perekond

Pinaceocladichnus Mayoral, 1988

Taksoni kirjeldused

Gaaloul et al., 2023

Diagnosis.—Boring pattern constituted by a regular network of fine tunnels, slightly curved and laterally opposite (cited from Botquelen and Mayoral 2005).

Remarks.—This boring is a network of stolon tunnels with apertures produced by ctenostome bryozoans similar to those produced by the genus Immergentia Silén, 1946, or Terebripora d’Orbigny, 1847 (Mayoral 1988). This trace fossil occurs in marine environments from the littoral to neritic zones on calcareous substrates. Pinaceocladichnus occurs since the Ordovician (Mayoral 1991; Toom et al. 2019).

Wisshak et al., 2019a

Microboring; substrate calcareous; tracemaker invertebrate

Buatois et al., 2017

Category of architectural design: 2.70. Camerate network borings.

Knaust, 2012a

Branched, network.

Botquelen & Mayoral, 2005

Ichnogeneric diagnosis. Boring pattern constituted by a regular network of fine tunnels, slightly curved and laterally opposite.

Mayoral, 1988

Diagnosis. Modelo de perforation formade por un sistema muy regular de tunels finos, suavemente arqueadod, que se bifurcan de forma verticelada en sentidos opuestos. Esta diposicion del sistema recuerda a las hojas de los pinos o abetos, aspecto del cual toma el nombre.[Perforation model formed by a very regular system of fine, gently arched tunnels, which branch in a whorled manner in opposite directions. This arrangement of the system is reminiscent of the leaves of pine or fir trees, the aspect from which it takes its name.]

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
Richiano, S., Schwarz, E., Veiga, G. D., Trentini, G. Á. 2019. Non-depositional and erosional “offshore” bioeroded hardgrounds from the Lower Cretaceous of the Neuquén Basin, Argentina: Insights into their sequence-stratigraphic implications and controls. Marine and Petroleum Geology 104, 1-10. DOI:10.1016/j.marpetgeo.2019.03.020
Botquelen, A., Mayoral, E. 2005. Early Devonian bioerosion in the Rade de Brest, Armorican massif, France. Palaeontology 48, 5, 1057-1064. DOI:10.1111/j.1475-4983.2005.00492.x
Mayoral, E. 1988. Pennatichnus nov. icnogen.; Pinaceocladichnus nov. icnogen. e Iramena. Huellas de bioerósion debidas a Bryozoa perforantes (Ctenostomata, Plioceno inferior) en la cuenca del Bajo Guadalquivir [Pennatichnus nov. icnogen; Pinaceocladichnus nov. icnogen. and Iramena. Bioerósion traces due to perforating Bryozoa (Ctenostomata, lower Pliocene) in the Lower Guadalquivir basin]. Revista Española de Paleontología 3, 13–23.
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