About: Mollusc trace fossils Ptychoplasma Fenton and Fenton, 1937 and Oravaichnium Plička and Uhrová, 1990: Their type material and ichnospecies     Goto   Sponge   NotDistinct   Permalink

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  • Ichnogenera belonging to cleft-foot and wedge-foot bivalves can in most cases be distinguished. This paper addresses the taxonomy of locomotion traces made by wedge-foot bivalves. Ichnogenera Ptychoplasma Fenton and Fenton and Oravaichnium Plička and Uhrová are reviewed together with related ichnotaxa. Both are interpreted as the locomotion traces of non-cleft, wedge-foot bivalves. Both are usually preserved as hypichnial ridges that include a distinctive bioprint of amygdaloid segments. Ptychoplasma is dominated by amygdaloid segments whereas Oravaichnium is wall-like with only sporadic amygdaloid segments. Ichnospecies of Ptychoplasma are distinguished on the basis of their continuity: P. excelsum Fenton and Fenton (the type) is a relatively continuous trace fossil consisting largely of welded, imbricated amygdaloid segments; P. conica Pieńkowski and Uchman is less welded and consists of conical mounds; and P. vagans (Książkiewicz) consists of a largely discontinuous series of such segments. Only one ichnospecies of Oravaichnium is yet recognized, the type O. hrabei Plička and Uhrová. Tuberculichnus Książkiewicz is a valid ichnogenus, based on its type species T. meandrinus Książkiewicz, but another ichnospecies, T. vagans Książkiewicz, belongs to Ptychoplasma. Hostynichnium Plička and Siráňová is regarded as a junior synonym of Ptychoplasma; its only ichnospecies, H. duplex Plička and Siráňová, is a junior synonym of P. vagans. Lockeia serialis Seilacher and Seilacher, 1994 is a nomen nudum and belongs to Ptychoplasma.
  • Ichnogenera belonging to cleft-foot and wedge-foot bivalves can in most cases be distinguished. This paper addresses the taxonomy of locomotion traces made by wedge-foot bivalves. Ichnogenera Ptychoplasma Fenton and Fenton and Oravaichnium Plička and Uhrová are reviewed together with related ichnotaxa. Both are interpreted as the locomotion traces of non-cleft, wedge-foot bivalves. Both are usually preserved as hypichnial ridges that include a distinctive bioprint of amygdaloid segments. Ptychoplasma is dominated by amygdaloid segments whereas Oravaichnium is wall-like with only sporadic amygdaloid segments. Ichnospecies of Ptychoplasma are distinguished on the basis of their continuity: P. excelsum Fenton and Fenton (the type) is a relatively continuous trace fossil consisting largely of welded, imbricated amygdaloid segments; P. conica Pieńkowski and Uchman is less welded and consists of conical mounds; and P. vagans (Książkiewicz) consists of a largely discontinuous series of such segments. Only one ichnospecies of Oravaichnium is yet recognized, the type O. hrabei Plička and Uhrová. Tuberculichnus Książkiewicz is a valid ichnogenus, based on its type species T. meandrinus Książkiewicz, but another ichnospecies, T. vagans Książkiewicz, belongs to Ptychoplasma. Hostynichnium Plička and Siráňová is regarded as a junior synonym of Ptychoplasma; its only ichnospecies, H. duplex Plička and Siráňová, is a junior synonym of P. vagans. Lockeia serialis Seilacher and Seilacher, 1994 is a nomen nudum and belongs to Ptychoplasma. (en)
Title
  • Mollusc trace fossils Ptychoplasma Fenton and Fenton, 1937 and Oravaichnium Plička and Uhrová, 1990: Their type material and ichnospecies
  • Mollusc trace fossils Ptychoplasma Fenton and Fenton, 1937 and Oravaichnium Plička and Uhrová, 1990: Their type material and ichnospecies (en)
skos:prefLabel
  • Mollusc trace fossils Ptychoplasma Fenton and Fenton, 1937 and Oravaichnium Plička and Uhrová, 1990: Their type material and ichnospecies
  • Mollusc trace fossils Ptychoplasma Fenton and Fenton, 1937 and Oravaichnium Plička and Uhrová, 1990: Their type material and ichnospecies (en)
skos:notation
  • RIV/67985831:_____/11:00363166!RIV12-AV0-67985831
http://linked.open...avai/predkladatel
http://linked.open...avai/riv/aktivita
http://linked.open...avai/riv/aktivity
  • P(GA205/05/0917), Z(AV0Z30130516)
http://linked.open...iv/cisloPeriodika
  • 4
http://linked.open...vai/riv/dodaniDat
http://linked.open...aciTvurceVysledku
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http://linked.open...iv/duvernostUdaju
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http://linked.open...dnocenehoVysledku
  • 213531
http://linked.open...ai/riv/idVysledku
  • RIV/67985831:_____/11:00363166
http://linked.open...riv/jazykVysledku
http://linked.open.../riv/klicovaSlova
  • locomotion trace fossils; Bivalves; flysch; Carboniferous; Cretaceous; Paleogene (en)
http://linked.open.../riv/klicoveSlovo
http://linked.open...odStatuVydavatele
  • FR - Francouzská republika
http://linked.open...ontrolniKodProRIV
  • [E1AEC13325C4]
http://linked.open...i/riv/nazevZdroje
  • Geobios
http://linked.open...in/vavai/riv/obor
http://linked.open...ichTvurcuVysledku
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http://linked.open...vavai/riv/projekt
http://linked.open...UplatneniVysledku
http://linked.open...v/svazekPeriodika
  • 44
http://linked.open...iv/tvurceVysledku
  • Mikuláš, Radek
  • Rindsberg, A. K.
  • Uchman, A.
http://linked.open...ain/vavai/riv/wos
  • 000294380000006
http://linked.open...n/vavai/riv/zamer
issn
  • 0016-6995
number of pages
http://bibframe.org/vocab/doi
  • 10.1016/j.geobios.2010.08.001
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