Hokkaidoconcha morenoensis, Kiel & Campbell & Elder & Little, 2008
publication ID |
https://doi.org/ 10.4202/app.2008.0412 |
persistent identifier |
https://treatment.plazi.org/id/03DC9B54-FFE3-337F-FF89-40537F0BCBBF |
treatment provided by |
Felipe |
scientific name |
Hokkaidoconcha morenoensis |
status |
sp. nov. |
Hokkaidoconcha morenoensis sp. nov.
Fig. 5F, G View Fig .
Etymology: After the type locality at Moreno Gulch, California, USA.
Type material: Holotype: LACMIP 13483 . Specimen with five whorls showing axial ribs across the entire height of the whorls and spiral sculpture on the base; paratype: LACMIP 13484 , from the type locality.
Type locality: Moreno Gulch , California, USA .
Type horizon: Santonian (Upper Cretaceous) seep carbonates at Moreno Gulch, Great Valley Group.
Material.— Type specimens and several specimens from the type locality and from Romero Creek (site 13) .
Diagnosis.—Slender turriculate shell with slightly convex whorls; ribs widely spaces, variably opisthocyrt to opisthocline, on entire whorl or restricted to upper part; base with fine spiral cords.
Description.—Teleoconch with eight or more whorls, suture incised; whorls sculptured by eight to ten varix−like ribs per whorl, interspaces between ribs two to four times the width of the ribs; ribs variably developed on the entire height of the whorl to completely obsolete; aperture unknown. Holotype with five whorls 8 mm high and 3 mm wide, tallest specimen with eight whorls 16 mm high and 4 mm wide.
Discussion.— Hokkaidoconcha morenoensis is most similar to H. tehamaensis but differs in having whorls that are more convex and in lacking the spiral sculpture present on whorl flanks of H. tehamaensis , H. occidentalis , and H. bilirata .
Stratigraphic and geographic range.—Santonian–Campanian (Upper Cretaceous) seep carbonates, Great Valley Group, California, USA.
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