Taylorius litoralis

Taylorius litoralis

Britton, 1960

Common name Weevil
Fossil group Insects
Order Coleoptera
Family Curculionidae
Genus Taylorius
Taxonomic status Accepted
Geological age Ypresian

Summary

The most striking adaptation of Taylorius litoralis was the channel running along the underside of the thorax for its rostrum. The gently curved snout could be drawn back from the prosternum across the mesosternum to the front of the metasternum, where raised flanges enclosed it between the legs. Together with the large basal abdominal segments and parallel-sided elytra, this gave the beetle the protected “hidden-snout” construction seen in several specialised weevil lineages.

Modern work places Taylorius among Aedemonini, a predominantly palaeotropical group that is conspicuous in the London Clay weevil fauna. The fossil does not reveal its host, but plant feeding is strongly expected and an association with woody or robust vegetation is plausible rather than demonstrated. The type series includes a near-complete adult as well as numerous hindbodies, so both the rostral mechanism and the rear body are unusually well represented.

Quick Identification

Look for: a weevil about 4.4 mm long with a moderately slender, gently curved cylindrical rostrum lying in a deep underside channel that continues behind the front coxae across the mesosternum to the front of the metasternum. Vertical flanges border the channel between the front and middle coxae, and the parallel-sided elytra carry rows of large round punctures.

Diagnostic Features

  • Deep median rostral channel continues from the prosternum across the mesosternum to the anterior part of the metasternum.
  • Between the anterior and middle coxae, the rostral channel is laterally enclosed by a raised vertical flange.
  • Rostrum is moderately slender, cylindrical and slightly curved, extending backwards to the level between the middle coxae when retracted.
  • First and second abdominal ventrites together are about twice as long medially as the third to fifth ventrites combined.
  • Elytra are elongate and nearly parallel-sided without tubercles; the third stria has about thirty-three large circular punctures that decrease in size towards the apex.

Fossil Details

Typical size
about 4.4 mm
Preservation
Dorsoventral compression can flatten the rostral channel and make its posterior extent difficult to follow. Legs are often absent, and abrasion can reduce both dense ventral puncturation and elytral rows. Species level separation from other channelled London Clay weevils needs the course of the rostral channel as well as elytral sculpture.

Similar Species

Recorded Fossil Sites

No fossil-site occurrences have yet been recorded for this species.

References

  • Britton, E. B. (1960). Beetles from the London clay (Eocene) of Bognor Regis, Sussex. Bulletin of the British Museum (Natural History), Geology, 4(2), 27–50 View reference
  • Legalov, A. A. (2020). Fossil History of Curculionoidea (Coleoptera) from the Paleogene. Geosciences, 10(9), 358 View reference
Last Reviewed
16 August 2026 Reviewed by Sam Harris