Cleoniceras mm 185 Ammonite Couple Extra Large kg 1.2 (9)

Description

Origin : Northwestern Madagascar (Mahajanga)

Geological era : Lower Cretaceous (Albian)

Age : 112 million of years

Size : cm 18.5

Fossil Ammonite Couple Extra-Large Cleoniceras cm 18.5 diameter - weight: 629 and 616 gr. Double section polished, rooms with deposits of quartz and calcite.
Only a piece as in pictures.
Presumable specie: Cleoniceras besairei.
Also available in small size, bamboo frame, with mother of pearl, in opal and pendant, at this link.

The Ammonites are an extinct group of cephalopods, which appeared in the Lower Devonian about 400 million years ago and extinguished at the end of the Cretaceous, together with the dinosaurs (65 million years ago), leaving no known descendants. Like all cephalopods known this organisms were carnivorous: active predators of marine animals, microphagous (plankton), scavengers, and even cannibals. The shell of ammonites in general has the form of a spiral wound on a plan (although some species, such heteromorphy, have a more complex three-dimensional winding) and it is this feature that has given their name. The appearance infact resembles a coiled horn, like that of a ram (the Egyptian god Amon was commonly depicted as a man with ram's horns). Pliny the Elder described the fossils of these animals ammonis cornua, "horns of Ammon." Often the name of the species of Ammonites ends with -ceras, from a greek word (κέρας) whose meaning is, in fact, "horn" (eg. Pleuroceras etymologically means horn with the coast).
The shell was divided by septa into several rooms, including the clam occupied only the last. The others were used as "tubes" filled with gas and liquid to control the floating body. The ammonite could well change its depth in a manner similar to the current Nautilus.
Because of their extraordinary variability and distribution in marine sediments around the world the ammonites are considered fossils for excellence and guide-fossils of exceptional value, used for dating in stratigraphy of the sedimentary rocks.
The classification of ammonites is made on the basis of morphology and ornamentation of the shell, and the shape of septa, depending on the suture line.