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| ] is the ] country have fossils. | ] is the ] country have fossils. | ||
| ==Precambrian fossils== | ==Precambrian fossils== | ||
| In ] and ], layers from ancient ], and three layers such as ], ] and ] at 1650 Ga.<ref>{{Cite book |title=Precambrian Geology of Finland | |
In ] and ], layers from ancient ], and three layers such as ], ] and ] at 1650 Ga.<ref>{{Cite book |title=Precambrian Geology of Finland |year=2005 |publisher= Elsevier|isbn= 978-0-08-045759-8|language=English |url=https://books.google.com/books?id=3D5R3vexH1sC|via=]}}</ref> | ||
| ==Cenozoic fossils== | ==Cenozoic fossils== | ||
| in ], horns of Finnish ].<ref>{{Cite journal |title=The Morphology and Paleobiological Significance of the Horns of Coelodonta antiquitatis (Mammalia: Rhinocerotidae) |journal=Journal of Vertebrate Paleontology |first=Mikael Fortelius |url=https://www.jstor.org/stable/4522937 |
in ], horns of Finnish ].<ref>{{Cite journal |title=The Morphology and Paleobiological Significance of the Horns of Coelodonta antiquitatis (Mammalia: Rhinocerotidae) |journal=Journal of Vertebrate Paleontology |first=Mikael Fortelius |volume=3 |issue=2 |pages=125–135 |doi=10.1080/02724634.1983.10011964 |url=https://www.jstor.org/stable/4522937 |jstor=4522937 |bibcode=1983JVPal...3..125F |publication-date=1983-09-01|via=]}}</ref> | ||
| ==References== | ==References== | ||
| <references /> | <references /> | ||
Revision as of 14:53, 1 January 2025
Finland is the Northern European country have fossils.
Precambrian fossils
In Archean and Proterozoic, layers from ancient soils, and three layers such as siltsones, mudstones and sandstones at 1650 Ga.
Cenozoic fossils
in Pleistocene, horns of Finnish woolly rhinoceros.
References
- Precambrian Geology of Finland. Elsevier. 2005. ISBN 978-0-08-045759-8 – via Google Books.
- "The Morphology and Paleobiological Significance of the Horns of Coelodonta antiquitatis (Mammalia: Rhinocerotidae)". Journal of Vertebrate Paleontology. 3 (2): 125–135. 1983-09-01. Bibcode:1983JVPal...3..125F. doi:10.1080/02724634.1983.10011964. JSTOR 4522937 – via JSTOR.
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