WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?

Detalhes bibliográficos
Autor(a) principal: Villwock, Fernando Henrique
Data de Publicação: 2023
Outros Autores: Parolin, Mauro, Parellada, Claudia Inês
Tipo de documento: Artigo
Idioma: por
Título da fonte: Caminhos de Geografia
Texto Completo: https://seer.ufu.br/index.php/caminhosdegeografia/article/view/65891
Resumo: The different past human occupations are correlated to cultural filters intertwined with paleoenvironmental conditions, among these vestiges are the sambaquis, which can be characterized as artificial hills. The research was carried out in the sambaqui of Foz do Rio Poruquara, city of Guaraqueçaba, Paraná, aiming to interpret the paleoenvironmental significance of phytoliths, sponge spicules and mollusc shells recovered in the study area. In the samples of stratigraphic profiles, from the Museu Paranaense collection, for the recovery of phytoliths and sponge spicules, protocols had already described in the literature for these "proxies" were used, while the shells were identified by means of a comparative method. A relative dating of approximately 4,000 years BP has been established for the sambaqui of Foz do Rio Poruquara. Based on the occurrence of phytoliths along the profile, it was possible to establish three zones with different vegetation characteristics: I) base: grasses; II) intermediate: grasses-shrub; III) top: arboreal-grassy. As for sponge spicules, it was found that the sambaqui area was always under the influence of sea level fluctuations. The mollusc shells indicate that during the entire period of construction of the sambaqui the vegetation maintained characteristics similar to those observed today (bays, estuaries and mangroves).
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spelling WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?O QUE FITÓLITOS, ESPÍCULAS DE ESPONJAS E CONCHAS NOS “CONTAM” SOBRE O PASSADO DO SAMBAQUI DA FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?Dados “proxies”Sítio ArqueológicoPaleoambientesData “proxies”Archaeological SitePaleoenvironmentsThe different past human occupations are correlated to cultural filters intertwined with paleoenvironmental conditions, among these vestiges are the sambaquis, which can be characterized as artificial hills. The research was carried out in the sambaqui of Foz do Rio Poruquara, city of Guaraqueçaba, Paraná, aiming to interpret the paleoenvironmental significance of phytoliths, sponge spicules and mollusc shells recovered in the study area. In the samples of stratigraphic profiles, from the Museu Paranaense collection, for the recovery of phytoliths and sponge spicules, protocols had already described in the literature for these "proxies" were used, while the shells were identified by means of a comparative method. A relative dating of approximately 4,000 years BP has been established for the sambaqui of Foz do Rio Poruquara. Based on the occurrence of phytoliths along the profile, it was possible to establish three zones with different vegetation characteristics: I) base: grasses; II) intermediate: grasses-shrub; III) top: arboreal-grassy. As for sponge spicules, it was found that the sambaqui area was always under the influence of sea level fluctuations. The mollusc shells indicate that during the entire period of construction of the sambaqui the vegetation maintained characteristics similar to those observed today (bays, estuaries and mangroves).As diferentes ocupações humanas pretéritas estão correlacionadas a filtros culturais entrelaçados às condições paleoambientais, dentre esses vestígios estão os sambaquis, que podem ser caracterizados como morros artificiais. A pesquisa foi realizada no sambaqui da Foz do Rio Poruquara, município de Guaraqueçaba, Paraná, tendo como objetivo interpretar o significado paleoambiental dos fitólitos, das espículas de esponja e das conchas de moluscos recuperados na área de estudo. Nas amostras de perfis estratigráficos, do acervo do Museu Paranaense, para a recuperação dos fitólitos e espículas de esponja utilizou-se de protocolos já descritos na literatura para esses “proxies”, enquanto as conchas foram identificadas por meio de método comparativo. Estabeleceu-se para o sambaqui da Foz do Rio Poruquara datação relativa de aproximadamente 4.000 anos AP. Com base na ocorrência dos fitólitos ao longo do perfil, foi possível estabelecer três zonas com características de vegetação diferentes: I) base: gramíneas; II) intermediária: gramíneas-arbustivo; III) topo: arbóreo-gramíneas. Quanto às espículas de esponjas verificou-se que a área do sambaqui sempre esteve sob influência das oscilações do nível do mar. As conchas de moluscos indicam que durante todo o período de construção do sambaqui a vegetação manteve características similares às observadas na atualidade (baías, estuários e mangues).EDUFU - Editora da Universidade Federal de Uberlândia2023-08-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionAvaliado pelos paresapplication/pdfhttps://seer.ufu.br/index.php/caminhosdegeografia/article/view/6589110.14393/RCG249465891Caminhos de Geografia; Vol. 24 No. 94 (2023): Agosto; 99–117Caminhos de Geografia; Vol. 24 Núm. 94 (2023): Agosto; 99–117Caminhos de Geografia; v. 24 n. 94 (2023): Agosto; 99–1171678-6343reponame:Caminhos de Geografiainstname:Universidade Federal de Uberlândia (UFU)instacron:UFUporhttps://seer.ufu.br/index.php/caminhosdegeografia/article/view/65891/36486Copyright (c) 2023 Fernando Henrique Villwock, Mauro Parolin, Claudia Inês Parelladahttp://creativecommons.org/licenses/by-nc-nd/4.0info:eu-repo/semantics/openAccessVillwock, Fernando HenriqueParolin, MauroParellada, Claudia Inês2023-08-01T12:40:54Zoai:ojs.www.seer.ufu.br:article/65891Revistahttps://seer.ufu.br/index.php/caminhosdegeografia/indexPUBhttp://www.seer.ufu.br/index.php/caminhosdegeografia/oaiflaviasantosgeo@gmail.com1678-63431678-6343opendoar:2023-08-01T12:40:54Caminhos de Geografia - Universidade Federal de Uberlândia (UFU)false
dc.title.none.fl_str_mv WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
O QUE FITÓLITOS, ESPÍCULAS DE ESPONJAS E CONCHAS NOS “CONTAM” SOBRE O PASSADO DO SAMBAQUI DA FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
title WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
spellingShingle WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
Villwock, Fernando Henrique
Dados “proxies”
Sítio Arqueológico
Paleoambientes
Data “proxies”
Archaeological Site
Paleoenvironments
title_short WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
title_full WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
title_fullStr WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
title_full_unstemmed WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
title_sort WHAT DO THE PHYTOLITES, SPONGE SPICS AND SHELLS “TELL US” ABOUT THE PAST OF THE SHELL-MIDDEN OF THE FOZ DO RIO PORUQUARA, GUARAQUEÇABA, PARANÁ?
author Villwock, Fernando Henrique
author_facet Villwock, Fernando Henrique
Parolin, Mauro
Parellada, Claudia Inês
author_role author
author2 Parolin, Mauro
Parellada, Claudia Inês
author2_role author
author
dc.contributor.author.fl_str_mv Villwock, Fernando Henrique
Parolin, Mauro
Parellada, Claudia Inês
dc.subject.por.fl_str_mv Dados “proxies”
Sítio Arqueológico
Paleoambientes
Data “proxies”
Archaeological Site
Paleoenvironments
topic Dados “proxies”
Sítio Arqueológico
Paleoambientes
Data “proxies”
Archaeological Site
Paleoenvironments
description The different past human occupations are correlated to cultural filters intertwined with paleoenvironmental conditions, among these vestiges are the sambaquis, which can be characterized as artificial hills. The research was carried out in the sambaqui of Foz do Rio Poruquara, city of Guaraqueçaba, Paraná, aiming to interpret the paleoenvironmental significance of phytoliths, sponge spicules and mollusc shells recovered in the study area. In the samples of stratigraphic profiles, from the Museu Paranaense collection, for the recovery of phytoliths and sponge spicules, protocols had already described in the literature for these "proxies" were used, while the shells were identified by means of a comparative method. A relative dating of approximately 4,000 years BP has been established for the sambaqui of Foz do Rio Poruquara. Based on the occurrence of phytoliths along the profile, it was possible to establish three zones with different vegetation characteristics: I) base: grasses; II) intermediate: grasses-shrub; III) top: arboreal-grassy. As for sponge spicules, it was found that the sambaqui area was always under the influence of sea level fluctuations. The mollusc shells indicate that during the entire period of construction of the sambaqui the vegetation maintained characteristics similar to those observed today (bays, estuaries and mangroves).
publishDate 2023
dc.date.none.fl_str_mv 2023-08-01
dc.type.driver.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
Avaliado pelos pares
format article
status_str publishedVersion
dc.identifier.uri.fl_str_mv https://seer.ufu.br/index.php/caminhosdegeografia/article/view/65891
10.14393/RCG249465891
url https://seer.ufu.br/index.php/caminhosdegeografia/article/view/65891
identifier_str_mv 10.14393/RCG249465891
dc.language.iso.fl_str_mv por
language por
dc.relation.none.fl_str_mv https://seer.ufu.br/index.php/caminhosdegeografia/article/view/65891/36486
dc.rights.driver.fl_str_mv Copyright (c) 2023 Fernando Henrique Villwock, Mauro Parolin, Claudia Inês Parellada
http://creativecommons.org/licenses/by-nc-nd/4.0
info:eu-repo/semantics/openAccess
rights_invalid_str_mv Copyright (c) 2023 Fernando Henrique Villwock, Mauro Parolin, Claudia Inês Parellada
http://creativecommons.org/licenses/by-nc-nd/4.0
eu_rights_str_mv openAccess
dc.format.none.fl_str_mv application/pdf
dc.publisher.none.fl_str_mv EDUFU - Editora da Universidade Federal de Uberlândia
publisher.none.fl_str_mv EDUFU - Editora da Universidade Federal de Uberlândia
dc.source.none.fl_str_mv Caminhos de Geografia; Vol. 24 No. 94 (2023): Agosto; 99–117
Caminhos de Geografia; Vol. 24 Núm. 94 (2023): Agosto; 99–117
Caminhos de Geografia; v. 24 n. 94 (2023): Agosto; 99–117
1678-6343
reponame:Caminhos de Geografia
instname:Universidade Federal de Uberlândia (UFU)
instacron:UFU
instname_str Universidade Federal de Uberlândia (UFU)
instacron_str UFU
institution UFU
reponame_str Caminhos de Geografia
collection Caminhos de Geografia
repository.name.fl_str_mv Caminhos de Geografia - Universidade Federal de Uberlândia (UFU)
repository.mail.fl_str_mv flaviasantosgeo@gmail.com
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