Tips
17. september 2023
Vandring
They appear in the fossil record during the Devonian and disappear shortly after the Cretaceous-Paleogene crisis. They were characterized by a more or less coiled univalve shell of which only the last chamber was occupied by the animal, the other chambers serving to control its flotation; the siphon that connects them is in an external (ventral) position, along the wall, whereas it is axial in nautiluses. Their fossil shells are excellent chronological markers. Their size ranges from a few millimeters to more than 2 meters in diameter.
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Bedste ruter nær Fossilized Ammonite Stone Bench
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Højdemeter 270 m
Vejr
Drevet af Foreca
fredag 10. juli
32°C
18°C
0 %
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