Tibetothyris hamishi, MACFARLAN, 2023

MACFARLAN, DONALD ALEXANDER BANKIER, 2023, Otapirian (Rhaetian) Terebratulida (Brachiopoda) of Zealandia, Zootaxa 5374 (1), pp. 1-34 : 9-12

publication ID

https://doi.org/ 10.11646/zootaxa.5374.1.1

publication LSID

lsid:zoobank.org:pub:072341AB-7693-4DF3-9286-D69D0BBD8FAD

DOI

https://doi.org/10.5281/zenodo.10168048

persistent identifier

https://treatment.plazi.org/id/073F87AD-FFA7-5A76-FF4B-FA59FACFF883

treatment provided by

Plazi

scientific name

Tibetothyris hamishi
status

sp. nov.

Tibetothyris hamishi View in CoL n. sp.

Fig. 7 1–9, 8A–B View FIGURE 7 View FIGURE 1 View FIGURE 2 View FIGURE 3 View FIGURE 4 View FIGURE 5 View FIGURE 6 View FIGURE 8 View FIGURE 9 .

2019: Aulacothyris sp. A MacFarlan p. 574, fig. 13 a-d. (NZGS BR 3207 only).

Holotype. OU 47309 , a shelly specimen with an external mould of the dorsal valve and beak, from F45/f329, JDC 4216 , west of Dolamore Park , Hokonui Hills. Collected by J.D. Campbell and S. R. Owen, 21/10/1992. Shell material altered to clay or zeolite.

Derivation of name. This species is named for Dr Hamish Campbell of GNS Science.

Material. The data series consists of fifteen specimens, thirteen of which yielded valid measurements.

New Caledonia. île Ducos: NC/f050 ( GS 12763), NC/f0087 (AU 7168)

Kawhia Syncline. Coast south of Arataura Pt: R 15/f8837 (AU 69), R 15/f8838 (AU 70). North Marokopa Coast: R 16/f6898 ( GS 10009), R 16/f8645 (? GS 10006). Marokopa: R 16/f0337 (AU 12074). Pomarangai Rd E of Moeatoa: R 16/f8877A (AU 8987).

Southland Syncline. Otapiri – Taylors Stream: E45/f0279 ( JDC 4059), E45/f9622 ( JDC 1296). Dolamore Park: F45/f0329 ( JDC 4216). Waimumu Valley: F45/f8523 ( GS 5188).

Description. Small to medium sized terebratulide with elongate elliptical outline. The dorsal valve is moderately convex posteriorly and flatter anteriorly, with a shallow, rounded sulcus developing close to the beak and extending anteriorly.

The ventral valve is strongly convex posteriorly. The anterior part has concave flanks, and a strongly convex central part. The anterior commissure is shallowly sulcate. The shell surface is smooth or has a few strong, stepped concentrics anteriorly. Punctae are coarse and closely spaced.

The beak is large and triangular with a bluntly rounded tip. The foramen is large, circular, mesothyrid, and is surrounded by a short pedicle collar ( Fig. 7.1a, 7.3a View FIGURE 7 , 8B View FIGURE 8 ). The beak ridges are strong, bluntly rounded. Deltidial plates are poorly shown and are small and widely disjunct (fig. 7.1a, 7.3a).

On the dorsal valve the hingeplate has a broad, shallow U-shaped septalium supported by a wide, shallow median septum with fine longitudinal grooves which appear to be muscle attachments ( Fig 7.8a View FIGURE 7 , 8A, B View FIGURE 8 ), and a small cardinal process ( Fig. 8B View FIGURE 8 ). The posterior tip of the dorsal valve reaches the anterior of foramen. The dental plates are short, widely separated and divergent ( Fig. 7.8a, b View FIGURE 7 , 8B View FIGURE 8 ).

Dimensions. Dimensions of the holotype and representative specimens, and statistics for all measurable specimens are shown in Table 2. A View TABLE 2 length vs width graph is shown in Fig. 9A View FIGURE 9 .

Range and Distribution. Otapirian of New Caledonia, Kawhia Syncline and Southland. Nearly all the material is late Otapirian, but the specimen from NC/f0087 (île Ducos, New Caledonia) is early Otapirian.

Remarks. The shape is distinctive. Specimens from the Oretian and Otamitan of Southland are of similar shape and size but lack the strongly convex central part and concave flanks of the new species. From the limited material examined, they appear to belong to a separate but related species.

BR 3207 (R16/f6898, GS 10009) was figured in MacFarlan (2019, fig 13:13a-d) as Aulacothyris sp. A . It is badly distorted, but re-examination shows that it is much better placed in the new species.

This species is larger than T. johnstoni , less inflated, and lacks the strong folding on the ventral valve. The dental plates are short and widely separated, resembling those of T. johnstoni rather than T. depressa .

R

Departamento de Geologia, Universidad de Chile

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