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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/254523
Ver los metadatos del registro completo
id |
CONICETDig_09d46970867e67d577073fee0545c799 |
---|---|
oai_identifier_str |
oai:ri.conicet.gov.ar:11336/254523 |
network_acronym_str |
CONICETDig |
repository_id_str |
3498 |
network_name_str |
CONICET Digital (CONICET) |
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 |
_version_ |
1844613094381191168 |
score |
13.070432 |