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Limopsis marwicki

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Limopsis marwicki
Temporal range: 2.40  Ma
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Limopsis marwicki MA70398-a.jpg
Holotype from Auckland War Memorial Museum
Scientific classification OOjs UI icon edit-ltr.svg
Kingdom: Animalia
Phylum: Mollusca
Class: Bivalvia
Order: Arcida
Family: Limopsidae
Genus: Limopsis
Species:
L. marwicki
Binomial name
Limopsis marwicki

Limopsis marwicki is an extinct species of marine bivalve mollusc in the family Limopsidae. [1] Fossils of the species date to the Pleistocene in New Zealand.

Contents

Description

Reverse view of holotype Limopsis marwicki MA70398-b.jpg
Reverse view of holotype

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

Shell small, obliquely-oval, moderately inflated, beaks low. Sculpture weak, consisting of concentric linear grooves which cut up the surface into flat, closely spaced interspaces, and are crossed by weak radials on and near to the anterior and posterior areas. These radials are produced into microscopic scale-like projections where they cross the lower edge of each interspace. Hinge typical. In young specimens the hinge teeth extend right across the hinge plate, but in the adults the teeth in the middle part of the hinge are sub-obsolete. The fully developed teeth number six on each extremity of the hinge. Ligamental area rather narrowly triangular. Valve margins smooth and bevelled. [2]

The holotype of the species has a height of 11.5 mm (0.45 in), length of 11 mm (0.43 in) and a single valve thickness of 3.25 mm (0.128 in). [2] It can be differentiated from L. invalida due to L. invalida being narrower, thinner-shelled, smaller, more inflated and having a smooth marginal flange. [3]

Taxonomy

The species was first described by A.W.B. Powell in 1938, [2] who named the species after New Zealand paleontologist John Marwick. [4] The species likely represents a Limopsis lineage that has become extinct, due to differences seen between it and extant New Zealand members of Limopsis. [3] The holotype was collected at a date prior to 1939 by A. W. B. Powell, from lighthouse reef, Castlepoint, Wairarapa, New Zealand, and is held by the Auckland War Memorial Museum. [5] [6]

Distribution

This extinct marine species occurs in Pleistocene (Nukumaruan stage) of New Zealand, dating to 2.40 million years before the present, [7] including the Castlepoint Formation. [8]

References

  1. Limopsis marwicki A. W. B. Powell, 1938 † . 5 March 2026. Retrieved through: World Register of Marine Species .
  2. 1 2 3 Powell, A. W. B. (1938). "A Pliocene Molluscan Faunule from Castle Point". Records of the Auckland Institute and Museum . 2: 157–164. ISSN   0067-0464. JSTOR   42905977. Wikidata   Q58676603.CC BY icon-80x15.png This article incorporates text from this source, which is under a CC BY 4.0 license.
  3. 1 2 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. Keyes, I. W. (December 1971). "Genera and species of living and fossil organisms named in honour of Dr John Marwick". New Zealand Journal of Geology and Geophysics . 14 (4): 631–633. doi:10.1080/00288306.1971.10426325. ISSN   0028-8306. Wikidata   Q114642760.
  5. 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.
  6. "Limopsis marwicki". Collections Online. Auckland War Memorial Museum . Retrieved 5 March 2026.
  7. 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. 234. ISBN   978-1-877257-72-8.
  8. Buckeridge, John S.; Beu, Alan G.; Gordon, Dennis P. (19 September 2018). "Depositional environment of the early Pleistocene Castlepoint Formation, New Zealand: a canyon fill in situ". New Zealand Journal of Geology and Geophysics . 61 (4): 524–542. doi:10.1080/00288306.2018.1516227. ISSN   0028-8306. Wikidata   Q129215981.
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