Ichnofauna

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Ichnofauna is the diversity of fauna based on the ichnological (tracks and footprints) evidences. This term is often used by vertebrate paleontologists. [1] [2]

Ichnofauna often uses parataxonomical names for tracks such as Deltapodus, Eubrontes, or Cruziana . Ichnofauna does not give a true content of the fauna assemblage, because of bias of preservation.

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<i>Palmichnium</i>

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The Broome Sandstone, formerly known as the Broome Beds, is an Early Cretaceous geologic formation found in Western Australia, and formerly considered part of Dampier Group. Fossil sauropod tracks, belonging to an unknown ichnotaxon, and stegosaur tracks belonging to the ichnogenus and species Garbina roeorum have been reported from the formation.

<i>Ceratopsipes</i> Dinosaur footprint

Ceratopsipes goldenensis is an ichnospecies of dinosaur footprint, described in 1995 from the Laramie Formation in Colorado. It is represented by massive pes prints approaching 80 centimetres (31 in) in width. If undistorted, the tracks may represent an unusually large Ceratopsian dinosaur that could have potentially been as large as 12 metres.

Tetrapodium is an ichnogenus of fossil footprints found in the Etjo Sandstone and Omingonde Formations of Namibia. The Etjo Sandstone fossils were initially identified as rounded, featureless depressions presumed to have been made by a quadrupedal animal, but more recent examination in 2016 could not identify such tracks and concluded they are most likely non-biogenic features of the rock surface.

Wintonopus is an ichnogenus of dinosaur footprint. Its footprints have been found at Lark Quarry in Queensland Australia. The genus is named after the Winton Formation in which the tracks were found. Other tracks were found in the Broome Sandstone of Dampier Peninsula, Western Australia.

<span class="mw-page-title-main">Botucatu Formation</span>

The Botucatu Formation is an Aptian geologic formation of the Paraná and Pelotas Basins in southern Brazil and northern Uruguay. The formation is composed of quartzitic sandstones, deposited in an eolian environment. Fossil theropod tracks have been reported from the formation.

Eba Island Conservation Park is a protected area in the Australian state of South Australia. It comprises 134 hectares of land, proclaimed in 1972 to conserve island habitat within Streaky Bay and sea bird breeding colonies. Eba Island is located 700 metres offshore and 4 kilometres south of Perlubie Hill. It is entirely composed of calcarenite, often overlaid with a limestone capping.

Neosauroides is a Cretaceous ichnogenus of lizard found in South Korea. N. koreanensis is discovered from the Haman Formation, while N. innovatus is discovered from the Jinju Formation.

<i>Pentasaurus</i> Genus of dicynodont therapsid from the late Triassic of South Africa

Pentasaurus is an extinct genus of dicynodont of the family Stahleckeriidae, closely related to the well known Placerias. It was found in the Lower Elliot Formation of South Africa, dated to the Norian of the Late Triassic period. The genus contains the type and only species, Pentasaurus goggai. Pentasaurus is named after the ichnogenus Pentasauropus, fossil footprints that were originally described from the lower Elliot Formation in 1970 decades before the body fossils of Pentasaurus itself were recognised. Pentasauropus footprints were likely made by dicynodonts, and in South Africa Pentasaurus itself was the likely trackmaker. The name reflects the fact that a large dicynodont was predicted to have existed in the lower Elliot Formation before any body fossils were recognised, and so Pentasaurus was named after its probable footprints. This is a reversal of the more typical occurrence where fossil footprints are named after their presumed trackmakers. The name of the species honours its collector Alfred Brown, nicknamed "Gogga", which means "bug" in Afrikaans.

Rhynchosauroides is an ichnogenus, a form taxon based on footprints. The organism producing the footprints was likely a lepidosaur and may have been a sphenodont, an ancestor of the modern tuatara. The footprint consists of five digits, of which the fifth is shortened and the first highly shortened.

Amphisauropus is an amphibian ichnogenus commonly found in assemblages of ichnofossils dating to the Permian to Triassic. It has been found in Europe, Morocco, and North America.

References

  1. Walker, Elaine F. (January 1985). "Arthropod ichnofauna of the Old Red Sandstone at Dunure and Montrose, Scotland" . Transactions of the Royal Society of Edinburgh: Earth Sciences. Cambridge University Press. 76 (2–3): 287–297. doi:10.1017/S0263593300010506. S2CID   131281292 . Retrieved 14 January 2013.
  2. Mateus, O., & Milàn, J. 2010. A diverse Upper Jurassic dinosaur ichnofauna from central‐west Portugal. Lethaia, 43(2), 245-257.