Zolotytsia: Difference between revisions
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Removing Zolotytsia.jpg; it has been deleted from Commons by Krd because: No permission since 3 August 2023. |
the formation is called Yarishyvska which is part of the larger Mohyliv-Podilskyi Group, which I guess caused the confusion. Tags: Visual edit Mobile edit Mobile web edit |
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==Occurrence== |
==Occurrence== |
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Fossils have been found in the [[Ust' Pinega Formation]], located in Northern [[Russia]];<ref>{{Cite web|url=https://ipfs.fleek.co/ipfs/QmXoypizjW3WknFiJnKLwHCnL72vedxjQkDDP1mXWo6uco/wiki/Ust%E2%80%99_Pinega_Formation.html|title=Ust' Pinega Formation|website=ipfs.fleek.co|access-date=Mar 16, 2022}}</ref> the [[Valdai Group]], located in Russia; the [[Bernashevka Beds]]; the [[ |
Fossils have been found in the [[Ust' Pinega Formation]], located in Northern [[Russia]];<ref>{{Cite web|url=https://ipfs.fleek.co/ipfs/QmXoypizjW3WknFiJnKLwHCnL72vedxjQkDDP1mXWo6uco/wiki/Ust%E2%80%99_Pinega_Formation.html|title=Ust' Pinega Formation|website=ipfs.fleek.co|access-date=Mar 16, 2022}}</ref> the [[Valdai Group]], located in Russia; the [[Bernashevka Beds]]; the [[Yarishyvska Formation]], located in [[Ukraine]]<ref name=Fedonkin1983Ukr>{{cite book | title=The Vendian of the Ukraine | year=1983 | publisher=Naukova Dumka | pages=128–139 | author=Fedonkin, M. A. |editor1=Velikanov, V. A. |editor2=Asseeva, E. A. |editor3=Fedonkin, M. A. | chapter=Non-skeletal fauna of Podolia, Dniester River valley | language = Russian | location=Kiev}}</ref> and in the [[Krol Formation]], located in [[India]].<ref>{{Cite journal |last1=Tiwari |first1=Meera |last2=Pant |first2=Charu C. |date=January 2004 |title=Neoproterozoic silicified microfossils in Infra Krol Formation, Lesser Himalaya, India |url=https://www.researchgate.net/publication/281350593 |journal=Himalayan Geology |volume=25 |issue=1 |pages=1–21 |via=researchgate.net}}</ref> |
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==See also== |
==See also== |
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Revision as of 20:54, 19 January 2024
| Zolotytsia Temporal range: about
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| Zolotytsia biserialis | |
Scientific classification 
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| Domain: | Eukaryota |
| Kingdom: | Animalia |
| Phylum: | Cnidaria |
| Genus: | †Zolotytsia Fedonkin, 1981 |
| Species: | †Z. biserialis
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| Binomial name | |
| †Zolotytsia biserialis Fedonkin, 1981
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Zolotytsia is an extinct genus of fossil animals from the late Ediacaran period (Vendian) which contains only one known species, Z. biserialis. Specimens of this species have been found in Russia, Ukraine and India.[1]
Description
Specimens exhibit two distinctive rows of oval-shaped structures, positioned either side of a mid-line groove, each row being divided by a deep, but narrow groove. The lack of symmetry in the oval bodies has been attributed to possible deformation after death.[1]
Occurrence
Fossils have been found in the Ust' Pinega Formation, located in Northern Russia;[2] the Valdai Group, located in Russia; the Bernashevka Beds; the Yarishyvska Formation, located in Ukraine[3] and in the Krol Formation, located in India.[4]
See also
References
- ^ a b Fedonkin, Mikhail A.; Sciences), Mikhail A. (Head Fedonkin, Laboratory of Precambrian Organisms Russian Academy of; Gehling, James G.; Museum), James G. (Senior Curator Gehling, retired 6 27 2019 South Australian; Grey, Kathleen; Narbonne, Guy M.; Vickers-Rich, Patricia; University), Patricia (Director Vickers-Rich, Monash (Mar 16, 2007). The Rise of Animals: Evolution and Diversification of the Kingdom Animalia. JHU Press. ISBN 9780801886799. Retrieved Mar 16, 2022 – via Google Books.
{{cite book}}: CS1 maint: multiple names: authors list (link) CS1 maint: numeric names: authors list (link) - ^ "Ust' Pinega Formation". ipfs.fleek.co. Retrieved Mar 16, 2022.
- ^ Fedonkin, M. A. (1983). "Non-skeletal fauna of Podolia, Dniester River valley". In Velikanov, V. A.; Asseeva, E. A.; Fedonkin, M. A. (eds.). The Vendian of the Ukraine (in Russian). Kiev: Naukova Dumka. pp. 128–139.
- ^ Tiwari, Meera; Pant, Charu C. (January 2004). "Neoproterozoic silicified microfossils in Infra Krol Formation, Lesser Himalaya, India". Himalayan Geology. 25 (1): 1–21 – via researchgate.net.