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Planolites

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An ichnotaxon (plural ichnotaxa ) is "a taxon based on the fossilized work of an organism", i.e. the non-human equivalent of an artifact . Ichnotaxon comes from the Ancient Greek ἴχνος ( íchnos ) meaning "track" and English taxon , itself derived from Ancient Greek τάξις ( táxis ) meaning "ordering".

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4-874: See text. Planolites is an ichnogenus found throughout the Ediacaran and the Phanerozoic that is made during the feeding process of worm -like animals. The traces are generally small, 1–5 mm (0.039–0.197 in), unlined, and rarely branched, with fill that differs from the host rock. Planolites fossils have been found in Africa, Asia, Europe, Antarctica, and the Americas (with most specimens found in North America). Ichnospecies in Planolites include: This trace fossil -related article

8-849: Is a stub . You can help Misplaced Pages by expanding it . This Ediacaran biota -related article is a stub . You can help Misplaced Pages by expanding it . Ichnogenus Ichnotaxa are names used to identify and distinguish morphologically distinctive ichnofossils , more commonly known as trace fossils ( fossil records of lifeforms ' movement, rather than of the lifeforms themselves). They are assigned genus and species ranks by ichnologists , much like organisms in Linnaean taxonomy . These are known as ichnogenera and ichnospecies , respectively. "Ichnogenus" and "ichnospecies" are commonly abbreviated as "igen." and "isp.". The binomial names of ichnospecies and their genera are to be written in italics . Most researchers classify trace fossils only as far as

12-504: The ichnogenus rank, based upon trace fossils that resemble each other in morphology but have subtle differences. Some authors have constructed detailed hierarchies up to ichnosuperclass, recognizing such fine detail as to identify ichnosuperorder and ichnoinfraclass, but such attempts are controversial. Due to the chaotic nature of trace fossil classification, several ichnogenera hold names normally affiliated with animal body fossils or plant fossils. For example, many ichnogenera are named with

16-545: The suffix -phycus due to misidentification as algae. Edward Hitchcock was the first to use the now common -ichnus suffix in 1858, with Cochlichnus . Due to trace fossils' history of being difficult to classify, there have been several attempts to enforce consistency in the naming of ichnotaxa. The first edition of the International Code of Zoological Nomenclature , published in 1961, ruled that names of taxa published after 1930 should be 'accompanied by

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