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Zemes un vides zinātnes Earth and Environment Sciences - Latvijas ...

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Olga Afanassieva. Microrelief on the exoskeleton of early osteostracans<br />

17<br />

arranged in longitudinal rows (diameter at the base about 1 mm), tubercles of medium<br />

size with straight tips (about 0,3 mm), <strong>and</strong> numerous small (0,03-0,15 mm) ribbed tubercles<br />

(Afanassieva 1985). A row (sometimes two or three rows) of shiny flattened tubercles is<br />

arranged along the anterior <strong>and</strong> lateral edges of the cephalic shield. As in Ungulaspis<br />

arctoa, thin ribbing of Thyestes verrucosus is located on the surface of the tubercles of<br />

small size, in the lower parts of medium-sized tubercles, <strong>and</strong> on the surface of the<br />

marginal tubercles. The hypermineralized tissue of the superficial layer is present only<br />

in the apical parts (tips) of the large tubercles, of medium-sized tubercles, <strong>and</strong> of marginal<br />

ones. The basal layer is poorly developed. The exoskeleton mainly consists of relatively<br />

friable bony tissue of the middle layer, with numerous cavities of various sizes.<br />

The assumption that the exoskeleton of this type was covered by soft tissue (Stensiö<br />

1927, 1932) is supported by the position of the elements of the sensory system in the<br />

covering of Thyestes verrucosus (Denison 1951a, b). In my opinion, the arrangement of<br />

the main sensory lines in the exoskeleton of this species is marked by the elongated<br />

tubercles of medium size, disposed in pairs along the conjectural sensory canals<br />

(Afanassieva 1985, 1991, pl. VI, fig. 6). The set of the main sensory lines <strong>and</strong> their<br />

distribution pattern, marked by the tubercles of that type, are characteristic of this<br />

osteostracan group. It is possible to identify the infraorbital, postorbital, transversal<br />

<strong>and</strong> main lateral sensory lines in the Thyestes exoskeleton. The sensory lines of Thyestes<br />

were located between the “sensory” tubercles, i.e. superficially to the exoskeleton. In<br />

addition, I suppose that variously sized cavities at the bases of marginal flattened<br />

tubercles in Thyestes verrucosus <strong>and</strong> Aestiaspis viitaensis contained soft tissues of the<br />

cutaneous covering.<br />

Thus an analysis of mutual arrangement of the exoskeletal structures in Thyestes<br />

verrucosus reveals that the external skeleton was covered by soft tissue. In this<br />

connection it is important to note that the fine ribbing is fo<strong>un</strong>d on the surface of the<br />

exoskeletal structures that were surro<strong>un</strong>ded by soft tissue (small tubercles, lower parts<br />

of medium-sized tubercles <strong>and</strong> of marginal ones). I suppose the fine ribbing was used<br />

for optimal conj<strong>un</strong>ction between the layers of the soft <strong>and</strong> hard tissues within the cover.<br />

The same assumption st<strong>and</strong>s for the external skeleton of Ungulaspis, Aestiaspis,<br />

Septaspis <strong>and</strong> other osteostracans, <strong>and</strong> early vertebrates, with the similar type of<br />

exoskeleton microrelief.<br />

As is known, numerous microapertures (2-5 microns in diameter) are located on the<br />

surface of the exoskeleton of some early osteostracans. They are often grouped in pore<br />

Fig. 1. A-D, surface of the Tremataspis exoskeleton: A, smooth surface of Tremataspis cf. milleri<br />

Patten, specimen PIN 4765/30, Ust’-Spokojnaya Formation, Ludlow, Upper Silurian; 14, locality<br />

47, Spokoinaya River, October Revolution Isl<strong>and</strong>, Severnaya Zemlya Archipelago, Russia; B,<br />

C, Tremataspis sp., specimen PIN 4765/20, Ust’-Spokojnaya Formation, Ludlow, Upper Silurian;<br />

locality 31 (talus), Ushakov River, October Revolution Isl<strong>and</strong>; D, Tremataspis milleri, fragment<br />

of the specimen PIN 4219/ 7, Kuusnymme Beds of Rootsiküla Regional Stage, Upper Wenlockian,<br />

Lower Silurian; Elda Cliff, Saaremaa Isl<strong>and</strong>, Estonia. E, F, Ungulaspis arctoa Afanassieva et<br />

Karatajute-Talimaa, Severnaya Zemlya Formation, Lochkovian, Lower Devonian; Pod’emnaya<br />

River, October Revolution Isl<strong>and</strong>, Severnaya Zemlya Archipelago, Russia; microfragment (PIN<br />

4766/1) of the holotype LIG 35-670; tubercles with fine ribbing on the surface of the cephalic<br />

shield.

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