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Väike Pakri, Estonia
| Lat/Long (Decimal) | 59.3347,24 |
|---|---|
| Co-ordinates Derivation | estimated from map |
| Mindat.org Region (for given coordinates) | Estonia |
Collections
| Collection | Reference | Stratigraphic Name | Comments | Lithology | Age |
|---|---|---|---|---|---|
| Väike Pakri, B III gamma zone | Rubel M. P. (1963) | "B III gamma", in Rubel (1963) "B III gamma zone mit Asaphus eichwaldi, Vaginatenkalk", in Öpik (1932) | "limestone" | 466 - 460.9 Ma Middle Ordovician | |
| Väike Pakri, Osmussar Member | Rubel M. P. (1963) | Osmussar | "B III gamma O", in Rubel (1963) | "limestone" | 466 - 460.9 Ma Middle Ordovician |
| Väike Pakri, Orthoceras Lst. | Bassler R. S. (1911) | "Orthoceras Limestone, B3", in Bassler (1911) | "limestone" | 468.1 - 463.5 Ma Middle Ordovician | |
| Väike Pakri, B II alpha zone | Rubel M. (1961) | "B II alpha", in Rubel (1961) = Törva substage | "limestone" | 471.8 - 468.1 Ma Ordovician | |
| Väike Pakri, B II beta zone | Rubel M. (1961) | "B II beta", in Rubel (1961) = Vääna substage "B II beta, Megalaspiskalk ", in Öpik (1932) | "limestone" | 471.8 - 468.1 Ma Ordovician | |
| Väike Pakri, B III beta zone | Öpik A. (1932) | "B III beta", in Öpik (1932) | "limestone" | 471.8 - 466 Ma Ordovician | |
| Väike Pakri, Kalvi Member | Rubel M. (1961) | Kalvi | "B II gamma K", in Rubel (1961) | "limestone" | 471.8 - 468.1 Ma Ordovician |
| Väike Pakri, Lahepera Member | Rubel M. (1961) | Lahepera | "B II gamma L", in Rubel (1961) | "limestone" | 471.8 - 468.1 Ma Ordovician |
| Väike Pakri, Saka Member | Rubel M. (1961) | Saka | "B II alpha S", in Rubel (1961) = Törva substage | "limestone" | 471.8 - 468.1 Ma Ordovician |
| Väike Pakri, Telinõmme Member | Rubel M. (1961) | Telinõmme | "B II beta T", in Rubel (1961) = Vääna substage | "limestone" | 471.8 - 468.1 Ma Ordovician |
Recorded Fossils
References
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
