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'''Fossils in Finland''' span the ] and ] eras.

There are precambrian fossils n ] 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>

In the ] layer, horns of a Finnish ] were discovered.<ref>{{Cite journal |title=The Morphology and Paleobiological Significance of the Horns of Coelodonta antiquitatis (Mammalia: Rhinocerotidae) |journal=Journal of Vertebrate Paleontology |first=Mikael |last=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}}</ref>

==References==
<references />

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{{Paleo-stub}}

Latest revision as of 01:16, 8 January 2025

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Fossils in Finland span the Precambrian and Cenozoic eras.

There are precambrian fossils n Archean and Proterozoic layers from ancient soils, and three layers such as siltsones, mudstones and sandstones at 1650 Ga.

In the Pleistocene layer, horns of a Finnish woolly rhinoceros were discovered.

References

  1. Precambrian Geology of Finland. Elsevier. 2005. ISBN 978-0-08-045759-8 – via Google Books.
  2. Fortelius, Mikael (1983-09-01). "The Morphology and Paleobiological Significance of the Horns of Coelodonta antiquitatis (Mammalia: Rhinocerotidae)". Journal of Vertebrate Paleontology. 3 (2): 125–135. Bibcode:1983JVPal...3..125F. doi:10.1080/02724634.1983.10011964. JSTOR 4522937.


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