A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica
- Autores
- Bomfleur, Benjamin; Escapa, Ignacio Hernán; Serbet, Rudolph; Taylor, Edith L.; Taylor, Thomas N.
- Año de publicación
- 2013
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Sphenophytes are a common floral element in the Triassic of Gondwana. Most sphenophyte compression fossils have been conventionally assigned to a few, presumably very widespread species of Neocalamites based on vegetative features of the stems (or pith casts) and the foliage. During recent decades, however, new reports on morphological and anatomical details of some of these fossils have cast doubt on the systematic affinities of many Gondwanan Triassic sphenophytes. Here we describe Neocalamites suberosus (Artabe & Zamuner) nov. comb. et emend. and Schizoneura africana Feistmantel emend. from several Triassic deposits in the central Transantarctic Mountains and Victoria Land, East Antarctica. The material enables a critical reevaluation of morphological and anatomical features that have been historically used to define the two genera, including leaf- base morphology, degree of leaf fusion, stem vasculature and vallecular canals, and features of the nodal diaphragm. The diagnoses of Neocalamites and Schizoneura are emended so that they more accurately reflect recent advances in our understanding of the anatomy and ontogeny of these plants.
Fil: Bomfleur, Benjamin. University of Kansas; Estados Unidos de América;
Fil: Escapa, Ignacio Hernán. Museo Paleontologico Egidio Feruglio; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Serbet, Rudolph. University of Kansas; Argentina
Fil: Taylor, Edith L.. University of Kansas; Estados Unidos de América;
Fil: Taylor, Thomas N.. University of Kansas; Estados Unidos de América; - Materia
-
NODODENDRON
PARASCHIZONEURA
SPHENOPHYTA
TRANSANTARCTIC MOUNTAINS
VICTORIA LAND - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
- Repositorio
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/1608
Ver los metadatos del registro completo
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spelling |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East AntarcticaBomfleur, BenjaminEscapa, Ignacio HernánSerbet, RudolphTaylor, Edith L.Taylor, Thomas N.NODODENDRONPARASCHIZONEURASPHENOPHYTATRANSANTARCTIC MOUNTAINSVICTORIA LANDhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Sphenophytes are a common floral element in the Triassic of Gondwana. Most sphenophyte compression fossils have been conventionally assigned to a few, presumably very widespread species of Neocalamites based on vegetative features of the stems (or pith casts) and the foliage. During recent decades, however, new reports on morphological and anatomical details of some of these fossils have cast doubt on the systematic affinities of many Gondwanan Triassic sphenophytes. Here we describe Neocalamites suberosus (Artabe & Zamuner) nov. comb. et emend. and Schizoneura africana Feistmantel emend. from several Triassic deposits in the central Transantarctic Mountains and Victoria Land, East Antarctica. The material enables a critical reevaluation of morphological and anatomical features that have been historically used to define the two genera, including leaf- base morphology, degree of leaf fusion, stem vasculature and vallecular canals, and features of the nodal diaphragm. The diagnoses of Neocalamites and Schizoneura are emended so that they more accurately reflect recent advances in our understanding of the anatomy and ontogeny of these plants.Fil: Bomfleur, Benjamin. University of Kansas; Estados Unidos de América;Fil: Escapa, Ignacio Hernán. Museo Paleontologico Egidio Feruglio; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Serbet, Rudolph. University of Kansas; ArgentinaFil: Taylor, Edith L.. University of Kansas; Estados Unidos de América;Fil: Taylor, Thomas N.. University of Kansas; Estados Unidos de América;Taylor & Francis Ltd2013-05info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/1608Bomfleur, Benjamin; Escapa, Ignacio Hernán; Serbet, Rudolph; Taylor, Edith L.; Taylor, Thomas N.; A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica; Taylor & Francis Ltd; Alcheringa; 37; 3; 5-2013; 349-3650311-5518enginfo:eu-repo/semantics/altIdentifier/doi/10.1080/03115518.2013.764693info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:57:03Zoai:ri.conicet.gov.ar:11336/1608instacron: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:34982025-09-29 09:57:03.829CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse |
dc.title.none.fl_str_mv |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica |
title |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica |
spellingShingle |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica Bomfleur, Benjamin NODODENDRON PARASCHIZONEURA SPHENOPHYTA TRANSANTARCTIC MOUNTAINS VICTORIA LAND |
title_short |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica |
title_full |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica |
title_fullStr |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica |
title_full_unstemmed |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica |
title_sort |
A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica |
dc.creator.none.fl_str_mv |
Bomfleur, Benjamin Escapa, Ignacio Hernán Serbet, Rudolph Taylor, Edith L. Taylor, Thomas N. |
author |
Bomfleur, Benjamin |
author_facet |
Bomfleur, Benjamin Escapa, Ignacio Hernán Serbet, Rudolph Taylor, Edith L. Taylor, Thomas N. |
author_role |
author |
author2 |
Escapa, Ignacio Hernán Serbet, Rudolph Taylor, Edith L. Taylor, Thomas N. |
author2_role |
author author author author |
dc.subject.none.fl_str_mv |
NODODENDRON PARASCHIZONEURA SPHENOPHYTA TRANSANTARCTIC MOUNTAINS VICTORIA LAND |
topic |
NODODENDRON PARASCHIZONEURA SPHENOPHYTA TRANSANTARCTIC MOUNTAINS VICTORIA LAND |
purl_subject.fl_str_mv |
https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
dc.description.none.fl_txt_mv |
Sphenophytes are a common floral element in the Triassic of Gondwana. Most sphenophyte compression fossils have been conventionally assigned to a few, presumably very widespread species of Neocalamites based on vegetative features of the stems (or pith casts) and the foliage. During recent decades, however, new reports on morphological and anatomical details of some of these fossils have cast doubt on the systematic affinities of many Gondwanan Triassic sphenophytes. Here we describe Neocalamites suberosus (Artabe & Zamuner) nov. comb. et emend. and Schizoneura africana Feistmantel emend. from several Triassic deposits in the central Transantarctic Mountains and Victoria Land, East Antarctica. The material enables a critical reevaluation of morphological and anatomical features that have been historically used to define the two genera, including leaf- base morphology, degree of leaf fusion, stem vasculature and vallecular canals, and features of the nodal diaphragm. The diagnoses of Neocalamites and Schizoneura are emended so that they more accurately reflect recent advances in our understanding of the anatomy and ontogeny of these plants. Fil: Bomfleur, Benjamin. University of Kansas; Estados Unidos de América; Fil: Escapa, Ignacio Hernán. Museo Paleontologico Egidio Feruglio; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Serbet, Rudolph. University of Kansas; Argentina Fil: Taylor, Edith L.. University of Kansas; Estados Unidos de América; Fil: Taylor, Thomas N.. University of Kansas; Estados Unidos de América; |
description |
Sphenophytes are a common floral element in the Triassic of Gondwana. Most sphenophyte compression fossils have been conventionally assigned to a few, presumably very widespread species of Neocalamites based on vegetative features of the stems (or pith casts) and the foliage. During recent decades, however, new reports on morphological and anatomical details of some of these fossils have cast doubt on the systematic affinities of many Gondwanan Triassic sphenophytes. Here we describe Neocalamites suberosus (Artabe & Zamuner) nov. comb. et emend. and Schizoneura africana Feistmantel emend. from several Triassic deposits in the central Transantarctic Mountains and Victoria Land, East Antarctica. The material enables a critical reevaluation of morphological and anatomical features that have been historically used to define the two genera, including leaf- base morphology, degree of leaf fusion, stem vasculature and vallecular canals, and features of the nodal diaphragm. The diagnoses of Neocalamites and Schizoneura are emended so that they more accurately reflect recent advances in our understanding of the anatomy and ontogeny of these plants. |
publishDate |
2013 |
dc.date.none.fl_str_mv |
2013-05 |
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/11336/1608 Bomfleur, Benjamin; Escapa, Ignacio Hernán; Serbet, Rudolph; Taylor, Edith L.; Taylor, Thomas N.; A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica; Taylor & Francis Ltd; Alcheringa; 37; 3; 5-2013; 349-365 0311-5518 |
url |
http://hdl.handle.net/11336/1608 |
identifier_str_mv |
Bomfleur, Benjamin; Escapa, Ignacio Hernán; Serbet, Rudolph; Taylor, Edith L.; Taylor, Thomas N.; A reappraisal of Neocalamites and Schizoneura (fossil Equisetales) based on material from the Triassic of East Antarctica; Taylor & Francis Ltd; Alcheringa; 37; 3; 5-2013; 349-365 0311-5518 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/doi/10.1080/03115518.2013.764693 |
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 |
dc.publisher.none.fl_str_mv |
Taylor & Francis Ltd |
publisher.none.fl_str_mv |
Taylor & Francis Ltd |
dc.source.none.fl_str_mv |
reponame:CONICET Digital (CONICET) instname:Consejo Nacional de Investigaciones Científicas y Técnicas |
reponame_str |
CONICET Digital (CONICET) |
collection |
CONICET Digital (CONICET) |
instname_str |
Consejo Nacional de Investigaciones Científicas y Técnicas |
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 |
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1844613709632110592 |
score |
13.070432 |