In geology, depositional environment or sedimentary environment describes the combination of physical, chemical and biological processes associated with the deposition of a particular type of sediment and, therefore, the rock types that will be formed after lithification, if the sediment is preserved in the rock record. In most cases the environments associated with particular rock types or associations of rock types can be matched to existing analogues. However, the further back in geological time sediments were deposited, the more likely that direct modern analogues are not available (e.g. banded iron formations).
Types of depositional environments
- Deltaic – Silt deposition landform at the mouth of a river
- Lagoonal – A shallow body of water separated from a larger body of water by barrier islands or reefs
- Beach – Area of loose particles at the edge of the sea or other body of water
- Lake – A body of relatively still water, in a basin surrounded by land
- Shallow water marine environment
- Deep water marine environment – Flat area on the deep ocean floor
- Reef – A bar of rock, sand, coral or similar material, lying beneath the surface of water
Recognition of depositional environments in ancient sediments
Depositional environments in ancient sediments are recognised using a combination of sedimentary facies, facies associations, sedimentary structures and fossils, particularly trace fossil assemblages, as they indicate the environment in which they lived.
- Harold G. Reading. 1996. Sedimentary Environments: Processes, Facies and Stratigraphy. Blackwell Publishing Limited.