Mesopeplum Iredale, 1929
publication ID |
https://doi.org/ 10.3853/j.2201-4349.70.2018.1670 |
publication LSID |
lsid:zoobank.org:pub:8084C---- |
DOI |
https://doi.org/10.5281/zenodo.5305901 |
persistent identifier |
https://treatment.plazi.org/id/039A87AD-F825-3678-FEDE-2CCFFAF5FD3A |
treatment provided by |
Felipe |
scientific name |
Mesopeplum Iredale, 1929 |
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Mesopeplum Iredale, 1929 View in CoL
Mesopeplum Iredale, 1929: 162 View in CoL . Type species (by original designation): Mesopeplum caroli Iredale, 1929 View in CoL (= Chlamys fenestrata Hedley, 1901 View in CoL ); Recent, New South Wales, Australia.
Dendopecten Hertlein, 1936: 26 View in CoL . Type species (by original designation): Pecten dendyi Hutton, 1902 View in CoL ; early Pliocene , Momoe-a-toa Shellbed, Chatham Island, New Zealand.
Diagnosis. Mesopeplini with weakly subdivided radial plicae or costae on large radial plicae (five plicae in many species); left valve flat to weakly convex, right valve strongly convex; pre-radial dissoconch with reticulate commarginal and antimarginal microsculpture; radially sculptured area of disc with widely spaced commarginal lamellae; internal rib carinae prominent near ventral margin; resilial teeth prominent early in ontogeny but weak or absent in late ontogeny; ctenolium obsolete or almost so in late ontogeny in some species, functional in others.
Distribution. Late Eocene–Recent. New Zealand, temperate Western Australia, South Australia, Tasmania, New South Wales and southern Queensland, living in the littoral to bathyal zones on soft sediment.
For fossil records see Beu & Maxwell (1990), Beu (1995) and Beu & Darragh (2001). The holotype of Mesopeplum polymorphoides ( Zittel, 1865) (Beu et al., 2012: fig. 11B) from Glen Massey Formation at Waikato South Head, southwest Auckland, is early Whaingaroan in age, and so late Eocene (Priabonian). Also, a specimen of a typical Mesopeplum species collected by Prof. T. Kotaka from the Point Elizabeth section, north of Greymouth, Westland (IGPS96853) is Kaiatan or Runangan in age (Bartonian– Priabonian). Mesopeplum definitely occurs in late Eocene rocks in New Zealand, although suitable facies for it apparently are rare.
Discussion. Hertlein (1969, p. N366) treated Mesopeplum and its supposed junior synonym Notochlamys Cotton, 1930 as a subgenus of Semipallium Jousseaume in Lamy, 1928, placed in the Decatopecten group. Currently Mesopeplum and Notochlamys are considered to be valid genera ( Waller, 1991) with different ancestries. Mesopeplum was placed in Mesopeplini by Waller (2006a) whereas Notochlamys is retained in Pedini .
Figure 28. Distribution of Mesopeplum fenestratum (Hedley) .
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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Mesopeplum Iredale, 1929
Dijkstra, Henk H. & Beu, Alan G. 2018 |
Mesopeplum
Iredale, T 1929: 162 |