Lucinoma zapotalensis ( Olsson, 1931 )
publication ID |
https://doi.org/ 10.4202/app.00631.2019 |
persistent identifier |
https://treatment.plazi.org/id/F104879E-3B25-AD2B-F521-7402FE3AFB21 |
treatment provided by |
Felipe |
scientific name |
Lucinoma zapotalensis ( Olsson, 1931 ) |
status |
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Lucinoma zapotalensis ( Olsson, 1931) View in CoL
Fig. 5 View Fig .
1931 Phacoides (Lucinoma) zapotalensis View in CoL sp. nov.; Olsson 1931: 49, pl. 5: 2, 5.
Material.— Three specimens ( NRM Mo187011–187013) and several unnumbered, mostly fragmentary specimens from Cerro La Salina blocks 1, 3, 6–9, upper Oligocene, Talara Basin, Peru .
Remarks.—This species was reported by Olsson (1931) only from the Mambri shales near Zapotal in southern Ecuador, but not from any of the seep deposits in the Heath shale in northern Peru. According to Olsson (1931), the Mambri shales are the equivalent of the Heath shale and also of late Oligocene age. Similar is the “middle” Oligocene Lucinoma playaensis ( Olsson, 1964) from the Playa Rica grits in northern Ecuador, though it differs from L. zapotalensis by having more numerous and more narrowly spaced ribs and a more rounded posterodorsal margin ( Olsson 1964: pl. 6: 7). Lucinoma acutilineatum ( Conrad, 1849) from the Miocene Astoria Formation in Oregon and Washington state, USA, is quite similar, but appears to differ from L. zapotalensis by being less inflated and having more widely spaced, and sharper, commarginal ribs; it also seems to have a more angular outline than L. zapotalensis ( Conrad 1849; Moore 1963).
Stratigraphic and geographic range.—Early Oligocene of the Talara Basin, northern Peru.
NRM |
Swedish Museum of Natural History - Zoological Collections |
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