Nostovicina undetermined

Burrow, Carole Jan, Murphy, Michael & Turner, Susan, 2023, Late Silurian to earliest Devonian vertebrate biostratigraphy of the Birch Creek II section, Roberts Mountains, Nevada, U. S. A., PaleoBios 40 (1975), pp. 1-32 : 13

publication ID

https://doi.org/ 10.5070/P940454153

publication LSID

lsid:zoobank.org:pub:58312615-0833-432E-BF5D-3DFFBF361AAA

persistent identifier

https://treatment.plazi.org/id/B21CD55B-FFD0-FFEE-5863-8E8CFB1A2308

treatment provided by

Felipe

scientific name

Nostovicina undetermined
status

 

NOSTOVICINA SP. CF. N. ELEGANS

( FIG. 4A View Figure 4 ; TABLE 1; SUPPL. 1, FIG. 13)

Referred specimens —One scale from level 470.2’

(143.3 m): Roberts Mountains Formation.

Description —The solitary medium-sized scale assigned to this species is characterized by having an elevated central area in the elongate crown, with just one or two short ridges leading back from the anterior edge. Narrow lower ledges run along each side of the central crown plane. The base is moderately convex, a neck is lacking, and the crown is inclined anteroposterially.

Comparison —The type material of N. elegans was found in Lower Devonian erratics of the Baltic basin, and the species has been reported from Ludlow to Lochkovian deposits, including from the Přidolí of southern Sweden ( Vergoossen 1999b, pl. 2.16, 2.17), Lithuania (Valiukevičius 2005, figs. 2I, 2J, 7, 8) and Lat- via ( Valiukevičius 2004b, table, fig. 5A–M). The work by those authors indicates that Nostovicina elegans is a valid species, countering Gross’ (1947) dismissal of Diplacanthoides elegans as a junior synonym of Nostolepis striata . Certainly, in the BC II section, this is amongst the few Nostolepis -type scales sensu Gross (1947) found in the upper Silurian below the 513’ level, with no scales comparable with the holotype of N. striata found at any level. The scale is only tentatively assigned to N. elegans based on its morphology, because the histological structure was not investigated.

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF