Kakabekia


Kakabekia is an about two billion-year-old fossil genus of microorganism from the Gunflint Chert. Kakabekia barghoorniana is a living fossil of this genus.

Anatomy

Kakabekia umbellata, as described by Barghoorn and Tyler in 1965 has an umbellate “mantle”, a stalk-like “stipe” and a “bulb” attached to it. Morphology of K. barhoorniana differs; it has a round structure with radial segmentation. They have a ring around this structure. Feulgen-positive material was seen in “clots” in K. barghooriniana cytoplasms, placing them in the Prokaryotes.

Distribution

Kakabekia umbellata is known from the Gunflint chert of Canada. K. barghoorniana was first discovered in a soil sample cultured in ammonia from Harlech Castle, Wales in 1968. Further research found K. b. in Iceland and Alaska, as well as other locations in Wales.

Metabolism

Kakabekia has an unusual metabolism. While it has no need for oxygen in its growth, it is not inhibited by it, like Clostridium. This, and the fact that it has some of the oxygen-utilising enzymes, suggest that it is a transition stage of oxygen-utilisation. Kakabekia barghoorni can only be grown in ammonia-rich conditions. This may reflect ancient atmosphere composition.

Ontogeny

Barghoorn and Tyler propose an ontogeny where, starting from a spore, the stipe is grown which then produced the umbellate "mantle". In 1967, Licari and Cloud noted that many fossil "Huroniosporas" have holes or "apertures" in them, suggesting a detachment point from Kakabekia stipes. However, based on observations of living K. barghoorniana, Siegel et. al. came to a very different conclusion. They found that the spore-like bodies would grow into a larger, spherical organism, encircled by the ring described above. Then, divisions form radiating from the center, and a stipe grows and releases a spore. After about 10 days, the organism degenerates and dies.