Glaciations in South America

Neoproterozoic successions in South America are recordedin many areas of Brazil, Paraguay, Bolivia, Uruguay andArgentina. Some of these units show glaciogenic forma-tions like those represented in the Puga and Serra Azulformations in the Northern Paraguay Belt (Brazil) inagreement with their accumul...

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Main Authors: Poire, Daniel Gustavo, Gómez Peral, Lucia, Arrouy, Maria Julia
Other Authors: Siegesmund, Siegfried, Stipp Basei, Miguel Angelo, Oyhantçabal, Pedro, Oriolo, Sebastián
Format: Book Part
Language:English
Published: Springer
Subjects:
Online Access:http://hdl.handle.net/11336/98497
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author Poire, Daniel Gustavo
Gómez Peral, Lucia
Arrouy, Maria Julia
author2 Siegesmund, Siegfried
Stipp Basei, Miguel Angelo
Oyhantçabal, Pedro
Oriolo, Sebastián
author_facet Poire, Daniel Gustavo
Gómez Peral, Lucia
Arrouy, Maria Julia
author_sort Poire, Daniel Gustavo
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_start_page 527
description Neoproterozoic successions in South America are recordedin many areas of Brazil, Paraguay, Bolivia, Uruguay andArgentina. Some of these units show glaciogenic forma-tions like those represented in the Puga and Serra Azulformations in the Northern Paraguay Belt (Brazil) inagreement with their accumulation in a Snowball Earthcontext. However, in other cases, tillites or other glacio-marine deposits are absent, which may indicate a distantposition (tropical) regarding the ice cap, as occurs in theTandilia System (Argentina) related to a“Phantom glacial”context. In this contribution we show the comparisonbetween direct and indirect evidence of glaciations in theNeoproterozoic successions of South America. The Pugaand Serra Azul formations in the Paraguay Belt and SierrasBayas Group in the Río de la Plata Craton have beenchosen to describe the“Snowball Earth”and“Phantomglacial”models, respectively. By means of multiproxyanalysis it is also possible to indicate changes in paleocli-mate conditions in both cases. The presence of tillites isconsidered to be direct evidence of the extreme climaticconditions during deposition during a glaciation. Mean-while, more subtle evidence such as regional unconformi-ties related to drastic sea level changes, trends ind13C,events of phosphogenesis, constitute, among others, thetools to indicate the influence of Neoproterozoic globalglaciations during the deposition of the sedimentary units. Fil: Poire, Daniel Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Gómez Peral, Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: ...
format Book Part
genre Ice cap
genre_facet Ice cap
geographic Argentina
Uruguay
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geographic_facet Argentina
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op_doi https://doi.org/10.1007/978-3-319-68920-3_19
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http://hdl.handle.net/11336/98497
Poire, Daniel Gustavo; Gómez Peral, Lucia; Arrouy, Maria Julia; Glaciations in South America; Springer; 2018; 527-541
978-3-319-68919-7
CONICET Digital
CONICET
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/98497 2025-01-16T22:23:14+00:00 Glaciations in South America Poire, Daniel Gustavo Gómez Peral, Lucia Arrouy, Maria Julia Siegesmund, Siegfried Stipp Basei, Miguel Angelo Oyhantçabal, Pedro Oriolo, Sebastián application/pdf http://hdl.handle.net/11336/98497 eng eng Springer info:eu-repo/semantics/altIdentifier/url/https://doi.org/10.1007/978-3-319-68920-3_19 info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007%2F978-3-319-68920-3_19 http://hdl.handle.net/11336/98497 Poire, Daniel Gustavo; Gómez Peral, Lucia; Arrouy, Maria Julia; Glaciations in South America; Springer; 2018; 527-541 978-3-319-68919-7 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess Atribución-NoComercial-CompartirIgual 2.5 Argentina (CC BY-NC-SA 2.5 AR) https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Glacial events Southamerica Río de La Plata Craton Criogeniana to Neoproterozoic https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/publishedVersion info:eu-repo/semantics/bookPart info:ar-repo/semantics/parte de libro ftconicet https://doi.org/10.1007/978-3-319-68920-3_19 2023-09-24T19:59:22Z Neoproterozoic successions in South America are recordedin many areas of Brazil, Paraguay, Bolivia, Uruguay andArgentina. Some of these units show glaciogenic forma-tions like those represented in the Puga and Serra Azulformations in the Northern Paraguay Belt (Brazil) inagreement with their accumulation in a Snowball Earthcontext. However, in other cases, tillites or other glacio-marine deposits are absent, which may indicate a distantposition (tropical) regarding the ice cap, as occurs in theTandilia System (Argentina) related to a“Phantom glacial”context. In this contribution we show the comparisonbetween direct and indirect evidence of glaciations in theNeoproterozoic successions of South America. The Pugaand Serra Azul formations in the Paraguay Belt and SierrasBayas Group in the Río de la Plata Craton have beenchosen to describe the“Snowball Earth”and“Phantomglacial”models, respectively. By means of multiproxyanalysis it is also possible to indicate changes in paleocli-mate conditions in both cases. The presence of tillites isconsidered to be direct evidence of the extreme climaticconditions during deposition during a glaciation. Mean-while, more subtle evidence such as regional unconformi-ties related to drastic sea level changes, trends ind13C,events of phosphogenesis, constitute, among others, thetools to indicate the influence of Neoproterozoic globalglaciations during the deposition of the sedimentary units. Fil: Poire, Daniel Gustavo. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: Gómez Peral, Lucia. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - La Plata. Centro de Investigaciones Geológicas. Universidad Nacional de La Plata. Facultad de Ciencias Naturales y Museo. Centro de Investigaciones Geológicas; Argentina Fil: ... Book Part Ice cap CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Argentina Uruguay Gustavo ENVELOPE(-62.917,-62.917,-64.833,-64.833) 527 541
spellingShingle Glacial events
Southamerica
Río de La Plata Craton
Criogeniana to Neoproterozoic
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
Poire, Daniel Gustavo
Gómez Peral, Lucia
Arrouy, Maria Julia
Glaciations in South America
title Glaciations in South America
title_full Glaciations in South America
title_fullStr Glaciations in South America
title_full_unstemmed Glaciations in South America
title_short Glaciations in South America
title_sort glaciations in south america
topic Glacial events
Southamerica
Río de La Plata Craton
Criogeniana to Neoproterozoic
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Glacial events
Southamerica
Río de La Plata Craton
Criogeniana to Neoproterozoic
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/98497