Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites

Late Paleozoic glacial diamictites occur in many localities in western Argentina, indicating that the region was strongly affected by glaciation during the mid-Carboniferous (late Serpukhovian–early Bashkirian). In most instances these diamictites are found in steeply walled paleovalley settings in...

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Published in:Gondwana Research
Main Authors: Gulbranson, Erik L., Isbell, John L., Montañez, Isabel P., Limarino, Carlos Oscar, Marenssi, Sergio Alfredo, Meyer, Kyle, Hull, Clara
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier
Subjects:
Online Access:http://hdl.handle.net/11336/33592
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author Gulbranson, Erik L.
Isbell, John L.
Montañez, Isabel P.
Limarino, Carlos Oscar
Marenssi, Sergio Alfredo
Meyer, Kyle
Hull, Clara
author_facet Gulbranson, Erik L.
Isbell, John L.
Montañez, Isabel P.
Limarino, Carlos Oscar
Marenssi, Sergio Alfredo
Meyer, Kyle
Hull, Clara
author_sort Gulbranson, Erik L.
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 4
container_start_page 1369
container_title Gondwana Research
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description Late Paleozoic glacial diamictites occur in many localities in western Argentina, indicating that the region was strongly affected by glaciation during the mid-Carboniferous (late Serpukhovian–early Bashkirian). In most instances these diamictites are found in steeply walled paleovalley settings in the Andean Precordillera. This study presents new data from a locality north of the Precordillera that suggests an additional, distinct, volume of ice existed in the region during the Carboniferous. The glacigenic diamictites in the Rio Blanco Basin were ultimately emplaced as gravity flows, precluding inferences of paleo-ice volume. Fold nose orientation and soft-sediment groove orientations within the diamictites indicate that the deposits were emplaced from north to south, suggesting that glacial ice was most likely not sourced from the proto-Precordillera at this locality, requiring the need for another ice center to the north of the basin. Diamictite facies indicates that the sediment was initially supplied to the study area by a warm-based glacier. Fil: Gulbranson, Erik L. University of California at Davis; Estados Unidos. University of Wisconsin; Estados Unidos Fil: Isbell, John L. University of Wisconsin; Estados Unidos Fil: Montañez, Isabel P. University of California at Davis; Estados Unidos Fil: Limarino, Carlos Oscar. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Marenssi, Sergio Alfredo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina Fil: Meyer, Kyle. University of California at Davis; Estados Unidos Fil: Hull, Clara. University of California at Davis; Estados Unidos
format Article in Journal/Newspaper
genre Dirección Nacional del Antártico
Instituto Antártico Argentino
genre_facet Dirección Nacional del Antártico
Instituto Antártico Argentino
geographic Argentino
Argentina
Blanco
Isbell
geographic_facet Argentino
Argentina
Blanco
Isbell
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op_doi https://doi.org/10.1016/j.gr.2013.03.017
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/33592 2025-01-16T21:37:57+00:00 Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites Gulbranson, Erik L. Isbell, John L. Montañez, Isabel P. Limarino, Carlos Oscar Marenssi, Sergio Alfredo Meyer, Kyle Hull, Clara application/pdf http://hdl.handle.net/11336/33592 eng eng Elsevier info:eu-repo/semantics/altIdentifier/url/https://www.sciencedirect.com/science/article/pii/S1342937X13001172 info:eu-repo/semantics/altIdentifier/doi/10.1016/j.gr.2013.03.017 http://hdl.handle.net/11336/33592 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-nd/2.5/ar/ Late Paleozoic ice age Mass transport Diamictite Gondwana Carboniferous 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/10.1016/j.gr.2013.03.017 2024-10-04T09:34:03Z Late Paleozoic glacial diamictites occur in many localities in western Argentina, indicating that the region was strongly affected by glaciation during the mid-Carboniferous (late Serpukhovian–early Bashkirian). In most instances these diamictites are found in steeply walled paleovalley settings in the Andean Precordillera. This study presents new data from a locality north of the Precordillera that suggests an additional, distinct, volume of ice existed in the region during the Carboniferous. The glacigenic diamictites in the Rio Blanco Basin were ultimately emplaced as gravity flows, precluding inferences of paleo-ice volume. Fold nose orientation and soft-sediment groove orientations within the diamictites indicate that the deposits were emplaced from north to south, suggesting that glacial ice was most likely not sourced from the proto-Precordillera at this locality, requiring the need for another ice center to the north of the basin. Diamictite facies indicates that the sediment was initially supplied to the study area by a warm-based glacier. Fil: Gulbranson, Erik L. University of California at Davis; Estados Unidos. University of Wisconsin; Estados Unidos Fil: Isbell, John L. University of Wisconsin; Estados Unidos Fil: Montañez, Isabel P. University of California at Davis; Estados Unidos Fil: Limarino, Carlos Oscar. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina Fil: Marenssi, Sergio Alfredo. Universidad de Buenos Aires. Facultad de Ciencias Exactas y Naturales. Departamento de Geología; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas; Argentina. Ministerio de Relaciones Exteriores, Comercio Interno y Culto. Dirección Nacional del Antártico. Instituto Antártico Argentino; Argentina Fil: Meyer, Kyle. University of California at Davis; Estados Unidos Fil: Hull, Clara. University of California at Davis; Estados Unidos Article in Journal/Newspaper Dirección Nacional del Antártico Instituto Antártico Argentino CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentino Argentina Blanco ENVELOPE(-55.233,-55.233,-61.250,-61.250) Isbell ENVELOPE(156.400,156.400,-82.367,-82.367) Gondwana Research 25 4 1369 1379
spellingShingle Late Paleozoic ice age
Mass transport
Diamictite
Gondwana
Carboniferous
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Gulbranson, Erik L.
Isbell, John L.
Montañez, Isabel P.
Limarino, Carlos Oscar
Marenssi, Sergio Alfredo
Meyer, Kyle
Hull, Clara
Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites
title Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites
title_full Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites
title_fullStr Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites
title_full_unstemmed Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites
title_short Reassessment of mid-Carboniferous glacial extent in southwestern Gondwana (Rio Blanco Basin, Argentina) inferred from paleo-mass transport of diamictites
title_sort reassessment of mid-carboniferous glacial extent in southwestern gondwana (rio blanco basin, argentina) inferred from paleo-mass transport of diamictites
topic Late Paleozoic ice age
Mass transport
Diamictite
Gondwana
Carboniferous
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Late Paleozoic ice age
Mass transport
Diamictite
Gondwana
Carboniferous
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/33592