Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil

Detalhes bibliográficos
Autor(a) principal: Silva, Douglas Rosa da
Data de Publicação: 2019
Outros Autores: Mansur, Kátia Leite, Almeida, Leonardo Fonseca Borghi de
Tipo de documento: Artigo
Idioma: eng
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/30642
Resumo: Organosedimentary deposits formed by interaction of carbonate and terrigenous sediments are commonly found in the Lagoa Salgada, a holocenic environment located on the north of Rio de Janeiro state which records environmental and biological information of their evolution. Microbial mats are widespread however stromatolites are very prominent and exposed nowadays in the lagoon. Microbial mats were distinguished into two main morphologies, colloform and polygonal mats. It is interesting to note that the colloform ones are not lithified unlike the polygonal ones. Related to stromatolites three main morphologies were defined and classified based on their external morphology and internal structure. Internal structure was further analyzed by sample cutting and thin section study to confirm field classification. Stromatolites are mostly bioherms dome-like and vary from 10 to 40cm high. Morphologically stromatolites are columnar or branched to columnar and coalescence among them are very common resulting in stratiform morphologies. Stromatolitic domal-like bioherms though showing similar internal structure were separated in small and large according to their size; the differences in size are clearly observed and have different areal distribution, which possibly reflects changes in the lagoon paleogeography during the geological time. Also, the identification of differences in the internal structure of stromatolites allows the formulation of hypothesis supporting environmental changes in the Lagoa Salgada.
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spelling Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazilrobial mats; Recent stromatoliteOrganosedimentary deposits formed by interaction of carbonate and terrigenous sediments are commonly found in the Lagoa Salgada, a holocenic environment located on the north of Rio de Janeiro state which records environmental and biological information of their evolution. Microbial mats are widespread however stromatolites are very prominent and exposed nowadays in the lagoon. Microbial mats were distinguished into two main morphologies, colloform and polygonal mats. It is interesting to note that the colloform ones are not lithified unlike the polygonal ones. Related to stromatolites three main morphologies were defined and classified based on their external morphology and internal structure. Internal structure was further analyzed by sample cutting and thin section study to confirm field classification. Stromatolites are mostly bioherms dome-like and vary from 10 to 40cm high. Morphologically stromatolites are columnar or branched to columnar and coalescence among them are very common resulting in stratiform morphologies. Stromatolitic domal-like bioherms though showing similar internal structure were separated in small and large according to their size; the differences in size are clearly observed and have different areal distribution, which possibly reflects changes in the lagoon paleogeography during the geological time. Also, the identification of differences in the internal structure of stromatolites allows the formulation of hypothesis supporting environmental changes in the Lagoa Salgada.Universidade Federal do Rio de JaneiroSilva, Douglas Rosa daMansur, Kátia LeiteAlmeida, Leonardo Fonseca Borghi de2019-12-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/3064210.11137/2019_1_439_453Anuário do Instituto de Geociências; Vol 42, No 1 (2019); 439-453Anuário do Instituto de Geociências; Vol 42, No 1 (2019); 439-4531982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJenghttps://revistas.ufrj.br/index.php/aigeo/article/view/30642/17326Copyright (c) 2019 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccess2019-12-10T15:03:30Zoai:www.revistas.ufrj.br:article/30642Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2019-12-10T15:03:30Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil

title Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
spellingShingle Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
Silva, Douglas Rosa da
robial mats; Recent stromatolite
title_short Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
title_full Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
title_fullStr Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
title_full_unstemmed Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
title_sort Distribution and Growth Morphology of the Recent Microbialites: the Case of Lagoa Salgada, Rio de Janeiro - Brazil
author Silva, Douglas Rosa da
author_facet Silva, Douglas Rosa da
Mansur, Kátia Leite
Almeida, Leonardo Fonseca Borghi de
author_role author
author2 Mansur, Kátia Leite
Almeida, Leonardo Fonseca Borghi de
author2_role author
author
dc.contributor.none.fl_str_mv

dc.contributor.author.fl_str_mv Silva, Douglas Rosa da
Mansur, Kátia Leite
Almeida, Leonardo Fonseca Borghi de
dc.subject.none.fl_str_mv
dc.subject.por.fl_str_mv robial mats; Recent stromatolite
topic robial mats; Recent stromatolite
description Organosedimentary deposits formed by interaction of carbonate and terrigenous sediments are commonly found in the Lagoa Salgada, a holocenic environment located on the north of Rio de Janeiro state which records environmental and biological information of their evolution. Microbial mats are widespread however stromatolites are very prominent and exposed nowadays in the lagoon. Microbial mats were distinguished into two main morphologies, colloform and polygonal mats. It is interesting to note that the colloform ones are not lithified unlike the polygonal ones. Related to stromatolites three main morphologies were defined and classified based on their external morphology and internal structure. Internal structure was further analyzed by sample cutting and thin section study to confirm field classification. Stromatolites are mostly bioherms dome-like and vary from 10 to 40cm high. Morphologically stromatolites are columnar or branched to columnar and coalescence among them are very common resulting in stratiform morphologies. Stromatolitic domal-like bioherms though showing similar internal structure were separated in small and large according to their size; the differences in size are clearly observed and have different areal distribution, which possibly reflects changes in the lagoon paleogeography during the geological time. Also, the identification of differences in the internal structure of stromatolites allows the formulation of hypothesis supporting environmental changes in the Lagoa Salgada.
publishDate 2019
dc.date.none.fl_str_mv 2019-12-01
dc.type.none.fl_str_mv

dc.type.driver.fl_str_mv info:eu-repo/semantics/article
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format article
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dc.identifier.uri.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/30642
10.11137/2019_1_439_453
url https://revistas.ufrj.br/index.php/aigeo/article/view/30642
identifier_str_mv 10.11137/2019_1_439_453
dc.language.iso.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv https://revistas.ufrj.br/index.php/aigeo/article/view/30642/17326
dc.rights.driver.fl_str_mv Copyright (c) 2019 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2019 Anuário do Instituto de Geociências
http://creativecommons.org/licenses/by/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
publisher.none.fl_str_mv Universidade Federal do Rio de Janeiro
dc.source.none.fl_str_mv Anuário do Instituto de Geociências; Vol 42, No 1 (2019); 439-453
Anuário do Instituto de Geociências; Vol 42, No 1 (2019); 439-453
1982-3908
0101-9759
reponame:Anuário do Instituto de Geociências (Online)
instname:Universidade Federal do Rio de Janeiro (UFRJ)
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reponame_str Anuário do Instituto de Geociências (Online)
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