Ammonites (Ammonoidea) are an extinct subclass of the Cephalopoda (squid). They are marine animals that were abundant worldwide in the late Paleozoïcum and throughout the Mesozoïcum. They are found as a fossil. Ammonites have a flat spiral-shaped shell that is made up of several chambers. Each time the animal outgrows the current chamber, a new larger outer chamber is formed. The animal lives in this outer chamber, which further uses the other empty chambers as a means of vertical movement. The ammonite excretes gas in these chambers to regulate the lifting force on the shell. Ammonites came in hundreds of species and varieties. They almost all have the same ground plan: a flat spiral-shaped shell. There are some exceptions: some heteromorphic species that do not have a spiral shell. The size of the ammonites varies from less than a centimeter to more than 2.5 meters across. The closest living relatives are the Nautilidae (nautiluses). The name comes from the Egyptian god Amun, who was depicted as a man with the head of a ram. Ammonites resemble the curled ram's horns with which Amon was represented. In the case of the Roman author Pliny the Elder we find descriptions of fossils of these animals which he called "ammonis cornu" (horn of Ammon). Ammonites first appeared in the late Silurian, survived the Permian-Triassic extinction with remarkably few species, and flourished during the Mesozoic. At the end of this period (65 million years ago) most ammonites became extinct, just like the dinosaurs. Fossils from the Netherlands and Denmark, however, seem to show that the last ammonites still existed in the oldest layers of the Paleocene. The youngest known fossil of an ammonite comes from Denmark and belongs to Hoploscaphites constrictus, which existed until about 65.3 million years ago, some 0.2 to 0.65 million years after the mass extinction, and possibly even another half million years longer. However, these small populations were not enough to save the last ammonites from extinction. It is thought that the ammonites became extinct due to their reproductive strategy. The young were part of the plankton that floated on the surface of the sea. Acid rain and the obscuration of the sun by dust clouds probably created poor conditions for the eggs and young to develop.