perekond

Treptichnus Miller, 1889

Taksoni kirjeldused

Hammersburg et al., 2018

Diagnosis.—Chains of horizontal to subhorizontal, straight to curved, zigzagging burrow segments associated with vertical to oblique tubes producing a three-dimensional burrow structure; pits and nodules may occur near top or base of burrow segments at sediment interfaces (Buatois & Mángano, 1993a; Uchman, Bromley, & Leszczyński, 1998).

 

Buatois & Mángano, 1993a

Ethology. Treptichnus has been interpreted as both a feeding structure (Seilacher and Hemleben, 1966; Häntzschel, 1975; Rindsberg, 1990) and a farming trace (Rindsberg,1990), probably produced by vermiform animals.Treptichnus represents an eurytopic form of behavior; the trace has been recorded from lacustrine (Archer and Maples, 1984; Buatois and Mángano, 1990a, b), brackish tidal flat (Rindsberg, 1990), shallow-water marine (Banks, 1970; Fedonkin et al., 1983; among many others), bathyal (Seilacher and Hemleben, 1966), and submarine fan environments (Crimes et al., 1981). Although of little use at the ichnogeneric level, some ichnospecies of Treptichnus seem to be useful as environmental indicator.

Uchman et al., 1998

Diagnosis: Chains of zigzag, straight or curved burrow-segments associated with vertical or oblique tubes comprising three-dimensional structures. Unbranched, except wheresegments diverge from each other, at which places small pits or twig-like projections occur (modified from Buatois and Mângano, 1993).

Hofmann et al., 2012

Remarks.—Treptichnus is interpreted as a fodinichnion made by vermiform animals (Buatois et al., 1998). Recent neoichnologic work has convincingly argued for a priapulid origin for Treptichnus pedum (Vannier et al., 2010). Originally described as Phycodes pedum (Seilacher, 1955), Jensen (1997) referred this ichnospecies to Treptichnus whereas Geyer and Uchman (1995) placed it in Trichophycus. The type specimen (Seilacher, 1955, p. 387, fig. 4a) shows branching at the end of the burrow system resulting in a sickle-shaped appearance. Jensen (1997) included more irregular branching patterns with curved to highly winded courses and alternating or single sided segments. The proposal by Jensen (1997) became generally accepted (e.g., Seilacher et al., 2005; Seilacher, 2007; Vannier et al., 2010). Although the scarcity and incomplete nature of the Hanneh specimens prevent from a definite assignment, the overall morphology corresponds with descriptions by Jensen (1997

Valik taksonit käsitlevast teaduskirjandusest
Toom, U., Vinn, O., Hints, O. 2019. Ordovician and Silurian ichnofossils from carbonate facies in Estonia: A collection-based review. Palaeoworld 28, 1-2, 123-144. DOI:10.1016/j.palwor.2018.07.001
Jensen, S., Grant, S. W. F. 1998. Trace fossils from the Dividalen Group, northern Sweden: implications for Early Cambrian biostratigraphy of Baltica. Norsk Geologisk Tidsskrift 78, 4, 305-317.
Orłowski, S., Żylińska, A. 1996. Non-arthropod burrows from the Middle and Late Cambrian of the Holy Cross Mountains, Poland. Acta Palaeontologica Polonica 41, 4, 385-409.
Mens, K. 1994. Kambriumi alumine piir ja kivistis Phycodes pedum. Eesti Loodus 12, 360.
Kowalski, W. R. 1987. Trace fossils of the Upper Vendian and lowermost Cambrian in southern Poland. Bulletin of the Polish Academy of Sciences 35, 1, 21–32.
Palij, V. M., Posti, E., Fedonkin, M. A. 1979. Soft-bodied Metazoa and trace fossils of Vendian and Lower Cambrian. Upper Precambrian and Cambrian Paleontology of East-European Platform, pp. 49-82. Nauka.
Palij, V. M. 1976. Ostatki besskeletnoj fauny i sledy žiznedeâtel'nosti iz otloženij verhnego dokembriâ i nižnego kembriâ Podolii. Paleontology and stratigraphy of the Upper Precambrian and Lower Paleozoic of the southwest of the East European Platform, pp. 63-77. Naukova Dumka.
Leitud liigid
1. Treptichnus bifurcus Miller, 1889 | KambriumKarbon
3. Treptichnus triplex Palij, 1976 | EdiacaraAlam-Kambrium (endine liigestus)
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Klassifikatsioon
organismirühmBiota
ihnorühmIchnofossils
Bioturbation trace fossils
Trackways and scratch imprints
seltsBiformitidae
sugukondArenicolitidae
Arthrophycidae
Asteriacitidae
Rhizocoralliidae
Rosselichnidae
Siphonichnidae
perekondAcanthorhaphe
Aglaspidichnus
Agrichnium
Altichnus
Amanitichnus
Amphorichnus
Ancorichnus
Angulichnus
Arachnomorphichnus
Arachnostega
Arborichnus
Archaeonassa
Arcuatichnus
Arenituba
Artharia
Asaphoidichnus
Asterichnus
Asterosoma
Astropolichnus
Aulichnites
Avipeda
Avolatichnium
Balanoglossites
Baroccoichnites
Bathichnus
Beaconites
Bergaueria
Bestiopeda
Bicavichnites
Bichordites
Bifasciculus
Bifungites
Bilinichnus
Bolonia
Bornichnus
Bromleyia
Bunyerichnus
Caletichnus
Calycraterion
Camborygma
Capodistria
Caprionichnius
Cardioichnus
Caridolites
Catenarichnus
Catenichnus
Chagrinichnites
Cheiichnus
Chomatichnus
Chondrites
Circulichnis
Cladichnus
Clematischnia
Climactichnites
Cochlichnus
Compaginatichnus
Conichnus
Conostichus
Cruziana
Ctenopholeus
Curvolithus
Cycloichnus
Cylindricum
Dactyloidites
Deliatynichnis
Dendrorhaphe
Dendrotichnium
Dictyodora
Didymaulichnus
Didymaulyponomos
Diplopodichnus
Echinospira
Egoreichnis
Elingua
Enigmatichnus
Entradichnus
Epibaion
Estrellichnus
Falcichnites
Fimbritubichnus
Foveichnus
Fucoides circinatus
Fuersichnus
Funalichnus
Furculosus
Fustiglyphus
Glossifungites
Glyphichnus
Gordia
Guanshanichnus
Gyrochorte
Gyrolithes
Gyrophyllites
Haentzschelinia
Halimedides
Halopoa
Hartsellea
Heimdallia
Helicodromites
Heliochone
Helminthoida
Helminthoidichnites
Helminthopsis
Herpystezoum
Hondichnus
Hormosiroidea
Ilmenichnus
Imponoglyphus
Isopodichnus
Jamesonichnites
Katbergia
Keilorites
Kimberichnus
Koptichnus
Korymbichnus
Kouphichnium
Labyrintichnus
Lajasichnus
Lamellaeichnus
Lamonte
Lanicoidichna
Lennea
Lepeichnus
Lepidenteron
Liholites
Lingulichnites
Lingulichnus
Lithoplaision
Lockeia
Loloichnus
Lophoctenium
Lorenzinia
Macaronichnus
Maiakarichnus
Mammillichnis
Margaritichnus
Megagrapton
Mermia
Microspherichnus
Minterichnus
Monocraterion
Monofungites
Multilamella
Multina
Multipodichnus
Musculopodus
Naviculichnium
Nenoxites
Neoeione
Neonereites
Nereites (trace fossil)
Nummipera
Oikobesalon
Oldhamia
Olenichnus
Oniscoidichnus
Ophiomorpha
Oravaichnium
Palaeophycus
Paleodictyon
Paracanthorhaphe
Parahaentzschelina
Parapsammichnites
Parataenidium
Paratisoa
Parmaichnus
Parundichnia
Pentichnus
Petalichnus
Phoebichnus
Pholeus
Phycosiphon
Pilichnus
Piscichnus
Plagiogmus
Plangtichnus
Planispiralichnus
Planolites
Polarichnus
Polykampton
Polykladichnus
Protopaleodictyon
Protospiralichnus
Protovirgularia
Psammichnites
Psilonichnus
Pteraspisichnis
Ptychoplasma
Radiichnus
Radionereites
Rhadhostium
Rotamedusa
Rusophycus
Saerichnites
Sagittichnus
Saportia
Scalaridomus
Schaubcylindrichnus
Scolecocoprus
Scolicia
Scotolithus
Scoyenia
Selenichnites
Shanwangichnus
Sinusichnus
Skolichnus
Skolithos
Sokolovichnites
Solemyatuba
Sphaerichnus
Spirocosmorhaphe
Spirodesmos
Spirophycus
Spongelimorpha
Squamichnus
Squamodictyon
Steinsfjordichnus
Stelloglyphus
Streptichnus
Sustergichnus
Svalbardichnus
Syringomorpha
Taenidium
Tambia
Taotieichnus
Taphrhelminthopsis
Taxichnites
Teichichnus
Ternavites
Tetraichnites
Thalassinoides
Torrowangea
Transexcrementum
Treptichnus
liikaequalternus
apsorum
bifurcus
coronatum
lublinensis
meandrinus
pedum
pollardi
rectangularis
triplex
vagans
perekondTriacliichnis
Trichichnus
Trichophycus
Trisulcus
Tuapseichnium
Tuberculichnus
Tubichnus
Tubotomaculum
Tylichnus
Undichna
Vagorichnus
Vermichnus
Virgaichnus
Volkichnium
Walcottia
Zoophycos
määratlemataTrusheimichnus