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Ichnofacies

Trace fossil

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

01Concept

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 Adolf Seilacher 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.

02Significance

Ichnofacies can provide information about water depth, salinity, turbidity 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 plankton, in the shallower waters of the photic zone, 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 nutrients 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.

03Recognized invertebrate ichnofacies

Marine Invertebrate Ichnofacies
Name Common Ichnogenera Substrate Inferred Paleoenvironment
Scoyenia Skolithos, Cruziana, Diplichnites, Rusophycus Variable - typically sandstones; red beds may be nearby Diagnostic of terrestrial/freshwater facies.
Psilonichnus Psilonichnus, Coenobichnus, Cellicalichnus, Macanopsis Highly variable grain size, sand, soft substrate Coastal barrier islands, strand plains, delta plains, estuaries, lagoons, and bays.
Trypanites Entobia, Trypanites, Gastrochaenolites, Caulostrepsis, Maeandropolydora, Conchotrema Hardground, endurated substrates Coastal cliffs, reefs, beachrock
Teredolites Teredolites, Thalassinoides Resistant woody and coaly substrates Driftwood, peat
Glossifungites Diplocraterion, Skolithos, Spongeliomorpha, Rhizocorallium, Arenicolites, Thalassinoides, Fuersichnus Firmground, dewatered muds Shallow, marginal marine, deltaic or estuarine erosion surfaces.
Skolithos Skolithos, Ophiomorpha, Arenicolites, Diplocraterion Unconsolidated littoral sands Beaches and sandy tidal flats, shallow water, foreshore to upper-shoreface, above wavebase
Cruziana Arthrophycus, Phycodes, Rhizocorallium, Teichichnus, Arenicolites, Rosselia, Bergaueria, Thalassinoides, Lockeia, Protovirgularia, Curvolithus, Dimorphichnus, Cruziana, Rusophycus Sand and silt heterolithic successions and organic detritus Mid to distal continental shelves. Below normal wave base, but not necessarily below storm wave base
Zoophycos Zoophycos, Phycosiphon, Chondrites Marine softground, impure sands and silts Deeper water, bottom of shelf; turbidite facies
Nereites Nereites, Megagrapton, Protopaleodictyon, Spirophycus, Helminthoraphe, Glockerichnus, Spiroraphe, Cosmoraphe, Urohelminthoida, Desmograpton, Paleodictyon, Scolicia Fine-grained muds and clays interbedded with turbidite silts Deep water, pelagic, base-of-slope turbidity systems

04Recognized vertebrate ichnofacies

Vertebrate Ichnofacies
Name Common Ichnogenera Substrate Inferred Paleoenvironment
Chelichnus (Laoporus) Chelichnus, Brasilichnium Unconsolidated, larger-grained sands Aeolian sand dunes
Grallator Grallator, Jindongornipes, Koreanoformis, Avipeda, Brachychirotherium, Rhynchosauroides, Eubrontes Lacustrine shorelines
Brontopodus Charirichnium, Ceratopsipes, Amblydactylus, Brontopodus Clastic or carbonate Coastal plain, marine shoreline
Batrachichnus Batrachichnus, Limnopus, Amphisauropus, Dromopus, Dimetropus, Gilmoreichnus, Chirotherium Tidal flat-fluvial plain
Characichnos Characichnos, Undichna, Lunichnium, Puertollanopus, Serpentichnus, Batrachichnus, Hatcherichnus Semi-consolidated firmgrounds Subaqueous lacustrine, estuarine, and deltaic environments
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Sources and credits

This article is adapted from the Wikipedia article Ichnofacies, written by its contributors and licensed under CC BY-SA 4.0. Fathomly has changed the layout, removed citation markers, navigation and maintenance notices, and adjusted punctuation. This adapted version is shared under the same license. For references, see the original article.

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