Nikolivia aligera, Karatajūtē-Talimaa, 2002

Karatajūtē-Talimaa, Valentina N., 2002, Lower Devonian (Lochkovian) thelodonts from October Revolution Island (Severnaya Zemlya Archipelago, Russia), Geodiversitas 24 (4), pp. 791-804 : 799-802

publication ID

https://doi.org/ 10.5281/zenodo.4664989

persistent identifier

https://treatment.plazi.org/id/039287C5-FFA3-FFBA-FEE9-FE6C667FFB16

treatment provided by

Felipe

scientific name

Nikolivia aligera
status

sp. nov.

Nikolivia aligera n. sp. ( Fig. 6 View FIG )

HOLOTYPE. — Transitional(?) scale (LIG 35-474) ( Fig. 6H View FIG ).

ETYMOLOGY. — Aligera (Latin): containing wings.

TYPE LOCALITY AND HORIZON. — Sample 4-3 (outcrop 4, bed 3) from the Matusevich River, October Revolution Island, Pod”emnaya Fm., Lochkovian, Lower Devonian.

MATERIAL EXAMINED. — About 80 scales well-preserved.

OCCURRENCE. — N. aligera n. sp. scales are identified only from a single sample (outcrop 4, bed 3) along the Matusevich River (October Revolution Island), Lower Devonian, Lochkovian, Pod’’emnaya Fm.

DIAGNOSIS. — Small and medium-sized scales (0.3- 1.3 mm long). Head scales smaller (0.3-0.5 mm), with high, spine-like crown, composed of concave central area and one to two pairs of laterals. Transitional scales comparatively small (0.4-0.7 mm). Crown consists of widened central area and wing-like laterals. Trunk scales the largest (0.8-1.3 mm), drop-shared or keel-like. Crown composed of wide central area with smooth surface and pair of narrowed laterals (type A), or of narrow groove-like central and one to two pairs of laterals (type B). Base of transitional and trunk scales of type A low, roller-like, displaced anteriorly. Keel-like trunk scales of type B with more convex and higher base.

DESCRIPTION

Division of scales into head and transitional types is rather conventional ( Fig. 6 View FIG A-M, O, Q). Head scales smaller, with higher, sometimes spine-like crown ( Fig. 6 View FIG A-E) and upward sloping distal area. Crown composed of central area and one or two pairs of laterals, sometimes widened and wing-like ( Fig. 6A View FIG ). Crowns of transitional scales distinguished by wing-like lateral areas with sometimes notched margins. Central area keel-like, somewhat highered, with smooth surface and usually not prolonged to the crown edge ( Fig. 6 View FIG F-M, O, Q).

As typical trunk scales are recognized large drop- or keel-like examples (type A) with central area having wide, flat and smooth surface ( Fig. 6N View FIG , U-Y). Narrow keel-like scales ( Fig. 6U, V, Y View FIG ), probably covered the tail area and fins. To type B are conventionally attributed trunk scales with more complicated ridged crowns, having narrow, central area. Lateral areas are not always strongly symmetric and may consist of one pair of widened or several pairs of narrowed members ( Fig. 6P View FIG , R-T).

Bases of scales of all types anteriorly vaulted, low, roller-like and only in keel-like variety reaching a larger height. Pulp opening comparatively large even in older scales.

COMPARISON

Scales of N. aligera n. sp. are close to scales of N. gutta Karatajūtē- Talimaa, 1978 in size. Trunk scales of type A do not differ in form from the drop-like scales of N. gutta . N. aligera n. sp. differs from all known species by presence within the morphologic set of transitional scales with wing-like lateral areas and also more distinctly recognizable head scales.

Order FURCACAUDIFORMES Wilson & Caldwell, 1998 Family FURCACAUDIDAE ? Wilson & Caldwell, 1998

Genus Canonia Vieth, 1980

TYPE SPECIES. — Canonia grossi Vieth, 1980 .

Canonia sp. cf. C. grossi Vieth, 1980 ( Figs 4 View FIG I-R; 7; 8)

OCCURRENCE. — Scales of Canonia sp. in the Lower Devonian of Severnaya Zemlya are found in samples from the outcrop 4, bed 3 at the Matusevich River and outcrop 69, bed 26 at the Pod’’emnaya River, in the middle and upper parts of the Pod”emnaya Fm., Lochkovian, Lower Devonian.

REMARKS

Vieth (1980) made the following diagnosis of Canonia grossi : small symmetric scales; distal crown area frequently three-pointed; 55% of scales have concave and raised medial area compared with laterals; lateral areas ornamented with longitudinal ridgelets (two or fewer); neck well developed, base high; 45% of scales have flattened crown surface, ornamented with foureight narrow longitudinal ridgelets, and low base; rather smooth linear dentine tubules arise only from the pulp cavity.

Concerning size and morphologic features the Severnaya Zemlya specimens insignificantly differ from the Canadian ones. More representative material (about 150 scales) was found in outcrop 4, bed 3 at the Matusevich River. A minority consist of the simplest scales – crown of smooth central and one pair of lateral areas,

dt

separated by deep longitudinal grooves ( Fig. 7A View FIG ). Small numbers of scales have more complicated crown morphology: central area slightly concave and laterals ornamented with longitudinal grooves ( Fig. 7B, C View FIG ). All scales with three distinctly separated areas have three-pointed posterior crown edge, with the central point significantly longer than the laterals ( Fig. 7C View FIG ). The majority consists of large scales (up to 0.5 mm), in which crown shape resembles a quadrangle, comparatively widen and flattened. Proximal crown margin slightly convex or linear, lateral margins linear and distal area three-pointed ( Figs 4 View FIG J-O; 7D-F). All scales of that type have developed narrow central area, flat or with longitudinal groovelet, and one to three pairs of lateral areas also narrow, ornamented with shallow longitudinal groovelets. The central area is usually separated from the laterals by deeper and wider grooves. Generally speaking, crowns of scales have well distinctive longitudinal sculpture.

The sample yielded also some scales with asymmetric crown ( Fig. 4I View FIG ), base small, displaced anteriorly ( Fig. 4 View FIG P-R), comparatively low, only rarely higher, pulp opening in all observed scales large.

Fig. 8A View FIG illustrates the extent of the pulp cavity, and also the type of dentine forming the crown ( Fig. 8 View FIG ).

Vieth (1980) described for Canonia scales characteristic smooth, linear dentine canals, arising only from the pulp cavity, and also their short branch connecting arcade tubules. Based on drawings ( Vieth 1980: text-fig. 18), they are not dominated by such linear dentine canals, but by comparatively wide and interwoven, lacuna-like structures. Tissue with dentine tubules is developed only superficially, confirmed also by our material ( Fig. 8A View FIG ).

Dentine tubules, developed in scales of Canonia sp. from Severnaya Zemlya, have a rather unusual form, not characteristic of orthodentine, forming crowns in representatives of the Nikoliviidae family ( Fig. 8 View FIG ). Short linear or slightly curved arcades of branch connect vertically upswept dentine canals. Sometimes they form small lacuna-like widenings. Similar dentine tissue is developed in scales of loganiid thelodonts and is not characteristic of representatives of order Thelodontida . At present, the attribution of the genus Canonia to family Nikoliviidae is rather doubtful.

Kingdom

Animalia

Phylum

Chordata

Class

Pteraspidomorphi

Genus

Nikolivia

Loc

Nikolivia aligera

Karatajūtē-Talimaa, Valentina N. 2002
2002
Loc

FURCACAUDIFORMES

Wilson & Caldwell 1998
1998
Loc

FURCACAUDIDAE

Wilson & Caldwell 1998
1998
Loc

Canonia

Vieth 1980
1980
Loc

Canonia

Vieth 1980
1980
Loc

C. grossi

Vieth 1980
1980
Loc

Canonia

Vieth 1980
1980
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