Gigarimaneta samsoni is a species of epifaunal Petalonamid from the Ediacaran deposits of the Canadian Mistaken Point Formation.[1] G. samsoni grew is a similar manner to Fractofusus and/or Beothukis and grew slightly into the substrate.
| Gigarimaneta Temporal range:
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| Artists interpretation of Gigarimaneta samsoni by Robert Nicholls. A: Top view of G. samsoni. B: Side view. | |
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| Genus: | †Gigarimaneta Glaessner, 1959
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| Species: | †G. samsoni
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| †Gigarimaneta samsoni Taylor et al, 2021
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Gigarimaneta was roughly round and composed of multiple rows of allantoid-like units that further sub-divided into smaller spherocylindrical units but they do not show the signature fractal branching of related fronds however the many divisions in the units of the organism are thought to represent invaginations of the a presumed lower epithelium that increased the surface-are - volume ratio without branching glide symmetry.[1] These divisions from the units probably allowed the taxon to gain a great number of nutrients from the substrate underneath it by culturing the sulfur-oxidizing bacteria; a way of life similar to Chemosynthetic phagotrophy.[2]
See also
editReferences
edit- ^ a b Taylor, Rod S.; Matthews, Jack J.; Nicholls, Robert; McIlroy, Duncan (2021). "A re-assessment of the taxonomy, palaeobiology and taphonomy of the rangeomorph organism Hapsidophyllas flexibilis from the Ediacaran of Newfoundland, Canada". PalZ. 95 (2): 187–207. doi:10.1007/s12542-020-00537-4. S2CID 232377991.
- ^ Taylor, Rod S.; Nicholls, Robert; Neville, Jenna M.; McIlroy, Duncan (2022). "Morphological variation in the rangeomorph organism Fractofusus misrai from the Ediacaran of Newfoundland, Canada". Geological Magazine. 160: 146–166. doi:10.1017/S0016756822000723. S2CID 251687679.