Barlowodus, SP. CF. B. FLORALIS

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 : 25

publication ID

https://doi.org/ 10.5070/P940454153

publication LSID

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

DOI

https://doi.org/10.5281/zenodo.11489435

persistent identifier

https://treatment.plazi.org/id/B21CD55B-FFC4-FFFA-5867-8D29FAFB25E7

treatment provided by

Felipe

scientific name

Barlowodus
status

 

BARLOWODUS SP. CF. B. FLORALIS ( FIG. 8A–K View Figure 8 ; TABLE 1 View Table 1 ; SUPPL. 1, FIGS. 4 View Figure 4 , 5 View Figure 5 , 7 View Figure 7 )

Referred specimens — Circa 20 specimens from BC II level 430.5' (131.2 m); two from level 453' (138.1 m): Roberts Mountains Formation .

Description and comparison —Small scales with complex crown sculpture, all with fine ribbed ultrasculpture ( Fig. 8A–K View Figure 8 ). One possible head or oral scale has a high multi-ridged crown and high neck with a rounded base and large central pulp opening ( Fig. 8A View Figure 8 ). One possible cephalopectoral scale has a flattened rhombic crown which rises only slightly to a posterior point; fine ultrasculpture as well as borings can be seen on the surface ( Fig. 8B View Figure 8 ). Most scales are trunk scales. The crowns rise gently posteriad with three flat ridges or a system of bifurcating ridges separated by deep or wide grooves. The posterior or posterolateral crown margin is multi-pointed ( Fig. 8A, C–F, H–K View Figure 8 ).

Most scales in level 430.5’ seem affected by fungal damage (as noted for other specimens above). Histology was attempted using anise oil but the structure is disrupted and so we cannot verify the apparent “criss-cross aspidine ‘pegs’” noted as characteristic for the genus and separate family by Märss et al. (2006, p. 121). However, a similar criss-cross pattern of Sharpey’s fiber bundle spaces is found in other deep and swollen old bases of other thelodont scale taxa such as Thelodus laevis (e.g., Bystrow 1957, Gross 1967).

Remarks —Most of the scales from Nevada seem closest to B. floralis . The type locality for the latter is at 34.5* m in the same section where it co-occurs with the other two Barlowodus species ( Märss et al. 2006).

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