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