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
SEDICI (UNLP)
Institución
Universidad Nacional de La Plata
OAI Identificador
oai:sedici.unlp.edu.ar:10915/118851

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spelling 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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