Superb structure and in a complete form, (not deformed by the pressure of plate movement during the fossilisation process within the fossiliferous layers) a three-dimensional fossil Cenoceras nautiloid, elegantly surmounted on an in-house custom chrome stand. The three metal elements, Iron pyrite, bronze and chrome blended here in the art of the mounting exhibiting the fossil shell for a maximum appeal. Internally; the shell viewed from the wide mouth aperture displays a rare opalescent mineralised beauty, an array of iridescent colours gleam upward.
The Madagascan Nautiloids are found in fossil layers that have unearthed some of the best Triassic to Cretaceous period mineralised fossil specimens yet discovered. The mineral content of the fossil bed some millions of years ago has caused the wonderful effects of colourful inclusions of several semi-precious minerals, renowned as of a 'gemmy' quality. Quartz in the form of calcites and jaspers have infilled the internal phragmacone (shells), of some fossil nautili. The septa (chamber wall divisions) are picked out with lighter and darker colour minerals, the chambers creating patterns in dark and lighter caramel colours which delight the onlooker today.
Both the Ammonites and Nautili evolved from cephalopod beginnings in the Cambrian period. The Ammonoid group eventually dominating the prehistoric marine environment, being free swimmers above the seabed, before the arrival of vertebrate fishes to the marine scene. Nautiloids having early success were later in the Cretaceous period seemingly in decline. The Cretaceous mass extinction, the KT boundary event, which is the marker for the extinction of dinosaurs and many other life forms gave the tenacious Nautili a chance to regain a secure foothold under the oceans as the only surviving Ammonoid
The Nautiloids are an enigmatic group of cephalopods, extant (living), genus types, the Nautilus pompilius and Nautilus umbilicalis survive today in the S.W.Pacific ocean. With ancestral lineage in the late Permian to Ordovician periods, since evolving Nautiloids have suffered extinctions in the Devonian, Carboniferous and Cretaceous. The Nautiloids seem in a state of contraction for much of this varied history. Seemingly in decline as the Ammonites were increasing successfully and in variety, a direct reflection of the ecology of the prehistoric marine environment concerning both cephalopod branches.
The Ammonites eventually becoming extinct in the Maastrichtian age, just before the mass KT extinction event. That the Nautiloids survived probably due to their benthic ecology. Laying small batch eggs often, at depth or on the sea floor with more frequency, throughout their life, thus protecting the eggs from most major climatic changes. Whereas the Ammonites laid one batch of numerous eggs at the end of life and attached these to marine planktonic environments, close to the surface which made them more susceptible to any major planetary climatic change.
Nautili are nektobenthic carnivores and pelagic. The umbilicus of this shell of the genus is involute and globose. Cenoceras described by Hyatt C.1884, Pseudocenoceras by Sparth C.1927.