BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems
Toyen - Slemmestad, Skedsmo, Lillestrøm, Viken, Norway
Formation | Toyen |
---|---|
Member | Slemmestad |
Age: | 479 - 466 Ma Ordovician |
Interval | Arenig |
Lithology | shale |
Number of Collections | 1 |
Number of Occurrences | 9 |
Recorded Sample Locations
Location | Region | Stratigraphic Name |
---|---|---|
Trematis-bivalve assemblages | Skedsmo, Lillestrøm, Viken, Norway | Toyen - Slemmestad |
Associated Units
Stratigraphic Name | Age | Lithology | Occurrence Records |
---|---|---|---|
Alum Shale | 182 - 176 Ma Early Jurassic | shale/"limestone", "shale", "limestone"/"shale", grainstone, mudstone, "shale"/lime mudstone, "limestone" | 428 |
Arnestad | 458 - 450 Ma Late/Upper Ordovician | shale/"limestone", "shale", "limestone"/"shale", "limestone" | 159 |
Arnestad or Frognerkilen | 453 - 445 Ma Late/Upper Ordovician | lime mudstone/"limestone" | 1 |
Elnes | 464 - 461 Ma Middle Ordovician | shale/"limestone", "shale", "limestone" | 122 |
Elnes - Engervik | 464 - 461 Ma Middle Ordovician | shale/"limestone", "limestone", "shale" | 124 |
Elnes - Hakavik | 466 - 461 Ma Middle Ordovician | sandstone/"shale", "shale"/"limestone", mudstone/grainstone | 25 |
Elnes - Helskjer | 466 - 458 Ma Middle Ordovician | limestone/"shale", "limestone" | 25 |
Elnes - Sjostrand | 464 - 461 Ma Middle Ordovician | shale/"limestone" | 16 |
Frognerkilen | 458 - 452 Ma Late/Upper Ordovician | limestone/"shale", "limestone", "shale"/"limestone" | 74 |
Hovinsholm | 461 - 456 Ma Ordovician | shale/sandstone | 13 |
Husbergoya Shale | 456 - 446 Ma Late/Upper Ordovician | shale/siltstone | 32 |
Langara | 445 - 443 Ma Paleozoic | limestone/"shale", siltstone, "limestone", sandstone | 297 |
Langoyen | 445 - 443 Ma Paleozoic | sandstone, "limestone", "limestone"/"shale", siltstone | 122 |
Nakholmen | 456 - 452 Ma Late/Upper Ordovician | lime mudstone/"limestone", "shale"/"limestone", "limestone", "shale" | 93 |
Solvang | 456 - 446 Ma Late/Upper Ordovician | limestone/"shale", "limestone", "shale" | 216 |
Solvang - Upper | 452 - 450 Ma Late/Upper Ordovician | limestone | 40 |
Steinvika Limestone - Bunes | 458 - 452 Ma Late/Upper Ordovician | reef rocks | 24 |
Toyen - Galgeberg | 479 - 466 Ma Ordovician | shale | 6 |
Toyen - Hagastrand | 479 - 466 Ma Ordovician | shale/"limestone" | 10 |
Venstop | 450 - 446 Ma Late/Upper Ordovician | shale/"limestone" | 37 |
Vollen | 458 - 450 Ma Ordovician | limestone/"shale", "shale"/"limestone", "limestone" | 136 |
Recorded Fossils
Accepted Name | Hierarchy | Age |
---|---|---|
Glyptograptus sp. genus | Animalia : Hemichordata : Graptolithina : Bireclinata : Retiolitidae : Glyptograptus | 478.6 - 466 Ma Ordovician |
Didymograptus sp. genus | Animalia : Hemichordata : Dichograptidae : Didymograptus | 478.6 - 466 Ma Ordovician |
Dichograptus sp. genus | Animalia : Hemichordata : Graptolithina : Dichograptus | 478.6 - 466 Ma Ordovician |
Glossograptus sp. genus | Animalia : Hemichordata : Graptolithina : Glossograptus | 478.6 - 466 Ma Ordovician |
Isograptus sp. genus | Animalia : Hemichordata : Graptolithina : Isograptus | 478.6 - 466 Ma Ordovician |
Schizograptus sp. genus | Animalia : Hemichordata : Graptolithina : Schizograptus | 478.6 - 466 Ma Ordovician |
Trigonograptus sp. genus | Animalia : Hemichordata : Graptolithina : Trigonograptus | 478.6 - 466 Ma Ordovician |
Phyllograptus sp. genus | Animalia : Hemichordata : Graptolithina : Phyllograptidae : Phyllograptus | 478.6 - 466 Ma Ordovician |
Tetragraptus sp. genus | Animalia : Hemichordata : Dichograptidae : Tetragraptus | 478.6 - 466 Ma Ordovician |
References
Erdtmann B. D. (1965) Outline stratigraphy of graptolite-bearing 3B (Lower Ordovician) strata in the Oslo region, Norway, Norsk Geologiske Tidsskrift 45, 481-547 |
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!