The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean
- Autores
- Figueroa, Daniel Enrique; Barbini, Santiago Aldo; Belleggia, Mauro; Sabadin, David Ezequiel; Román, Jorge Martín; De Wysiecki, Agustín María
- Año de publicación
- 2023
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Here, we highlight the geological processes that resulted in the current conformation of the southern Southwest Atlantic Ocean, and explore the heterogeneous composition of the marine ichthyofauna found between 33° and 56° from a paleobiological perspective. During the early Cretaceous (140 Mya), the South Atlantic was still not formed, and Gondwana was probably a set of united plates with shallow continental waters. In the middle Cretaceous (112 Mya), the major Gondwanan plates started diverging from each other, allowing shallow marine intrusions and the diversification of an endemic fish fauna. By the end of the Mesozoic (66 Mya), the proto-South Atlantic connected with the North Atlantic, which was still part of the Tethys Sea, allowing its ichthyofauna to colonize the south and reach the Antarctic region. The opening of the Drake Passage in the Oligocene (33 Mya) enabled the cold waters of the Pacific Ocean to reach the South Atlantic, causing drastic effects on the thermophilic fauna and favoring the dispersion of cold-water species. Successive glaciations during the Quaternary (2 Myr to 10,000 years ago) resulted in the prevalence of Antarctic climatic conditions in the southern Southwest Atlantic. The long history of changing scenarios in the constitution of the southern Southwest Atlantic is reflected in the heterogeneous composition of the marine ichthyofauna between 33° and 56°S, which is characterized by a mixture of cosmopolitan, Tethyan, Pacific, Gondwanan, Antarctic, and endemic origins.
- Materia
-
Biología Marina, Limnología
Drake Passage
endemism
evolutionary history
ichthyofauna
phylogeography
Weddellian Province - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by-nc-sa/4.0/
- Repositorio
- Institución
- Comisión de Investigaciones Científicas de la Provincia de Buenos Aires
- OAI Identificador
- oai:digital.cic.gba.gob.ar:11746/12136
Ver los metadatos del registro completo
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The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic OceanFigueroa, Daniel EnriqueBarbini, Santiago AldoBelleggia, MauroSabadin, David EzequielRomán, Jorge MartínDe Wysiecki, Agustín MaríaBiología Marina, LimnologíaDrake Passageendemismevolutionary historyichthyofaunaphylogeographyWeddellian ProvinceHere, we highlight the geological processes that resulted in the current conformation of the southern Southwest Atlantic Ocean, and explore the heterogeneous composition of the marine ichthyofauna found between 33° and 56° from a paleobiological perspective. During the early Cretaceous (140 Mya), the South Atlantic was still not formed, and Gondwana was probably a set of united plates with shallow continental waters. In the middle Cretaceous (112 Mya), the major Gondwanan plates started diverging from each other, allowing shallow marine intrusions and the diversification of an endemic fish fauna. By the end of the Mesozoic (66 Mya), the proto-South Atlantic connected with the North Atlantic, which was still part of the Tethys Sea, allowing its ichthyofauna to colonize the south and reach the Antarctic region. The opening of the Drake Passage in the Oligocene (33 Mya) enabled the cold waters of the Pacific Ocean to reach the South Atlantic, causing drastic effects on the thermophilic fauna and favoring the dispersion of cold-water species. Successive glaciations during the Quaternary (2 Myr to 10,000 years ago) resulted in the prevalence of Antarctic climatic conditions in the southern Southwest Atlantic. The long history of changing scenarios in the constitution of the southern Southwest Atlantic is reflected in the heterogeneous composition of the marine ichthyofauna between 33° and 56°S, which is characterized by a mixture of cosmopolitan, Tethyan, Pacific, Gondwanan, Antarctic, and endemic origins.2023-02-26info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfhttps://digital.cic.gba.gob.ar/handle/11746/12136enginfo:eu-repo/semantics/altIdentifier/issn/1439-0485info:eu-repo/semantics/altIdentifier/issn/0173-9565info:eu-repo/semantics/altIdentifier/doi/10.1111/maec.12742info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by-nc-sa/4.0/reponame:CIC Digital (CICBA)instname:Comisión de Investigaciones Científicas de la Provincia de Buenos Airesinstacron:CICBA2025-09-04T09:43:43Zoai:digital.cic.gba.gob.ar:11746/12136Institucionalhttp://digital.cic.gba.gob.arOrganismo científico-tecnológicoNo correspondehttp://digital.cic.gba.gob.ar/oai/snrdmarisa.degiusti@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:94412025-09-04 09:43:43.946CIC Digital (CICBA) - Comisión de Investigaciones Científicas de la Provincia de Buenos Airesfalse |
dc.title.none.fl_str_mv |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean |
title |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean |
spellingShingle |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean Figueroa, Daniel Enrique Biología Marina, Limnología Drake Passage endemism evolutionary history ichthyofauna phylogeography Weddellian Province |
title_short |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean |
title_full |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean |
title_fullStr |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean |
title_full_unstemmed |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean |
title_sort |
The ichthyofaunistic colonization and complex biogeographic history of the southern portion of the Southwest Atlantic Ocean |
dc.creator.none.fl_str_mv |
Figueroa, Daniel Enrique Barbini, Santiago Aldo Belleggia, Mauro Sabadin, David Ezequiel Román, Jorge Martín De Wysiecki, Agustín María |
author |
Figueroa, Daniel Enrique |
author_facet |
Figueroa, Daniel Enrique Barbini, Santiago Aldo Belleggia, Mauro Sabadin, David Ezequiel Román, Jorge Martín De Wysiecki, Agustín María |
author_role |
author |
author2 |
Barbini, Santiago Aldo Belleggia, Mauro Sabadin, David Ezequiel Román, Jorge Martín De Wysiecki, Agustín María |
author2_role |
author author author author author |
dc.subject.none.fl_str_mv |
Biología Marina, Limnología Drake Passage endemism evolutionary history ichthyofauna phylogeography Weddellian Province |
topic |
Biología Marina, Limnología Drake Passage endemism evolutionary history ichthyofauna phylogeography Weddellian Province |
dc.description.none.fl_txt_mv |
Here, we highlight the geological processes that resulted in the current conformation of the southern Southwest Atlantic Ocean, and explore the heterogeneous composition of the marine ichthyofauna found between 33° and 56° from a paleobiological perspective. During the early Cretaceous (140 Mya), the South Atlantic was still not formed, and Gondwana was probably a set of united plates with shallow continental waters. In the middle Cretaceous (112 Mya), the major Gondwanan plates started diverging from each other, allowing shallow marine intrusions and the diversification of an endemic fish fauna. By the end of the Mesozoic (66 Mya), the proto-South Atlantic connected with the North Atlantic, which was still part of the Tethys Sea, allowing its ichthyofauna to colonize the south and reach the Antarctic region. The opening of the Drake Passage in the Oligocene (33 Mya) enabled the cold waters of the Pacific Ocean to reach the South Atlantic, causing drastic effects on the thermophilic fauna and favoring the dispersion of cold-water species. Successive glaciations during the Quaternary (2 Myr to 10,000 years ago) resulted in the prevalence of Antarctic climatic conditions in the southern Southwest Atlantic. The long history of changing scenarios in the constitution of the southern Southwest Atlantic is reflected in the heterogeneous composition of the marine ichthyofauna between 33° and 56°S, which is characterized by a mixture of cosmopolitan, Tethyan, Pacific, Gondwanan, Antarctic, and endemic origins. |
description |
Here, we highlight the geological processes that resulted in the current conformation of the southern Southwest Atlantic Ocean, and explore the heterogeneous composition of the marine ichthyofauna found between 33° and 56° from a paleobiological perspective. During the early Cretaceous (140 Mya), the South Atlantic was still not formed, and Gondwana was probably a set of united plates with shallow continental waters. In the middle Cretaceous (112 Mya), the major Gondwanan plates started diverging from each other, allowing shallow marine intrusions and the diversification of an endemic fish fauna. By the end of the Mesozoic (66 Mya), the proto-South Atlantic connected with the North Atlantic, which was still part of the Tethys Sea, allowing its ichthyofauna to colonize the south and reach the Antarctic region. The opening of the Drake Passage in the Oligocene (33 Mya) enabled the cold waters of the Pacific Ocean to reach the South Atlantic, causing drastic effects on the thermophilic fauna and favoring the dispersion of cold-water species. Successive glaciations during the Quaternary (2 Myr to 10,000 years ago) resulted in the prevalence of Antarctic climatic conditions in the southern Southwest Atlantic. The long history of changing scenarios in the constitution of the southern Southwest Atlantic is reflected in the heterogeneous composition of the marine ichthyofauna between 33° and 56°S, which is characterized by a mixture of cosmopolitan, Tethyan, Pacific, Gondwanan, Antarctic, and endemic origins. |
publishDate |
2023 |
dc.date.none.fl_str_mv |
2023-02-26 |
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 |
https://digital.cic.gba.gob.ar/handle/11746/12136 |
url |
https://digital.cic.gba.gob.ar/handle/11746/12136 |
dc.language.none.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
info:eu-repo/semantics/altIdentifier/issn/1439-0485 info:eu-repo/semantics/altIdentifier/issn/0173-9565 info:eu-repo/semantics/altIdentifier/doi/10.1111/maec.12742 |
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info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-sa/4.0/ |
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openAccess |
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http://creativecommons.org/licenses/by-nc-sa/4.0/ |
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application/pdf |
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Comisión de Investigaciones Científicas de la Provincia de Buenos Aires |
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CIC Digital (CICBA) - Comisión de Investigaciones Científicas de la Provincia de Buenos Aires |
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