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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/21269
Ver los metadatos del registro completo
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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 Técnicas2025-09-29T10:11:53Zoai: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:34982025-09-29 10:11:54.143CONICET 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) |
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CONICET Digital (CONICET) |
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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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13.070432 |