Where: Russian Federation (64.4° N, 40.7° E: paleocoordinates 62.1° S, 23.0° E)
• coordinate based on political unit
When: Mezen' Formation, Ediacaran (635.0 - 541.0 Ma)
• Encompasses the Vendian Period. The unit containing the Y. waggoneri specimens lies at the base of the ""Fifth Cyclite"" or slightly above the base of the Yorga Beds. The imprints occur completely on the bottom of beds. Level 2: This level is stratigraphically slightly higher than Level 1 and corresponds to the base of the lense like sandstone bed. The beds' thickness is about 0.10m and can be traced 200-300m.
• bed-level stratigraphic resolution
Environment/lithology: transition zone or lower shoreface; lithified siltstone and lithified shale
Preservation: cast, replaced with silica, replaced with pyrite
Collection methods: bulk,
Primary reference: A. Y. Ivantsov. 1999. A new Dickinsonid from the Upper Vendian of the White Sea Winter Coast (Russia, Arkhangelsk Region). Paleontological Journal 33(3):211-221 [M. Patzkowsky/P. Borkow/P. Wagner]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 10774: authorized by Mark Patzkowsky, entered by Phil Borkow on 21.06.2001
Creative Commons license: CC BY (attribution)
Taxonomic list
Dickinsonia costata Sprigg 1947
Dickinsonia cf. tenuis Glaessner and Wade 1966 | |
unclassified | |
| |
Vendiamorpha | |
Vendia sokolovi Keller 1969 | |
Cephalozoa | |
Yorgia waggoneri Ivantsov 1999 |