Holocene coastal vegetation changes at the mouth of the Amazon River

Autores
Smith, Clarisse Beltrão; Cohen, Marcelo Cancela Lisboa; Pessenda, Luiz Carlos Ruiz; França, Marlon Carlos; Guimarães, José Tasso Felix; Rossetti, Dilce de Fátima; Lara, Ruben Jose
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Wetland dynamics in the eastern Amazon region during the past 7000 years were studied using pollen, textural and structural analyses of sediment cores, as well as AMS radiocarbon dating. Four sediment cores were sampled from Marajó Island, which is located at the mouth of the Amazon River. Marajó Island is covered mainly by Amazon coastal forest, as well as herbaceous and varzea vegetation. Three cores were sampled from Lake Arari, which is surrounded by herbaceous vegetation flooded by freshwater. One core was sampled from a herbaceous plain located 15 km southeast of Lake Arari. Pollen preservation in the sedimentary deposits from this lake and from its drainage basin suggests significant vegetation changes on Marajó Island during the mid- and late-Holocene. Between 7328–7168 and 2306–2234 cal. yr BP, mangrove vegetation was more widely distributed on the island than it is today. During the past 2306–2234 cal. yr BP herbaceous vegetation expanded. Sedimentary structures and pollen data suggest a lagoon system until ~ 2300 cal. yr BP. The current distribution of mangroves along the Pará littoral, together with the presence of mangrove pollen and the sedimentary structures of the cores, indicates greater marine influence during the mid-Holocene. This may be attributed to the association between the eustatic sea-level change and the dry period recorded in Amazonia during the early- and mid-Holocene, followed by a wet phase over the past 2000 years.
Fil: Smith, Clarisse Beltrão. Federal University of Pará; Brasil
Fil: Cohen, Marcelo Cancela Lisboa. Federal University of Pará; Brasil
Fil: Pessenda, Luiz Carlos Ruiz. São Paulo University; Brasil
Fil: França, Marlon Carlos. Federal University of Pará; Brasil
Fil: Guimarães, José Tasso Felix. Federal University of Pará; Brasil
Fil: Rossetti, Dilce de Fátima. National Space Research Institute; Brasil
Fil: Lara, Ruben Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Center for Tropical Marine Ecology; Alemania
Materia
Amazon
Climate
Vegetation
Palynology
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/21269
Acceder
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network_name_str CONICET Digital (CONICET)
spelling Holocene coastal vegetation changes at the mouth of the Amazon RiverSmith, Clarisse BeltrãoCohen, Marcelo Cancela LisboaPessenda, Luiz Carlos RuizFrança, Marlon CarlosGuimarães, José Tasso FelixRossetti, Dilce de FátimaLara, Ruben JoseAmazonClimateVegetationPalynologyhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Wetland dynamics in the eastern Amazon region during the past 7000 years were studied using pollen, textural and structural analyses of sediment cores, as well as AMS radiocarbon dating. Four sediment cores were sampled from Marajó Island, which is located at the mouth of the Amazon River. Marajó Island is covered mainly by Amazon coastal forest, as well as herbaceous and varzea vegetation. Three cores were sampled from Lake Arari, which is surrounded by herbaceous vegetation flooded by freshwater. One core was sampled from a herbaceous plain located 15 km southeast of Lake Arari. Pollen preservation in the sedimentary deposits from this lake and from its drainage basin suggests significant vegetation changes on Marajó Island during the mid- and late-Holocene. Between 7328–7168 and 2306–2234 cal. yr BP, mangrove vegetation was more widely distributed on the island than it is today. During the past 2306–2234 cal. yr BP herbaceous vegetation expanded. Sedimentary structures and pollen data suggest a lagoon system until ~ 2300 cal. yr BP. The current distribution of mangroves along the Pará littoral, together with the presence of mangrove pollen and the sedimentary structures of the cores, indicates greater marine influence during the mid-Holocene. This may be attributed to the association between the eustatic sea-level change and the dry period recorded in Amazonia during the early- and mid-Holocene, followed by a wet phase over the past 2000 years.Fil: Smith, Clarisse Beltrão. Federal University of Pará; BrasilFil: Cohen, Marcelo Cancela Lisboa. Federal University of Pará; BrasilFil: Pessenda, Luiz Carlos Ruiz. São Paulo University; BrasilFil: França, Marlon Carlos. Federal University of Pará; BrasilFil: Guimarães, José Tasso Felix. Federal University of Pará; BrasilFil: Rossetti, Dilce de Fátima. National Space Research Institute; BrasilFil: Lara, Ruben Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Center for Tropical Marine Ecology; AlemaniaElsevier Science2011-08info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/21269Smith, Clarisse Beltrão; Cohen, Marcelo Cancela Lisboa; Pessenda, Luiz Carlos Ruiz; França, Marlon Carlos; Guimarães, José Tasso Felix; et al.; Holocene coastal vegetation changes at the mouth of the Amazon River; Elsevier Science; Review of Palaeobotany and Palynology; 168; 8-2011; 21-300034-6667CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2011.09.008info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0034666711001400?via%3Dihubinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-15T15:08:58Zoai:ri.conicet.gov.ar:11336/21269instacron: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:34982025-10-15 15:08:58.72CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Holocene coastal vegetation changes at the mouth of the Amazon River
title Holocene coastal vegetation changes at the mouth of the Amazon River
spellingShingle Holocene coastal vegetation changes at the mouth of the Amazon River
Smith, Clarisse Beltrão
Amazon
Climate
Vegetation
Palynology
title_short Holocene coastal vegetation changes at the mouth of the Amazon River
title_full Holocene coastal vegetation changes at the mouth of the Amazon River
title_fullStr Holocene coastal vegetation changes at the mouth of the Amazon River
title_full_unstemmed Holocene coastal vegetation changes at the mouth of the Amazon River
title_sort Holocene coastal vegetation changes at the mouth of the Amazon River
dc.creator.none.fl_str_mv Smith, Clarisse Beltrão
Cohen, Marcelo Cancela Lisboa
Pessenda, Luiz Carlos Ruiz
França, Marlon Carlos
Guimarães, José Tasso Felix
Rossetti, Dilce de Fátima
Lara, Ruben Jose
author Smith, Clarisse Beltrão
author_facet Smith, Clarisse Beltrão
Cohen, Marcelo Cancela Lisboa
Pessenda, Luiz Carlos Ruiz
França, Marlon Carlos
Guimarães, José Tasso Felix
Rossetti, Dilce de Fátima
Lara, Ruben Jose
author_role author
author2 Cohen, Marcelo Cancela Lisboa
Pessenda, Luiz Carlos Ruiz
França, Marlon Carlos
Guimarães, José Tasso Felix
Rossetti, Dilce de Fátima
Lara, Ruben Jose
author2_role author
author
author
author
author
author
dc.subject.none.fl_str_mv Amazon
Climate
Vegetation
Palynology
topic Amazon
Climate
Vegetation
Palynology
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Wetland dynamics in the eastern Amazon region during the past 7000 years were studied using pollen, textural and structural analyses of sediment cores, as well as AMS radiocarbon dating. Four sediment cores were sampled from Marajó Island, which is located at the mouth of the Amazon River. Marajó Island is covered mainly by Amazon coastal forest, as well as herbaceous and varzea vegetation. Three cores were sampled from Lake Arari, which is surrounded by herbaceous vegetation flooded by freshwater. One core was sampled from a herbaceous plain located 15 km southeast of Lake Arari. Pollen preservation in the sedimentary deposits from this lake and from its drainage basin suggests significant vegetation changes on Marajó Island during the mid- and late-Holocene. Between 7328–7168 and 2306–2234 cal. yr BP, mangrove vegetation was more widely distributed on the island than it is today. During the past 2306–2234 cal. yr BP herbaceous vegetation expanded. Sedimentary structures and pollen data suggest a lagoon system until ~ 2300 cal. yr BP. The current distribution of mangroves along the Pará littoral, together with the presence of mangrove pollen and the sedimentary structures of the cores, indicates greater marine influence during the mid-Holocene. This may be attributed to the association between the eustatic sea-level change and the dry period recorded in Amazonia during the early- and mid-Holocene, followed by a wet phase over the past 2000 years.
Fil: Smith, Clarisse Beltrão. Federal University of Pará; Brasil
Fil: Cohen, Marcelo Cancela Lisboa. Federal University of Pará; Brasil
Fil: Pessenda, Luiz Carlos Ruiz. São Paulo University; Brasil
Fil: França, Marlon Carlos. Federal University of Pará; Brasil
Fil: Guimarães, José Tasso Felix. Federal University of Pará; Brasil
Fil: Rossetti, Dilce de Fátima. National Space Research Institute; Brasil
Fil: Lara, Ruben Jose. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Argentino de Oceanografía. Universidad Nacional del Sur. Instituto Argentino de Oceanografía; Argentina. Center for Tropical Marine Ecology; Alemania
description Wetland dynamics in the eastern Amazon region during the past 7000 years were studied using pollen, textural and structural analyses of sediment cores, as well as AMS radiocarbon dating. Four sediment cores were sampled from Marajó Island, which is located at the mouth of the Amazon River. Marajó Island is covered mainly by Amazon coastal forest, as well as herbaceous and varzea vegetation. Three cores were sampled from Lake Arari, which is surrounded by herbaceous vegetation flooded by freshwater. One core was sampled from a herbaceous plain located 15 km southeast of Lake Arari. Pollen preservation in the sedimentary deposits from this lake and from its drainage basin suggests significant vegetation changes on Marajó Island during the mid- and late-Holocene. Between 7328–7168 and 2306–2234 cal. yr BP, mangrove vegetation was more widely distributed on the island than it is today. During the past 2306–2234 cal. yr BP herbaceous vegetation expanded. Sedimentary structures and pollen data suggest a lagoon system until ~ 2300 cal. yr BP. The current distribution of mangroves along the Pará littoral, together with the presence of mangrove pollen and the sedimentary structures of the cores, indicates greater marine influence during the mid-Holocene. This may be attributed to the association between the eustatic sea-level change and the dry period recorded in Amazonia during the early- and mid-Holocene, followed by a wet phase over the past 2000 years.
publishDate 2011
dc.date.none.fl_str_mv 2011-08
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/11336/21269
Smith, Clarisse Beltrão; Cohen, Marcelo Cancela Lisboa; Pessenda, Luiz Carlos Ruiz; França, Marlon Carlos; Guimarães, José Tasso Felix; et al.; Holocene coastal vegetation changes at the mouth of the Amazon River; Elsevier Science; Review of Palaeobotany and Palynology; 168; 8-2011; 21-30
0034-6667
CONICET Digital
CONICET
url http://hdl.handle.net/11336/21269
identifier_str_mv Smith, Clarisse Beltrão; Cohen, Marcelo Cancela Lisboa; Pessenda, Luiz Carlos Ruiz; França, Marlon Carlos; Guimarães, José Tasso Felix; et al.; Holocene coastal vegetation changes at the mouth of the Amazon River; Elsevier Science; Review of Palaeobotany and Palynology; 168; 8-2011; 21-30
0034-6667
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2011.09.008
info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0034666711001400?via%3Dihub
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Science
publisher.none.fl_str_mv Elsevier Science
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
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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score 13.22299

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