A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil

Detalhes bibliográficos
Autor(a) principal: Leme, Juliana M.
Data de Publicação: 2022
Outros Autores: Van Iten, Heyo, Simões, Marcello G. [UNESP]
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Repositório Institucional da UNESP
Texto Completo: http://dx.doi.org/10.3389/feart.2022.777746
http://hdl.handle.net/11449/240384
Resumo: Paraconularia ediacara n. sp., the oldest documented conulariid cnidarian, is described based on a compressed thin specimen from the terminal Ediacaran Tamengo Formation near Corumbá, Mato Grosso do Sul State, Brazil. The conulariid was collected from a laminated silty shale bed also containing Corumbella werneri and vendotaenid algae. The specimen consists of four partial faces, two of which are mostly covered, and one exposed corner sulcus. The two exposed faces exhibit 32 bell-curve-shaped, nodose transverse ribs, with some nodes preserving a short, adaperturally directed interspace ridge (spine). The transverse ribs bend adapertureward on the shoulders of the corner sulcus, within which the ribs terminate, with the end portions of the ribs from one face alternating with and slightly overlapping those from the adjoining face. This is the first Ediacaran body fossil showing compelling evidence of homology with a particular conulariid genus. However, unlike the periderm of Phanerozoic conulariids, the periderm of P. ediacara lacks calcium phosphate, a difference which may be original or an artifact of diagenesis or weathering. The discovery of P. ediacara in the Tamengo Formation corroborates the hypothesis, based in part on molecular clock studies, that cnidarians originated during mid-late Proterozoic times, and serves as a new internal calibration point, dating the split between scyphozoan and cubozoan cnidarians at no later than 542 Ma. Furthermore, P. ediacara reinforces the argument that the final phase of Ediacaran biotic evolution featured the advent of large-bodied eumetazoans, including, possibly, predators.
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spelling A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of BrazilconulariidsEdiacaranPaleoecologysystematicsTamengo FormationParaconularia ediacara n. sp., the oldest documented conulariid cnidarian, is described based on a compressed thin specimen from the terminal Ediacaran Tamengo Formation near Corumbá, Mato Grosso do Sul State, Brazil. The conulariid was collected from a laminated silty shale bed also containing Corumbella werneri and vendotaenid algae. The specimen consists of four partial faces, two of which are mostly covered, and one exposed corner sulcus. The two exposed faces exhibit 32 bell-curve-shaped, nodose transverse ribs, with some nodes preserving a short, adaperturally directed interspace ridge (spine). The transverse ribs bend adapertureward on the shoulders of the corner sulcus, within which the ribs terminate, with the end portions of the ribs from one face alternating with and slightly overlapping those from the adjoining face. This is the first Ediacaran body fossil showing compelling evidence of homology with a particular conulariid genus. However, unlike the periderm of Phanerozoic conulariids, the periderm of P. ediacara lacks calcium phosphate, a difference which may be original or an artifact of diagenesis or weathering. The discovery of P. ediacara in the Tamengo Formation corroborates the hypothesis, based in part on molecular clock studies, that cnidarians originated during mid-late Proterozoic times, and serves as a new internal calibration point, dating the split between scyphozoan and cubozoan cnidarians at no later than 542 Ma. Furthermore, P. ediacara reinforces the argument that the final phase of Ediacaran biotic evolution featured the advent of large-bodied eumetazoans, including, possibly, predators.Department of Sedimentary and Environmental Geology Geosciences Institute Universidade de São PauloDepartment of Geology Hanover CollegeDepartment of Invertebrate Paleontology Research Associate Cincinnati Museum CenterSector of Zoology Universidade Estadual Paulista IB UNESPSector of Zoology Universidade Estadual Paulista IB UNESPUniversidade de São Paulo (USP)Hanover CollegeCincinnati Museum CenterUniversidade Estadual Paulista (UNESP)Leme, Juliana M.Van Iten, HeyoSimões, Marcello G. [UNESP]2023-03-01T20:14:48Z2023-03-01T20:14:48Z2022-06-08info:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articlehttp://dx.doi.org/10.3389/feart.2022.777746Frontiers in Earth Science, v. 10.2296-6463http://hdl.handle.net/11449/24038410.3389/feart.2022.7777462-s2.0-85133380850Scopusreponame:Repositório Institucional da UNESPinstname:Universidade Estadual Paulista (UNESP)instacron:UNESPengFrontiers in Earth Scienceinfo:eu-repo/semantics/openAccess2023-03-01T20:14:48Zoai:repositorio.unesp.br:11449/240384Repositório InstitucionalPUBhttp://repositorio.unesp.br/oai/requestopendoar:29462023-03-01T20:14:48Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)false
dc.title.none.fl_str_mv A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
title A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
spellingShingle A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
Leme, Juliana M.
conulariids
Ediacaran
Paleoecology
systematics
Tamengo Formation
title_short A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
title_full A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
title_fullStr A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
title_full_unstemmed A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
title_sort A New Conulariid (Cnidaria, Scyphozoa) From the Terminal Ediacaran of Brazil
author Leme, Juliana M.
author_facet Leme, Juliana M.
Van Iten, Heyo
Simões, Marcello G. [UNESP]
author_role author
author2 Van Iten, Heyo
Simões, Marcello G. [UNESP]
author2_role author
author
dc.contributor.none.fl_str_mv Universidade de São Paulo (USP)
Hanover College
Cincinnati Museum Center
Universidade Estadual Paulista (UNESP)
dc.contributor.author.fl_str_mv Leme, Juliana M.
Van Iten, Heyo
Simões, Marcello G. [UNESP]
dc.subject.por.fl_str_mv conulariids
Ediacaran
Paleoecology
systematics
Tamengo Formation
topic conulariids
Ediacaran
Paleoecology
systematics
Tamengo Formation
description Paraconularia ediacara n. sp., the oldest documented conulariid cnidarian, is described based on a compressed thin specimen from the terminal Ediacaran Tamengo Formation near Corumbá, Mato Grosso do Sul State, Brazil. The conulariid was collected from a laminated silty shale bed also containing Corumbella werneri and vendotaenid algae. The specimen consists of four partial faces, two of which are mostly covered, and one exposed corner sulcus. The two exposed faces exhibit 32 bell-curve-shaped, nodose transverse ribs, with some nodes preserving a short, adaperturally directed interspace ridge (spine). The transverse ribs bend adapertureward on the shoulders of the corner sulcus, within which the ribs terminate, with the end portions of the ribs from one face alternating with and slightly overlapping those from the adjoining face. This is the first Ediacaran body fossil showing compelling evidence of homology with a particular conulariid genus. However, unlike the periderm of Phanerozoic conulariids, the periderm of P. ediacara lacks calcium phosphate, a difference which may be original or an artifact of diagenesis or weathering. The discovery of P. ediacara in the Tamengo Formation corroborates the hypothesis, based in part on molecular clock studies, that cnidarians originated during mid-late Proterozoic times, and serves as a new internal calibration point, dating the split between scyphozoan and cubozoan cnidarians at no later than 542 Ma. Furthermore, P. ediacara reinforces the argument that the final phase of Ediacaran biotic evolution featured the advent of large-bodied eumetazoans, including, possibly, predators.
publishDate 2022
dc.date.none.fl_str_mv 2022-06-08
2023-03-01T20:14:48Z
2023-03-01T20:14:48Z
dc.type.status.fl_str_mv info:eu-repo/semantics/publishedVersion
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv http://dx.doi.org/10.3389/feart.2022.777746
Frontiers in Earth Science, v. 10.
2296-6463
http://hdl.handle.net/11449/240384
10.3389/feart.2022.777746
2-s2.0-85133380850
url http://dx.doi.org/10.3389/feart.2022.777746
http://hdl.handle.net/11449/240384
identifier_str_mv Frontiers in Earth Science, v. 10.
2296-6463
10.3389/feart.2022.777746
2-s2.0-85133380850
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv Frontiers in Earth Science
dc.rights.driver.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.source.none.fl_str_mv Scopus
reponame:Repositório Institucional da UNESP
instname:Universidade Estadual Paulista (UNESP)
instacron:UNESP
instname_str Universidade Estadual Paulista (UNESP)
instacron_str UNESP
institution UNESP
reponame_str Repositório Institucional da UNESP
collection Repositório Institucional da UNESP
repository.name.fl_str_mv Repositório Institucional da UNESP - Universidade Estadual Paulista (UNESP)
repository.mail.fl_str_mv
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