BETA TEST - Fossil data and pages are very much experimental and under development. Please report any problems
Odernheim-Lauterecken, Alsenz, Nordpfälzer Land, Donnersbergkreis, Rhineland-Palatinate, Germany
Formation | Odernheim-Lauterecken |
---|---|
Age: | 299 - 296 Ma Paleozoic |
Interval | Asselian |
Lithology | shale/sandstone |
Number of Collections | 1 |
Number of Occurrences | 36 |
Recorded Sample Locations
Location | Region | Stratigraphic Name |
---|---|---|
Alsenz | Alsenz, Nordpfälzer Land, Donnersbergkreis, Rhineland-Palatinate, Germany | Odernheim-Lauterecken |
Recorded Fossils
Accepted Name | Hierarchy | Age |
---|---|---|
Calamostachys sp. genus | Plantae : Tracheophyta : Polypodiopsida : Equisetales : Calamitaceae : Calamostachys | 298.9 - 295.5 Ma Paleozoic |
Lepidostrobophyllum sp. genus | Plantae : Lepidodendraceae : Lepidostrobophyllum | 298.9 - 295.5 Ma Paleozoic |
Pecopteris sp. genus | Plantae : Tracheophyta : Polypodiopsida : Marattiales : Asterothecaceae : Pecopteris | 298.9 - 295.5 Ma Paleozoic |
Sphenopteris sp. genus | Plantae : Tracheophyta : Lyginopteridaceae : Sphenopteris | 298.9 - 295.5 Ma Paleozoic |
Cordaites sp. genus | Plantae : Tracheophyta : Pinopsida : Cordaitaceae : Cordaites | 298.9 - 295.5 Ma Paleozoic |
Annularia sp. genus | Plantae : Tracheophyta : Polypodiopsida : Equisetales : Calamitaceae : Annularia | 298.9 - 295.5 Ma Paleozoic |
Walchia sp. genus | Plantae : Pteridophyta : Lycopsida : Lycopodiaceae : Walchia | 298.9 - 295.5 Ma Paleozoic |
Megaphyton sp. genus | Plantae : Tracheophyta : Polypodiopsida : Marattiales : Asterothecaceae : Megaphyton | 298.9 - 295.5 Ma Paleozoic |
References
Trunko L., Munk W. (1990) Makrofloren aus dem Unterrotliegenden (Unterperm) von Alsenz bei Bad Kreuznach/Rheinland Pfalz, Carolinea 48, 21-30 |
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!