Ustʹ Pinega Formation
The Ust Pinega Formation is an Upper Ediacaran geological formation in northwestern Russia. It spans from around to and contains fossils of the Ediacaran biota throughout its sequence.
Geology
The formation was first established and described from the core of the Ust-Pinega borehole drilled in the settlement of Ust-Pinega, Arkhangelsk Region of Russia, where its thickness is 284 m. Its natural outcrops within the same region are known from the Onega Peninsula and the Winter Coast of the White Sea, as well as from small, isolated outcrops in the basin of the Onega River and on the northern slope of the Vetreny Poyas Ridge.The formation rests with erosion on Proterozoic terrigenous deposits or Archean crystalline rocks. It is subdivided, from bottom to top, into the following Subformations : Tamitsa, Lyamtsa, Arkhangelsk, Verkhovka, Syuzma, Vaizitsa, and Zimnegory. It is unconformably overlain by deposits of the Ediacaran Mezen Formation, as well as by Paleozoic or Quaternary sediments.
In 2003, D.V. Grazhdankin proposed an alternative subdivision scheme for these deposits, based on the original scheme by A.F. Stankovskiy. This scheme includes the Lyamtsa, the Verkhovka, and the Zimnegory Formations. In this revision, the use of the Ust' Pinega Formation was abandoned in favor of these three formations.
Currently, the Ust' Pinega Formation and its subformations remain the official stratigraphic scheme used on state geological maps of Russia.
Dating
The Lyamtsa, Verkhovka and Vaizitsa Subformations contain volcanic ashes. Zircon U-Pb dating of volcanic tuffs from the Verkhovka and Vaizitsa beds has yielded ages of and, respectively. Furthermore, an Rb–Sr age of was obtained for clays of the Arkhangelsk Subformation. The formation is unconformably overlain by the deposits of the Mezen Formation, from the lower part of which a U-Pb age of has been obtained for tuffites.Paleobiota
The Ustʹ Pinega Formation is home to many rare and common Ediacaran fauna, from the well known motile forms such as Dickinsonia and Kimberella, to the rarer, more elusive forms like Ventogyrus and Zolotytsia. All forms within this formation are preserved in layers of ash beds, which are not only good at preserving the fine exterior details of organisms, but also their internals, like Burykhia.Proarticulata
| Genus | Species | Notes | Images |
| Andiva |
| Elongated oval motile organism. | |
| Archaeaspinus | Oval motile organism. | ||
| Armillifera | Elongated oval motile organism. | ||
| Cephalonega | Oval motile organism. | ||
| Cyanorus | Elongated motile organism. | ||
| Dickinsonia | Oval to elongated motile organism. | ||
| Karakhtia | Oval motile organism. | ||
| Keretsa | Elongated motile organism. | ||
| Lossinia | Elongated motile organism. | ||
| Ovatoscutum | Rounded motile organism. | ||
| Palaeoplatoda | Elongated motile organism. | ||
| Paravendia | Elongated motile organism. | ||
| Vendia | Elongated motile organism. | ||
| Yorgia | Oval motile organism. |
Petalonamae
| Genus | Species | Notes | Images |
| Bomakellia |
| Sessile frondose organism. | |
| Charnia | Sessile frondose organism. | ||
| Charniodiscus | Sessile frondose organism. | ||
| Pteridinium | Sessile frondose organism. | ||
| Ramellina | Sessile frondose organism. |
Trilobozoan
| Genus | Species | Notes | Images |
| Albumares |
| Tri-radial organism. | |
| Anfesta | Tri-radial organism. | ||
| Tribrachidium | Tri-radial organism. |
Cnidarian
| Genus | Species | Notes | Images |
| Bonata |
| Discoid organism. | |
| Brachina | Discoid organism. | ||
| Ediacaria | Discoid organism. | ||
| Eoporpita | Discoid organism. | ||
| Inaria | Sac-like organism. | ||
| Medusinites | Discoid organism. | ||
| Staurinidia | Discoid organism. | ||
| Tirasiana | Discoid organism. | ||
| Zolotytsia | Deformed mass of ovals along a mid-line groove. |
Chordata
| Genus | Species | Notes | Images |
| Burykhia |
| Sac-like organism, possible tunicate. |
Annelida
| Genus | Species | Notes | Images |
| Calyptrina |
| Tubular organism. |
''incertae sedis''
| Genus | Species | Notes | Images |
| Cyclomedusa |
| Discoid organism. | |
| Hiemalora | Discoid organism, possibly holdfasts of petalonamids. | ||
| Kimberella | Egg-shaped organism, possible mollusc. | ||
| Mawsonites | Discoid organism. | ||
| Nimbia | Discoid organism. | ||
| Orbisiana | Palaeopascichnid organism. | ||
| Palaeopascichnus | Palaeopascichnid organism. | ||
| Parvancorina | Anchor-shaped organism, possible mollusc or arthropod. | ||
| Solza | Egg-shaped organism. | ||
| Vendotaenid | Ribbon-like organisms. |
Flora
| Genus | Species | Notes | Images |
| Archyfasma |
| Branching macroalgae. | |
| Beltanelliformis | Cyanobacterial colony. | ||
| Eoholynia | Branching macroalgae. | ||
| Favosiphycus | Flattened thallus crust-like, consisting of densely packed cells. | ||
| Gandvikia | Ribbon-shaped macroalgae. | ||
| Mezenia | Sausage shaped macroalgae. | ||
| Serebrina | Encrusting macroalgae. |
Ichnogenera
| Genus | Species | Notes | Images |
| Epibaion |
| Feeding traces of proarticulates. | |
| Kimberichnus | Feeding traces of Kimberella. | ||
| Nenoxites | Movement traces. | ||
| Neonereites | Burrows. | ||
| Planolites | Burrows. |