HETEROSTRACI

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 (4), pp. 1-32 : 19

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.13852155

persistent identifier

https://treatment.plazi.org/id/B21CD55B-FFCA-FFF4-599F-8F1EFAE224B3

treatment provided by

Felipe

scientific name

HETEROSTRACI
status

 

HETEROSTRACI LANKESTER, 1868

HETEROSTRACI INDET. GEN. ET SP.

( TABLE 1 View Table 1 ; SUPPL. 1, FIGS. 7 View Figure 7 , 11, 12, 14, 18)

Referred specimens —Scale fragments were collected from BC II section at six levels from 430.5’ to 513’ (131.2- 156.4 m): Roberts Mountains Formation.

Remarks —Most remains are conjoined tesserae such as the three small irregular tesserae from level 458.67’ (Suppl. 1, fig. 11). Some (Suppl. 1, figs. 7, 14, 18) resemble traquairaspid remains with slender oak-leaf pattern tubercles: traquairaspids typically range from Přidolí to early Lochkovian. One plate from level 468’ (Suppl. 1, fig. 12) is pteraspid- or poraspid-like, typical of early Lochkovian elsewhere (e.g., Turner et al. 2017). Turner and Murphy (1988, fig. 1.1-6, 8-15, 24) described heterostracan microremains from the Lochkovian Simpson Park section, Nevada. Parkes (1995) also identified heterostracan remains in two levels of BC II (402’, 446’).

As yet, there is no major review of heterostracan dermal scales; a handbook and major description of Cornwallis Island fauna are awaited (D.K. Elliott pers. comm. 2021, Thorsteinsson and Elliott 2022).

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