Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment

Dinoflagellate cyst assemblages recovered from the La Meseta Formation cropping out in Seymour Island, Antarctic Peninsula, are studied herein and their distribution is compared with the biostratigraphic scheme available for the Palaeogene of the Southern Ocean and other high-latitude regions. In th...

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Published in:Geological Magazine
Main Authors: Rodriguez Amenabar, Cecilia, Montes, Manuel, Nozal, Francisco, Santillana, Sergio Nestor
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press
Subjects:
Online Access:http://hdl.handle.net/11336/97402
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record_format openpolar
institution Open Polar
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
op_collection_id ftconicet
language English
topic ANTARCTICA
BIOSTRATIGRAPHY
EOCENE
PALAEOENVIRONMENT
PALYNOMORPHS
SOUTHERN OCEAN CIRCULATION
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
spellingShingle ANTARCTICA
BIOSTRATIGRAPHY
EOCENE
PALAEOENVIRONMENT
PALYNOMORPHS
SOUTHERN OCEAN CIRCULATION
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Rodriguez Amenabar, Cecilia
Montes, Manuel
Nozal, Francisco
Santillana, Sergio Nestor
Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment
topic_facet ANTARCTICA
BIOSTRATIGRAPHY
EOCENE
PALAEOENVIRONMENT
PALYNOMORPHS
SOUTHERN OCEAN CIRCULATION
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
description Dinoflagellate cyst assemblages recovered from the La Meseta Formation cropping out in Seymour Island, Antarctic Peninsula, are studied herein and their distribution is compared with the biostratigraphic scheme available for the Palaeogene of the Southern Ocean and other high-latitude regions. In this way, the La Meseta Formation is dated as middle Lutetian to Priabonian (46.2-36 Ma), which differs from the age provided by other fossils, isotopes and also with the magnetostratigraphic scheme recently performed for the unit. The dinoflagellate cyst data support the proposal of ocean circulation patterns on the South American Shelf prior to the opening of Drake Passage. Assemblages from the La Meseta Formation contain Antarctic-endemic taxa which are also dominant in several circum-Antarctic sites, located south of 45° S. Their distribution reflects an ocean-circulation scheme with wide clockwise gyres surrounding Antarctica that were disrupted as a consequence of the deepening and definitive apertures of the Tasmanian Gateway and Drake Passage towards the Eocene/Oligocene transition. The palaeoenvironmental inference based on the S/D ratio (sporomorphs versus dinoflagellate cysts) and the P/G ratio (peridinioid versus gonyaulacoid dinoflagellate cysts) suggests an overall trend through the section from marine-dominated assemblages with poorly productive waters in the lower part of the section to more terrestrially dominated assemblages with increasing productivity in the upper part of the unit, reflecting a shallowing trend to the top. Fil: Rodriguez Amenabar, Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina Fil: ...
format Article in Journal/Newspaper
author Rodriguez Amenabar, Cecilia
Montes, Manuel
Nozal, Francisco
Santillana, Sergio Nestor
author_facet Rodriguez Amenabar, Cecilia
Montes, Manuel
Nozal, Francisco
Santillana, Sergio Nestor
author_sort Rodriguez Amenabar, Cecilia
title Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment
title_short Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment
title_full Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment
title_fullStr Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment
title_full_unstemmed Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment
title_sort dinoflagellate cysts of the la meseta formation (middle to late eocene), antarctic peninsula: implications for biostratigraphy, palaeoceanography and palaeoenvironment
publisher Cambridge University Press
url http://hdl.handle.net/11336/97402
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geographic Antarctic
Southern Ocean
Antarctic Peninsula
Drake Passage
Argentino
Argentina
Seymour
Seymour Island
Rodriguez
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geographic_facet Antarctic
Southern Ocean
Antarctic Peninsula
Drake Passage
Argentino
Argentina
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Seymour Island
Rodriguez
Pablo
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Dirección Nacional del Antártico
Drake Passage
Instituto Antártico Argentino
Seymour Island
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Dirección Nacional del Antártico
Drake Passage
Instituto Antártico Argentino
Seymour Island
Southern Ocean
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http://hdl.handle.net/11336/97402
Rodriguez Amenabar, Cecilia; Montes, Manuel; Nozal, Francisco; Santillana, Sergio Nestor; Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment; Cambridge University Press; Geological Magazine; 7-2019; 1-16
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/97402 2023-10-09T21:45:18+02:00 Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment Rodriguez Amenabar, Cecilia Montes, Manuel Nozal, Francisco Santillana, Sergio Nestor application/pdf http://hdl.handle.net/11336/97402 eng eng Cambridge University Press info:eu-repo/semantics/altIdentifier/url/https://www.cambridge.org/core/journals/geological-magazine/article/dinoflagellate-cysts-of-the-la-meseta-formation-middle-to-late-eocene-antarctic-peninsula-implications-for-biostratigraphy-palaeoceanography-and-palaeoenvironment/287492E8DED4A6DF079D8C41D1B6151B info:eu-repo/semantics/altIdentifier/doi/10.1017/S0016756819000591 http://hdl.handle.net/11336/97402 Rodriguez Amenabar, Cecilia; Montes, Manuel; Nozal, Francisco; Santillana, Sergio Nestor; Dinoflagellate cysts of the la Meseta Formation (middle to late Eocene), Antarctic Peninsula: Implications for biostratigraphy, palaeoceanography and palaeoenvironment; Cambridge University Press; Geological Magazine; 7-2019; 1-16 0016-7568 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ ANTARCTICA BIOSTRATIGRAPHY EOCENE PALAEOENVIRONMENT PALYNOMORPHS SOUTHERN OCEAN CIRCULATION https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1017/S0016756819000591 2023-09-24T20:22:33Z Dinoflagellate cyst assemblages recovered from the La Meseta Formation cropping out in Seymour Island, Antarctic Peninsula, are studied herein and their distribution is compared with the biostratigraphic scheme available for the Palaeogene of the Southern Ocean and other high-latitude regions. In this way, the La Meseta Formation is dated as middle Lutetian to Priabonian (46.2-36 Ma), which differs from the age provided by other fossils, isotopes and also with the magnetostratigraphic scheme recently performed for the unit. The dinoflagellate cyst data support the proposal of ocean circulation patterns on the South American Shelf prior to the opening of Drake Passage. Assemblages from the La Meseta Formation contain Antarctic-endemic taxa which are also dominant in several circum-Antarctic sites, located south of 45° S. Their distribution reflects an ocean-circulation scheme with wide clockwise gyres surrounding Antarctica that were disrupted as a consequence of the deepening and definitive apertures of the Tasmanian Gateway and Drake Passage towards the Eocene/Oligocene transition. The palaeoenvironmental inference based on the S/D ratio (sporomorphs versus dinoflagellate cysts) and the P/G ratio (peridinioid versus gonyaulacoid dinoflagellate cysts) suggests an overall trend through the section from marine-dominated assemblages with poorly productive waters in the lower part of the section to more terrestrially dominated assemblages with increasing productivity in the upper part of the unit, reflecting a shallowing trend to the top. Fil: Rodriguez Amenabar, Cecilia. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Estudios Andinos "Don Pablo Groeber". Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Estudios Andinos "Don Pablo Groeber"; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina Fil: ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Dirección Nacional del Antártico Drake Passage Instituto Antártico Argentino Seymour Island Southern Ocean CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Southern Ocean Antarctic Peninsula Drake Passage Argentino Argentina Seymour ENVELOPE(-56.767,-56.767,-64.283,-64.283) Seymour Island ENVELOPE(-56.750,-56.750,-64.283,-64.283) Rodriguez ENVELOPE(-56.720,-56.720,-63.529,-63.529) Pablo ENVELOPE(-63.717,-63.717,-64.283,-64.283) Geological Magazine 157 3 351 366