] and 134 [ Fig. 2A, B View FIG ]) and the six remaining ones ( MNHN.F.1992-6-133 [ Fig. 3C, D View FIG ]; 135 [ Fig. 2C, D View FIG ]; 136 [ Fig. 8 View FIG ]; 137 [ Fig. 4B View FIG ]; 138 [ Fig. 4A View FIG ]; 139 [ Fig. 4C View FIG ]) are fragments. The borders and limits of the Saudi Arabian skull roof plates are clearly exposed, in particular on specimens that have been partially eroded.Two suture patterns are observed. The first, type A ( MNHN.F.1992-6-134 [ Fig. 2A, B View FIG ]; 135 [ Fig. 2C, D View FIG ]) shows two kinds of central plates (central plate [Ce] and posterior central plate [PtC]) ; in the second, type B, only one central plate (Ce) ( MNHN.F.1992-6-132 [ Fig. 3A, B View FIG ]; 133 [ Fig. 3C, D View FIG ]; 137 [ Fig. 4B View FIG ]; 138 [ Fig. 4A View FIG ]) .

The two different patterns could be interpreted as indicating different taxa. This hypothesis is not considered here because, given the information at hand, too many similarities exist in all the other anatomical skull features in the studied specimens. Therefore our best hypothesis is to consider all of them as belonging to a single species. The discovery of a specimen showing a mixed dissymmetrical pattern of the skull roof plates would be a proof against an interpretation of two different taxa.

The preorbital plates (Pro) are polygonal in shape, as wide as long and contact each other along the symmetry axis. They have the same size in both type A and type B skulls. Posteriorly they contact the nuchal plate along a sinusoidal suture. The supraorbital sensory line grooves (soc) pass right across the preorbitals, extending to the anterior third of the nuchal plate (Nu). The elongate nuchal plate separating the paired central plates is longer than that of other described Acanthothoraci (e.g., Romundina stellina Orvig, 1975 ). This special feature also occurs in some arthrodires like Baringaspis dineleyi Miles, 1973 and Proaethaspis ohioensis Denison, 1960 , but these forms lack the extension of the supraorbital sensory grooves onto the nuchal plate seen in A. variabilis n. gen., n. sp.

The postorbital plates (Pto) are about half the size of the preorbital ones. The main lateral sensory line groove (lc) crosses the plate to reach the lateral angle of the orbit. The main lateral sensory line groove is not distinguishable from the infra orbital canal since the central sensory line groove, which in most placoderm skulls marks the contact between both lines ( Denison 1978: 33, fig. 22), is not present on any specimen of Arabosteus n. gen.

The central plates (Ce) are quite elongate. The central plate of type B specimens covers, in length, almost half of the skull roof. In the type A, it covers only one third of it. Central plates are separated by an anterior extension of the nuchal plate. On the well-preserved external surface (specimens MNHN.F.1992-6-132 and 134; Figs 2A, B View FIG ; 3A, B View FIG ), the central plates bear distinctly the middle pit line (mpl) and the anterior part of the posterior pit line (ppl.a) .

The endolymphatic duct (d.end) opens in a small pit at the radiation center of a separate plate that occupies the position of a medial paranuchal plate, as named here (Pan.m). The implications in reference to other groups of placoderms, where this plate has been given various names, will be discussed later. This plate also carries the posterior branch of the posterior pit-line (ppl.p). On specimen MNHN.F.1992-6-134 ( Fig. 2B View FIG ), the medial paranuchal plate forms part of the posterior margin of the skull. On the other specimens (MNHN.F.1992-6-132, 133, 135; Figs 2D View FIG ; 3B, D View FIG ) the nuchal contacts the posterior paranuchal and excludes the medial paranuchal plate from the skull margin.

The anterior paranuchal plate (Pan.a) carries the confluence between the main lateral sensory line groove and the posterior part of the posterior pit line. Specimen MNHN.F.1992-6-132 ( Fig. 3A, B View FIG ) shows an interesting variation in the posterior pit line observation. The skull roof surface is not eroded on the left side and there is no visible external contact between this line and the main sensory line groove. The same region on the right side of specimen MNHN.F.1992-6-132 is broken. The break exposes this junction underneath the skull roof surface. A duct, within the bone, extends the posterior part of the posterior pit line to contact the main lateral line groove. Otherwise, on the lateral borders of the skull roof, some specimens present a postmarginal sensory line canal (pmc) on the lateral part of the anterior paranuchal (MNHN.F.1992-6-133 and 134; Figs 2B View FIG ; 3D View FIG ). This canal has not been observed on the other specimens.

The posterior paranuchal plate (Pan.p) forms the postero-lateral border of the skull roof, and bears the posterior part of the main lateral sensory line groove. This plate also carries the articular joint with the body armour, observable on the internal side (d.art; Figs 5 View FIG ; 6 View FIG ).

A pair of posterior central plates (PtC) characterizes the type A pattern. Those plates are located between the central plates and the medial paranuchal plates. The posterior central plates are hexagonal in shape and bear no grooves nor pit lines ( Fig. 2B, D View FIG ). Skull measurements indicate that these plates, when present, occupy space otherwise filled by a larger central plate. In fact, on specimen MNHN.F.1992-6-132, showing the type B pattern ( Fig. 3A, B View FIG ), the ratio “central plate length/skull medial length” is about 0.5 whereas on specimen MNHN.F.1992-6-134, showing the type A pattern ( Fig. 2A, B View FIG ) this ratio is about 0.3. In both specimens, the ratio “medial paranuchal plate length/ skull medial length” is approximately 0.25.

The marginal plate (Mg) is found between the postorbital to the anterior, and the anterior paranuchal to the posterior. It has mesial contact with the posterior part of the central plate and the anterior part of the posterior central plate on those specimens with the latter plate ( Fig. 2B, D View FIG ). Otherwise it is in mesial contact with the central plate along its length ( Fig. 3B, D View FIG ). The shape of the marginal plate is variable and has a different role concerning the lateral margin of the skull roof. On specimen MNHN.F.1992-6-134 ( Fig. 2B View FIG ), it is almost excluded from the lateral margin of the skull whereas it is completely excluded on the right side of the specimen MNHN.F.1992-6-132 ( Fig. 3B View FIG ). For this specimen, the right lateral margin is therefore composed of the postorbital, anterior paranuchal and posterior paranuchal plate margins. The left lateral margin comprises one more plate with the presence of the marginal that occupies moreover a large part of it.

The endocranium

The endocranium has been partially preserved and prepared on four specimens:all (MNHN.F.1992-6-132, 137-139) show the orbital cavity on one or both sides ( Fig. 7 View FIG ) and two (MNHN.F.1992-6-132, 138) exhibit the occipital region ( Fig. 6 View FIG ). One of them (MNHN.F.1992-6-132) has been more extensively prepared and shows an important part of the endocranium in ventral view ( Fig. 5 View FIG ). The anterior part of the endocranium is never preserved in front of the optic nerve groove. A perichondral lining demonstrates the presence of the classic optic fissure observed in many placoderms and interpreted as a primitive feature among gnathostomes ( Goujet 1984a, b; Young 1986). The ventral preorbital extension of the endocranium in other acanthothoracids supports the premedian plate. Neither this element of the dermal skull roof nor the rostral capsule has been recovered for Arabosteus variabilis n. gen., n. sp. Specimen MNHN.F.1992-6-132, with the most complete endocranial preservation, will serve as the basis for the present description ( Fig. 5 View FIG ).

The specimen is ventrally incomplete with the ventral surface missing except in its most posterior part ( Fig. 5 View FIG ), which shows the paired short glenoid condyles, on which a synarcual was presumably in contact with the articular surfaces ( Fig. 6 View FIG ).

The endocranium ( Fig. 5 View FIG ) is composed of a central body bearing paired lateral processes. These processes are disposed like in Romundina Orvig, 1975 and in “dolichothoracid” arthrodires (cf. Dicksonosteus Goujet, 1984 [ Goujet 1984a: figs 4; 6] and Kujdanowiaspis Stensiö, 1942 cf. Stensiö 1963). From front to back, the anterior postorbital process (pr.apo) is relatively wide; on the anterior face, at the end of the left process, opens the canal for the hyomandibular branch of the facial nerve (VII hm), the same disposition as in actinolepid arthrodires ( Stensiö 1969; Goujet 1984a) and other Acanthothoraci . On both sides, the processes have been eroded and the articular facet for the epihyal is not preserved.

The bifid posterolateral process (pr.ppo) is situated at the posterior third of the endocranium. Both branches are narrow and quite high, separated by a deep depression at the end of which opens a small foramen for the first branch of the vagus nerve (X 1). The main part of this nerve exits the endocranium in the peribranchial fossa (fo.pbr), which lies behind the posterior branch of the posterior postorbital process and in front of a narrow and elongate crest. This crest is assumed homologous to the supravagal process (pr.sv) of other groups of placoderms.

Dorsal to this crest is a deep depression, probably corresponding to a muscular cavity (m.o.fo, Figs 3B View FIG ; 6 View FIG ). It profoundly hollows the occipital face of the skull on both sides of a blunt median ridge leading to a triangular opening that corresponds to the cerebral cavity (c.e) just above a round aperture of the endocranial notochordal cavity (c.c) ( Fig. 6 View FIG ). The

B

occipital depressions may be homologous with the large cavities that are behind the supravagal process in petalichthyids (see Young 1978: fig. 4, where this cavity is called “cucullaris fossa”).

The canal for the jugular vein (cv.ju) is partially preserved ( Fig. 5 View FIG ) in the lateral part of the endocranium. Its path is more completely observable on the right hand side on the ventral view of specimen. It starts from the peribranchial chamber, at the root of the posterior branch of the posterior postorbital process. It is partially open behind the anterior postorbital process and crosses the process through a canal that opens in the posterior wall of the orbit. The exact extent of the groove is difficult to evaluate given the degree of ventral erosion of the endocranial body in its anterior half.

On the left side of the ventral view of specimen, two narrow and short lateral tubes (v.hm) starting from the jugular canal and opening on the lateral wall of the endocranium just behind the anterior postorbital process may represent tributaries for the hyoid arch drainage. Similar canals occur on the other side but are more difficult to represent.

IV V 1

III p

c. v.pit

Like in actinolepid and phlyctaeniid arthrodires ( Goujet 1984a), the glossopharyngeus nerve canal (IX) opens just under the jugular canal closely in front of the root of the anterior branch of the posterior postorbital process.On specimen MNHN.F.1992-6-132, it opens with two foramina observable only on the left side of the ventral view.

The front part of the endocranium is very incomplete on specimen MNHN.F.1992-6-132 but it has been prepared in lateral view in two better-preserved specimens (MNHN.F.1992-6-138, 139; Fig. 7 View FIG ). In both lateral and ventral views, a striking feature is the large diameter of the pituitary vein canal ( Fig. 7 View FIG , c. v.pit ) that connects both orbits behind a narrow prong corresponding to the interorbital wall, behind the optic nerve groove ( Fig. 7B View FIG , II). In specimen MNHN.F.1992-6-132 ( Fig. 5 View FIG ), given the ventral erosion of the endocranial body, it opens ventrally but in other specimens (MNHN.F.1992-6-138, 139; Fig. 7 View FIG ) it is still complete. Based on a difference with Romundina and arthrodires, where the canal remains relatively narrow, this large diameter could indicate that it may not be a passage for a simple vein but more likely a communication between two major orbital venous sinuses.

In front of this pituitary canal is the large oval eyestalk ( Fig.7 View FIG , eys), which opens ventrally. This is the result of a lack in all specimens of perichondral lining observed under the entire orbital endocranial area. This absence may be due either to the preservation conditions or to mechanical weathering prior to fossilization.

The eyestalk is surrounded dorsally by the myodome (my3) in which opens the oculomotor nerve canal (III). A posterior branch (III p) opens through the eyestalk base, just at the margin of the pituitary canal (c. v.pit ). In front of the eyestalk, the perichondral lining delimits dorsally the hind wall of the optic fissure and shows two clear embayments: ventrally for the optic nerve (II) and dorsally by the groove for the anterior cerebral vein (a.c.v). Such a pattern exists in the anterior end of the posterior endocranial ossification in all “loose nose” placoderms. In front was presumably a separate rostronasal ossification but this has not been recovered in our material.

Given this preservation in all our specimens, it is evident that, like Romundina and unlike Radotina Gross, 1950 and Kosoraspis Gross, 1959 ( Gross 1959: fig. 1), a separate rostral capsule sat in front of the post-rostral ossification in A. variabilis n. gen., n. sp.

Partial preparation of the internal structures ( Fig. 5 View FIG ) displays part of the encephalic cavity in the rhombencephalic region, and remains of both internal ear cavities with the canal for the acoustic nerve leading to them. The sacculus (sac) is very large relative to the space for the recessus utriculi (ru). The semicircular canals have not been observed. The external (horizontal) canal should be located between the lateral endocranial wall and the sacculus. On the left side of the holotype, it was probably lost due to erosion. On the right side, it is not evident. The original endocranial wall has been intentionally preserved during the mechanical preparation in order to maintain some important anatomical features. Possibly the external semicircular canal was located more dorsally. A CT scan would be necessary to determine its position.

The base of the left labyrinth cavity on left side of the ventral view ( Fig. 5 View FIG ) has been prepared, leaving the clear contour of the structure lined with perichondral bone. The posterior part shows two lobes continuous with the sacculus wall. These lobes may represent a section of the glossopharyngeus canal, which in many fish crosses at the bottom of the sacculus to exit laterally.

On the anterior right side of the ventral view ( Fig.5 View FIG ), the root of the trigemino-facial duct (V+VII) has been prepared; a narrow tube separated from this wide space to exit in the orbit in a small deep cavity, postero-ventrally to the pituitary vein canal, is observable. This tube corresponds to the passage of the abducens nerve (VI) and exits in a myodome (my6) most probably for the external rectus eye muscle ( Goujet & Young 2004; Young 2008).

Dermal ornamentation

Except on specimens MNHN.F.1992-6-133 and 135 that are superficially weathered, all the dermal skull roofs bear smooth oval and elongate tubercles (specimen MNHN.F.1992-6-136; Fig. 8 View FIG ) with variable sizes (from about 0.16 to 0.8 mm). The tubercles are randomly distributed and do not follow the pattern of plates contrary to the condition in many other placoderms, e.g., Dicksonosteus ( Goujet 1984a: pl. 2, fig. 2). This differs from other Acanthothoraci where stellate tubercles are present. However, a different ornamentation occurs also in Brindabellaspis Young, 1980 consisting of flattened roundish or angular tubercles ( Young 1980: pl. 1; figs 1, 3, 4, 8). In Arabosteus n. gen., the ornamentation, even if it resembles Brindabellaspis is nevertheless clearly different; the tubercles are not flattened.We do not consider the gross resemblance in the ornamentation sufficient to assign it to the “ Brindabellaspidae ” Gardiner, 1993. The other anatomical features are close to the Palaeacanthaspidae and, at present, we provisionally assign Arabosteus variabilis n. gen., n. sp. to this family.

DISCUSSION

Arthrodira were among the first described representatives of placoderms ( Agassiz 1833 -1844; Pander 1857) and their skull roof organization was traditionally used as a reference regarding the dermal skull roof pattern in other groups of placoderms. Some problems arising from using arthrodiran plate terminology to apply to a group such as acanthothoracids are discussed below.

The first point of discussion concerns the paranuchal complex. Arthrodira have only one paranuchal plate ( Fig. 9A View FIG ) but Petalichthyida have two (posterior and anterior; Fig. 9B View FIG ). The homology between these plates has been a source of debate ( Westoll 1967). The single arthrodiran plate and the petalichthyid anterior plate are both characterized by the confluence between the main lateral sensory line groove and the posterior pit line also named posterior part of the posterior pit line by Goujet (1984a), as well as the presence of the endolymphatic pore ( Goujet 1984b).

Definitions of paranuchal plates given by authors are relevant for Arthrodira but less useful for Acanthothoraci ( Westoll 1967; Denison 1978). Denison’s (1978) interpretation of paranuchal plates as the plates crossed by the main lateral sensory line groove and by the posterior part of the posterior pit line is relevant for Arthrodira , which have only one paranuchal but ambiguous for instance for Acanthothoraci , which present a different paranuchal complex.

In published Acanthothoraci specimens, one pair of anterior and one pair of posterior paranuchal plates are present, when identified ( Denison 1978: fig. 22). The endolymphatic pore opens, in some Acanthothoraci like Romundina stellina on a separate plate. This plate was interpreted as a medial paranuchal plate by Orvig (1975) and Goujet & Young (2004) ( Fig. 9C View FIG ) and as a second central (Ce2) by Denison (1978).

Arabosteus variabilis n. gen., n. sp. presents a similar paranuchal plate pattern to Romundina stellina . The posterior paranuchal plate is only crossed by the main lateral sensory line groove like in Romundina stellina and Lunaspis broilii Gross, 1937 . The name “posterior paranuchal” is then kept for the same plate in the Saudi taxon. Therefore, the posterior paranuchal would be characterized by the presence of the main sensory line groove, by its posterior marginal position and its articular joint with the body armor. In A. variabilis n. gen., n. sp., the plate anterior to the posterior paranuchal plate bears the confluence of the main lateral sensory line groove and the posterior pit line. This plate does not enclose the endolymphatic duct opening. Contrary to Arthrodira and Petalichthyida , there is not a single plate bearing the confluence and the duct opening, but each occurs on different plates: an anterior paranuchal characterized by the groove confluence and a medial paranuchal plate by the endolymphatic foramen and adjoining the paranuchals. This is also the case in Romundina stellina . The medial paranuchal plate could be named “endolymphatic plate” in order to highlight its characteristics and this terminology could be used as well in other acanthothoracids for the homologous structure (e.g., R. stellina ; Fig. 9C View FIG ). The position of the endolymphatic pore is very variable. For example in Antiarchi or Petalichthyida ( Denison 1978) it can be very close to the median line and in Arthrodira postero-lateral near the cephalic-lateral line, between the posterior pit-line posterior part and the occipital line ( Stensiö 1963; Goujet 1984b). Therefore, we prefer to keep the traditional plate nomenclature, generally connected with a strict positional situation of the different plates. Denison’s (1978) interpretation of this plate, as a second central, has less justification than as a medial paranuchal plate because the plate appears as a component of the paranuchal complex. Based on this interpretation, the hypotheses of fusion-fragmentation of dermal skull roof components in various placoderm groups can be discussed.

Regarding the paranuchal complex, two different processes can be invoked to interpret the pattern existing in other placoderm groups. An assumption of bone fusion process would imply that acanthothoracids are a “primitive” condition with the arthrodiran paranuchal formed by fusion of the three plates identified in A. variabilis n. gen., n. sp. If bone fragmentation is the model, then the anterior, posterior and medial paranuchal plates of Arabosteus n. gen. would be interpreted as derived and the single arthrodiran paranuchal as primitive.

In both cases, the pattern in Petalichthyida would be an intermediate condition.

A second remark concerns the anterior paranuchal plate versus the marginal plate. Traditionally, the marginal plate is defined in arthrodires as the skull component bearing the main lateral sensory line groove and the postmarginal sensory line groove ( Goujet 1984a: 102).

On some specimens of Arabosteus variabilis n. gen., n. sp. (specimens MNHN.F.1992-6-133 and 134; Figs 2A, B View FIG ; 3C, D View FIG ), the postmarginal sensory line groove is observable on the marginal part of the plate previously identified as an anterior paranuchal plate. Thus, that plate could also be named the marginal plate. It can be noted that the post-marginal sensory line groove of A. variabilis n. gen., n. sp. is inserted into the bone. Therefore, it should be better called “post-marginal canal”, even if it sometimes opens along a continuous slit.

This canal is not observable or present on that plate in some other Saudi specimens (MNHN.F.1992-6-132 and135; Figs 2C, D View FIG ; 3A, B View FIG ). Thus, the identification as a “marginal plate” is not obvious. Additionally, it contacts medially the medial paranuchal plate and the posterior paranuchal plate posteriorly. Therefore it belongs to the paranuchal complex and may also correspond to the anterior paranuchal plate. It also bears the confluence between the main sensory line groove and the posterior part of the posterior pit line, a characteristic for a paranuchal plate.

Thus, the lateral line system on its own is ambiguous for deciding bone homology and terminology (Graham-Smith 1978). This plate could be either called marginal plate or anterior paranuchal plate depending on the chosen reference system.

In the present work, we use the term “anterior paranuchal”. This interpretation is based on 1) the position of the confluence between the main sensory line groove and the posterior part of the posterior pit line, which seems to be a constant characteristic among placoderms, and 2) the position of the plate as part of the paranuchal complex. Therefore, the presence of the postmarginal canal is not used to characterize the marginal plate. This feature is used in arthrodires, but does not seem presently relevant for the establishment of homologies in acanthothoracids given its instability.

MNHN

Museum National d'Histoire Naturelle

Kingdom

Animalia

Phylum

Chordata

Class

Placodermi

Order

Acanthothoraci

Family

Palaeacanthaspidae

Genus

Arabosteus

Loc

Arabosteus variabilis

Olive, Sébastien, Goujet, Daniel, Lelièvre, Hervé & Janjou, Dominique 2011
2011
Loc

Arabosteus variabilis

Olive & Goujet & Lelièvre & Janjou 2011
2011
Loc

A. variabilis

Olive & Goujet & Lelièvre & Janjou 2011
2011
Loc

A. variabilis

Olive & Goujet & Lelièvre & Janjou 2011
2011
Loc

Arabosteus

Olive & Goujet & Lelièvre & Janjou 2011
2011
Loc

Romundina stellina

Orvig 1975
1975
Loc

Romundina stellina

Orvig 1975
1975
Loc

Romundina stellina

Orvig 1975
1975
Loc

R. stellina

Orvig 1975
1975
Loc

Romundina stellina

Orvig 1975
1975
Loc

Simblaspis cachensis

Denison 1958
1958
Loc

Lunaspis broilii

Gross 1937
1937
Loc

Lunaspis broilii

Gross 1937
1937
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