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Ichnology: Study of trace fossils (biogenic sedimentary structures).Ichnite: general term for a trace fossil.

An important distinction to remember is that every mark made by an organism (or fossil) isnecessarily a trace fossil. It could simply be atool mark (for instance, by a shell being bounced around in a current).

Ichnofabric &bioturbation: degree of overturning of sediment by organisms. Excessive biological activity obliterates individual trace fossils and sedimentary structures, mixing layers, etc.

Ichnotaxonomy: by tradition, individual trace fossil forms are given "ichnogenus" and "ichnospecies" (and "ichnofamily" and so on) names, even though they do NOT in reality represent a nested hierarchy based on patterns of descent!! Two trace fossils represent the same ichnospecies if they are identical in formregardless of whether they are made by the same species or different species; additionally, the same species can produce many different ichnospecies depending on its behavior, the substrate, etc.

Other Ichnonomenclature:

• By Behavior:
  • Cubichnia: resting
  • Domichnia: dwelling
  • Fugichia: escape traces
  • Repichnia: moving
  • Paschichnia: grazing
  • Agrichnia: farming
  • Fodinichnia: Deposit feeding (3-D)
• Ichnofacies: set of trace fossils associated with a particular set of environmental conditions. Form excellent record of paleoenvironment, esp. as many ichnogenera persist for hundreds of millions of years! Some major ichnofacies:
  • Skolithos: Rapidly moving sediment, made by filter feeders:
    • Skolithos: vertical tubes (Cam-K), unknown builder
    • Ophiomorpha: brick-built, (P-today), callianassid shrimp ("ghost shrimp") make these today
    • Diplocraterion: vertical U-shaped tubes withspreite (internal laminae indicating previous stages of the trace) (Cam-P)
  • Cruziana: Shallow marine, between low tideline and storm wave base (middle-outer shelf):
    • Cruziana: trilobitefurrowing traces (Cam-P)
    • Thalassinoides: complex mining (domichnia/fodinichnia) traces, probably by decapods (Cam-today)
    • Asteriacites: starfish cubichinia (Cam-P)
    • Rhizocorallium: horizonal version ofDiplocraterion (Cam-P)
  • Zoophycos: Low energy muds and muddy sands, dysaerobic and organic rich conditions:
    • Zoophycos: 3-D feeding trace (Cam-P)
  • Nereites: Deep water (associated with turbidites and pelagic muds)
    • Nereites itself is one of many complex surface pascichnia or fodinichnia (Cam-today)
    • Paleodictyon: a series ofhexagonal structures. Builder unknown, but deep sea submersibles have foundPaleodictyon is still being formed in the abyssal realm! (Cam-today)
  • Other zones are less significant

Terrestrial trace fossils:
Both arthropod and vertebrate trackways are common. Unlike marine ichnofossils, repichnia dominate by orders of magnitude. However, some domichnia present:

• Termite burrows
• Rodent burrows (such asDaemonelix)
• Evengiant ground sloth burrows!

Also, feeding traces can be found as bite marks on bones or leaves, and there are the occasional resting tracks.

Some aspects of terrestrial (primarily vertebrate (primarily locomotory)) ichnology:

• Relatively good at identifying trackmakers: perhaps not to the genus/species level, but often easier to resolve than marine ichnites:
  • In part because vertebrates have individual footfalls
  • In part because vertebrate diversity is generally lower than invertebrates (bigger, rarer animals)
  • However, there have been some famous mistakes (such as identifying limulid (horseshoe crab) tracks as pterosaurs, or pterosaur tracks as crocodilians)
• Relatively good ability to reconstruct aspects of locomotion
  • Individual attributes, such as size and stance of the animal
  • Dynamic attributes, such aspace angulation and stride length
  • From some basic mechanics, and by comparison with modern animals, one can estimatespeeds from trackways
• Can occasionally get estimates of other behaviors. For example,this one is REALLY cool: an apparent record of a large carnivorous dinosaur (Acrocanthosaurus or a close relative) attacking a large herbivorous dinosaur (Sauroposeidon or a close relative) in the Early Cretaceous of Texas. Note the "right-left-right-right-left-right" sequence in the carnivore's steps: one hypothesis is that the predator was grabbing onto the herbivore, and was dragged for a step before being dislodged.

Alimentary Canal Trace Fossils

There is (whoa, surprise!) a special set of terms for ichnites associated with the digestive tract (collectivelybromalites):

• Gastrolite: material still within the stomach
• Cololite: material still within the intestinal tract
• Coprolite: fossilized feces
• Vomitite (akaregurgitite akaregurgitalites): partially processed foods that went out the mouth rather than the anus (e.g., owl pellets)

An important thing to remember is that an ichnite isthe fossil of the animal while alive, not after it was dead!

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Last modified: 6 September 2022