Elphidium hiltermanni
Elphidium hiltermanni
Summary
Elphidium hiltermanni was a benthic elphidiid foraminifer with a planispiral calcitic test. Elphidiids commonly live in shallow-marine sediments and graze or collect bacteria, algae and organic detritus with an extensive pseudopodial network.
The organism itself was a single cell, but the fossil is its microscopic test. In the 2026 Hampshire Basin study this taxon occurs within the London Clay Formation assemblage used to construct the first foraminiferal zonation of the formation.
Quick Identification
Look for: a small lenticular planispiral test with a lobulate margin and distinctive sutural bridges or retral processes visible under good magnification.
Diagnostic Features
- Test planispiral and involute, with both sides broadly similar.
- Overall profile lenticular to compressed.
- Final chambers produce a gently lobulate peripheral outline.
- Sutural zones bear retral processes/bridges characteristic of Elphidium when well preserved.
- Apertural openings occur along the base of the final chamber rather than as one terminal neck.
Fossil Details
Recorded Fossil Sites
No fossil-site occurrences have yet been recorded for this species.
References
- Hart, M. B.; Alex-Sanders, M. E. A.; Smart, C. W. (2026). Can the distribution of foraminifera locate the Early Eocene Climatic Optimum (EECO) and Middle Eocene Climatic Optimum (MECO) events in the Eocene succession of the Isle of Wight (UK)?. Journal of Micropalaeontology, 45(1), 315–334 View reference