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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 />

19<br />

fields. These structures (or perforated septa in species with a well-developed exoskeleton),<br />

connected with the sensory system, are typical for most of the members of the suborder<br />

Tremataspidoidei (Tremataspis, Dartmuthia, Saaremaaspis, Oeselaspis, Procephalaspis,<br />

Thyestes, Aestiaspis, Septaspis). It should be noted that exoskeletal microstructure of<br />

Sclerodus <strong>and</strong> Tyriaspis (possible Tremataspidoidei) has never been investigated, <strong>and</strong> in<br />

Witaaspis similar structures were not fo<strong>un</strong>d (Afanassieva 1991). In my opinion their<br />

absence in Witaaspis is probably due to incomplete exoskeletal development in this form<br />

(the thin cephalothoracic shield is composed only of a part of the middle <strong>and</strong> basal layers).<br />

In Thyestes verrucosus a large number of pore fields is located on the surface of the<br />

shield <strong>and</strong> on the slopes of large <strong>and</strong> medium-sized tubercles. As a rule, no trace of the<br />

polygonal pattern typical of osteostracans is observed. I studied the cephalothoracic<br />

shield of Thyestes verrucosus (specimen PIN 1628/31), in which, as supposed, the<br />

processes of dermal ossification have not been completed. The material comes from the<br />

Viita or the Vesiku Beds of the Rootsiküla Regional Stage. In the posterolateral parts of<br />

the dorsal side of the shield radiating canals were fo<strong>un</strong>d opening on the surface of the<br />

exoskeleton (Fig. 2 C). It has been determined that pore fields on the slopes of large<br />

tubercles are aligned in rows along radiating canals (Fig. 2 D). Distal parts of these<br />

canals, open from above, form a pattern, typical of osteostracans, <strong>and</strong> determine<br />

approximate borders of “tesserae” of various sizes. It is assumed that the large tubercles<br />

of longitudinal rows (along the ribs of rigidity of the dorsal shield) emerged first. The<br />

formation of the exoskeleton began with the laying of dentine tips of the tubercles, <strong>and</strong><br />

proceeded centripetally. Middle-sized tubercles with thin tips were formed between<br />

them. Every tubercle was laid in the center of an individual “tessera”. Finally, small<br />

tubercles emerged last in ontogenesis, which is proved by their location on the slopes<br />

of larger tubercles. The exoskeleton of Thyestes verrucosus developed relatively rapidly<br />

but slower than in species of Tremataspis. The existence of a system of <strong>un</strong>its (tesserae),<br />

gradually increasing in size, allowed the individual to grow during a longer period of<br />

time up to complete consolidation of the shield, <strong>and</strong> also distributed the burden on the<br />

organism resulting from a rapid process of shield formation (Afanassieva 2002).<br />

In Oeselaspis pustulata (Patten) the tops of large tubercles are capped with a thick<br />

layer of enameloid tissue <strong>and</strong> mesodentine (Denison 1951b). Usually the surface of<br />

large tubercles is smooth (Fig. 2 E). The microfragment of the cephalothoracic shield of<br />

Oeselaspis pustulata (specimen PIN 4765/65) is distinguished from the others by the<br />

surface sculpture of one of the large tubercles (Fig. 2 F). A part of the largest tubercle<br />

Fig. 2. A-D, Thyestes verrucosus Eichwald, specimen PIN 1628/31, dorsal part of cephalothoracic<br />

shield; Viita or Vesiku Beds of Rootsiküla Regional Stage, Upper Wenlockian, Lower Silurian;<br />

Saaremaa Isl<strong>and</strong>, Estonia; A, fine ribbing on the surface of small tubercle; B, fine ribbing on the<br />

lower part of the medium-size tubercle with broken apical part; C, tubercles of different sizes<br />

<strong>and</strong> open radiating canals on the surface of the shield; D, pore fields on the slope of the large<br />

tubercle lining up along radiating canals. E, F, Oeselaspis pustulata (Patten), specimen PIN<br />

4765/65, microfragment of cephalothoracic shield; ?upper part of the Samojlovich Formation,<br />

Upper Wenlock, Lower Silurian; sample 5D/76, locality Sosednii, J<strong>un</strong>gsturm Strait, Pioneer<br />

Isl<strong>and</strong>, Severnaya Zemlya Archipelago, Russia; E, smooth surface of the large tubercle; F, surface<br />

of the horizontal section of the large tubercle as a result of acid-etching (or/<strong>and</strong> abrasion).

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