Filodrillia turricula

Extinct species of gastropod From Wikipedia, the free encyclopedia

Filodrillia turricula is an extinct species of sea snail, a marine gastropod mollusc, in the family Borsoniidae.[1] Fossils of the species date to middle Miocene strata of the Port Phillip Basin of Victoria, Australia.

Quick facts Scientific classification, Binomial name ...
Filodrillia turricula
Temporal range: middle Miocene
Holotype from Auckland War Memorial Museum
Scientific classification Edit this classification
Kingdom: Animalia
Phylum: Mollusca
Class: Gastropoda
Subclass: Caenogastropoda
Order: Neogastropoda
Family: Borsoniidae
Genus: Filodrillia
Species:
F. turricula
Binomial name
Filodrillia turricula
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Description

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

Shell slender, with sharply angled periphery, situated above middle; outline of whorls lightly concave on shoulder, straight and almost vertical below. Whorls 612, including papillate smooth protoconch of 134 whorls ending in a few brephic axials. Peripheral spiral narrow; three slightly narrower sharply raised spirals below it, lowest at lower suture, and a further 12 spirals on base and neck; those on neck closely spaced; those on base with interspaces 1 to 112 times width of spirals. Axials slender, slightly oblique, stopped at peripheral keel and extending weakly over the base, 15 on penultimate. The shoulder bears four very delicate spiral threads. Posterior sinus deep, rounded, subtubular. Outer lip arcuately projecting as a hollow varix.[2]

The holotype of the species measures 6.5 mm (0.26 in) in height and has a diameter of 2.4 mm (0.094 in).[2]

Taxonomy

The species was first described by A. W. B. Powell in 1944.[2] The holotype was collected at an unknown date prior to 1944 from Fossil Beach, Balcombe Bay / Jullul Bay, Victoria, Australia, and is held by the Auckland War Memorial Museum.[3][4]

Distribution

This extinct marine species occurs in middle Miocene strata of the Port Phillip Basin of Victoria, Australia, including the Gellibrand Formation.[3][5]

References

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