Gateways and climate: The Drake Passage opening

The Oligocene opening of the Drake Passage between the southern tip of South America and the Antarctic Peninsula, and the subsequent evolution of the Scotia plate, have definitively separated Antarctica from the other continental masses, and have created conditions for the development of the Antarct...

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Main Authors: Lodolo, Emanuele, Tassone, Alejandro Alberto
Format: Article in Journal/Newspaper
Language:English
Published: Istituto Nazionale di Oceanografia e di Geofisica
Subjects:
Online Access:http://hdl.handle.net/11336/68849
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author Lodolo, Emanuele
Tassone, Alejandro Alberto
author_facet Lodolo, Emanuele
Tassone, Alejandro Alberto
author_sort Lodolo, Emanuele
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
description The Oligocene opening of the Drake Passage between the southern tip of South America and the Antarctic Peninsula, and the subsequent evolution of the Scotia plate, have definitively separated Antarctica from the other continental masses, and have created conditions for the development of the Antarctic Circumpolar Current. This annular water flow has had a profound influence on the global climate system because it has allowed the free transfer of water masses between the Pacific and Atlantic Oceans at mid to high southerly latitudes. The comparative seismic analysis of the passive margins of the western sector of the Scotia plate, represented by the Tierra del Fuego continental margin to the north, and by the Terror Rise to the south, has shown significant morphological and structural similarities between these two margins, supporting the interpretation that they were conjugate before the Drake Passage opened. Moreover, the identification of the oldest magnetic anomalies present at the base of the two margin pairs, corresponding to about 32 million years ago, has allowed the reconstruction, through time, of the relative positions of the two continental margins, and to constrain the events that occurred immediately after the break-up and opening of the Drake Passage. These timings correlate with events seen in the oxygen isotope record from benthic foraminera, and support the view that the Drake Passage opening was the trigger for abrupt Eocene-Oligocene climate deterioration and the growth of extensive ice sheets on the Antarctic continent. Fil: Lodolo, Emanuele. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia Fil: Tassone, Alejandro Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ...
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Drake Passage
Tierra del Fuego
genre_facet Antarc*
Antarctic
Antarctic Peninsula
Antarctica
Drake Passage
Tierra del Fuego
geographic Antarctic
The Antarctic
Antarctic Peninsula
Drake Passage
Pacific
geographic_facet Antarctic
The Antarctic
Antarctic Peninsula
Drake Passage
Pacific
id ftconicet:oai:ri.conicet.gov.ar:11336/68849
institution Open Polar
language English
op_collection_id ftconicet
op_relation info:eu-repo/semantics/altIdentifier/url/http://www3.ogs.trieste.it/bgta/provapage.php?id_articolo=478
http://hdl.handle.net/11336/68849
Lodolo, Emanuele; Tassone, Alejandro Alberto; Gateways and climate: The Drake Passage opening; Istituto Nazionale di Oceanografia e di Geofisica; Bollettino di Geofisica Teorica ed Applicata; 51; 2-3; 6-2010; 77-88
0006-6729
CONICET Digital
CONICET
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
publisher Istituto Nazionale di Oceanografia e di Geofisica
record_format openpolar
spelling ftconicet:oai:ri.conicet.gov.ar:11336/68849 2025-01-16T19:38:48+00:00 Gateways and climate: The Drake Passage opening Lodolo, Emanuele Tassone, Alejandro Alberto application/pdf http://hdl.handle.net/11336/68849 eng eng Istituto Nazionale di Oceanografia e di Geofisica info:eu-repo/semantics/altIdentifier/url/http://www3.ogs.trieste.it/bgta/provapage.php?id_articolo=478 http://hdl.handle.net/11336/68849 Lodolo, Emanuele; Tassone, Alejandro Alberto; Gateways and climate: The Drake Passage opening; Istituto Nazionale di Oceanografia e di Geofisica; Bollettino di Geofisica Teorica ed Applicata; 51; 2-3; 6-2010; 77-88 0006-6729 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Scotia Drake Passage Gateways Climate 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 2023-09-24T20:21:22Z The Oligocene opening of the Drake Passage between the southern tip of South America and the Antarctic Peninsula, and the subsequent evolution of the Scotia plate, have definitively separated Antarctica from the other continental masses, and have created conditions for the development of the Antarctic Circumpolar Current. This annular water flow has had a profound influence on the global climate system because it has allowed the free transfer of water masses between the Pacific and Atlantic Oceans at mid to high southerly latitudes. The comparative seismic analysis of the passive margins of the western sector of the Scotia plate, represented by the Tierra del Fuego continental margin to the north, and by the Terror Rise to the south, has shown significant morphological and structural similarities between these two margins, supporting the interpretation that they were conjugate before the Drake Passage opened. Moreover, the identification of the oldest magnetic anomalies present at the base of the two margin pairs, corresponding to about 32 million years ago, has allowed the reconstruction, through time, of the relative positions of the two continental margins, and to constrain the events that occurred immediately after the break-up and opening of the Drake Passage. These timings correlate with events seen in the oxygen isotope record from benthic foraminera, and support the view that the Drake Passage opening was the trigger for abrupt Eocene-Oligocene climate deterioration and the growth of extensive ice sheets on the Antarctic continent. Fil: Lodolo, Emanuele. Istituto Nazionale di Oceanografia e di Geofisica Sperimentale; Italia Fil: Tassone, Alejandro Alberto. Consejo Nacional de Investigaciones Científicas y Técnicas. Oficina de Coordinación Administrativa Ciudad Universitaria. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires; ... Article in Journal/Newspaper Antarc* Antarctic Antarctic Peninsula Antarctica Drake Passage Tierra del Fuego CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic The Antarctic Antarctic Peninsula Drake Passage Pacific
spellingShingle Scotia
Drake Passage
Gateways
Climate
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Lodolo, Emanuele
Tassone, Alejandro Alberto
Gateways and climate: The Drake Passage opening
title Gateways and climate: The Drake Passage opening
title_full Gateways and climate: The Drake Passage opening
title_fullStr Gateways and climate: The Drake Passage opening
title_full_unstemmed Gateways and climate: The Drake Passage opening
title_short Gateways and climate: The Drake Passage opening
title_sort gateways and climate: the drake passage opening
topic Scotia
Drake Passage
Gateways
Climate
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Scotia
Drake Passage
Gateways
Climate
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/68849