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The vetulicolian body plan comprises two parts: a voluminous rostral (anterior) forebody, tipped with an anteriorly positioned mouth and lined with a lateral row of five round to oval-shaped openings on each side, which have been interpreted as gills (or at least orifices in the vicinity of the pharynx); and a caudal (posterior) section that primitively comprises seven body segments and functions as a tail. All vetulicolians lack preserved appendages of any kind, having no legs, feelers or even eye spots.[6] The area where the anterior and posterior parts join is constricted.[7]
Their taxonomic affinity has been uncertain; they have been interpreted as stem- and crown-grouparthropods, stem-group vertebrates,[8] and early deuterostomes (a group which as a whole includes the vertebrates, other invertebratechordates, echinoderms and hemichordates). The general scientific consensus before 2001 considered them early limbless arthropods but now considers them early deuterostomes.[9] Vetulicolian fossils examined in 2014 show the presence of notochord-like structures, and it was concluded that vetulicolians are crown-group chordates and probably related to modern tunicates.[10] Research from 2017 rather indicates vetulicolians are related to Saccorhytus, another basal deuterostome group,[11] although another study shows the possibility that Saccorhytus is an ecdysozoan instead of a deuterostome.[12] A 2024 paper, however, found vetulicolians to be a paraphyletic group at the base of Chordata. [13] Banffozoa’s inclusion within this group is dubious, due to their lack of gill slits and apparent gut diverticula, and so they may be within Protostomia instead.[14]
^Liu, Junping; Chen, Ailin; Li, Binglin; Tang, Feng; Zhao, Jiangtai; Chen, Ke (2024-10-06). "Problematic Ediacaran sail-shaped fossils from eastern Yunnan, China". Historical Biology. Informa UK Limited: 1–7. doi:10.1080/08912963.2024.2403588. ISSN0891-2963.
^Dominguez, Patricio and Jeffries, Richard. (2003). Fossil evidence on the origin of appendicularians. Paper read at International Urochordate Meeting 2003. Abstract at [2] – URL retrieved June 22, 2006.
^Caron, Jean-Bernard (June 2005). "Banffia constricta , a putative vetulicolid from the Middle Cambrian Burgess Shale". Transactions of the Royal Society of Edinburgh: Earth Sciences. 96 (2): 95–111. doi:10.1017/S0263593300001255.
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