Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem
Autor(a) principal: | |
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Data de Publicação: | 2019 |
Outros Autores: | , , , |
Tipo de documento: | Artigo |
Idioma: | eng |
Título da fonte: | Repositório Institucional do INPA |
Texto Completo: | https://repositorio.inpa.gov.br/handle/1/15223 |
Resumo: | The Amazonian landscape evolution is the result of the combined effect of Andean tectonism, climate and the Earth’s interior dynamics. To reconstruct the landscape evolution and its influence on paleoenvironmental variations within Amazonia since the Oligocene, we conducted numerical experiments that incorporate different surface and geodynamic processes, reproducing many paleogeographic features as inferred from the sedimentary record. We show that the evolution of the drainage pattern gradually reduced the area of sedimentation derived from the Guiana and Brazilian shields while expanded the Andean derived deposits during the Miocene, affecting the nutrient availability. First order biotic habitats were inferred from these paleogeographical reconstructions, showing an eastward expansion of várzea and terra firme forests and consequent retraction of igapó forests, with a millennial-scale reconfiguration of a mosaic of habitats in the lowlands. We conclude that this dynamism probably guided the observed patterns of speciation in the most biodiverse biome on Earth. © 2019, The Author(s). |
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Bicudo, Tacio CordeiroSacek, VictorAlmeida, Renato Paes deBates, John MarshallRibas, Camila Cherem2020-05-07T14:14:49Z2020-05-07T14:14:49Z2019https://repositorio.inpa.gov.br/handle/1/1522310.1038/s41598-019-53465-yThe Amazonian landscape evolution is the result of the combined effect of Andean tectonism, climate and the Earth’s interior dynamics. To reconstruct the landscape evolution and its influence on paleoenvironmental variations within Amazonia since the Oligocene, we conducted numerical experiments that incorporate different surface and geodynamic processes, reproducing many paleogeographic features as inferred from the sedimentary record. We show that the evolution of the drainage pattern gradually reduced the area of sedimentation derived from the Guiana and Brazilian shields while expanded the Andean derived deposits during the Miocene, affecting the nutrient availability. First order biotic habitats were inferred from these paleogeographical reconstructions, showing an eastward expansion of várzea and terra firme forests and consequent retraction of igapó forests, with a millennial-scale reconfiguration of a mosaic of habitats in the lowlands. We conclude that this dynamism probably guided the observed patterns of speciation in the most biodiverse biome on Earth. © 2019, The Author(s).Volume 9, Número 1Attribution-NonCommercial-NoDerivs 3.0 Brazilhttp://creativecommons.org/licenses/by-nc-nd/3.0/br/info:eu-repo/semantics/openAccessAndean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosysteminfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/articleScientific Reportsengreponame:Repositório Institucional do INPAinstname:Instituto Nacional de Pesquisas da Amazônia (INPA)instacron:INPAORIGINALartigo-inpa.pdfapplication/pdf7990844https://repositorio.inpa.gov.br/bitstream/1/15223/1/artigo-inpa.pdfca6e02b8ac502237f59400f3acb77e39MD51CC-LICENSElicense_rdfapplication/octet-stream914https://repositorio.inpa.gov.br/bitstream/1/15223/2/license_rdf4d2950bda3d176f570a9f8b328dfbbefMD521/152232020-07-14 10:59:28.753oai:repositorio:1/15223Repositório de PublicaçõesPUBhttps://repositorio.inpa.gov.br/oai/requestopendoar:2020-07-14T14:59:28Repositório Institucional do INPA - Instituto Nacional de Pesquisas da Amazônia (INPA)false |
dc.title.en.fl_str_mv |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem |
title |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem |
spellingShingle |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem Bicudo, Tacio Cordeiro |
title_short |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem |
title_full |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem |
title_fullStr |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem |
title_full_unstemmed |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem |
title_sort |
Andean Tectonics and Mantle Dynamics as a Pervasive Influence on Amazonian Ecosystem |
author |
Bicudo, Tacio Cordeiro |
author_facet |
Bicudo, Tacio Cordeiro Sacek, Victor Almeida, Renato Paes de Bates, John Marshall Ribas, Camila Cherem |
author_role |
author |
author2 |
Sacek, Victor Almeida, Renato Paes de Bates, John Marshall Ribas, Camila Cherem |
author2_role |
author author author author |
dc.contributor.author.fl_str_mv |
Bicudo, Tacio Cordeiro Sacek, Victor Almeida, Renato Paes de Bates, John Marshall Ribas, Camila Cherem |
description |
The Amazonian landscape evolution is the result of the combined effect of Andean tectonism, climate and the Earth’s interior dynamics. To reconstruct the landscape evolution and its influence on paleoenvironmental variations within Amazonia since the Oligocene, we conducted numerical experiments that incorporate different surface and geodynamic processes, reproducing many paleogeographic features as inferred from the sedimentary record. We show that the evolution of the drainage pattern gradually reduced the area of sedimentation derived from the Guiana and Brazilian shields while expanded the Andean derived deposits during the Miocene, affecting the nutrient availability. First order biotic habitats were inferred from these paleogeographical reconstructions, showing an eastward expansion of várzea and terra firme forests and consequent retraction of igapó forests, with a millennial-scale reconfiguration of a mosaic of habitats in the lowlands. We conclude that this dynamism probably guided the observed patterns of speciation in the most biodiverse biome on Earth. © 2019, The Author(s). |
publishDate |
2019 |
dc.date.issued.fl_str_mv |
2019 |
dc.date.accessioned.fl_str_mv |
2020-05-07T14:14:49Z |
dc.date.available.fl_str_mv |
2020-05-07T14:14:49Z |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://repositorio.inpa.gov.br/handle/1/15223 |
dc.identifier.doi.none.fl_str_mv |
10.1038/s41598-019-53465-y |
url |
https://repositorio.inpa.gov.br/handle/1/15223 |
identifier_str_mv |
10.1038/s41598-019-53465-y |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartof.pt_BR.fl_str_mv |
Volume 9, Número 1 |
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Attribution-NonCommercial-NoDerivs 3.0 Brazil http://creativecommons.org/licenses/by-nc-nd/3.0/br/ info:eu-repo/semantics/openAccess |
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Attribution-NonCommercial-NoDerivs 3.0 Brazil http://creativecommons.org/licenses/by-nc-nd/3.0/br/ |
eu_rights_str_mv |
openAccess |
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Scientific Reports |
publisher.none.fl_str_mv |
Scientific Reports |
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