Kakabekia barghoorniana
Classification
Kingdom: Plantae
Phylum: Plantaeincertaesedis
Class: Unclassified
Order: Unclassified
Family: Unclassified
Genus: Kakabekia
Species: Kakabekia barghoorniana
Kakabekia barghoorniana was named for the region
Description and Significance
Kakabekia barghoorniana was first described by Sanford Siegel in 1966 (it was first seen in culture in 1964) as a living organism that appeared nearly identical to a microfossil that had been discovered in Ontario which had been thought to have no relationship to any currently living species by a Harvard paleontologist Elso Barghoorn. The fossil was found in the gunflint range chert deposits that date back to the middle Precambrian period in what woiuld have likely been shallow lakes (cite main article). K. barghoorniana was first found in a high ammonium soil sample from Wales and was subsequently isolated from high ammonium environments in Alaska. Subsequently, Kakabekia was isolated from soil samples near the edge of a glacier in Iceland; the species is at least cold-tolerant. The soil from which Kakabekia was cultured was high in content of carbon, hydrogen, and organic nitrogen with low levels of sodium, potassium, and titanium. Kakabekia can be grown in glucose free media but growth is slowed significantly. Even with other nitrogen sources, Kakabekia cannot be grown without ammonia (Living relative article).
K. barghoorniana is a umbellate microbe that is not fully classified. The structure was initially described without distinct nuclei, however subsequent research revealed that the microbe is actually a eukaryote of the kingdom plantae. Structurally, the organism has a mantle with multiple rays that forms the top of the "umbrella" with a slender stalk leading to a sphrerical bulb (main article). The organism is oxygen indifferent, with few heme enzymes and no phenol oxidases. Furthermore, the species has absolutely no ability to store lipid or polysaccharide (main article). Kakabekia appears to preferentially utilize glucose as a carbon and energy source but it has the ability to function without; likely through photosynthetic machinery.
K. barghoorniana was discovered during research attempting to isolate organisms that could survive in high ammonia environments. This is of particular interest to astro-biology; for example multiple gas giant/moons have atmospheres with very high ammonium content. Kakabekia is also a living relative of a Precambrian microfossil and provides a model organism that would have survived and flourished in the primative, reducing environment of the Precambrian era.
