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Trace fossils

Chondrites bollensis, Jurassic, GER
Chondrites bollensis, Jurassic, GER
These finely branched, dendritic ducts were left behind in the sea floor by sediment-eating organisms such as bristle worms. In the 19th century, the bushy structures were misinterpreted as plant remains (e.g. seaweed), which led to the term ‘seaweed shale’. It was only later that it was recognised that these were fossilised traces of life (ichnofossils).Age: Jurassic, Upper lias;Locality: Kirchheim, Baden-Württemberg, GermanySize: approx. 8,2 x 10 x 1 cmThe colors of pictures can slightly differ from the original colors due to technical reasons.

€22.00

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Ediacara Fauna: Nemiana simplex, UA
Ediacara Fauna: Nemiana simplex, UA
It is debatable whether these are cnidarians, algae or stromatolites. The chemical signature of the clearly recognizable bumps indicates that this is the work of cyanobacteria. They are assigned to the Ediacara fauna of Eastern Europe.Age: Proterozoic, Tschernji-Kamen-Formation;Locality: Bernashivka, Vinnytsia Oblast, UkraineSize: approx. 5 - 7 cmThe pictures are examples. You will receive a piece of comparable quality.Colors on photos may differ slightly from those of the original specimen for technical reasons.

€15.00

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Filled worm burrows (Toledo) in wood, Eocene; IT
Filled worm burrows (Toledo) in wood, Eocene; IT
Worm holes in wood. The wood has weathered over time, leaving the limonitized worm burrows.Age: Middle Eocene;Locality: Monte Truffa near Valdagno, Vincenza, ItalySize: approx. 17 x 11 x 7 cmColors on the pictures may differ from the colors of the originals due to technical reasons.

€32.00

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Namacalathus hermanastes, Neoproterozoic; NAM
Namacalathus hermanastes, Neoproterozoic; NAM
RARITY! Imprints preserved on both sides.Age: Kuibis Quartzite, Nama Group, Ediacarium, Zaris Formation, Neoproterozoic (approx. 650 million years old);Locality: Fish River region (afrikaans Visrivier), //Kharas, NamibiaSize: 13 x 5 x 4 cmThe colors in the product photos may differ from those of the original specimen for technical reasons.

€95.00

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Tetrapod tracks, Permian; FRA - positiv and negativ
Tetrapod tracks, Permian; FRA - positiv and negativ
Very beautiful, clear traces of tetrapods preserved on both sides of the slab.The tetrapod tracks from this period are of particular importance for biostratigraphic analyses and paleoecological studies of the Rotliegend.RARITY!Age: Lower Permian, Autunian;Locality: Mas d'Alary, Lodève, Dept. Hérault, Occitanie region, FranceSize: 21 x 12 x 2 cmColors on product photos may differ slightly from those of the original specimen due to technical reasons

€260.00

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Trace fossil: Lennea schmidti, Devonian, GER
Trace fossil: Lennea schmidti, Devonian, GER
Lennea schmidti was originally considered a plant. In the paleontological journal of 1934, however, it was then stated clearly that it was a "plant-like animal trace from the Devonian".Rare!Age: Lower Middle Devonian, Cultrijugatus layers;Locality: Holzmülheim, near Bad Münstereifel, North Rhine-Westphalia, GermanySize: approx. 8,5 x 8,5 x 1,5 cmColors on photos may differ slightly from the original due to technical reasons.

€32.00

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Trace fossil: Phycodes circinatum, Ordovician, GER
Trace fossil: Phycodes circinatum, Ordovician, GER
On display are fossilized feeding holes of unknown animals, which burrowed in arcs through the seabed searching for food.Further information in German on the formation of the trace fossil can be found here: SpurenfossilAge: Lower Ordovician, O. Tremadoc, Phycodes Shale;Locality: Saalfeld, Thuringian Forest, GermanySize: 9,5 x 5,5 x 2,3 cmColors on our photos may differ slightly from those of the original specimen due to technical reasons.

€25.00

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Weevil (Leptopius duponti), Holocene, USA
Weevil (Leptopius duponti), Holocene, USA
Calcified cocoon of weevil Leptopius duponti / Weevil.Age: Holocene;Location: Dunes of Eyre Peninsula, South AustraliaSize: ca. 5,5 x 3,5 x 3,2 cmThe colours on the pictures may slightly differ from the original specimen.

€16.00

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