dc.contributorUniversidade de São Paulo (USP)
dc.contributorUniversidade Estadual Paulista (Unesp)
dc.contributorINC
dc.date.accessioned2014-05-20T13:54:08Z
dc.date.accessioned2022-10-05T14:31:13Z
dc.date.available2014-05-20T13:54:08Z
dc.date.available2022-10-05T14:31:13Z
dc.date.created2014-05-20T13:54:08Z
dc.date.issued2012-08-01
dc.identifierGeology. Boulder: Geological Soc Amer, Inc, v. 40, n. 8, p. 691-694, 2012.
dc.identifier0091-7613
dc.identifierhttp://hdl.handle.net/11449/19332
dc.identifier10.1130/G33005.1
dc.identifierWOS:000307093100005
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3893455
dc.description.abstractAlthough the basic morphology of the Ediacaran metazoan Corumbella werneri (the type species of the genus) is well established, little is known about its skeletal tissue. Carbonaceous fragments of this fossil from the Itapucumi Group (Paraguay) reveal details of the ultrastructure of its carapace, providing an unprecedented opportunity to understand a paradigmatic issue of the evolution of skeletogenesis in early metazoans. Corumbella was a sessile predator whose carapace consisted of organic polygonal plates with pores and papillae similar to features observed in some conulariids. Its occurrence with the shelly fossil Cloudina suggests that the acquisition of protective structures in metazoans involved penecontemporaneous processes of biomineralization and secretion of organic walls.
dc.languageeng
dc.publisherGeological Soc America
dc.relationGeology
dc.relation5.073
dc.relation3,114
dc.rightsAcesso restrito
dc.sourceWeb of Science
dc.titleThe dawn of animal skeletogenesis: Ultrastructural analysis of the Ediacaran metazoan Corumbella werneri
dc.typeArtigo


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