Alcyonidiopsis: Difference between revisions
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{{Short description|Trace fossil}} |
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⚫ | | authority = Massalongo, 1856 <ref name="google.co.uk">{{cite book|url=https://books.google.com/?id=NWnTgt5E-_QC |
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| taxon = Alcyonidiopsis |
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'''''Alcyonidiopsis ''''' is a genus of pellet-filled trace fossil, often branching, known from the Ordovician |
'''''Alcyonidiopsis ''''' is a [[genus]] of pellet-filled [[trace fossil]], often branching, known from the [[Ordovician]], or possibly earlier, to the recent. It is associated with the quiet, deeper waters of the ''[[Nereites]]'' [[ichnofacies]].<ref name="google.co.uk"/> The individual pellets that infill the burrow are sometimes referred to ''Tomaculum'', though this practice is discouraged.<ref name="google.co.uk"/> |
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==See also== |
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''[[Tubotomaculum]]'', {{cite journal|doi=10.1666/13-123|title=The ichnogenus Tubotomaculum: An enigmatic pellet-filled structure from Upper Cretaceous to Miocene deep-marine deposits of southern Spain|journal=Journal of Paleontology|volume=88|issue=6|pages=1189|year=2015|last1=García-Ramos|first1=Jose Carlos|last2=Mángano|first2=María Gabriela|last3=Piñuela|first3=Laura|last4=Buatois|first4=Luis A.|last5=Rodríguez-Tovar|first5=Francisco J.}} |
''[[Tubotomaculum]]'', {{cite journal|doi=10.1666/13-123|title=The ichnogenus Tubotomaculum: An enigmatic pellet-filled structure from Upper Cretaceous to Miocene deep-marine deposits of southern Spain|journal=Journal of Paleontology|volume=88|issue=6|pages=1189|year=2015|last1=García-Ramos|first1=Jose Carlos|last2=Mángano|first2=María Gabriela|last3=Piñuela|first3=Laura|last4=Buatois|first4=Luis A.|last5=Rodríguez-Tovar|first5=Francisco J.|s2cid=129635502}} |
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==References== |
==References== |
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{{Reflist}} |
{{Reflist}} |
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[[Category:Trace fossils]] |
[[Category:Trace fossils]] |
Latest revision as of 11:33, 19 February 2023
Alcyonidiopsis | |
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Trace fossil classification | |
Ichnogenus: | †Alcyonidiopsis Massalongo, 1856 [1] |
Ichnospecies | |
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Alcyonidiopsis is a genus of pellet-filled trace fossil, often branching, known from the Ordovician, or possibly earlier, to the recent. It is associated with the quiet, deeper waters of the Nereites ichnofacies.[1] The individual pellets that infill the burrow are sometimes referred to Tomaculum, though this practice is discouraged.[1]
See also
[edit]Tubotomaculum, García-Ramos, Jose Carlos; Mángano, María Gabriela; Piñuela, Laura; Buatois, Luis A.; Rodríguez-Tovar, Francisco J. (2015). "The ichnogenus Tubotomaculum: An enigmatic pellet-filled structure from Upper Cretaceous to Miocene deep-marine deposits of southern Spain". Journal of Paleontology. 88 (6): 1189. doi:10.1666/13-123. S2CID 129635502.
References
[edit]- ^ a b c Ordovician and Devonian Trace Fossils from Nevada. NV Bureau of Mines & Geology. 1977 – via Google Books.