Calyptrina striata is an Ediacaran tubular fossil, probably belonging to some kind of tube-dwelling annelid worm.[1][2] The tubes is preserved as a flat carbonaceous organic or pyrite shadows left behind in shales, and as a relief imprints and casts in sandstones.[1] Specimens have been found and documented in numerous Ediacaran localities of the White Sea area of Russia[1] and possibly in Southeast China.[3]

Calyptrina striata
Temporal range: Ediacaran, about 567–550 Ma
Reconstruction of Calyptrina striata.
Scientific classification Edit this classification
Domain: Eukaryota
Kingdom: Animalia
Phylum: Annelida
Family: Sabelliditida
Genus: Calyptrina
Sokolov, 1967
Species:
C. striata
Binomial name
Calyptrina striata
Sokolov, 1967

Morphology and behavior

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It was a very long unbranched cylindrical organic-walled tube, probably of a protein-chitinous composition. The surface of the tube is decorated with transverse wrinkles and rings, as well as thin longitudinal ribs. Most of the Calyptrina tube was located in the sediment under the microbial mats, in a toxic anoxic environment rich in hydrogen sulfide. The short front end of the tube rose vertically above the sea bottom surface.[1] The morphology and habitat of Calyptrina are similar to the tubes and habitat of siboglinids.[2][3][1] At the same time, the biomarker analysis of the organic fossil of Calyptrina indicates that the animal had an intestine and fed on green algae and bacteria, probably filtering them out of the water.[1]

References

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  1. ^ a b c d e f Bobrovskiy, I.; Nagovitsyn, A.; Hope, J. M.; Luzhnaya, E.; Brocks, J. J. (2022). "Guts, gut contents, and feeding strategies of Ediacaran animals". Current Biology. doi:10.1016/j.cub.2022.10.051. PMID 36417903.
  2. ^ a b Sokolov, B.S. (1965). "The most ancient Early Cambrian deposits and sabelliditids (in Russian): Abstracts". All-Union Syposium on Paleontology of Precambrian and Early Cambrian, Novosibirsk: 78–91.
  3. ^ a b Xiao, S. (2002). "Macroscopic Carbonaceous Compressions in a Terminal Proterozoic Shale: A Systemic Reassessment of the Miaohe Biota, South China". Journal of Paleontology. 76 (2): 347–376. doi:10.1666/0022-3360(2002)076<0347:MCCIAT>2.0.CO;2.