Publicação:
Alternative interpretations of some earliest ediacaran fossils from China

dc.contributor.authorIten, Heyo Van
dc.contributor.authorLeme, Juliana de M.
dc.contributor.authorMarques, Antonio C.
dc.contributor.authorSimões, Marcello G. [UNESP]
dc.contributor.institutionHanover College
dc.contributor.institutionCincinnati Museum Center
dc.contributor.institutionUniversidade de São Paulo (USP)
dc.contributor.institutionUniversidade Estadual Paulista (Unesp)
dc.date.accessioned2014-05-27T11:28:37Z
dc.date.available2014-05-27T11:28:37Z
dc.date.issued2013-03-01
dc.description.abstractIn a letter to Nature (February, 2011), Xunlai Yuan and collaborators recorded carbon compression fossils from black shales of the Lantian Formation (Ediacaran), southern Anhui Province, South China. The new fossils, described under five morphological types (Types A to E), exhibit degrees of morphological differentiation suggesting that they were multicellular eukaryotes. Some of the Lantian macrofossils were interpreted as algae, but others are of unknown affinities. For reasons noted in this discussion, Type A fossils attracted our particular attention, and we suggest an alternative interpretation of their affinities. According to our view, some of them (at least those with three faces and no globose holdfast at their base) may represent conulariid cnidarians or close medusozoan relatives. The undistorted organism probably was a three-sided cone in life. We believe that our suggested alternative interpretations of the anatomy and affinities of the fossils in question can be useful in guiding future research on the oldest currently known fossil assemblage of multicellular organisms. Copyright © 2012.en
dc.description.affiliationDeportment of Geology Hanover College, Hanover, IN 47243
dc.description.affiliationDepartment of Invertebrate Paleontology Cincinnati Museum Center, 1301 Western Avenue, Cincinnati, OH 45203
dc.description.affiliationDepartment of Sedimentary and Environmental Geology University of São Paulo, 05580-080, São Paulo, SP
dc.description.affiliationDepartment of Zoology University of São Paulo, Rua do Matão, Travessa 14, 101, 05508-090, São Paulo, SP
dc.description.affiliationDepartment of Zoology São Paulo State University, 18.618-000, Botucatu, SP
dc.description.affiliationUnespDepartment of Zoology São Paulo State University, 18.618-000, Botucatu, SP
dc.format.extent111-113
dc.identifierhttp://dx.doi.org/10.4202/app.2011.0096
dc.identifier.citationActa Palaeontologica Polonica, v. 58, n. 1, p. 111-113, 2013.
dc.identifier.doi10.4202/app.2011.0096
dc.identifier.file2-s2.0-84875299586.pdf
dc.identifier.issn0567-7920
dc.identifier.issn1732-2421
dc.identifier.scopus2-s2.0-84875299586
dc.identifier.urihttp://hdl.handle.net/11449/74762
dc.identifier.wosWOS:000318462900010
dc.language.isoeng
dc.relation.ispartofActa Palaeontologica Polonica
dc.relation.ispartofjcr1.887
dc.relation.ispartofsjr0,788
dc.rights.accessRightsAcesso aberto
dc.sourceScopus
dc.subjectblack shale
dc.subjectEdiacaran
dc.subjecteukaryote
dc.subjectfossil
dc.subjectmorphology
dc.subjectAnhui
dc.subjectChina
dc.titleAlternative interpretations of some earliest ediacaran fossils from Chinaen
dc.typeArtigo
dcterms.licensehttp://www.app.pan.pl/copyright-policy.html
dspace.entity.typePublication
unesp.author.orcid0000-0002-2884-0541[3]
unesp.author.orcid0000-0002-5833-4885[2]
unesp.author.orcid0000-0002-8706-3199[4]
unesp.campusUniversidade Estadual Paulista (UNESP), Instituto de Biociências, Botucatupt
unesp.departmentZoologia - IBBpt

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