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A new psammosteid (Agnatha, Heterostraci) from the Amata Regional Stage of the Main Devonian Field and morpho-histological types of discrete micromeric elements in the family Psammosteidae: in memory of an outstanding palaeoichthyologist Elga Mark-Kurik.

Abstract. The range of diversity of psammosteids from the family Psammosteidae is still poorly known. Here a new species, Psammosteus ramosus sp. nov. Glinskiy, from the Amata Regional Stage of the Main Devonian Field is described. Its morphology, ornamentation, histology of exoskeletal plates, and micromeric elements are compared with those of other representatives of the family Psammosteidae. The comparison shows a close relationship of the new species with Psammosteus falcatus Obruchev, P. kiaeri Halstead Tarlo and P. pectinatus Obruchev, a group of species that is significantly different from other representatives of the genus Psammosteus and constitutes a separate evolutionary lineage. On the basis of morphological and histological features we here differentiate in the fields of tesserae of Psammosteidae the discrete micromeric elements of the 'basic type', known in Psammosteus bergi (Obruchev), P. levis Obruchev, P. livonicus Obruchev, P. maeandrinus Agassiz, P. megalopteryx (Trautschold), P. praecursor Obruchev and Karelosteus weberi Obruchev, and micromeric elements of the 'progressive type', known in Psammosteus falcatus, P. cf. kiaeri and P. ramosus sp. nov. Glinskiy.

Key words: Agnatha, Heterostraci, Psammosteida, Late Devonian, Main Devonian Field, new species.

INTRODUCTION

Psammosteids are a group of jawless vertebrates from the order Pteraspidiformes (suborder Psammosteida sensu Tarlo 1962). They are known from the Early--Late Devonian (from Pragian to Frasnian stages), primarily of Laurussia (Halstead Tarlo 1967a; Halstead 1987) and, to a lesser extent, of the peri-Gondwanan shelf, Armorica, Barentsian, Kara-Tajmyr and Siberian palaeocontinents (Bystrow 1959; Blieck et al. 2002; Delsate et al. 2004; Vaskaninova & Kraft 2016). The exoskeleton of psammosteids is composed of macromeric and mesomeric elements (plates of the cephalothorax, scales in the tail region) and micromeric elements (mostly tesserae). Discrete micromeric elements, situated between the main plates of the cephalothorax, form so-called 'fields of tesserae'. Praepineal and paired lateral fields on the dorsal surface, and postoral and ventrolateral fields on the ventral surface of the cephalothorax can be distinguished (Obruchev & Mark-Kurik 1965, p. 40). In numerous articulated specimens of Drepanaspis gemuendenensis Schluter, 1887 and in a single articulated cephalothorax of Psammosteus megalopteryx (Trautschold, 1880), fields of tesserae may be found in their original articulation (Gross 1963; Halstead Tarlo 1965, pl. XVI, figs 1, 2), but in most cases their micromeric elements are found isolated (e.g. Mark-Kurik 1999; Blom et al. 2006). As a rule, these elements can be determined to the species level (Halstead Tarlo 1965; Obruchev & Mark-Kurik 1965; Glinskiy & Mark-Kurik 2016) on the basis of species-specific tubercles.

Discrete micromeric elements in the family Psammosteidae sensu Novitskaya (2004) are the most diverse morphologically. They possess a smaller base than other psammosteids. Rooted tesserae are also weakly connected with the cancellous aspidin of the plates (Gross 1933, p. 15, fig. 4; Obruchev 1947a, p. 197; Mark-Kurik 1999, p. 7). The small base size of discrete micromeric elements in representatives of Psammosteidae results in their higher concentration in the fields of tesserae and on the plates of the cephalothorax. Our study of micromeric elements of psammosteids from Frasnian deposits of the Main Devonian Field has shown that discrete elements of the representatives of the family Psammosteidae can generally be classified into two morpho-histological types: the 'basal' and the 'progressive' ones. The aim of this research is the description of the earliest psammosteid species with a 'progressive' type of tesserae, Psammosteus ramosus sp. nov. Glinskiy, and comparative description of morphohistological types of discrete micromeric elements.

MATERIALS AND METHODS

The ornamentation of the specimens was cleaned mechanically by an instrument consisting of an air pump and a hypodermic needle (Selden 2003). The material was studied mainly under the stereo zoom microscope Leica M205 C, and also under the scanning electron microscope (SEM) Hitachi S-3400N in SE and BSE mode. The study of the inner structure of some micromeric specimens was undertaken with Bruker-microCT SkyScan 1172. Projection images were reconstructed with the software NRecon into cross section images rotated upright in the software DataViewer. The software CTAnalyzer was used to correct the visualization and interpretation of the reconstructed images. CTVox software was used for 3D volume rendering. The specimens were scanned by applying different parameters according to the sample type at a voltage of 40-100 kV and a current of 100-250 [micro]A, with a copper and aluminium filter for a half rotation of 180[degrees] at the highest camera resolution. Thin sections were made with the use of Technovit[R] EPOX Resin and Technovit[R] EPOX Hardener fast. The specimens enclosed in the epoxy resin were wet-ground on a glass slide to a needed level with the use of Mirka WPF finishing sandpaper P 120-1000. The sandpaper with a grade P 1200-2000 was used subsequently to polish a thin section. The photographs of thin section PM SPU 80-7 were taken with a polarization microscope Leica DM4500 P with the use of aniseed oil.

All specimens studied are stored in the collections of the Palaeontological Museum of St. Petersburg State University (the new taxon: PM SPU 80; material for comparison: PM SPU 71, 72, 75), St. Petersburg, Russia; Natural History Museum of Latvia (G 43), Riga, Latvia and Department of Geology, Tallinn University of Technology (GIT 680), Tallinn, Estonia.

GEOLOGICAL BACKGROUND

The material comes from two localities of the Amata Regional Stage (RS) in Northwest Russia and one locality in eastern Latvia (Fig. 1A). Most specimens (including the holotype) were found at the Andoma Hill locality on the southeastern bank of Lake Onega in the Vytegra District, Vologda Region, NW Russia (Fig. 1D). The Andoma Hill locality is represented by a series of outcrops, stretching along the lake for a couple of kilometres. Remains of Psammosteus ramosus sp. nov. Glinskiy (Fig. 2A-F, Q, R; Fig. 3A-D, I, J; Fig. 4A-G; Fig 5A; Fig. 6A-E, G, H) occur in layer AG 1-2, in the upper part of outcrop N-2 at Gnevashevskaya village (Ivanov et al. 2006). This layer is composed of red, fine and very fine, poorly cemented sandstones intercalated with thin layers of silty clay and siltstone. These deposits are assigned to the lower part of the Andoma Formation, which is correlated with the Amata-Plavinas interval (Luksevics et al. 2012). Remains of the new species were found by A. Ivanov in 1984 in association with numerous isolated branchial plates, lateral scales and various micromeric elements of Psammolepis undulata (Agassiz, 1844), Psammosteus livonicus Obruchev, 1965 (see hereinafter in Obruchev & Mark-Kurik 1965), P. praecursor Obruchev, 1947a and P. cf. cuneatus Obruchev, 1965 (Glinskiy & Ivanov 2015).

The Borschovo locality is situated in the Luga District of the Leningrad Region, NW Russia. It is represented by a series of outcrops on the south bank of Lake Antonovskoe, in the Oredezh River basin (Fig. 1C). Remains of P. ramosus sp. nov. were found in the terminal eastern outcrop 3, situated to the east of the road from Borschovo village to the lake (Fig. 2N-P; Fig. 3K, L; Fig. 4H-O). The deposits in this outcrop are represented by variegated (pink, yellowish-grey, reddish-brown to light bluish-grey), cross-bedded, medium- and fine-grained sandstones, with intercalations of purple and greenish clay. Vertebrate remains, including those of the new species, were collected by a team of Russian--French--Latvian expedition in 2010 at the level (No. 12) of light bluish-grey sandstones of the Amata RS in the middle part of the outcrop. The only branchial plate of P. ramosus sp. nov. was found in association with numerous branchial plates, dorsal plates, ridge scales and rare micromeric elements of different psammosteids (Glinskiy 2013): Psammolepis venyukovi Obruchev, 1965, Psammolepis undulata, Psammosteus livonicus, P. praecursor. The presence of P. cf. cuneatus Obruchev at the same level needs further confirmation. One of the branchial plates of P. praecursor from this assemblage was previously misdiagnosed by V. Glinskiy as that of P. levis (Ivanov et al. 2011).

The KuKu locality is situated on the right bank of the Gauja River, Raiskums parish, Pargauja municipality, eastern Latvia (Fig. 1B). In 1965 fragments of branchial plates of the new species were gathered there by L. A. Lyarskaya (Fig. 2G-M; Fig. 3E-H; Fig. 5B-F). They were previously identified as the scales of Psammosteidae indet. These remains can be found in the upper part of the outcrop in white fine-grained sandstones (at the base of the Amata RS) together with numerous branchial and median plates of Psammolepis undulata (Lyarskaya 1981).

Three positions of the boundary between the Middle and Upper Devonian in the Main Devonian Field have been proposed: at the base of the Amata RS, in the Amata RS at the base of the Podsnetogorskie Regional Beds (RB) and at the base of the Snetnaya Gora RB of the Plavinas RS (Ivanov & Lebedev 2011). The first position is accepted in the current research (Fig. 1E).

MORPHOLOGY AND TERMINOLOGY OF MICROMERIC ELEMENTS

The following morphological structures can be distinguished in the discrete and rooted micromeric elements of the family Psammosteidae sensu Novitskaya (2004): a crown, formed by one or several dentine tubercles and a base composed of cancellous aspidin (Figs 5A, G; 6A). Discrete micromeric elements are characterized also by the presence of a neck (a transitional part between a crown and a base) composed of cancellous aspidin and by a comparatively short base. Rooted tesserae are usually recognized by a missing neck, and a large base area. Crown tubercles of all micromeric elements in the representatives of Psammosteidae vary substantially in shape (dome-shaped, cone- or peak-shaped) and orientation, which can be connected with their position on the body.

Various exoskeletal elements, including micromeric elements of psammosteids, can be formed by cyclomorial or synchronomorial (also syncronomorial) growth (Orvig 1951; Halstead Tarlo 1964, p. 44). Cyclomorial elements possess a centre of growth or primordium. There is usually a primordial dentine tubercle in the superficial layer, which was formed prior to the other tubercles and around which the subsequent growth of an element took place. Main plates, scales and cyclomorial tesserae of psammosteids are characterized by cyclomorial growth. This type of growth usually manifests itself in areal (concentric) zones of growth of tubercles in the superficial layer. Cancellous and lamellar aspidin layers may also have areal zones of growth, visible on the visceral side of macromeric elements. Sometimes these zones are weakly developed, but the primordial tubercle, which gives evidence of cyclomorial growth type, can be distinguished. Synchronomorial elements are characterized by the absence of a centre of growth. Growth of the whole element is contemporaneous. The synchronomorial type of growth is characteristic of mesomeric unnamed plates, positioned on the periphery of dorsal and ventral plates and often rooted (fused) with them (Halstead Tarlo 1964, p. 44), and of some micromeric elements, such as synchronomorial tesserae and simpler complex elements (Mark-Kurik 1999, p. 16).

Discrete cyclomorial tesserae are dominant in the fields of tesserae in Drepanaspis and can also be rooted with larger median plates (Halstead Tarlo 1964, p. 44). In Schizosteus striatus (Gross, 1933), Schizosteus splendens (Eichwald, 1844) (family Guerichosteidae) and Psammolepis venyukovi Obruchev, 1965 (family Psammolepididae), the tesserae, rooted with rostral and postorbital plates are also cyclomorial and belong to praepineal and lateral fields (Obruchev & Mark-Kurik 1965). Psammosteids from the family Drepanaspididae (e.g. Drepanaspis) and Guerichosteidae (e.g. Schizosteus) possessed rooted unnamed plates and tesserae showing a synchronomorial type of growth in the vicinity and on the margins of dorsal and ventral plates (Halstead Tarlo 1964, p. 44). In the representatives of the families Psammolepididae and Psammosteidae, rooted tesserae (Obruchev & Mark-Kurik 1965, p. 49) of synchronomorial and/or cyclomorial types of growth partially or completely cover the dorsal and ventral plates. This evolutionary tendency in the psammosteid lineage is called 'advanced tesserization' (Obruchev & Mark-Kurik 1965, p. 64). Thus, in the representatives of Psammosteus it is expressed in full substitution of median plates by cyclomorial tesserae and in coverage of the most part of the ventral side of branchial plates by them.

The following morphological terms were proposed to distinguish various isolated micromeric elements of Psammosteus sp. from Givetian deposits (Burtnieki RS) of the Essi locality, Estonia: single elements, complex elements and 'tesserae' (Mark-Kurik 1999). A single element is a solitary primordial odontode (Orvig 1977), mounted on an aspidin base (Mark-Kurik 1999, p. 9). A complex element has a crown that consists of two or more primordial odontodes (Mark-Kurik 1999). In the case of simpler (basic) complex elements, the bases are fused to form one common base and developed synchronomorially (Ibid., p. 18). Mark-Kurik (1999) distinguishes one more type of complex elements. Such elements are developed cyclomorially; they have a narrow overlap area and the primordial tubercle, which is situated at their posterior margin (Ibid., pp. 16, 17). A cyclomorial platelet or 'tessera' is a polygonal element with a primordial tubercle (it can be situated concentrically or eccentrically in relation to a geometric centre of a tessera), concentrically surrounded by much smaller and simpler tubercles (Ibid., pp. 15, 16).

The terms proposed by Mark-Kurik (1999) for describing micromeric elements are used in this article. It should be noted that the term 'complex element' is used by that author to refer to several types of micromeric elements in Psammosteus, namely: (1) basic complex elements with the synchronomorial type of growth and (2) scales and scale-like elements with the cyclomorial type of growth, which probably come from the tail and the caudal part of the cephalothorax. The description of these elements is the same as that of the lateral scales of Psammosteus sp. from Givetian deposits (Burtnieki RS) of the Joosu quarry locality, Estonia (Mark-Kurik 1993). In the text below, we use the term 'complex element' to refer to the elements of the first type mentioned above.

The term 'tessera of concentric or eccentric structure' was earlier used for the description of cyclomorial tesserae (Obruchev 1947b, p. 517, 1964, p. 73; Obruchev & Mark-Kurik 1965). In Obruchev's opinion, 'concentric tesserae' possess a primordial tubercle, situated concentrically (centrally) and concentric zones of satellite tubercles (Obruchev 1947a, p. 197; Obruchev & Mark-Kurik 1965, pp. 211, 215). According to him, such tesserae are characteristic only of Psammosteus (e.g. Obruchev 1947b). He applied the term 'eccentric tesserae' in two meanings: to refer to tesserae with an offset centre of growth and to refer to those devoid of concentric lines of growth. He reckoned that they are characteristic of Psammolepis (Obruchev 1947b, 1964, p. 73; Obruchev & Mark-Kurik 1965, pp. 86, 211). However, cyclomorial tesserae with an eccentric position of a tubercle as well as concentric lines of growth are known in Psammosteus (Obruchev & Mark-Kurik 1965, p. 234; Mark-Kurik 1999, p. 16). Thus, in order to characterize cyclomorial tesserae more thoroughly, the following features must be noted: the position of the primordial tubercle (concentric, eccentric) and the presence or absence of concentric zones of growth of satellite tubercles.

On the basis of morphological and histological differences it is proposed to differentiate two types of discrete micromeric elements in the fields of tesserae in representatives of Psammosteidae sensu Novitskaya (2004): the 'basic type' and the 'progressive type'. In micromeric elements belonging to the 'basic type', tubercles are similar both in general shape and in inner structure. In the discrete tesserae of the 'basic type', the crown is formed by a primordial tubercle and satellite tubercles (Fig. 5A-C, E-G, I, J). The primordial tubercle is as a rule larger than satellite tubercles or has a comparable size. Pulp cavities of the tubercles are identical, usually hollow; rarely trabeculae of cancellous aspidin can penetrate into them (Fig. 5J, Q). Micromeric elements belonging to the 'basic type' are known in early representatives of the genus, such as Psammosteus sp. from the Early Devonian (Givetian) of Estonia (Mark-Kurik 1999, fig. 8). We assign these micromeric elements, defined by Mark-Kurik (1999) as those of Psammosteus sp., to Psammosteus bergi (Obruchev, 1943) (Fig. 5R, S). The same micromeric elements are also present in Psammosteus levis Obruchev 1965, P. livonicus Obruchev, 1965, P. maeandrinus Agassiz, 1844, P. megalopteryx (Trautschold, 1880), P. praecursor Obruchev, 1947b (Fig. 5G-Q) and also Karelosteus weberi Obruchev, 1933 (q.v. Glinskiy 2014, p. 23, fig. 1:3).

In micromeric elements belonging to the 'progressive type', the crown is formed by a large primordial tubercle (Fig. 6A-C, G, H, I-K, N, O). It is situated centrally on the top of a conical aspidin mound (neck) and covers the upper half of the neck by its long and complicated marginal crenulations (Fig. 6E, M, Q). A primordial tubercle can have one or several pulp cavities, usually filled in by aspidin trabeculae. Satellite tubercles in the tesserae belonging to the 'progressive type' can retain simple inner structure, characteristic of the 'basic type'. Discrete tesserae of 'progressive type' differ from discrete single elements by the presence of satellite tubercles, arranged in concentric zones on the neck (Fig. 6A, B, G). Often in the fossil record, elements of 'progressive type' that are devoid of dentine are found, with the remaining aspidin part represented by a conical aspidin mound (neck) and a base (Fig. 6F).

The first morphological description of discrete micromeric elements of 'progressive type' was based on the material of Psammosteus falcatus Obruchev in Gross, 1942 (Obruchev 1964, pl. 6, fig. 5; Obruchev & Mark-Kurik 1965, pp. 219, 254; Halstead Tarlo 1965, pp. 135, 137, fig. 4: C, D). The unusual shape and large sizes of these elements were noted (the height of the tesserae of P. falcatus, specimen PM SPU 75-9, can attain 7-8 mm). Micromeric elements of 'progressive type' belonging to Psammosteus falcatus, P. cf. kiaeri Halstead Tarlo, 1964, P. ramosus sp. nov. are known. Single elements and tesserae similar to them are dominant in the fields of tesserae in this psammosteid lineage.

SYSTEMATIC PALAEONTOLOGY

Class PTERASPIDOMORPHI Goodrich, 1909

Subclass HETEROSTRACI Lankester, 1868

Order PTERASPIDIFORMES Berg, 1937

Suborder PSAMMOSTEIDA Kiaer, 1932

Family PSAMMOSTEIDAE Traquair, 1896

Genus Psammosteus Agassiz, 1844

Psammosteus ramosus sp. nov. Glinskiy

Figures 2-4; 5A-F; 6A-E, G, H; 7

2015 Psammosteus sp. nov. 2, Glinskiy & Ivanov, p. 57.

Etymology. From Latin 'ramus' (branch) and 'ramosus' (full of branches), referring to the shape of marginal crenulations on dentine tubercles.

Holotype. PM SPU 80-2, fragment of the left branchial plate, Andoma Hill, southeastern bank of Lake Onega, outcrop N-2, layer AG 1-2 (Andoma Formation, Upper Devonian, Frasnian, Amata RS).

Material. Fragments of the left branchial plate: PM SPU 80-1, Borschovo, outcrop 3; PM SPU 80-2, PM SPU 80-3, Andoma Hill, outcrop N-2; G 43/292:2, KuKu outcrop. Fragment of branchial plate G 43/292:1, KuKu outcrop. Lateral (body) scale: PM SPU 80-4, Andoma Hill, outcrop N-2. Discrete tesserae: PM SPU 80-5, PM SPU 80-6, PM SPU 80-7, Andoma Hill, outcrop N-2. Thin sections: thin section of discrete tessera PM SPU 80-7, Andoma Hill, outcrop N-2; thin section of isolated tubercle PM SPU 80-8 from branchial plate PM SPU 80-1; thin section across branchial plate PM SPU 80-3.

Occurrence. Amata RS, Frasnian, Upper Devonian, Psammolepis praecursor Zone (Glinskiy 2013), Leningrad and Vologda Regions of Northwest Russia, eastern Latvia.

Diagnosis. Moderate-sized branchial plates, discrete tesserae belong to 'progressive type'. Dentine tubercles large (up to 2.6 mm in total), conical and dome-shaped; their bases mostly rounded; marginal crenulations (6-19) massive, penetrate deeply into crown and their tips may branch; flanks of crenulations along their whole length covered by large, massive ramifications; tips of crenulations and ramifications truncated; ramifications of large tubercles bear indentations on their flanks; radial ribs pass from crowns of tubercles onto their crenulations, ramifications and indentations, where they form plumose wrinkles; large microtubercles (up to 12) situated on the upper side of marginal crenulations. Ridges of tubercles better developed on the dorsal side of branchial plates.

Description

1. General morphology. Branchial plates are very short and wide or extremely stenobasal (the term first mentioned in Obruchev & Mark-Kurik 1965, pp. 134, 219). They are semicircularly expanded in width and flattened (Fig. 2A, B, G, H, N, O). The anterolateral margin is partly represented in specimen G 43/292:2 (Fig. 2G, H); it is generally convex. Straight anterolateral margin of PM SPU 80-3 is a result of lifetime abrasion (Fig. 2D, E; Fig. 3C, D). The posterior margin is concave. The distal tip of the plates is curved backwards or medially (Fig. 2A, B, N, O). Branchial plates without deformation are insignificantly dorsally convex in width (0.5 mm) (Fig. 2C, F). The distal part of the branchial plates (PM SPU 80-2) is slightly dorsally convex in length (1.4 mm from the proximal side, less than 1 mm from the distal side). The ornamented surface is developed on the distal part of the branchial plates. The area of the ornamented surface on the dorsal side is more or less equal to that on the ventral side of the plates (Fig. 3A, B, E-H, K, L) or slightly smaller (Fig. 3C, D). The boundary between the ornamented and unornamented surfaces of the branchial plates is usually distally convex. Branchial plates are of moderate sizes. The measurements of the fragments are given in Table 1.

[FIGURE 7 OMITTED]

Lateral scales have rounded margins; they are short, wide and flattened. In specimen PM SPU 80-4 the right margin is concave (Fig. 2Q, R). Ornamentation is developed in the posterior part on both sides of scales (Fig. 3I, J). On the external side the area of the ornamented surface slightly exceeds half of the total area of this side of the plate (shortened ornamented zone). The area of the anterior unornamented surface is large. On the visceral side the ornamented surface covers approximately a quarter of the total area. The length of scale PM SPU 80-4 is 6.8 mm; the width is 8.9 mm. The thickness of the plate in the unornamented part is 0.8 mm; it is 2.5 mm in the zone with ornamentation.

The micromeric elements belonging to the species are discrete tesserae (Fig. 6A-H) and rooted tessera (Fig. 5A), preserved on the ventral side of branchial plate PM SPU 80-2. Discrete tesserae of 'progressive type' have a high crown, formed by a large single primordial tubercle, a high neck and a rounded small base (Fig. 6A-D, G, H). The crown is subvertically oriented (Fig. 6A, B, G) or slanted (PM SPU 80-6). Satellite tubercles sit on the neck, forming up to two areal zones (Fig. 6A, B, G). The area of the base is equal to or slightly exceeds that of the crown. Its visceral side has a medial depression (Fig. 6D, E). The most complete specimen PM SPU 80-5 is 4.5 mm in height and 4 mm in length of the base. The rooted tesserae on the ventral side of the branchial plates are low and small (3 mm in length). Tubercles are situated concentrically; the primordial tubercle does not differ from them either in shape or in size.

2. Ornamentation. Ornamentation is represented by large tubercles with the area of the base up to 1-1.5 mm in diameter. The mean length of marginal crenulations is 0.8-1 mm, ranging in number (without their branch tips) from 6 to 19, 13-16 on average. The general size of the tubercles including the length of marginal crenulations can attain 2.6 mm in total (Fig. 4B, I). The crowns of the tubercles have a conical and dome-like, rarely peaked shape. They are oriented vertically or can be slightly slanted towards the surface of the plate (Fig. 4H). The mean height of the tubercles is 1 mm. Tubercles with round or oval bases are dominant (Fig. 4E, F, J, O) and those with angular, fan- or poleaxe-shaped bases are more rare (Fig. 4I-K). As a rule, thin radial ribs diverge from the top of the crown, which can be observed on low-crowned unabraded tubercles (Fig. 4L-O). Ribs branch on the marginal crenulations and ramifications (second-order marginal crenulations) forming fine plumose wrinkles (Fig. 4H, M-O; Fig. 5B, C, E). Marginal crenulations are massive and complicated, but not tapered. Finer and simpler crenulations may be present between them (Fig. 4B, C, I). The crenulations on the proximal side of branchial plates tubercles attain substantial length (up to 2.2 mm) and are more complicated (Fig. 4A, B, F, I), in comparison with those on the distal side of these tubercles. The tips of marginal crenulations often ramify into two or three long branches (Fig. 4A, B, F, I, L, O). Massive ramifications occur on the flanks of marginal crenulations. They can attain substantial length and can bear indentations on their margins in large tubercles (Fig. 4A, B). Ramifications are usually densely distributed along the whole length of marginal crenulations (Fig. 4C-G, I-O; Fig. 5B, C, D, F; Fig. 6A, B, F, G). Large microtubercles are situated along the whole length of marginal crenulations (up to 12 in discrete tesserae); small, scarcely discernible microtubercles are also observed on the ramifications (Fig. 6A, B).

Tubercles on the branchial plates often fuse into long ridges. The length of the ridges is up to 1 cm (Fig. 2A; Fig. 4B, C, G, I, N). The number of crenulations of fused tubercles exceeds 17. The tubercles of the lateral scale have predominantly round or oval bases; the crowns are oriented vertically; short ridges are present. Discrete tesserae bear a large primordial tubercle with very long marginal crenulations, covering the conical aspidin mound almost totally. Small tubercles of later generations on the branchial plates and tesserae are usually rounded, more rarely elongated; they bear 6-11 marginal crenulations, which are usually short, simple and unbranched (Fig. 4B, J, K; Fig. 6A, B, F). Some small tubercles on the ventral side of branchial plate PM SPU 80-2 (holotype) have a low (Fig. 4E-H) count of marginal crenulations, which intensely ramify towards their tips (Fig. 4E, F). The diameter of the bases of these small tubercles of later generations is 0.3-0.5 mm. There are also blisters with simple marginal crenulations, covering injuries on the plates (Fig. 2E, G, H; Fig. 3D, G, H).

3. Ornamentation topography. On the plates and micromeric elements of the new species known to date tubercles are arranged predominantly in regular concentric rows. The tubercles are not situated densely relative to each other (Fig. 4F, K, O). Rows of tubercles are oriented generally subperpendicular to the long axis (=to anterolateral and posterior margins) of branchial plates (Fig. 2A, G). The tubercles in rows are larger and have more massive and pronounced ridges on the dorsal side of the plates. The rows of the branchial plates can also have a slight proximal curvature (Fig. 3A, B, G, H). Small tubercles of later generations are situated between the large ones on the branchial plates. The ornamented surface on the branchial plates can generally be divided into two zones, the distal and the proximal one. In the distal zone the tubercles have a predominantly conical and peak-like shape; the crowns are usually slanted distally, the ridges in the rows are large and long, and the rows stand far from each other due to proximally developed marginal crenulations. In the proximal zone the tubercles have predominantly a simpler structure. They are dome-shaped and low cone-shaped with a vertically oriented crown. They possess short marginal crenulations, weakly growing longer in the proximal direction. The shapes of the bases are various in both zones and their topography is unique for every specimen. Small tubercles of late generations are situated in the proximal zone. The shape and orientation of the tubercles' crowns on the lateral scales is the same as in the proximal zones of the ornamented parts of the branchial plates. On the external surface of the lateral scale, the tubercles with conical and dome-shaped crowns are arranged in concentric rows around the large primordial tubercle (Figs 2Q, 3I).

4. Internal structure. The superficial layer of the plates consists of orthodentine tubercles, covered by a thin layer (up to 1.5 [micro]m) of hypermineralized tissue (PM SPU 80-8). The pulp cavities of dentine tubercles can be either hollow (Fig. 7D) or filled with aspidin trabeculae (Fig. 6E; Fig. 7B, C). Pulp cavities are connected with radial pulp canals, which run under marginal crenulations. Large dentine tubercles on the branchial plates, lateral scales and the primordial tubercle of micromeric elements are situated on cancellous aspidin mounds (Fig. 6E; Fig. 7A, D). The mounds on the branchial plates can also fuse into aspidin ridges (Fig. 2A, B). Satellite tubercles of discrete tesserae and small tubercles on the branchial plates generally have hollow pulp cavities. Cancellous aspidin has large spaces and vascular canals of aspidones; the reticular layer of the branchial plates is weakly developed (Fig. 7D).

Comparison. The branchial plates of the new species are more stenobasal than those of typical representatives of the genus Psammosteus. Psammosteus ramosus sp. nov. Glinskiy resembles P. falcatus Obruchev in Gross, 1942, P. kiaeri Halstead Tarlo, 1964, P. pectinatus Obruchev, 1965 and, to a lesser extent, P. tenuis Obruchev, 1965 in the extremely stenobasal shape of the branchial plates, details of ornamentation and its topography (Kiaer 1915, pl. 5, fig. 5; Halstead Tarlo 1964, pl. 2, fig. 2; Obruchev & Mark-Kurik 1965, pls 87-89, 91, 93). The rows of tubercles on branchial plates of P. ramosus sp. nov. can have a slight proximal curvature, as opposed to what can be seen in P. kiaeri and P. pectinatus. In the new species the tubercles in the rows on the branchial plates fuse into rather long ridges, just like in P. falcatus, P. kiaeri and P. pectinatus. However, in the new species these ridges are shorter than in P. kiaeri and they are very weakly developed on the proximal side of the plates, which differentiates it from P. pectinatus and places it somewhat closer to P. falcatus. The new species also differs from P. pectinatus in the size of the branchial plates, in the latter species they are small (Obruchev & Mark-Kurik 1965, pl. 93, fig. 2; Glinskiy & Ivanov 2015, fig. 1: 6). Lateral scales, both in size and in shape, most closely resemble those of Psammosteus bergi (Obruchev, 1943) and P. megalopteryx (Trautschold, 1880). The concentric arrangement of tubercles around the primordial tubercle (like on the tesserae) and their position at the posterior end of scales is seen in some scales of Psammosteus sp. (Mark-Kurik 1993, fig. 3B) and also in isolated scales of P. bergi (Mark-Kurik 1999, fig. 7D, E, G-I). Lateral scales of P. ramosus sp. nov. are also similar to those of P. bergi (Mark-Kurik 1999, fig. 7D) in a greater reduction of the external ornamented surface. The new species comes close to P. cf. kiaeri and P. falcatus (Fig. 6 A-Q) in terms of morphology and inner structure of discrete elements, and is substantially different from other species of Psammosteus. High and complicated tubercles of exoskeletal elements in P. ramosus sp. nov. are situated on cancellous aspidin mounds or ridges, like in P. falcatus (Novitskaya 1965, fig. 227), P. cf. kiaeri and P. pectinatus.

The species in the genus Psammosteus differ from each other primarily in details of ornamentation on branchial plates (Halstead Tarlo 1964, p. 39). General details of ornamentation, its topography and histological characteristics of branchial plates of Psammosteus ramosus sp. nov. are close to those of P. falcatus Obruchev in Gross, 1942, P. kiaeri Halstead Tarlo, 1964 and P. pectinatus Obruchev, 1965. In the details of tubercle morphology the new species also resembles P. asper Obruchev, 1965, P. bystrowi Obruchev, 1965, P. livoncius Obruchev, 1965 and P. tenuis, and is different from other species of the genus Psammosteus. It resembles P. asper, P. livonicus and P. tenuis in the massiveness of its crenulations and ramifications. As in P. asper, P. falcatus, P. kiaeri and P. pectinatus, marginal crenulations go deep into the crowns of the tubercles in the species described herein. The new species is similar to P. asper in its indented and rugose marginal crenulations. In the latter species such morphology of marginal crenulations is formed by microtubercles, not ramifications. The new species differs from P. bystrowi in a more complex form of marginal crenulations and the presence of ramifications. In the new species, ramifications are situated along the whole length of marginal crenulations as opposed to P. livonicus, in which they are confined to the tips of marginal crenulations (Glinskiy & Mark-Kurik 2016, fig. 6: 9, 10, fig. 7A). The new species is most closely similar to P. falcatus, P. kiaeri and P. pectinatus in the presence of ramifications along the whole length of the marginal crenulations. The main species-specific difference of the new species is that ramifications are large, massive, and densely and evenly distributed along the whole length of the flanks of marginal crenellations. Psammosteus ramosus sp. nov. differs from P. kiaeri (Kiaer 1915, pl. 5, fig. 5; Halstead Tarlo 1964, pl. 2, fig. 2) in larger structural elements: each crenulation is thicker and more massive; these crenulations do not fork at the very crown base and bear larger ramifications and microtubercles. The new species is closest to P. pectinatus in details of tubercle structure. It generally differs from the latter in short branching tips of the marginal crenulations and longer ramifications (Fig. 6A, B). In their general morphology the tubercles of the new species resemble those of P. falcatus (and P. tenuis), but they differ in bearing microtubercles, in larger, short, massive ramifications without fine branching and in having more simple plumose wrinkles.

Remarks. The exoskeletal elements of P. ramosus sp. nov. include discrete micromeric elements, tesserae of 'progressive type', which are also known in P. falcatus and P. cf. kiaeri and, probably, will be discovered in P. pectinatus. This group is substantially different from the main evolutionary lineage of species in the genus Psammosteus and also Karelosteus (q.v. Glinskiy 2014) in all these characters, and especially in possessing the discrete micromeric elements of 'progressive type' instead of those of 'basic type'. Specimen PM SPU 80-9 is defined as P. cf. ramosus sp. nov., because it possesses a naked aspidin mound without dentine tubercles.

The extension of cancellous aspidin trabeculae into the pulp cavity of large dentine tubercles is well known in Ganosteus stellatus Rohon, 1901 (Novitskaya 1965, figs 206, 208). The microstructure of large tubercles and micromeric elements of 'progressive type' in the described Psammosteus lineage and in the plates of Traquairosteus pustulatus (Traquair, 1897) is similar, because in both cases the undergrowth of cancellous aspidin and development of a cancellous aspidin mound are seen under growing dentine tubercles (Tarlo 1961, fig. 3C). However, dentine tubercles in T. pustulatus are simple, reduced in size (Halstead Tarlo 1965, p. 150). A similar model of skeletal development is also seen in a heterostracan Lepidaspis serrata Dineley & Loeffler, 1976: it possesses dentine ridges on the aspidin ridges, filled with aspidin trabeculae (Keating et al. 2015, fig. 2A-D).

DISCUSSION

The evolution of the exoskeleton in the representatives of the family Psammosteidae sensu Novitskaya (2004) resulted in the reduction of exoskeletal structures in comparison with other psammosteids, which made it possible to lighten the skeleton and improve locomotion capabilities. A number of evolutionary transformations are observed in major plates of the exoskeleton (progressive development of stenobasal branchial plates, elongation of median plates), which are connected with contraction in width of the cephalothorax (Obruchev & Mark-Kurik 1965, pp. 54, 55). The extremely stenobasal shape of branchial plates, characteristic of the juvenile stage of development in many Psammosteus species (Obruchev & Mark-Kurik 2016), is retained in some species of Psammosteus in the adult stage (paedomorphism). This phenomenon is manifested independently in different evolutionary lineages of Psammosteus. All representatives of Psammosteus, as opposed to other groups of psammosteids, are also characterized by the reduction in size of mesomeric exoskeletal elements, the lateral scales. According to Obruchev, this is connected with an increase in the mobility of the tail (Obruchev 1945, p. 263; Obruchev & Mark-Kurik 1965, p. 217). Psammosteus is characterized by a general constriction of the base of rooted micromeric elements--tesserae. At the same time they occupy most of the surface of cephalothoracic plates (advanced tesserization). Morphotypes of micromeric exoskeletal elements in Psammosteidae are probably more varied than in other psammosteids (as they are known only in Psammosteidae to date). In discrete micromeric elements of the cephalothorax an increase in height is observed. The height of such elements corresponds to the usual thickness of a dorsal median plate in representatives of the family Psammosteidae, suggesting that discrete exoskeletal elements could be situated in the skin at approximately the same level as the plate.

Thus, discrete tesserae of 'progressive type', characteristic of one of the lineages in the genus Psammosteus, stand out by their height, which is attained by the enlargement of an aspidin mound (neck) and its overgrowth by the dentine of the primordial tubercle. The development of discrete tesserae of 'progressive type' in the lineage P. ramosus sp. nov.--P. falcatus was by successive accretion of satellite tubercles to the neck of single elements. Tesserae of this type, formally circular tesserae (Halstead Tarlo 1967b; Karatajute-Talimaa 1998), are a result of multifunctional adaptation through paedomorphism, because the reduction in the count of tubercles in the crown provides the lightening and improvement of locomotion while preserving the protective function. Single elements represent the first ontogenetic stage of development of micromeric elements in psammosteids.

According to Obruchev (Obruchev & Mark-Kurik 1965, p. 43), the presence of lateral dorsal canals of the lateral line sensory system on the dorsal plate of Psammosteus points at the general constriction of the cephalothorax. Thus, lateral fields of tesserae were much narrower in Psammosteus than in other psammosteids, in which lateral dorsal canals were situated in wide fields of tesserae. The increase in the mobility of Psammosteidae in comparison with other psammosteids is also indicated by a progressive complication of the pattern of the lateral line system on the dorsal plate. Thus, in a late representative of the group, cf. Psammosteus from the Frasnian of Arctic Canada, sensory canal grooves have a very elaborate pattern (Elliott & Mark-Kurik 2005).

Psammosteid heterostracans underwent the stages of assimilative (e.g. Drepanaspididae, Obrucheviidae) and regressive (Psammosteidae) phases of exoskeletal development during their evolution. The phase of exoskeletal regression usually coincided with the increase in the mobility of the animals. Thus the ecological specialization changed from demersal Drepanaspis (Blieck 2016) with armoured body type to the most active demersal forms like Psammosteus.

RESULTS

At least two evolutionary lineages within Psammosteidae sensu Novitskaya (2004) can be distinguished now based on the differences in the morphology and histological details of the exoskeleton. The species Psammosteus ramosus sp. nov. Glinskiy is the oldest known representative of the psammosteid lineage with discrete cyclomorial tesserae of 'progressive type' and a peculiar histological structure of the other plates. The new species comes close to P. falcatus Obruchev in Gross, 1942, P. kiaeri Halstead Tarlo, 1964 and P. pectinatus Obruchev, 1965, but is strongly different from other known representatives of the genera Psammosteus and Karelosteus weberi Obruchev, 1933. Obruchev did not exclude the possibility that the genus Psammosteus may be divided into several genera in the future (Obruchev & Mark-Kurik 1965, p. 219).

Acknowledgements. We are grateful to A. Ivanov (St. Petersburg State University), I. Zupins (Natural History Museum of Latvia) and U. Toom (Department of Geology at Tallinn University of Technology) for assistance and providing access to the psammosteid collections, and A. Ivanov and E. Luksevics (University of Latvia) for useful discussions. The first author thanks D. Pinakhina (St. Petersburg State University) for helping with the translation of the article. The authors acknowledge D. Elliott (Northern Arizona University) for his valuable remarks and improvement of English. We also thank E. Mark-Kurik, T. Marss and U. Toom (Department of Geology at Tallinn University of Technology) for help and valuable advice. We are grateful to T. Marss and M. V. H. Wilson (University of Alberta) for their constructive reviews and text correction. We are obliged to N. Vlasenko and V. Shilovskikh (Research Park of St. Petersburg State University) for great help with SEM photographs. We would like to thank all the members of the team of the Russian--French--Latvian expedition 2009, 2010, and also I. Evdokimova and E. Sokiran (A. P. Karpinsky Russian Geological Research Institute) for collecting psammosteid specimens.

The first author acknowledges Saint Petersburg State University for research grants 0.38.292.2015, 3.42.975.2016 (Internship at the University of Latvia), 3.42.1103.2016 (Expedition to Estonia to collect comparative material on Devonian vertebrates) and the European Social Fund's Doctoral Studies and Internationalisation Programme DoRa, which is carried out by Foundation Archimedes. The reported study was partially supported by RFBR, research project No. 14-04-01507 a. The research was performed at the Center for Geo-Environmental Research and Modeling (GEOMODEL) of the Research Park of St. Petersburg State University.

The publication costs of this article were covered by the Estonian Academy of Sciences.

REFERENCES

Agassiz, L. 1844. Monographie des Poissons fossiles du vieux gres rouge ou systeme Devonien (Old Red Sandstone) des Isles Britanniques et de Russie. Neuchatel, 188 pp.

Berg, L. S. 1937. A classification of fish-like vertebrates. Izvestiya Akademii Nauk SSSR (Bulletin of the Academy of Sciences of the USSR), Otdelenie matematicheskikh i estestvennykh nauk, seriya biologicheskaya, 4, 1277-1280.

Blieck, A. 2016. Heterostracan vertebrates and the Great Eodevonian Biodiversification Event--an essay. Palaeobiodiversity and Palaeoenvironments, doi:10.1007/s12549-016-0260-1.

Blieck, A. R. M., Karatajute-Talimaa, V. N. & Mark-Kurik, E. 2002. Upper Silurian and Devonian heterostracan pteraspidomorphs (Vertebrata) from Severnaya Zemlya (Russia): a preliminary report with biogeographical and biostratigraphical implications. Geodiversitas, 24, 805-820.

Blom, H., Carlsson, A. & Marshall, J. E. A. 2006. Vertebrate micro-remains from the Upper Devonian of East Greenland with comments of the Frasnian--Famennian boundary. Bulletin of the Geological Society of Denmark, 53, 39-46.

Bystrow, A. P. 1959. The microstructure of skeleton elements in some vertebrates from Lower Devonian deposits of the USSR. Acta Zoologica, 40, 59-83.

Delsate, D., Blieck, A. & Steemans, P. 2004. A psammosteid heterostracan (Vertebrata: Pteraspidomorphi) from the Emsian (Lower Devonian) of the Grand Duchi of Luxembourg. Geologica Belgica, 7, 21-26.

Dineley, D. L. & Loeffler, E. J. 1976. Ostracoderm faunas of the Delorme and associated Siluro-Devonian formations North West Territories Canada. Special Papers in Palaeontology, 18, 1-214.

Eichwald, E. 1844. O rybakh" pervobytnogo okeana v" okrestnostyakh" Pavlovska [About fishes from the primeval ocean in the Pavlovsk surroundings]. Otechestvennye Zapiski, 36(9), 1-22 [in Russian].

Elliott, D. K. & Mark-Kurik, E. 2005. A review of the lateral line sensory system in psammosteid heterostracans. Revista Brasileia de Paleontologia, 8, 99-108.

Glinskiy, V. N. 2013. Kompleksy srednedevonskikh psammosteidnykh beschelyustnykh vostochnoj chasti Glavnogo devonskogo polya [The assemblages of Middle Devonian psammosteid agnathans from the eastern part of Main Devonian Field]. Vestnik Saint-Petersburg University, Series 7, Geology, Geography, 4, 62-71 [in Russian, with English summary].

Glinskiy, V. N. 2014. Novye dannye po Karelosteus weberi Obruchev (Agnatha: Heterostraci) [New data on Karelosteus weberi Obruchev (Agnatha: Heterostraci)]. In Paleontologiya v muzejnoj praktike. Sbornik nauchnykh rabot [Palaeontology in the Museum Practice. Collection of the Scientific Articles] (Naugolnykh, S. V., ed.), pp. 22-25. Media-Grand, Moscow [in Russian, with English summary].

Glinskiy, V. N. & Ivanov, A. O. 2015. The assemblages of psammosteid agnathans from the Middle-Late Devonian of the Andoma Hill (Russia). In IGCP596-SDS Symposium: Climate Change and Biodiversity Patterns in the Mid-Palaeozoic (Mottequin, B., Denayer, J., Konigshof, P., Prestianni, C. & Olive, S., eds), Strata (Travaux de Geologie Sedimentaire et Paleontologie), Serie 1: Communications, 16, 57-59.

Glinskiy, V. N. & Mark-Kurik, E. 2016. Revision of Psammosteus livonicus Obruchev (Agnatha, Heterostraci) from the Devonian Amata Regional Stage of the NW of the East European Platform. Estonian Journal of Earth Sciences, 65, 1-18.

Goodrich, E. S. 1909. Vertebrata Craniata (First fascile: cyclostomes and fishes). In A Treatise on Zoology. Part IX (Lankester, R., ed.), pp. XVI+518. Adam and Charles Black, London.

Gross, W. 1933. Die Fische des Baltischen Devons. Palaeontographica, 79, 1-74.

Gross, W. 1942. Die Fischfaunen des baltischen Devons und ihre biostratigraphische Bedeutung. Korrespondenzblatt des Naturforscher--Vereins zu Riga, 64, 373-436.

Gross, W. 1963. Drepanaspis gemuendenensis Schluter Neuuntersuchung. Palaeontographica. Abt. A, 121(4-6), 133-155.

Halstead, L. B. 1987. Agnathan extinctions in the Devonian. Memoires de la Societe Geologique de France, 150, 7-11.

Halstead Tarlo, L. B. 1964. Psammosteiformes (Agnatha)--A review with descriptions of new material from the Lower Devonian of Poland. I. General part. Palaeontologia Polonica, 13, 1-135.

Halstead Tarlo, L. B. 1965. Psammosteiformes (Agnatha)--A review with descriptions of new material from the Lower Devonian of Poland. II. Systematic part. Palaeontologia Polonica, 15, 1-168.

Halstead Tarlo, L. B. 1967a. Major faunal provinces in the Old Red Sandstone of the Northern Hemisphere. In International Symposium on the Devonian System, Calgary (Oswald, D. H., ed.), pp. 1231-1238. Alberta Society of Petroleum Geologists, Calgary.

Halstead Tarlo, L. B. 1967b. The tessellated pattern of the dermal armour in the Heterostraci. Journal of the Linnean Society of London, Zoology, 47, 45-54.

Ivanov, A. & Lebedev, O. 2011. Devonian Vertebrate Localities in the Luga River Basin (Leningrad Region, Russia). Guidebook for the Field Trip. St. Petersburg University Press, St. Petersburg, 37 pp.

Ivanov, A. O., Luksevics, E. V., Stinkulis, G. V., Tovmasyan, K. A., Zupins, I. A. & Beznosov, P. A. 2006. Stratigrafiya devonskikh otlozhenij Andomskoj gory [Stratigraphy of the Devonian deposits of Andoma Hill]. In Problemy geologii i mineralogii [Problems of Geology and Mineralogy] (Pystin, A. M., ed.), pp. 385-396. Geoprint, Syktyvkar [in Russian].

Ivanov, A., Luksevics, E. & Glinskiy, V. 2011. Vertebrate assemblages from the Givetian--Frasnian boundary beds of the Borschovo locality (Leningrad region, Russia). In The Eighth Baltic Stratigraphical Conference. Abstracts (Luksevics, E., Stinkulis, G. & Vasilkova, J., eds), p. 29. University of Latvia, Riga.

Karatajute-Talimaa, V. 1998. Determination methods for the exoskeletal remains of Early Vertebrates. Mitteilungen aus dem Museum fur Naturkunde in Berlin, Geowissenschaftliche Reihe, 1, 21-51.

Keating, J. N., Marquart, C. L. & Donoghue, P. C. J. 2015. Histology of the heterostracan dermal skeleton: insight into the origin of the vertebrate mineralised skeleton. Journal of Morphology, 276, 657-680.

Kiaer, J. 1915. Upper Devonian fish remains from Ellesmere Land with remarks on Drepanaspis. Report of the Second Norwegian Arctic Expedition in the "Fram" 1898-1902, 33, 1-72.

Kiaer, J. 1932. The Downtonian and Devonian vertebrates of Spitsbergen. IV. Suborder Cyathaspida. A preliminary report edited by A. Heintz. Skrifter om Svalbard og Ishavet, 52, 1-26.

Lankester, E. R. 1868. The fishes of the Old Red Sandstone of Britain. Part I.--The Cephalaspididae. Palaeontographical Society, 21, 1-33.

Luksevics, E. V., Ivanov, A. O. & Zupins, I. A. 2012. Kompleksy devonskikh pozvonochnykh Andomskoj gory i korrelyatsiya s razrezami Glavnogo devonskogo polya [Assemblages of Devonian vertebrates from Andoma Hill and correlation with sections of the Main Devonian Field]. In Palaeozoj Rossii: regional'naya stratigrafiya, paleontologiya, geo- i biosobytiya. Materialy III Vserossijskogo soveshchaniya [Palaeozoic of Russia: Regional Stratigraphy, Palaeontology, Geo- and Bioevents. Materials of the Third All-Russian Conference] (Zhamojda, A. I., ed.), pp. 128-130. VSEGEI, St. Petersburg [in Russian].

Lyarskaya, L. A. 1981. Pantsirnye ryby devona Pribaltiki. Asterolepididae [Armoured Fishes from Devonian of the Baltic States. Asterolepididae]. Zinatne, Riga, 153 pp. [in Russian, with English summary].

Mark-Kurik, E. 1993. Notes on the squamation in psammosteids. Modern Geology, 18, 107-114.

Mark-Kurik, E. 1999. Psammosteid microremains from the Middle Devonian (Givetian) of Estonia. Modern Geology, 24, 1-21.

Novitskaya, L. I. 1965. Microstructure of some Psammosteida. In Psammosteidy (Agnatha, Psammosteidae) devona SSSR [Devonian Psammosteids (Agnatha, Psammosteidae) of the USSR] (Obruchev, D. V. & Mark-Kurik, E. Yu., eds), pp. 257-282. Institute of Geology, Academy of Sciences of the Estonian SSR, Tallinn [in Russian].

Novitskaya, L. I. 2004. Subclass Heterostraci. In Iskopaemye pozvonochnye Rossii i sopredel'nykh stran. Beschelyustnye i drevnie ryby [Fossil Vertebrates of Russia and Adjacent Countries. Agnathans and Early Fishes] (Novitskaya, L. I. & Afanassieva, O. B., eds), pp. 69-207. GEOS, Moscow [in Russian].

Obruchev, D. V. 1933. Opisanie chetyrekh novykh vidov ryb Leningradskogo devona [Description of four new fish species from the Devonian of Leningrad Province]. Materialy Tsentral'nogo Nauchno-Issledovatel'skogo Geologo-Razvedochnogo Instituta. Paleontologiya i Stratigraphiya, 1, 12-15 [in Russian, with English summary].

Obruchev, D. V. 1943. Yoglinia n. g., latest pteraspid from the Middle Devonian of the Leningrad District. Comptes Rendus (Doklady) de l'Academie des Sciences de l'URSS, 41, 41-43.

Obruchev, D. V. 1945. Evolyutsiya Agnatha [Evolution of Agnatha]. Zoologicheskij Zhurnal, 24(5), 257-272 [in Russian].

Obruchev, D. V. 1947a. Tip Chordata. Hordovye. Podtip Vertebrata. Pozvonochnye [Phylum Chordata. Chordates. Subphylum Vertebrata. Vertebrates]. In Atlas rukovodyashchikh form iskopaemykh faun SSSR. Tom III. Devonskaya sistema [Atlas of the Guide Forms of the Fossil Faunas of the USSR. Volume III. Devonian] (Nalivkin, D. V., ed.), pp. 191-206. State Editorial Office for Geological Literature, USSR Ministry of Geology, Moscow--Leningrad [in Russian].

Obruchev, D. V. & Mark-Kurik, E. Yu. 1965. Psammosteidy (Agnatha, Psammosteidae) devona SSSR [Devonian Psammosteids (Agnatha, Psammosteidae) of the USSR]. Institute of Geology, Academy of Sciences of the Estonian SSR, Tallinn, 304 pp. [in Russian, with English summary].

Orvig, T. 1951. Histologic studies of placoderms and fossil elasmobranchs. I: The endoskeleton, with remarks on the hard tissues of lower vertebrates in general. Arkiv for Zoologi, 2, 321-454.

Orvig, T. 1977. A survey of odontodes ('dermal teeth') from developmental, structural, functional and phyletic points of view. In Problems in Vertebrate Evolution (Andrews, S. M., Miles, R. S. & Walker, A. D., eds), Linnean Society Symposium Series, 4, 53-75.

Rohon, J. V. 1901. Beitrage zur Anatomie und Histologie der Psammosteiden. Vestnik Kralovske Ceske Spolecnosti Nauk, 16, 1-31.

Schluter, C. A. J. 1887. Uber Panzerfische und legte neue Arten aus dem rheinisch-westfalischen Devon vor. Verhandlungen des Naturhistorischen Vereines der Preussischen Rheinlande und Westphalens (Naturwissenschaftliche Sektion), 44, 120-128.

Selden, P. A. 2003. A new tool for fossil preparation. The Geological Curator, 7, 337-339.

Tarlo, L. B. 1961. Psammosteids from the Middle and Upper Devonian of Scotland. The Quarterly Journal of the Geological Society of London, 117, 193-212.

Tarlo, L. B. 1962. The classification and evolution of the Heterostraci. Acta Palaeontologica Polonica, 7, 249-290.

Traquair, R. H. 1896. The extinct vertebrata animals of the Moray Firth Area. In A Vertebrate Fauna of the Moray Basin, Vol. 2 (Harvie-Brown, J. H. & Buckley, T. E., eds), pp. 235-285. Edinburgh.

Traquair, R. H. 1897. Additional notes on the fossil fishes of the Upper Old Red Sandstone of the Moray Firth Area. Proceedings of the Royal Physical Society of Edinburgh, 13, 376-385.

Trautschold, H. 1880. Ueber Dendrodus und Coccosteus. Verhandlungen der Russisch-Kaiserlichen Mineralogischen Gesellschaft zu St. Petersburg, Zweite Serie, 15, 139-156.

Vaskaninova, V. & Kraft, P. 2016. A unique occurrence of a psammosteid heterostracan on the peri-Gondwanan shelf in the Lower/Middle Devonian boundary marine deposits. Fossil Imprint, 72, 155-160.

Uus psammosteiid (Agnatha, Heterostraci) Amata regionaalsest lademest Peadevonivaljalt ja diskreetsete mikromeersete elementide tuubid sugukonnas Psammosteidae

Saint Petersburg State University, 7/9 Universitetskaya nab., St. Petersburg, 199034 Russia; vadim.glinskiy@gmail.com

Received 28 October 2016, accepted 8 February 2017

Vadim N. Glinskiy ja Sergey P. Nilov

Sugukonda Psammosteidae Novitskaya (2004) kuuluvate psammosteiidide mitmekesisus on siiani puudulikult teada. Artiklis kirjeldame uut liiki Psammosteus ramosus sp. nov. Glinskiy Amata regionaalsest lademest Peadevonivaljalt ja vordleme selle valisskeleti plaatide morfoloogiat, ornamente ning histoloogiat, aga ka nende mikromeerseid elemente selle sugukonna teiste esindajate omadega. Vordlus naitab lahedast seost uue liigi ja Psammosteus falcatus Obruchev (vt Gross, 1942), P. kiaeri Halstead Tarlo, 1964 ning P. pectinatus Obruchev, 1965 vahel. Viimased kuuluvad liikide ruhma, mis oluliselt erineb perekonna Psammosteus teistest esindajatest ja moodustab eraldiseisva evolutsioonilise liini. Morfoloogiliste ja histoloogiliste tunnuste alusel eristame sugukonnas Psammosteidae diskreetseid primaarset tuupi (basic type) ning progressiivset tuupi (progressive type) mikromeerseid elemente.
Table 1. Measurements of fragments of branchial plates (in mm)

                          PM SPU 80-1  PM SPU 80-2  PM SPU 80-3

Length of the fragment    30           31           17
Width of the fragment     70           63           12
Maximal thickness in the   3            2.9          5
 distal part
Maximal thickness in the   2.4          2.6         --
 proximal part

                          G 43/292:1  G 43/292:2

Length of the fragment    13          20
Width of the fragment     20.2        22.9
Maximal thickness in the   5           6.7
 distal part
Maximal thickness in the   3.3         5.5
 proximal part
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Author:Glinskiy, Vadim N.; Nilov, Sergey P.
Publication:Estonian Journal of Earth Sciences
Article Type:Report
Date:Jun 1, 2017
Words:8573
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