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- W2910552908 abstract "Undichna quadrisulcata isp. nov. is described from the Eocene of Spitsbergen, where it occurs together with xiphosuran (horseshoe crabs) traces in upper shoreface to foreshore deltaic sandstone. This is the first record of a marine (deltaic) Undichna from the Eocene. The trail consists of two or three pairs of paralleling sinusoidal grooves (in epirelief) or ridges (in hyporelief). Previous records of this trace fossil from the Carboniferous and Permian were assigned to U. insolentia Anderson, 1976 Anderson, A. M. 1976. Fish trails from the early Permian of South Africa. Palaeontology 19(2): 397–409. [Google Scholar], which, however, comprises a more complex pattern. The repeated occurrence of U. quadrisulcata isp. nov. in the Carboniferous, Permian, Triassic and Eocene, independent from U. insolentia, justifies its own ichnospecies name and suggests a different kind of producer. U. quadrisulcata isp. nov. is interpreted as a fish trail, probably produced by a representative of Amiiformes (actinopterygian, ray-finned fish) or coelacanth fish." @default.
- W2910552908 created "2019-01-25" @default.
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- W2910552908 date "2019-01-17" @default.
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- W2910552908 title "The Fish Trail <i>Undichna quadrisulcata</i> isp. nov. from the Eocene of Spitsbergen" @default.
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- W2910552908 doi "https://doi.org/10.1080/10420940.2018.1532901" @default.
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