Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary

Autores
Mourelle Civano, Dominique; Prieto, Aldo Raul; Perez, Laura; Garcia Rodriguez, Felipe; Borel, Claudia Marcela
Año de publicación
2015
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
In the present study, we carried out pollen, diatom and other palynomorph analyses from asedimentary sequence from the marshes of Arroyo Solís Grande, in the Río de la Plata northeastern coast (Uruguay), and compared the results with a regional model of surface pollen-vegetation relationship from the Atlantic coastal salt marshes (30°-37° S). Results indicated that salt marsh vegetation developed around the estuary between 8000 and 5100 cal yr BP, as the sea level rose and reached the Holocene sea-level highstand. Brackish marshes around the estuary between 5100 and 2900 cal yr BP reflect the late Holocene sea-level fall and associated increased input of freshwater. Brackish marshes and shallow salt pond environments between 2900 and 1000 cal yr BP are most probably linked to the Paraná delta formation and a further sea-level fall. Present-day marshes behind the sand bar characterize the last 1000 cal yr BP. The integration of our results with multiproxy records from the Río de la Plata southern coast (Argentina) and from the coastal plain of the southern Atlantic margin of South America (30°-37° S) revealed that marine influence during the maximum sea-level highstand resulted in the development of vegetation similar to that of the geographical region.However, after ca. 3000 cal yr BP, local differentiation related to different climate and geomorphology occurred at each area, thus resulting in the establishment of different modern plant communities at different times during the late Holocene.
Fil: Mourelle Civano, Dominique. Universidad Nacional de Mar del Plata. Facultad de Cs.exactas y Naturales. Laboratorio de Paleoecologia y Palinologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Mar del Plata. Instituto de Investigaciones Marinas y Costeras; Argentina
Fil: Prieto, Aldo Raul. Universidad Nacional de Mar del Plata. Facultad de Cs.exactas y Naturales. Laboratorio de Paleoecologia y Palinologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Mar del Plata. Instituto de Investigaciones Marinas y Costeras; Argentina
Fil: Perez, Laura. Universidad de la República. Facultad de Ciencias; Uruguay
Fil: Garcia Rodriguez, Felipe. Universidad de la República. Facultad de Ciencias; Uruguay
Fil: Borel, Claudia Marcela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Geológico del Sur; Argentina. Universidad Nacional del Sur; Argentina
Materia
Pollen
Non-Pollen Palynomorphs
Diatoms
Holocene Sea-Level Change
Uruguay
Argentina
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/6624

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network_name_str CONICET Digital (CONICET)
spelling Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuaryMourelle Civano, DominiquePrieto, Aldo RaulPerez, LauraGarcia Rodriguez, FelipeBorel, Claudia MarcelaPollenNon-Pollen PalynomorphsDiatomsHolocene Sea-Level ChangeUruguayArgentinahttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1In the present study, we carried out pollen, diatom and other palynomorph analyses from asedimentary sequence from the marshes of Arroyo Solís Grande, in the Río de la Plata northeastern coast (Uruguay), and compared the results with a regional model of surface pollen-vegetation relationship from the Atlantic coastal salt marshes (30°-37° S). Results indicated that salt marsh vegetation developed around the estuary between 8000 and 5100 cal yr BP, as the sea level rose and reached the Holocene sea-level highstand. Brackish marshes around the estuary between 5100 and 2900 cal yr BP reflect the late Holocene sea-level fall and associated increased input of freshwater. Brackish marshes and shallow salt pond environments between 2900 and 1000 cal yr BP are most probably linked to the Paraná delta formation and a further sea-level fall. Present-day marshes behind the sand bar characterize the last 1000 cal yr BP. The integration of our results with multiproxy records from the Río de la Plata southern coast (Argentina) and from the coastal plain of the southern Atlantic margin of South America (30°-37° S) revealed that marine influence during the maximum sea-level highstand resulted in the development of vegetation similar to that of the geographical region.However, after ca. 3000 cal yr BP, local differentiation related to different climate and geomorphology occurred at each area, thus resulting in the establishment of different modern plant communities at different times during the late Holocene.Fil: Mourelle Civano, Dominique. Universidad Nacional de Mar del Plata. Facultad de Cs.exactas y Naturales. Laboratorio de Paleoecologia y Palinologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Mar del Plata. Instituto de Investigaciones Marinas y Costeras; ArgentinaFil: Prieto, Aldo Raul. Universidad Nacional de Mar del Plata. Facultad de Cs.exactas y Naturales. Laboratorio de Paleoecologia y Palinologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Mar del Plata. Instituto de Investigaciones Marinas y Costeras; ArgentinaFil: Perez, Laura. Universidad de la República. Facultad de Ciencias; UruguayFil: Garcia Rodriguez, Felipe. Universidad de la República. Facultad de Ciencias; UruguayFil: Borel, Claudia Marcela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Geológico del Sur; Argentina. Universidad Nacional del Sur; ArgentinaElsevier2015-01-10info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfapplication/pdfapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/6624Mourelle Civano, Dominique; Prieto, Aldo Raul; Perez, Laura; Garcia Rodriguez, Felipe; Borel, Claudia Marcela; Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary; Elsevier; Palaeogeography, Palaeoclimatology, Palaeoecology; 421; 10-1-2015; 75-880031-0182enginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.palaeo.2015.01.006info:eu-repo/semantics/altIdentifier/doi/info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018215000073info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:05:39Zoai:ri.conicet.gov.ar:11336/6624instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-09-03 10:05:39.554CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
title Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
spellingShingle Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
Mourelle Civano, Dominique
Pollen
Non-Pollen Palynomorphs
Diatoms
Holocene Sea-Level Change
Uruguay
Argentina
title_short Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
title_full Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
title_fullStr Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
title_full_unstemmed Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
title_sort Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary
dc.creator.none.fl_str_mv Mourelle Civano, Dominique
Prieto, Aldo Raul
Perez, Laura
Garcia Rodriguez, Felipe
Borel, Claudia Marcela
author Mourelle Civano, Dominique
author_facet Mourelle Civano, Dominique
Prieto, Aldo Raul
Perez, Laura
Garcia Rodriguez, Felipe
Borel, Claudia Marcela
author_role author
author2 Prieto, Aldo Raul
Perez, Laura
Garcia Rodriguez, Felipe
Borel, Claudia Marcela
author2_role author
author
author
author
dc.subject.none.fl_str_mv Pollen
Non-Pollen Palynomorphs
Diatoms
Holocene Sea-Level Change
Uruguay
Argentina
topic Pollen
Non-Pollen Palynomorphs
Diatoms
Holocene Sea-Level Change
Uruguay
Argentina
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv In the present study, we carried out pollen, diatom and other palynomorph analyses from asedimentary sequence from the marshes of Arroyo Solís Grande, in the Río de la Plata northeastern coast (Uruguay), and compared the results with a regional model of surface pollen-vegetation relationship from the Atlantic coastal salt marshes (30°-37° S). Results indicated that salt marsh vegetation developed around the estuary between 8000 and 5100 cal yr BP, as the sea level rose and reached the Holocene sea-level highstand. Brackish marshes around the estuary between 5100 and 2900 cal yr BP reflect the late Holocene sea-level fall and associated increased input of freshwater. Brackish marshes and shallow salt pond environments between 2900 and 1000 cal yr BP are most probably linked to the Paraná delta formation and a further sea-level fall. Present-day marshes behind the sand bar characterize the last 1000 cal yr BP. The integration of our results with multiproxy records from the Río de la Plata southern coast (Argentina) and from the coastal plain of the southern Atlantic margin of South America (30°-37° S) revealed that marine influence during the maximum sea-level highstand resulted in the development of vegetation similar to that of the geographical region.However, after ca. 3000 cal yr BP, local differentiation related to different climate and geomorphology occurred at each area, thus resulting in the establishment of different modern plant communities at different times during the late Holocene.
Fil: Mourelle Civano, Dominique. Universidad Nacional de Mar del Plata. Facultad de Cs.exactas y Naturales. Laboratorio de Paleoecologia y Palinologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Mar del Plata. Instituto de Investigaciones Marinas y Costeras; Argentina
Fil: Prieto, Aldo Raul. Universidad Nacional de Mar del Plata. Facultad de Cs.exactas y Naturales. Laboratorio de Paleoecologia y Palinologia; Argentina. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Mar del Plata. Instituto de Investigaciones Marinas y Costeras; Argentina
Fil: Perez, Laura. Universidad de la República. Facultad de Ciencias; Uruguay
Fil: Garcia Rodriguez, Felipe. Universidad de la República. Facultad de Ciencias; Uruguay
Fil: Borel, Claudia Marcela. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Bahía Blanca. Instituto Geológico del Sur; Argentina. Universidad Nacional del Sur; Argentina
description In the present study, we carried out pollen, diatom and other palynomorph analyses from asedimentary sequence from the marshes of Arroyo Solís Grande, in the Río de la Plata northeastern coast (Uruguay), and compared the results with a regional model of surface pollen-vegetation relationship from the Atlantic coastal salt marshes (30°-37° S). Results indicated that salt marsh vegetation developed around the estuary between 8000 and 5100 cal yr BP, as the sea level rose and reached the Holocene sea-level highstand. Brackish marshes around the estuary between 5100 and 2900 cal yr BP reflect the late Holocene sea-level fall and associated increased input of freshwater. Brackish marshes and shallow salt pond environments between 2900 and 1000 cal yr BP are most probably linked to the Paraná delta formation and a further sea-level fall. Present-day marshes behind the sand bar characterize the last 1000 cal yr BP. The integration of our results with multiproxy records from the Río de la Plata southern coast (Argentina) and from the coastal plain of the southern Atlantic margin of South America (30°-37° S) revealed that marine influence during the maximum sea-level highstand resulted in the development of vegetation similar to that of the geographical region.However, after ca. 3000 cal yr BP, local differentiation related to different climate and geomorphology occurred at each area, thus resulting in the establishment of different modern plant communities at different times during the late Holocene.
publishDate 2015
dc.date.none.fl_str_mv 2015-01-10
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/6624
Mourelle Civano, Dominique; Prieto, Aldo Raul; Perez, Laura; Garcia Rodriguez, Felipe; Borel, Claudia Marcela; Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary; Elsevier; Palaeogeography, Palaeoclimatology, Palaeoecology; 421; 10-1-2015; 75-88
0031-0182
url http://hdl.handle.net/11336/6624
identifier_str_mv Mourelle Civano, Dominique; Prieto, Aldo Raul; Perez, Laura; Garcia Rodriguez, Felipe; Borel, Claudia Marcela; Mid and late Holocene multiproxy analysis of environmental changes linked to sea-level fluctuation and climate variability of the Río de la Plata estuary; Elsevier; Palaeogeography, Palaeoclimatology, Palaeoecology; 421; 10-1-2015; 75-88
0031-0182
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.palaeo.2015.01.006
info:eu-repo/semantics/altIdentifier/doi/
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0031018215000073
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
application/pdf
application/pdf
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dc.publisher.none.fl_str_mv Elsevier
publisher.none.fl_str_mv Elsevier
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
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reponame_str CONICET Digital (CONICET)
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instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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