Vesicomya margotae Beets, 1953
publication ID |
https://doi.org/ 10.4202/app.00756.2020 |
publication LSID |
lsid:zoobank.org:pub:3B7C70AD-CC73-44D5-921E-B1BA0503FC29 |
persistent identifier |
https://treatment.plazi.org/id/03D8B71B-FFB8-F244-A03B-FD917172920A |
treatment provided by |
Felipe |
scientific name |
Vesicomya margotae Beets, 1953 |
status |
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Vesicomya margotae Beets, 1953 View in CoL
Fig. 18 View Fig .
1953 Vesicomya (Waisiuconcha) margotae View in CoL sp. nov.; Beets 1953: 255, pl. 1: 11–15.
Material.— Seven specimens from the Pliocene of Liog-Liog Point : NMNS PM 28410 , 28411 View Materials , 28412 View Materials (five individuals) .
Dimensions (in mm).— NMNS PM 28410, L = 8.3, H = 6.9; NMNS PM 28411, L = 12.5, H = 10.0.
Remarks.— Vesicomya margotae has a hinge dentition like Vesicomya ( Beets 1953: pl. 1: 11, 15) and should therefore not be associated with Waisiuconcha . A very similar extant species is Vesicomya katsuae Kuroda, 1952 from 200–400 m depth in Sagami and Tosa Bays, Japan. That species has a Vesicomya -like hinge ( Kuroda 1952: figs. 7–9) and a lunular incision ( Kuroda 1952: fig. 5), which identifies it as a member of Vesicomya and not of Waisiuconcha (cf., Habe 1976b; Cosel and Salas 2001). Vesicomya margotae differs from V. katsuae by being less elongate and having larger and more elevated umbones. The extant Japanese species Vesicomya nakaii Okutani, 1962 , reported here from the late Pliocene of Cambantug Point (below), differs from both V. margotae and V. katsuae by being shorter and higher, and by having more prominent and elevated umbones.
Stratigraphic and geographic range.—Late Miocene: southern Sulawesi, Indonesia. Late Pliocene: Leyte, Philippines.
NMNS |
National Museum of Natural Science |
PM |
Pratt Museum |
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