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An ichnofacies is an assemblage of that provides an indication of the conditions that their formative organisms inhabited.


Concept
Trace fossil assemblages are far from random; the range of fossils recorded in association is constrained by the environment in which the trace-making organisms dwelt. Palaeontologist pioneered the concept of ichnofacies, whereby the state of a sedimentary system at its time of deposition could be deduced by noting the trace fossils in association with one another.


Significance
Ichnofacies can provide information about water depth, , and energy. In general, traces found in shallower water are vertical, those in deeper water are more horizontal and patterned. This is partly because of the relative abundance of suspended food particles, such as , in the shallower waters of the , and partly because vertical burrows are more secure in the turbulent conditions of shallow water. In deeper waters, there is a necessary transition to sediment feeding (extracting from the mud). Food availability, hence trace type, is also controlled by energy: high energy environments keep food particles suspended, whereas in lower energy areas, food settles out evenly, and burrows will tend to spread out to cover as much area as economically as possible.

Ichnofacies have a major advantage over using body fossils to gauge the same factors: body fossils can be transported, but trace fossils are always in situ.


Recognized invertebrate ichnofacies
, , , Variable - typically sandstones; red beds may be nearbyDiagnostic of terrestrial/freshwater facies.
PsilonichnusPsilonichnus, Coenobichnus, , MacanopsisHighly variable grain size, sand, soft substrateCoastal barrier islands, strand plains, delta plains, estuaries, lagoons, and bays.
, Trypanites, Gastrochaenolites, Caulostrepsis, Maeandropolydora, ConchotremaHardground, endurated substratesCoastal cliffs, reefs, beachrock
, Resistant woody and coaly substratesDriftwood, peat
Glossifungites, , Spongeliomorpha, , , , Fuersichnus
(2026). 9780521855556, Cambridge University Press.
Firmground, dewatered mudsShallow, marginal marine, deltaic or estuarine .
, , , Unconsolidated littoral sandsBeaches and sandy tidal flats, shallow water, foreshore to upper-shoreface, above wavebase
Arthrophycus, Phycodes, , , , , , , , , Curvolithus, , , Sand and silt heterolithic successions and organic detritusMid to distal continental shelves. Below normal wave base, but not necessarily below storm wave base
, , ChondritesMarine softground, impure sands and siltsDeeper water, bottom of shelf; turbidite facies
NereitesNereites, Megagrapton, Protopaleodictyon, Spirophycus, Helminthoraphe, Glockerichnus, , Cosmoraphe, Urohelminthoida, Desmograpton, , Fine-grained muds and clays interbedded with turbidite siltsDeep water, pelagic, base-of-slope turbidity systems


Recognized vertebrate ichnofacies
NameCommon IchnogeneraSubstrateInferred Paleoenvironment
(Laoporus), BrasilichniumUnconsolidated, larger-grained sandsAeolian sand dunes
, , Koreanoformis, , Brachychirotherium, Rhynchosauroides, Lacustrine shorelines
Charirichnium, , , Clastic or carbonateCoastal plain, marine shoreline
BatrachichnusBatrachichnus, , Amphisauropus, Dromopus, Dimetropus, Gilmoreichnus, Tidal flat-fluvial plain
CharacichnosCharacichnos, , Lunichnium, Puertollanopus, Serpentichnus, Batrachichnus, Semi-consolidated firmgroundsSubaqueous lacustrine, estuarine, and deltaic environments


See also


External links

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