Last interglacial (MIS 5e) sea-level proxies in southeastern South America
- Autores
- Gowan, Evan J.; Rovere, Alessio; Ryan, Deirdre D.; Richiano, Sebastián Miguel; Montes, Alejandro; Pappalardo, Marta; Aguirre, Marina Laura
- Año de publicación
- 2021
- Idioma
- inglés
- Tipo de recurso
- artículo
- Estado
- versión publicada
- Descripción
- Coastal southeast South America is one of the classic locations where there are robust, spatially extensive records of past high sea level. Sea-level proxies interpreted as last interglacial (Marine Isotope Stage 5e, MIS 5e) exist along the length of the Uruguayan and Argentinian coast with exceptional preservation especially in Patagonia. Many coastal deposits are correlated to MIS 5e solely because they form the next-highest terrace level above the Holocene highstand; however, dating control exists for some landforms from amino acid racemization, U=Th (on molluscs), electron spin resonance (ESR), optically stimulated luminescence (OSL), infrared stimulated luminescence (IRSL), and radiocarbon dating (which provides minimum ages). As part of theWorld Atlas of Last Interglacial Shorelines (WALIS) database, we have compiled a total of 60 MIS 5 proxies attributed, with various degrees of precision, to MIS 5e. Of these, 48 are sea-level indicators, 11 are marinelimiting indicators (sea level above the elevation of the indicator), and 1 is terrestrial limiting (sea level below the elevation of the indicator). Limitations on the precision and accuracy of chronological controls and elevation measurements mean that most of these indicators are considered to be low quality. The database is available at https://doi.org/10.5281/zenodo.3991596 (Gowan et al., 2020).
Facultad de Ciencias Naturales y Museo - Materia
-
Geología
Last interglacial
South America
Limitations
Indicators - Nivel de accesibilidad
- acceso abierto
- Condiciones de uso
- http://creativecommons.org/licenses/by/4.0/
- Repositorio
- Institución
- Universidad Nacional de La Plata
- OAI Identificador
- oai:sedici.unlp.edu.ar:10915/118851
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Last interglacial (MIS 5e) sea-level proxies in southeastern South AmericaGowan, Evan J.Rovere, AlessioRyan, Deirdre D.Richiano, Sebastián MiguelMontes, AlejandroPappalardo, MartaAguirre, Marina LauraGeologíaLast interglacialSouth AmericaLimitationsIndicatorsCoastal southeast South America is one of the classic locations where there are robust, spatially extensive records of past high sea level. Sea-level proxies interpreted as last interglacial (Marine Isotope Stage 5e, MIS 5e) exist along the length of the Uruguayan and Argentinian coast with exceptional preservation especially in Patagonia. Many coastal deposits are correlated to MIS 5e solely because they form the next-highest terrace level above the Holocene highstand; however, dating control exists for some landforms from amino acid racemization, U=Th (on molluscs), electron spin resonance (ESR), optically stimulated luminescence (OSL), infrared stimulated luminescence (IRSL), and radiocarbon dating (which provides minimum ages). As part of theWorld Atlas of Last Interglacial Shorelines (WALIS) database, we have compiled a total of 60 MIS 5 proxies attributed, with various degrees of precision, to MIS 5e. Of these, 48 are sea-level indicators, 11 are marinelimiting indicators (sea level above the elevation of the indicator), and 1 is terrestrial limiting (sea level below the elevation of the indicator). Limitations on the precision and accuracy of chronological controls and elevation measurements mean that most of these indicators are considered to be low quality. The database is available at https://doi.org/10.5281/zenodo.3991596 (Gowan et al., 2020).Facultad de Ciencias Naturales y Museo2021info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionArticulohttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdf171-197http://sedici.unlp.edu.ar/handle/10915/118851enginfo:eu-repo/semantics/altIdentifier/issn/1866-3516info:eu-repo/semantics/altIdentifier/doi/10.5194/essd-13-171-2021info:eu-repo/semantics/openAccesshttp://creativecommons.org/licenses/by/4.0/Creative Commons Attribution 4.0 International (CC BY 4.0)reponame:SEDICI (UNLP)instname:Universidad Nacional de La Platainstacron:UNLP2025-10-15T11:19:51Zoai:sedici.unlp.edu.ar:10915/118851Institucionalhttp://sedici.unlp.edu.ar/Universidad públicaNo correspondehttp://sedici.unlp.edu.ar/oai/snrdalira@sedici.unlp.edu.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:13292025-10-15 11:19:51.441SEDICI (UNLP) - Universidad Nacional de La Platafalse |
dc.title.none.fl_str_mv |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America |
title |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America |
spellingShingle |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America Gowan, Evan J. Geología Last interglacial South America Limitations Indicators |
title_short |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America |
title_full |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America |
title_fullStr |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America |
title_full_unstemmed |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America |
title_sort |
Last interglacial (MIS 5e) sea-level proxies in southeastern South America |
dc.creator.none.fl_str_mv |
Gowan, Evan J. Rovere, Alessio Ryan, Deirdre D. Richiano, Sebastián Miguel Montes, Alejandro Pappalardo, Marta Aguirre, Marina Laura |
author |
Gowan, Evan J. |
author_facet |
Gowan, Evan J. Rovere, Alessio Ryan, Deirdre D. Richiano, Sebastián Miguel Montes, Alejandro Pappalardo, Marta Aguirre, Marina Laura |
author_role |
author |
author2 |
Rovere, Alessio Ryan, Deirdre D. Richiano, Sebastián Miguel Montes, Alejandro Pappalardo, Marta Aguirre, Marina Laura |
author2_role |
author author author author author author |
dc.subject.none.fl_str_mv |
Geología Last interglacial South America Limitations Indicators |
topic |
Geología Last interglacial South America Limitations Indicators |
dc.description.none.fl_txt_mv |
Coastal southeast South America is one of the classic locations where there are robust, spatially extensive records of past high sea level. Sea-level proxies interpreted as last interglacial (Marine Isotope Stage 5e, MIS 5e) exist along the length of the Uruguayan and Argentinian coast with exceptional preservation especially in Patagonia. Many coastal deposits are correlated to MIS 5e solely because they form the next-highest terrace level above the Holocene highstand; however, dating control exists for some landforms from amino acid racemization, U=Th (on molluscs), electron spin resonance (ESR), optically stimulated luminescence (OSL), infrared stimulated luminescence (IRSL), and radiocarbon dating (which provides minimum ages). As part of theWorld Atlas of Last Interglacial Shorelines (WALIS) database, we have compiled a total of 60 MIS 5 proxies attributed, with various degrees of precision, to MIS 5e. Of these, 48 are sea-level indicators, 11 are marinelimiting indicators (sea level above the elevation of the indicator), and 1 is terrestrial limiting (sea level below the elevation of the indicator). Limitations on the precision and accuracy of chronological controls and elevation measurements mean that most of these indicators are considered to be low quality. The database is available at https://doi.org/10.5281/zenodo.3991596 (Gowan et al., 2020). Facultad de Ciencias Naturales y Museo |
description |
Coastal southeast South America is one of the classic locations where there are robust, spatially extensive records of past high sea level. Sea-level proxies interpreted as last interglacial (Marine Isotope Stage 5e, MIS 5e) exist along the length of the Uruguayan and Argentinian coast with exceptional preservation especially in Patagonia. Many coastal deposits are correlated to MIS 5e solely because they form the next-highest terrace level above the Holocene highstand; however, dating control exists for some landforms from amino acid racemization, U=Th (on molluscs), electron spin resonance (ESR), optically stimulated luminescence (OSL), infrared stimulated luminescence (IRSL), and radiocarbon dating (which provides minimum ages). As part of theWorld Atlas of Last Interglacial Shorelines (WALIS) database, we have compiled a total of 60 MIS 5 proxies attributed, with various degrees of precision, to MIS 5e. Of these, 48 are sea-level indicators, 11 are marinelimiting indicators (sea level above the elevation of the indicator), and 1 is terrestrial limiting (sea level below the elevation of the indicator). Limitations on the precision and accuracy of chronological controls and elevation measurements mean that most of these indicators are considered to be low quality. The database is available at https://doi.org/10.5281/zenodo.3991596 (Gowan et al., 2020). |
publishDate |
2021 |
dc.date.none.fl_str_mv |
2021 |
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http://sedici.unlp.edu.ar/handle/10915/118851 |
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eng |
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