West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link

Autores
Casadio, Silvio Alberto; Nelson, Campbel; Taylor, Paul; Griffin, Miguel; Gordon, Dennis
Año de publicación
2010
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Crucial oceanographic modifications took place in the Southern Hemisphere during the period between 35 and 15 Ma. These included the establishment of broad zonal belts of surface-water masses separated by oceanic fronts. These belts had a paramount role in the isolation and evolution of the marine faunas in the Southern Hemisphere. However, paleontological evidence demonstrates that during this period paleobiogeographic connections between New Zealand and Patagonia were maintained, as shown by the presence of numerous common taxa. Here we postulate that the paleobiogeographic connection may have been along the West Antarctic Rift System (WARS). This system underwent an episode of significant extension during the Eocene-Oligocene and at the same time the full opening (c. 31 Ma) of the Tasmanian gateway possibly elicited the onset of a proto-circum-Antarctic flow of cold waters, perhaps through a West Antarctic seaway connecting the southern Pacific and Atlantic Oceans. While conclusive support for this hypothesis is presently limited, information assembled during the last decade after research in McMurdo Sound is very enlightening and there is an accumulating body of tectonic, sedimentary and paleontological information that the WARS could have afforded a principal paleobiogeographic seaway linkage between New Zealand and Patagonia in the Oligocene.
Fil: Casadio, Silvio Alberto. Universidad Nacional de La Pampa; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Nelson, Campbel. University of Waikato; Nueva Zelanda
Fil: Taylor, Paul. Natural History Museum; Reino Unido
Fil: Griffin, Miguel. Natural History Museum; Reino Unido. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Gordon, Dennis. No especifíca;
Materia
Paleobiogeography
Oligocene
Antarctica
Patagonia
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/254523

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spelling West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic linkCasadio, Silvio AlbertoNelson, CampbelTaylor, PaulGriffin, MiguelGordon, DennisPaleobiogeographyOligoceneAntarcticaPatagoniahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Crucial oceanographic modifications took place in the Southern Hemisphere during the period between 35 and 15 Ma. These included the establishment of broad zonal belts of surface-water masses separated by oceanic fronts. These belts had a paramount role in the isolation and evolution of the marine faunas in the Southern Hemisphere. However, paleontological evidence demonstrates that during this period paleobiogeographic connections between New Zealand and Patagonia were maintained, as shown by the presence of numerous common taxa. Here we postulate that the paleobiogeographic connection may have been along the West Antarctic Rift System (WARS). This system underwent an episode of significant extension during the Eocene-Oligocene and at the same time the full opening (c. 31 Ma) of the Tasmanian gateway possibly elicited the onset of a proto-circum-Antarctic flow of cold waters, perhaps through a West Antarctic seaway connecting the southern Pacific and Atlantic Oceans. While conclusive support for this hypothesis is presently limited, information assembled during the last decade after research in McMurdo Sound is very enlightening and there is an accumulating body of tectonic, sedimentary and paleontological information that the WARS could have afforded a principal paleobiogeographic seaway linkage between New Zealand and Patagonia in the Oligocene.Fil: Casadio, Silvio Alberto. Universidad Nacional de La Pampa; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; ArgentinaFil: Nelson, Campbel. University of Waikato; Nueva ZelandaFil: Taylor, Paul. Natural History Museum; Reino UnidoFil: Griffin, Miguel. Natural History Museum; Reino Unido. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; ArgentinaFil: Gordon, Dennis. No especifíca;Asociación Paleontológica Argentina2010-03info: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/11336/254523Casadio, Silvio Alberto; Nelson, Campbel; Taylor, Paul; Griffin, Miguel; Gordon, Dennis; West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link; Asociación Paleontológica Argentina; Ameghiniana; 47; 1; 3-2010; 129-1320002-70141851-8044CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://www.ameghiniana.org.ar/index.php/ameghiniana/article/view/227info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-29T09:35:11Zoai:ri.conicet.gov.ar:11336/254523instacron: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 09:35:11.284CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
title West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
spellingShingle West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
Casadio, Silvio Alberto
Paleobiogeography
Oligocene
Antarctica
Patagonia
title_short West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
title_full West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
title_fullStr West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
title_full_unstemmed West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
title_sort West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link
dc.creator.none.fl_str_mv Casadio, Silvio Alberto
Nelson, Campbel
Taylor, Paul
Griffin, Miguel
Gordon, Dennis
author Casadio, Silvio Alberto
author_facet Casadio, Silvio Alberto
Nelson, Campbel
Taylor, Paul
Griffin, Miguel
Gordon, Dennis
author_role author
author2 Nelson, Campbel
Taylor, Paul
Griffin, Miguel
Gordon, Dennis
author2_role author
author
author
author
dc.subject.none.fl_str_mv Paleobiogeography
Oligocene
Antarctica
Patagonia
topic Paleobiogeography
Oligocene
Antarctica
Patagonia
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Crucial oceanographic modifications took place in the Southern Hemisphere during the period between 35 and 15 Ma. These included the establishment of broad zonal belts of surface-water masses separated by oceanic fronts. These belts had a paramount role in the isolation and evolution of the marine faunas in the Southern Hemisphere. However, paleontological evidence demonstrates that during this period paleobiogeographic connections between New Zealand and Patagonia were maintained, as shown by the presence of numerous common taxa. Here we postulate that the paleobiogeographic connection may have been along the West Antarctic Rift System (WARS). This system underwent an episode of significant extension during the Eocene-Oligocene and at the same time the full opening (c. 31 Ma) of the Tasmanian gateway possibly elicited the onset of a proto-circum-Antarctic flow of cold waters, perhaps through a West Antarctic seaway connecting the southern Pacific and Atlantic Oceans. While conclusive support for this hypothesis is presently limited, information assembled during the last decade after research in McMurdo Sound is very enlightening and there is an accumulating body of tectonic, sedimentary and paleontological information that the WARS could have afforded a principal paleobiogeographic seaway linkage between New Zealand and Patagonia in the Oligocene.
Fil: Casadio, Silvio Alberto. Universidad Nacional de La Pampa; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina
Fil: Nelson, Campbel. University of Waikato; Nueva Zelanda
Fil: Taylor, Paul. Natural History Museum; Reino Unido
Fil: Griffin, Miguel. Natural History Museum; Reino Unido. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. División Paleozoología Invertebrados; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata; Argentina
Fil: Gordon, Dennis. No especifíca;
description Crucial oceanographic modifications took place in the Southern Hemisphere during the period between 35 and 15 Ma. These included the establishment of broad zonal belts of surface-water masses separated by oceanic fronts. These belts had a paramount role in the isolation and evolution of the marine faunas in the Southern Hemisphere. However, paleontological evidence demonstrates that during this period paleobiogeographic connections between New Zealand and Patagonia were maintained, as shown by the presence of numerous common taxa. Here we postulate that the paleobiogeographic connection may have been along the West Antarctic Rift System (WARS). This system underwent an episode of significant extension during the Eocene-Oligocene and at the same time the full opening (c. 31 Ma) of the Tasmanian gateway possibly elicited the onset of a proto-circum-Antarctic flow of cold waters, perhaps through a West Antarctic seaway connecting the southern Pacific and Atlantic Oceans. While conclusive support for this hypothesis is presently limited, information assembled during the last decade after research in McMurdo Sound is very enlightening and there is an accumulating body of tectonic, sedimentary and paleontological information that the WARS could have afforded a principal paleobiogeographic seaway linkage between New Zealand and Patagonia in the Oligocene.
publishDate 2010
dc.date.none.fl_str_mv 2010-03
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/11336/254523
Casadio, Silvio Alberto; Nelson, Campbel; Taylor, Paul; Griffin, Miguel; Gordon, Dennis; West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link; Asociación Paleontológica Argentina; Ameghiniana; 47; 1; 3-2010; 129-132
0002-7014
1851-8044
CONICET Digital
CONICET
url http://hdl.handle.net/11336/254523
identifier_str_mv Casadio, Silvio Alberto; Nelson, Campbel; Taylor, Paul; Griffin, Miguel; Gordon, Dennis; West Antarctic Rift system: a possible New Zealand-Patagonia Oligocene paleobiogeographic link; Asociación Paleontológica Argentina; Ameghiniana; 47; 1; 3-2010; 129-132
0002-7014
1851-8044
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://www.ameghiniana.org.ar/index.php/ameghiniana/article/view/227
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 Asociación Paleontológica Argentina
publisher.none.fl_str_mv Asociación Paleontológica Argentina
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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