Myadora kaiiwiensis

Myadora kaiiwiensis
Temporal range:
Holotype from Auckland War Memorial Museum (right valve)
Scientific classification
Kingdom: Animalia
Phylum: Mollusca
Class: Bivalvia
Family: Myochamidae
Genus: Myadora
Species:
M. kaiiwiensis
Binomial name
Myadora kaiiwiensis

Myadora kaiiwiensis is a species of bivalve, a marine mollusc in the family Myochamidae.[1] Fossils of the species date to the Castlecliffian stage (1.63 million years ago) of the Early–Middle Pleistocene in New Zealand, and are only known from fossil deposits from the Wanganui Basin.

Description

In the original description, Powell described the species as follows:

Shell of moderate size, transversely elongate-oval, posterior end broadly truncated. The convex right valve has a ridge running from the umbo to the lower extremity of the truncation, and this cuts off a shallowly-concave posterior area. Sculpture consisting of irregularly developed concentric ridges (about 22), which are subobsolete, except towards the margins and where they intersect the posterior ridge. Left valve almost flat, often very slightly convex. Posterior area marked off by a slight flattening. Sculpture of subobsolete flattened concentric ridges, very irregular in their development.[2]

The holotype of the species has a height of 10.50 mm (0.413 in), a length of 13.75 mm (0.541 in), and a thickness of 2.90 mm (0.114 in).[2]

M. kaiiwiensis can be differentiated from modern-day species M. boltoni and M. antipodum due to its smaller size and being less elongated.[3] It has significantly weaker commarginal sculpture when compared to M. antipodum, and while its sculpture resembles M. boltoni, it is more ovate, differently proportioned, and has nearly central beaks and approximately equal ends.[3][2]

Taxonomy

The species was first described by A. W. B. Powell in 1931.[2] The holotype was collected in January 1931 by Powell from 800 m (2,600 ft) northwest of the Kai Iwi Stream mouth near Kai Iwi in the Whanganui District. It is held in the collections of Auckland War Memorial Museum.[4][5]

Distribution

This extinct marine species occurs in the early Castlecliffian stage (1.63 million years ago) of the Early–Middle Pleistocene in New Zealand,[3] with some fossils potentially dating back to the Nukumaruan stage (2.40 million years ago).[6][3][4] Fossils of the species are only known from the Wanganui Basin of New Zealand,[3] including the Wickham Formation.[7]

References

  1. ^ a b Myadora kaiiwiensis A. W. B. Powell, 1931 †. Retrieved through: World Register of Marine Species on 2 February 2026.
  2. ^ a b c d Powell, A. W. B. (1931). "Waitotaran Faunules of the Wanganui System and Descriptions of New Species of Mollusca from the New Zealand Pliocene". Records of the Auckland Institute and Museum. 1: 85–112. ISSN 0067-0464. JSTOR 42905938. Wikidata Q58676540. This article incorporates text from this source, which is under a CC BY 4.0 license.
  3. ^ a b c d e Beu, A. G. (December 2006). "Marine Mollusca of oxygen isotope stages of the last 2 million years in New Zealand. Part 2. Biostratigraphically useful and new Pliocene to recent bivalves". Journal of the Royal Society of New Zealand. 36 (4): 151–338. doi:10.1080/03014223.2006.9517808. ISSN 0303-6758. Wikidata Q99955157.
  4. ^ a b Blom, Wilma M. (2025). "Annotated Catalogue of Fossil and Extant Molluscan Types in the Auckland War Memorial Museum". Bulletin of the Auckland Museum. 22. doi:10.32912/BULLETIN/22. ISSN 1176-3213. OCLC 1550165130. Wikidata Q135397912.
  5. ^ "Myadora kaiiwiensis". Collections Online. Auckland War Memorial Museum. Retrieved 3 February 2026.
  6. ^ Maxwell, P.A. (2009). "Cenozoic Mollusca". In Gordon, D.P. (ed.). New Zealand Inventory of Biodiversity. Volume one. Kingdom Animalia: Radiata, Lophotrochozoa, Deuterostomia. Christchurch: Canterbury University Press. p. 238. ISBN 978-1-877257-72-8.
  7. ^ McIntyre, Avon P.; Kamp, Peter J. J. (1998). "Late Pliocene (2.8 ‐2.4 Ma) cyclothemic shelf deposits, Parikino, Wanganui Basin, New Zealand: Lithostratigraphy and correlation of cycles". New Zealand Journal of Geology and Geophysics. 41 (1): 69–84. doi:10.1080/00288306.1998.9514791.