Watsonacanthus costatus, Valiukevičius, 2003
publication ID |
https://doi.org/ 10.5281/zenodo.4665088 |
persistent identifier |
https://treatment.plazi.org/id/586B87E1-FFB1-FFBE-FF2C-F3386ACFC17A |
treatment provided by |
Felipe |
scientific name |
Watsonacanthus costatus |
status |
sp. nov. |
Watsonacanthus costatus n. sp. ( Figs 23 View FIG G-K; 32)
Watsonacanthus oervigi Sobolev, Karatajute-Talimaa & Valiukevicius, 1988 : pl. 1, figs 12, 13. — Valiukevičius 1994: 165, pl. 22, figs 1-5, text-figs 75.5, 76.1-4; 1995a: 394, 397, text-figs 2, 4, 6.
HOLOTYPE. — LIG 35-2074. Scale ( Fig. 23K View FIG ). October Revolution Island, Spokojnaya River, outcrop 48, bed 5.
PARATYPES. — LIG 35-1967, 2140, 1422, 1993: scales ( Fig. 23 View FIG G-J).
ETYMOLOGY. — From Costatus (Latin): ridged, with reference to the crown ornamentation.
MATERIAL EXAMINED. — 35 scales.
LOCALITY AND AGE. — October Revolution Island: Matusevich River, outcrop 5, bed 55; Spokojnaya River, outcrop 48, beds 5-7 and outcrop 49, bed 11. Pioneer Island: samples P-9-1 and 10-1. Lower Devonian, Emsian, lower Al’banov Subformation of the October Revolution Island and supposed age analogues of the Rusanov Formation on the Pioneer Island (Member 8).
DIAGNOSIS. — Watsonacanthus with scales ornamented by three to six sharp radial ridges pointing posteriorly or converging at crown midlength. Neck low, base massive, strongly anteriorly protruding crown. Scale crown composed of simple mesodentine network without principal canal branches and lacunae (anterior part, primordial lamella included), and dentine containing long ascending and radial vascular canals (posterior part). Base bone lowly cellular.
DESCRIPTION
Species described from isolated scales. Small and medium-sized scales with crown length of 0.4- 0.8 mm, dominate. Rare examples exceed 1 mm. Crown is of a rhombic, rarely elongated-rhombic ( Fig. 23H View FIG ) form, flat. Maximum elongated crowns overhang bases posteriorly. Three to six sharp radial ridges, highered anteriorly and gradually lowered, may point at the posterior edge or converge at the crown midlength. Their anterior transverse sections make characteristic triangle forms. Base massive, rhombic in outline, anteriorly vaulted and strongly protruding crown. Neck low.
Maximum six lamellae of superpositional growth in crown composed of simple networked mesodentine (anterior part, including primordial lamella) and dentine (posterior part). Mesodentine without principal branches of canals ( Fig. 32B, C View FIG ) and without lacunae. Rare osteocyte spaces observed only in primordial lamella ( Fig. 32A View FIG ). Posterior crown part penetrated by long widened ascending canals with numerous smaller side branches. For this of dentine composed part characteristic also long, multibranched radial vascular canals displaced at the junction strip between base and crown ( Fig. 32B, C View FIG ). Extremely thin-lamellar base bone includes small numbers of osteocytes.
DISCUSSION
Detailed study of Watsonacanthus scales from Tajmyr and Severnaya Zemlya has led to a final opinion assigning them to separate species differing from W. oervigi of Spitsbergen ( Valiukevičius 1979). W. costatus n. sp. has essentially higher, sharper and mostly longer crown ridges. W. oervigi differs both by its crown and base tissue structure. Simple networked mesodentine lacking main vascular canals composes entirely three to four growth lamellae in crown of W. oervigi . It includes osteocytes ( Valiukevičius 1994: text-fig. 75.5). Dentine-type tissue has not been observed. Scales from Tajmyr are identical in their morphological features to those of Severnaya Zemlya, but they differ in their crown mesodentine structure, which exhibits lacunae and osteocytes in the earliest growth lamellae ( Valiukevičius 1994: text-fig. 76.1-4). Stranggewebe is developed in very restricted area. W. sibiricus scales ( Valiukevičius 1994: pl. 22, figs 7, 8) differ from the species under consideration by their tiny size and the flatness of scales, ornamented by a pair of short medial ridges and two pairs of longer lateral ones almost reaching the posterior edge, but with no posterior point.
BIOSTRATIGRAPHIC SIGNIFICANCE
Index species among the acanthodian assemblage. It allows to distinguish on Severnaya Zemlya Archipelago the early Emsian beds with Watsonacanthus costatus n. sp. (lower Al’banov Subformation on October Revolution and Pioneer islands and Member 8, supposed Rusanov Formation on the Pioneer Island). In Tajmyr (Dolgan beds, formerly Favosites regularissimus Zone ) and Timan-Pechora (Varandei Formation) regions – index species for the nominate acanthodian Zone (earlier W. oervigi ; Valiukevičius 1995a: text-figs 2-6). It corresponds on Pioneer Island to dehiscens-inversus and in Tajmyr to gronbergi-inversus zones of the standard conodont scale.
Order DIPLACANTHIFORMES Berg, 1940
Acanthodian fishes having scales of the “ Diplacanthus ” - type histological structure ( Valiukevičius 1985, 1995b).
Family DIPLACANTHIDAE Woodward, 1891 Genus Diplacanthus Agassiz, 1844
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
Kingdom |
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Phylum |
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Class |
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Genus |
Watsonacanthus costatus
Valiukevičius, Juozas 2003 |
Watsonacanthus oervigi
Sobolev, Karatajute-Talimaa & Valiukevicius 1988 |