Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes

Dipterid ferns possess robust fossil record from Mesozoic times on, and they are considered to be a reliable indicator of warm to subtropical humid or seasonal paleoclimatic conditions. In this contribution, we revised and described new samples of fossil Dipteridaceae, from the Barreal and Cortaderi...

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Detalhes bibliográficos
Autores: Bodnar, Josefina, Drovandi, Juan Martín, Morel, Eduardo Manuel, Ganuza, Daniel Gustavo
Formato: artículo
Estado:Versión publicada
Fecha de publicación:2018
País:Argentina
Recursos:Consejo Nacional de Investigaciones Científicas y Técnicas
Repositorio:CONICET Digital (CONICET)
Idioma:inglés
OAI Identifier:oai:ri.conicet.gov.ar:11336/86632
Acesso em linha:http://hdl.handle.net/11336/86632
Access Level:acceso abierto
Palavra-chave:Monilophyta
Polypodiopsida
Gleicheniales
Thaumatopteris
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
id AR_b87e525eddb8c1c58db17b83f04da34a
oai_identifier_str oai:ri.conicet.gov.ar:11336/86632
network_acronym_str AR
network_name_str Argentina
repository_id_str
dc.title.none.fl_str_mv Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
title Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
spellingShingle Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
Bodnar, Josefina
Monilophyta
Polypodiopsida
Gleicheniales
Thaumatopteris
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
title_short Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
title_full Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
title_fullStr Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
title_full_unstemmed Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
title_sort Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes
dc.creator.none.fl_str_mv Bodnar, Josefina
Drovandi, Juan Martín
Morel, Eduardo Manuel
Ganuza, Daniel Gustavo
author Bodnar, Josefina
author_facet Bodnar, Josefina
Drovandi, Juan Martín
Morel, Eduardo Manuel
Ganuza, Daniel Gustavo
author_role author
author2 Drovandi, Juan Martín
Morel, Eduardo Manuel
Ganuza, Daniel Gustavo
author2_role author
author
author
dc.subject.none.fl_str_mv Monilophyta
Polypodiopsida
Gleicheniales
Thaumatopteris
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic Monilophyta
Polypodiopsida
Gleicheniales
Thaumatopteris
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description Dipterid ferns possess robust fossil record from Mesozoic times on, and they are considered to be a reliable indicator of warm to subtropical humid or seasonal paleoclimatic conditions. In this contribution, we revised and described new samples of fossil Dipteridaceae, from the Barreal and Cortaderita formations (Sorocayense Group), Middle Triassic (Anisian–Ladinian), central-western Argentina. We found out that three species of Dictyophyllum, one of Hausmannia, and one of Thaumatopteris are present in the Sorocayense Group. We erected a new species Dictyophyllum menendezi sp. nov., which is characterized by petiolate fan-shaped fronds, rachis dividing into two arms, each one bearing 5 or 6 oblanceolate pinnae, basal lamina of adjacent pinnae fused forming a wide web, pinnae margin entire to undulate, primary veins catadromous to isodromous, secondary veins subopposite, tertiary veins subopposite to alternate, falcate or with a zig-zag pattern, dichotomizing four times to form a fine reticulate mesh of polygonal irregular areoles. Temporal changes in the diversity of Dipteridaceae were identified in Sorocayense Group. The first record and the maximum species richness occur at the top of the Barreal Formation (late Anisian) with three species. The lower member of the Cortaderita Formation (early Ladinian) presents two species. Dipteridaceae fossils are not registered in the upper member of the Cortaderita Formation (late Ladinian). An important diversification pulse of the family is registered during the late Norian–Rhaetian in other areas of Argentina (Paso Flores, Malargüe, and Atuel depocenters). The flourishing of Dipteridaceae during the late Anisian–early Ladinian and the late Norian–Rhaetian could be related to the increasing humidity episodes of the subtropical seasonal climate that prevailed during the Triassic. Furthermore, Dipteridaceae appear important in the establishment of plant communities, being part of early stages of floristic succession.
publishDate 2018
dc.date.none.fl_str_mv 2018-06
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/86632
Bodnar, Josefina; Drovandi, Juan Martín; Morel, Eduardo Manuel; Ganuza, Daniel Gustavo; Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes; Polish Academy of Sciences. Institute of Paleobiology; Acta Palaeontologica Polonica; 63; 2; 6-2018; 397-417
0567-7920
1732-2421
CONICET Digital
CONICET
url http://hdl.handle.net/11336/86632
identifier_str_mv Bodnar, Josefina; Drovandi, Juan Martín; Morel, Eduardo Manuel; Ganuza, Daniel Gustavo; Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes; Polish Academy of Sciences. Institute of Paleobiology; Acta Palaeontologica Polonica; 63; 2; 6-2018; 397-417
0567-7920
1732-2421
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.4202/app.00459.2018
info:eu-repo/semantics/altIdentifier/url/https://www.app.pan.pl/article/item/app004592018.html
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
dc.publisher.none.fl_str_mv Polish Academy of Sciences. Institute of Paleobiology
publisher.none.fl_str_mv Polish Academy of Sciences. Institute of Paleobiology
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
_version_ 1799195698302812160
spelling Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changesBodnar, JosefinaDrovandi, Juan MartínMorel, Eduardo ManuelGanuza, Daniel GustavoMonilophytaPolypodiopsidaGleichenialesThaumatopterishttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Dipterid ferns possess robust fossil record from Mesozoic times on, and they are considered to be a reliable indicator of warm to subtropical humid or seasonal paleoclimatic conditions. In this contribution, we revised and described new samples of fossil Dipteridaceae, from the Barreal and Cortaderita formations (Sorocayense Group), Middle Triassic (Anisian–Ladinian), central-western Argentina. We found out that three species of Dictyophyllum, one of Hausmannia, and one of Thaumatopteris are present in the Sorocayense Group. We erected a new species Dictyophyllum menendezi sp. nov., which is characterized by petiolate fan-shaped fronds, rachis dividing into two arms, each one bearing 5 or 6 oblanceolate pinnae, basal lamina of adjacent pinnae fused forming a wide web, pinnae margin entire to undulate, primary veins catadromous to isodromous, secondary veins subopposite, tertiary veins subopposite to alternate, falcate or with a zig-zag pattern, dichotomizing four times to form a fine reticulate mesh of polygonal irregular areoles. Temporal changes in the diversity of Dipteridaceae were identified in Sorocayense Group. The first record and the maximum species richness occur at the top of the Barreal Formation (late Anisian) with three species. The lower member of the Cortaderita Formation (early Ladinian) presents two species. Dipteridaceae fossils are not registered in the upper member of the Cortaderita Formation (late Ladinian). An important diversification pulse of the family is registered during the late Norian–Rhaetian in other areas of Argentina (Paso Flores, Malargüe, and Atuel depocenters). The flourishing of Dipteridaceae during the late Anisian–early Ladinian and the late Norian–Rhaetian could be related to the increasing humidity episodes of the subtropical seasonal climate that prevailed during the Triassic. Furthermore, Dipteridaceae appear important in the establishment of plant communities, being part of early stages of floristic succession.Fil: Bodnar, Josefina. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Drovandi, Juan Martín. Universidad Nacional de San Juan; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Morel, Eduardo Manuel. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Ganuza, Daniel Gustavo. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Área Paleobotánica; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaPolish Academy of Sciences. Institute of Paleobiology2018-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/86632Bodnar, Josefina; Drovandi, Juan Martín; Morel, Eduardo Manuel; Ganuza, Daniel Gustavo; Middle Triassic dipterid ferns from west-central Argentina and their relationship to palaeoclimatic changes; Polish Academy of Sciences. Institute of Paleobiology; Acta Palaeontologica Polonica; 63; 2; 6-2018; 397-4170567-79201732-2421CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.4202/app.00459.2018info:eu-repo/semantics/altIdentifier/url/https://www.app.pan.pl/article/item/app004592018.htmlinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2024-05-08T14:00:41Zoai:ri.conicet.gov.ar:11336/86632instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982024-05-08 14:00:42.001CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
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