Saprosites cascus
Saprosites cascus
Summary
A compact little scarab, Saprosites cascus is known principally from its strongly sculptured hindbody. The underside carries coarse punctures and deeply marked basal bands across the abdominal segments, while the elytra bear punctured longitudinal rows. These features place the animal among the small saprositic scarabs rather than the larger, more familiar dung beetles and chafers.
Living Saprosites are usually found in rotting wood, beneath bark or in litter. That makes a concealed deadwood or litter habitat a reasonable interpretation for the London Clay species, but its actual food is not preserved and the immature stages of the genus are themselves poorly known. The four type specimens are small pyritised body fragments, so the ecology must remain more cautious than the morphology.
Quick Identification
Look for: a scarab hindbody about 2.6 mm long with a deep median groove on the metasternum, coarse ventral punctures and a distinctive row of squarish punctures along the front edge of each abdominal ventrite, producing a longitudinally strigose basal band. The elytra have punctured longitudinal striae.
Diagnostic Features
- Anterior margin of each visible abdominal ventrite carries a transverse row of quadrate punctures separated by narrow ridges, producing a longitudinally strigose basal band.
- Mesosternum has a median longitudinal ridge with a fine central groove that continues posteriorly into a deep median metasternal groove.
- Metasternum is coarsely punctured, with the punctures most crowded anteriorly and towards the sides.
- Abdominal ventrites are coarsely and densely punctured laterally but much more sparsely punctured, or nearly smooth, medially.
- Elytra bear longitudinal striae composed of deep punctures.
Fossil Details
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