Taphonomy is the study of how organisms decay and become fossilized or preserved in the paleontological record. The term taphonomy was introduced to paleontology in 1940 by Soviet scientist Ivan Efrem
Fossilization process of a pair of sauropod dinosaurs, illustrating their preservation into fossils
An articulated wombat skeleton in Imperial-Diamond cave (Jenolan Caves)
The La Brea Tar Pits represent an unusual depositional environment for their epoch (Pleistocene) and location (southern California).
Actualistic taphonomy seeks to understand taphonomic processes through experimentation, such as the burial of bone.
A fossil is any preserved remains, impression, or trace of any once-living thing from a past geological age. Examples include bones, shells, exoskeletons, stone imprints of animals or microbes, object
Taphonomy
…Taphonomy is the study of how organisms decay and become fossilized or preserved in the paleontological record. The term taphonomy (from Greek táphos, τάφος 'burial' and nomos, νόμος 'law') was introduced to paleontology…
Ceratopsian skulls are common in the Dzungarian Gate mountain pass in Asia, an area once famous for gold mines and cold winds. This has been attributed to legends of both gryphons and the land of Hyperborea.
Fossil shells from the cretaceous era sea urchin, Micraster, were used in medieval times as both shepherd's crowns to protect houses, and as painted fairy loaves by bakers to bring luck to their bread-making.
Georges Cuvier's 1812 skeletal reconstruction of Anoplotherium commune based on fossil remains of the extinct artiodactyl from Montmartre in Paris, France
Ichthyosaurus and Plesiosaurus from the 1834 Czech edition of Cuvier's Discours sur les revolutions de la surface du globe