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

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C.G.Miller, T. Marss, H. Blom. New anaspid material from Britain <strong>and</strong> Estonia<br />

55<br />

follows the previous ridge; ridges slightly oblique (Fig. 3J) to perpendicular to the long<br />

axis of the scale (Fig. 3I). One specimen with main scale area of chevron-like, continuous<br />

ridges crossing whole of preserved part of scale (Fig 3K). Articulation facet visible on<br />

most complete scale (Fig. 3I). Single, well-developed, central visceral rib occurs on the<br />

smooth lower surface of the scale (Fig. 3L). On two scales, vascular canals exposed<br />

where sculpture of the main scale area has been worn away (Figs 3J, K).<br />

Histology. Well developed vascular canal system present just below level of the main<br />

scale area (Figs 2B, D; 4B, D). Distinct parallel growth lines of compact structure in<br />

the visceral rib of one specimen (Figs 2D, 4D). Fine fibres present both in the sculpture<br />

ridges <strong>and</strong> visceral rib. Sharpey’s fibres fo<strong>un</strong>d in one scale (Figs 2B, 4B).<br />

Remarks. Less material was available from Gardner’s Bank than at Man Brook. The<br />

Gardner’s Bank scales were also broken but it was easier to make thin sections of them.<br />

The broken external surface on one specimen that has now been sectioned (Figs 2D,<br />

3K, 4D) suggests that there were a series of closely spaced fine elements forming each<br />

major ridge on the main scale area. These could have been similar to the ridges on<br />

Rhyncholepis parvula Kiær, 1924 (Blom et al. fig. 26m) or Schidiosteus mustelensis<br />

P<strong>and</strong>er, 1856 (Blom et al. 2002, fig. 30m). Histological sections (Figs 2B, D; 4B,D)<br />

show a well developed vascular canal system that suggest more of a similarity with the<br />

rhyncholepidids Rhyncholepis, Silmalepis, Vesikulepis, Schidiosteus or Rytidolepis. One<br />

specimen (Fig. 3J) also shows traces of vascular canals in a worn area below the sculpture<br />

on the main scale area. Well developed vascular canal systems are consistent with<br />

members of the Family Rhyncholepididae, which at present is confined to the late<br />

Wenlock to middle Ludlow (Blom et al. 2002). Identification of this material <strong>un</strong>der the<br />

Family Rhyncholepididae extends the range of the family to the late Prídolí. More<br />

material from Gardner’s Bank is certainly needed before the genus can be decided with<br />

any certainty.<br />

Conclusions<br />

1. Trimpleylepis gen. nov. is an anaspid that shows similarities to those from the Family<br />

Septentrionidae. However, there is some doubt that vascular canals are developed, so<br />

at present Trimpleylepis can only tentatively be assigned to this family.<br />

2. Two species have been described; Trimpleylepis j<strong>un</strong>cta gen. et sp. nov. from the<br />

Prídolí of the Welsh Borderl<strong>and</strong> at Man Brook <strong>and</strong> Trimpleylepis concatenata gen. et<br />

sp. nov. from the Ludlow of Estonia.<br />

3. Material described from Man Brook extends the range of the genus Silmalepis to<br />

Ludlow-latest Prídolí.<br />

4. New material from Gardner’s Bank, Welsh Borderl<strong>and</strong> significantly exp<strong>and</strong>s the<br />

range of the Family Rhyncholepididae to mid Wenlock-late Prídolí.<br />

Acknowledgements. - Illustrations of NHM material figured within remain copyright of the<br />

NHM. Sally Yo<strong>un</strong>g, Natural History Museum, provided useful information about sculptures of<br />

Siluro-Devonian vertebrate microremains. Some SEM images were taken in the Centre of Material<br />

Research at Tallinn Technical University by Dr. Valdek Mikli. T.M. acknowledges the receipt of<br />

an Estonian Science Fo<strong>un</strong>dation Grant No. 5726.

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