Anabarites
Anabarites is a problematic lower Cambrian genus, and is one of the small shelly fossils. It was abundant in the early Tommotian and is also found in the Nemakit-Daldynian.[1] The fossils represent the triradially symmetrical mineralised tube in which the organism dwelt; it was sedentary.[2] It is named after the Anabar region in Yakutia, Russia; its name does not imply 'heavy'.[3]
| Anabarites | |
|---|---|
| Scientific classification | |
| Kingdom: | |
| Phylum: | |
| Class: | Angustiochreida Valkov & Syssoiev, 1970 |
| Family: | Anabaritidae Glaessner, 1979 |
| Genus: | Anabarites Missarzhevsky, 1969 |
Further reading
For images, see Matthews, S. C.; Missarzhevsky, V. V. (1975). "Small shelly fossils of late Precambrian and early Cambrian age: a review of recent work". Journal of the Geological Society. 131 (3): 289–303. doi:10.1144/gsjgs.131.3.0289.
- Kouchinsky, Artem; Bengtson, Stefan (2002). "The tube wall of Cambrian anabaritids" (PDF). Acta Palaeontol. Pol. 47 (3): 431–444.
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References
- Felitsyn, S. B.; Gubanov, A. P. (2002). "Nd isotope composition of early Cambrian discrete basins". Geological Magazine. 139 (2). doi:10.1017/S0016756801006252.
- Yi, Q.; Bengtson, S. (1989). "FOSSILS AND STRATA Shards of the Cambrian explosion". Lethaia. 22 (3): 270–270. doi:10.1111/j.1502-3931.1989.tb01341.x.
- Matthews, S. C.; Missarzhevsky, V. V. (1975). "Small shelly fossils of late Precambrian and early Cambrian age: a review of recent work". Journal of the Geological Society. 131 (3): 289–303. doi:10.1144/gsjgs.131.3.0289.
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