The Glaciations in South America
Neoproterozoic successions in South America are recorded in many areas of Brazil, Paraguay, Bolivia, Uruguay and Argentina. Some of these units show glaciogenic formations like those represented in the Puga and Serra Azul formations in the Northern Paraguay Belt (Brazil) in agreement with their accu...
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Format: | Book Part |
Language: | English |
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Online Access: | http://hdl.handle.net/11336/98184 |
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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 recorded in many areas of Brazil, Paraguay, Bolivia, Uruguay and Argentina. Some of these units show glaciogenic formations like those represented in the Puga and Serra Azul formations in the Northern Paraguay Belt (Brazil) in agreement with their accumulation in a Snowball Earth context. However, in other cases, tillites or other glaciomarine deposits are absent, which may indicate a distant position (tropical) regarding the ice cap, as occurs in the Tandilia System (Argentina) related to a ?Phantom glacial? context. In this contribution we show the comparison between direct and indirect evidence of glaciations in the Neoproterozoic successions of South America. The Puga and Serra Azul formations in the Paraguay Belt and Sierras Bayas Group in the Río de la Plata Craton have been chosen to describe the ?Snowball Earth? and ?Phantom glacial? models, respectively. By means of multiproxy analysis it is also possible to indicate changes in paleoclimate conditions in both cases. The presence of tillites is considered to be direct evidence of the extreme climatic conditions during deposition during a glaciation. Meanwhile, more subtle evidence such as regional unconformities related to drastic sea level changes, trends in δ13C, events of phosphogenesis, constitute, among others, the tools to indicate the influence of Neoproterozoic global glaciations 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 ... |
format | Book Part |
genre | Ice cap |
genre_facet | Ice cap |
geographic | Argentina Uruguay Gustavo |
geographic_facet | Argentina Uruguay Gustavo |
id | ftconicet:oai:ri.conicet.gov.ar:11336/98184 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-62.917,-62.917,-64.833,-64.833) |
op_collection_id | ftconicet |
op_container_end_page | 541 |
op_doi | https://doi.org/10.1007/978-3-319-68920-3_19 |
op_relation | info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-68920-3_19 info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-319-68920-3_19 http://hdl.handle.net/11336/98184 Poire, Daniel Gustavo; Gómez Peral, Lucia; Arrouy, Maria Julia; The Glaciations in South America; Springer; 2018; 527-541 978-3-319-68919-7 CONICET Digital CONICET |
op_rights | info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
publisher | Springer |
record_format | openpolar |
spelling | ftconicet:oai:ri.conicet.gov.ar:11336/98184 2025-01-16T22:23:16+00:00 The 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/11336/98184 eng eng Springer info:eu-repo/semantics/altIdentifier/url/https://link.springer.com/chapter/10.1007/978-3-319-68920-3_19 info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-319-68920-3_19 http://hdl.handle.net/11336/98184 Poire, Daniel Gustavo; Gómez Peral, Lucia; Arrouy, Maria Julia; The Glaciations in South America; Springer; 2018; 527-541 978-3-319-68919-7 CONICET Digital CONICET info:eu-repo/semantics/restrictedAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ PALEOCLIMATIC PROXIES NEOPROTEROZOIC TILLITE RECORDS PHANTOM GLACIAL DEPOSITS 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 2023-09-24T19:17:07Z Neoproterozoic successions in South America are recorded in many areas of Brazil, Paraguay, Bolivia, Uruguay and Argentina. Some of these units show glaciogenic formations like those represented in the Puga and Serra Azul formations in the Northern Paraguay Belt (Brazil) in agreement with their accumulation in a Snowball Earth context. However, in other cases, tillites or other glaciomarine deposits are absent, which may indicate a distant position (tropical) regarding the ice cap, as occurs in the Tandilia System (Argentina) related to a ?Phantom glacial? context. In this contribution we show the comparison between direct and indirect evidence of glaciations in the Neoproterozoic successions of South America. The Puga and Serra Azul formations in the Paraguay Belt and Sierras Bayas Group in the Río de la Plata Craton have been chosen to describe the ?Snowball Earth? and ?Phantom glacial? models, respectively. By means of multiproxy analysis it is also possible to indicate changes in paleoclimate conditions in both cases. The presence of tillites is considered to be direct evidence of the extreme climatic conditions during deposition during a glaciation. Meanwhile, more subtle evidence such as regional unconformities related to drastic sea level changes, trends in δ13C, events of phosphogenesis, constitute, among others, the tools to indicate the influence of Neoproterozoic global glaciations 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 ... 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 | PALEOCLIMATIC PROXIES NEOPROTEROZOIC TILLITE RECORDS PHANTOM GLACIAL DEPOSITS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 Poire, Daniel Gustavo Gómez Peral, Lucia Arrouy, Maria Julia The Glaciations in South America |
title | The Glaciations in South America |
title_full | The Glaciations in South America |
title_fullStr | The Glaciations in South America |
title_full_unstemmed | The Glaciations in South America |
title_short | The Glaciations in South America |
title_sort | glaciations in south america |
topic | PALEOCLIMATIC PROXIES NEOPROTEROZOIC TILLITE RECORDS PHANTOM GLACIAL DEPOSITS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
topic_facet | PALEOCLIMATIC PROXIES NEOPROTEROZOIC TILLITE RECORDS PHANTOM GLACIAL DEPOSITS https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 |
url | http://hdl.handle.net/11336/98184 |