While dinosaurs ruled the land during the Late Cretaceous, the ammonite genus Pachydiscus🌌 ("thick disc") flourished in the oceans all around the world.

Ammonites were a𒅌 type of cephaꦗlopod—the taxonomic class that includes today's nautilus, octopus, and squid. Much like a submarine, ammonites employed gas- and liquid-filled chambers to regulate their position in the water column. The animal itself lived only in the outermost compartment, employing its tubular siphuncle to connect its chambers along the shell's ventral surface.

Pachydiscus fossils are an important index species in the stratigraphic record of the history of life on Earth, as they are used as the "defining biological marker" for the beginning of the Maastrichtian Stage, starting 72.1 ± 0.2 million years ago. The specimen offered here is even more remarkable, as evidenced by the calcite geodes that have taken up residence within many of this Pachydiscus fossil's chambers.