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Taphonomists study such phenomena as biostratinomy , decomposition, diagenesis, and epibiont encrustation.

The motivation behind the study of taphonomy is to better understand biases present in the fossil record. Fossils are ubiquitous in sedimentary rocks, yet paleontologists can not draw conclusions about the lives and ecology of the fossilized organisms without knowing about the processes involved in their fossilization. For example, if a fossil assemblage contains more of one type of fossil than another, one can either infer that that organism was present in greater numbers, or that its remains are more resistant to decomposition.

Experimental taphonomy usually consists of exposing the remains of organisms to various altering processes, and then examining the effects of the exposure.

1 References

• Greenwood, D. R. (1991), The taphonomy of plant macrofossils. In, Donovan, S. K. (Ed.), The processes of fossilisation, pp.141-169. Belhaven Press.
• Shipman, P. (1981), Life history of a fossil: An introduction to taphonomy and paleoecology. Harvard University Press.

2 External links

• The Shelf and Slope Experimental Taphonomy Initiative is the first long-term large-scale deployment and recollection of organism remains on the sea floor.
• The Journal of Taphonomy