Taphonomy

Taphonomy is the study of a decaying organism over time. The term taphonomy, (from the Greek taphos meaning burial, and nomos meaning law), was introduced to paleontology in 1940 by Russian scientist, Ivan Efremov, to describe the study of the transition of remains, parts, or products of organisms, from the biosphere, to the lithosphere, i.e. the creation of fossil assemblages, (e.g. see Shipman 1981 p.5-6, Greenwood 1991, Lyman 1994).