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Detalhes Referência

Tipo
Artigos em Revista

Tipo de Documento
Artigo Completo

Título
A Kralodvorian (upper Katian, Upper Ordovician) benthic association from the Ferradosa Formation (central Portugal) and its significance for the redefinition and subdivision of the Kralodvorian Stage

Participantes na publicação
J. Colmenar (Author)
S. Pereira (Author)
M. Pires (Author)
C. Marques da Silva (Author)
Dep. Geologia
IDL
A.A. Sá (Author)
T.P. Young (Author)

Resumo
AnewupperKatian(KralodvorianRegionalStage)benthicassociationfromtheRibadeCimaMemberoftheFerradosa Formation,Portugal,isdescribed.Itisdominatedbybryozoansandechinodermsbutbrachiopodsandtrilobitesarealso present.Morethan20speciesofbrachiopods,nineoftrilobitesandeightofechinodermshavebeenidentifiedinthefour studied localities. Among the brachiopods Kjaerina (Villasina) meloui Colmenar, 2016, Dolerorthis abeirensis Mélou, 1990 and Bicuspina cf. armoricana Mélou, 1990 are significant. These species were previously recorded only in the uppermostRosanFormation(ArmoricanMassif,France).PorambonitesdreyfussiHavlí?ek,1981isalsoreportedinthis paperforthefirsttimebesidesitstypehorizonintheupperpartoftheKralodvorianGabianFormation(MontagneNoire, France). Most of the identified trilobite taxa were previously documented only in the Kralodvorian Cystoid Limestone Formation (Iberian Chains, Spain), except Parillaenus? cf. creber Hammann, 1992 and Amphoriops cf. inflatus (Hammann,1992),whosereferredspeciesarealsopresentintheupperBerounian–KralodvorianPortixedduFormation in Sardinia. The record of “Ceraurinus” meridianus (Hammann, 1992), “Bumastus” aff. commodus Apollonov, 1980 andAmphoriopscf.inflatusrepresentthefirstoccurrenceofthesegenera-groupsinPortugal.Theserecordsareimportant additions to the knowledge of the Portuguese Late Ordovician benthic marine communities, providing crucial new data to constrain the biostratigraphy of the Riba de Cima Member and the palaeogeographical setting of this region at thattime.Inaddition,someofthebrachiopodoccurrenceswithmorerestrictedstratigraphicalrangesprovideinvaluable toolsforenablingmoreprecisesubdivisionoftheKralodvorianregionalstage.•Keywords:SouthGondwana,Ribade Cima Member, Buçaco Syncline, upper Katian, Nicolella Fauna.\\\\\\\\n

Data de Submissão/Pedido
2016-10-28
Data de Aceitação
2017-07-17
Data de Publicação
2017-12-18

Instituição
FACULDADE DE CIÊNCIAS DA UNIVERSIDADE DE LISBOA

Suporte
Bulletin of Geosciences

Identificadores da Publicação
ISSN - 1802-8225

Local
Prague, Czech Republic

Editora
Czech Geological Survey

Volume
92
Fascículo
4

Número de Páginas
21
Página Inicial
443
Página Final
464

Identificadores do Documento
DOI - https://doi.org/10.3140/bull.geosci.1643

Identificadores de Qualidade
SCIMAGO Q1 (2017) - 0.743 - Earth and Planetary Sciences (miscellaneous)
SCIMAGO Q2 (2017) - 0.743 - Environmental Science (miscellaneous)
SCOPUS Q2 (2017) - 0.743 - General Earth and Planetary Sciences
SCOPUS Q2 (2017) - 0.743 - General Environmental Science


Exportar referência

APA
J. Colmenar, S. Pereira, M. Pires, C. Marques da Silva, A.A. Sá, T.P. Young, (2017). A Kralodvorian (upper Katian, Upper Ordovician) benthic association from the Ferradosa Formation (central Portugal) and its significance for the redefinition and subdivision of the Kralodvorian Stage. Bulletin of Geosciences, 92, 443-464. ISSN 1802-8225. eISSN .

IEEE
J. Colmenar, S. Pereira, M. Pires, C. Marques da Silva, A.A. Sá, T.P. Young, "A Kralodvorian (upper Katian, Upper Ordovician) benthic association from the Ferradosa Formation (central Portugal) and its significance for the redefinition and subdivision of the Kralodvorian Stage" in Bulletin of Geosciences, vol. 92, pp. 443-464, 2017. 10.3140/bull.geosci.1643

BIBTEX
@article{39746, author = {J. Colmenar and S. Pereira and M. Pires and C. Marques da Silva and A.A. Sá and T.P. Young}, title = {A Kralodvorian (upper Katian, Upper Ordovician) benthic association from the Ferradosa Formation (central Portugal) and its significance for the redefinition and subdivision of the Kralodvorian Stage}, journal = {Bulletin of Geosciences}, year = 2017, pages = {443-464}, volume = 92 }