Pullenia reussi
Pullenia reussi
Summary
Pullenia reussi was a compact benthic foraminifer with an involute planispiral calcitic test. It lived in the sea-floor microhabitat and gathered bacteria and organic particles with pseudopodia extending from the aperture.
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 smooth, compact planispiral test with inflated chambers and a rounded, almost globular outline, but without the strongly five-lobed profile typical of Pullenia quinqueloba.
Diagnostic Features
- Test compact, involute and planispiral.
- Chambers are inflated and separated by depressed sutures.
- Peripheral outline rounded and smooth rather than sharply keeled.
- Final whorl lacks the strongly regular five-lobed outline characteristic of P. quinqueloba.
- Aperture is a low interiomarginal opening at the base of the final chamber.
Fossil Details
Similar Species
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