Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio
Autor(a) principal: | |
---|---|
Data de Publicação: | 2020 |
Tipo de documento: | Dissertação |
Idioma: | por |
Título da fonte: | Biblioteca Digital de Teses e Dissertações do UNIOESTE |
Texto Completo: | http://tede.unioeste.br/handle/tede/4843 |
Resumo: | The present work aimed to characterize a hillslopes dynamics in compartment dissected from the surface of the pinhão / guarapuava in the upper quaternary, based on the description of the surface formations by the litho-; alo- and chronostratigraphic criteria. The study object consists of a stratigraphic section in a context of paleovalleyhead located in the dissected border of Pinhão/Guarapuava-PR surface, individualized from a cross section of highway. To reach the objective, it was necessary to identify and describe the stratigraphic section; characterization of stratigraphic records; the chronology for the process recorded in the superficial formations; and the verification and correlation of the pedostratigraphic records of studies of the region with global paleoclimatic variations. The records found on the slope were individualized, being a paleosol buried with hydromorphic characteristics and cut by a linear incision, stratigraphic deposits of co-aluvium, an intermediate colluvial sequence of granular structure and na upper colluvial sequence. The last three records were responsible for the filling the gully, and the presence of alterite was identified throughout the slope base. These sedimentary records are the results of morphogenesis that favored the filling the gully, generating an inversion of relief in the area. Twenty-four pedostratigraphic horizons were characterized, the micromorphological description revealed that the records submitted to the method are of allochthonous origin and were transported by different processes, being channeled surface runoff (co-alluvial sequence), surface runoff (intermediate colluvial sequence) and earth flow (upper colluvial sequence). The data obtained by isotopic carbon analysis, suggest that the records follow an isotopic variation, consisting of C3 plants (shrubs and trees) and mixture (C3 + C4). From the LOE and 14C dating it was possible to establish the geochronological records 6Cb (18,850 ± 2,350 ky BP), 13Cb (24,750 ± 2,780 ky BP) and 16CAb (25,495 ± 25,013 ky BP), which were established between the Last Interstate ( EIM3) and the Last Glacial Maximum (EIM2). The phases of pedogenesis and morphogenesis identified in the Pinhão / Guarapuava summit surface are similar to those identified in the Planalto de Palmas / Caçador. |
id |
UNIOESTE-1_1e41a83baf6ecf0cd6b17542ca2246ca |
---|---|
oai_identifier_str |
oai:tede.unioeste.br:tede/4843 |
network_acronym_str |
UNIOESTE-1 |
network_name_str |
Biblioteca Digital de Teses e Dissertações do UNIOESTE |
repository_id_str |
|
spelling |
Paisani , Julio Cesarhttp://lattes.cnpq.br/1104080942110403Paisani , Julio Cesarhttp://lattes.cnpq.br/1104080942110403Pontelli, Marga Elizhttp://lattes.cnpq.br/5909311662921266Sordi, Michael Vinicius dehttp://lattes.cnpq.br/6233886021337527Camargo Filho , Mauriciohttp://lattes.cnpq.br/1455869486742599http://lattes.cnpq.br/7682899684035616Gazola , Karina de Cássia2020-07-20T12:25:03Z2020-02-28GAZOLA, Karina de Cássia. Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio. 2020.124f. Dissertação( Mestrado em Geografia) - Universidade Estadual do Oeste do Paraná,Francisco Beltrão, 2020.http://tede.unioeste.br/handle/tede/4843The present work aimed to characterize a hillslopes dynamics in compartment dissected from the surface of the pinhão / guarapuava in the upper quaternary, based on the description of the surface formations by the litho-; alo- and chronostratigraphic criteria. The study object consists of a stratigraphic section in a context of paleovalleyhead located in the dissected border of Pinhão/Guarapuava-PR surface, individualized from a cross section of highway. To reach the objective, it was necessary to identify and describe the stratigraphic section; characterization of stratigraphic records; the chronology for the process recorded in the superficial formations; and the verification and correlation of the pedostratigraphic records of studies of the region with global paleoclimatic variations. The records found on the slope were individualized, being a paleosol buried with hydromorphic characteristics and cut by a linear incision, stratigraphic deposits of co-aluvium, an intermediate colluvial sequence of granular structure and na upper colluvial sequence. The last three records were responsible for the filling the gully, and the presence of alterite was identified throughout the slope base. These sedimentary records are the results of morphogenesis that favored the filling the gully, generating an inversion of relief in the area. Twenty-four pedostratigraphic horizons were characterized, the micromorphological description revealed that the records submitted to the method are of allochthonous origin and were transported by different processes, being channeled surface runoff (co-alluvial sequence), surface runoff (intermediate colluvial sequence) and earth flow (upper colluvial sequence). The data obtained by isotopic carbon analysis, suggest that the records follow an isotopic variation, consisting of C3 plants (shrubs and trees) and mixture (C3 + C4). From the LOE and 14C dating it was possible to establish the geochronological records 6Cb (18,850 ± 2,350 ky BP), 13Cb (24,750 ± 2,780 ky BP) and 16CAb (25,495 ± 25,013 ky BP), which were established between the Last Interstate ( EIM3) and the Last Glacial Maximum (EIM2). The phases of pedogenesis and morphogenesis identified in the Pinhão / Guarapuava summit surface are similar to those identified in the Planalto de Palmas / Caçador.O presente trabalhou tem como objetivo caracterizar a dinâmica de encosta em compartimento dissecado da superfície de cimeira de pinhão/guarapuava no quaternário tardio, com base na descrição das formações superficiais pelos critérios lito- pedo- alo- e cronoestratigráficos. O objeto de estudo consiste em seção estratigráfica em contexto de paleocabeceira de drenagem situada na borda dissecada da superfície de Pinhão/Guarapuava-PR, individualizada a partir de corte transversal de rodovia. Para alcançar o objetivo, se fez necessária a identificação e descrição da seção estratigráfica; caracterização dos registros estratigráficos; a cronologia dos processos registrados nas formações superficiais; e a verificação e correlação dos registros pedoestratigráficos de estudos da região com as variações paleoclimáticas globais. Os registros encontrados na encosta foram individualizados sendo um paleossolo enterrado com características hidromórficas e cortado por uma incisão linear, depósitos estratigráficos de sequência co-alúvio, uma sequência coluvial intermédiaria de estrutura granular e uma sequência coluvial superior. Os três últimos registros foram responsáveis pela colmatação da voçoroca, e em toda a base da encosta foi identificada a presença de alterita. Esses registros sedimentares são resultados da morfogênese que favoreceu o entulhamento da voçoroca, gerando inversão de relevo na área. Foram caracterizados 24 horizontes pedoestratigráficos, cuja evolução é decorrente da dinâmica entre pedogênese e morfogênese. A descrição micromorfológica revelou que os registros submetidos ao método são de origem alóctone e foram transportados por processos distintos, sendo eles escoamento superficial canalizado (sequência co-alúvial), escoamento superficial (sequência coluvial intermédiaria) e fluxo de terra (sequência coluvial superior). Os dados obtidos pela análise isotópica de carbono, sugerem que os registros seguem variação isotópica, constituída por plantas C3 (arbustos e arbórea) e mistura (C3 + C4). A partir das datações via LOE e 14C foi possível estabelecer a geocronológico dos registros 6Cb (18.850±2.350 anos A.P.), 13Cb (24.750±2.780 anos A.P.) e 16CAb (25.254±482 anos A.P.), que foram estabelecidos entre o Último Interestadial (EIM3) e o Último Máximo Glacial (EIM2). As fases de pedogênese e morfogênese identificadas na Superfície de cimeira Pinhão/Guarapuava são similares às identificadas no Planalto de Palmas/Caçador.Submitted by Juliana Correa (juliana.correa@unioeste.br) on 2020-07-20T12:25:03Z No. of bitstreams: 2 Karina de Cássia Gazola - 2020.pdf: 6854007 bytes, checksum: baa7767039357a5e49f29b88639b9917 (MD5) license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5)Made available in DSpace on 2020-07-20T12:25:03Z (GMT). No. of bitstreams: 2 Karina de Cássia Gazola - 2020.pdf: 6854007 bytes, checksum: baa7767039357a5e49f29b88639b9917 (MD5) license_rdf: 0 bytes, checksum: d41d8cd98f00b204e9800998ecf8427e (MD5) Previous issue date: 2020-02-28Coordenação de Aperfeiçoamento de Pessoal de Nível Superior - CAPESapplication/pdfpor-5356284425524309716500Universidade Estadual do Oeste do ParanáFrancisco BeltrãoPrograma de Pós-Graduação em GeografiaUNIOESTEBrasilCentro de Ciências Humanashttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccessevolução do relevocritérios estratigráficospaleossolo hidromórfico,colúvico-alúvioevolution of reliefstratigraphic criteriahydromorphic paleosolcolluviumco-aluviumCIÊNCIAS HUMANAS: GEOGRAFIADinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardioHillslopes dynamics in compartment dissected from the surface of the Pinhão / Guarapuava in the upper quaternaryinfo:eu-repo/semantics/publishedVersioninfo:eu-repo/semantics/masterThesis567733122860342413860060060019642433089735170332075167498588264571reponame:Biblioteca Digital de Teses e Dissertações do UNIOESTEinstname:Universidade Estadual do Oeste do Paraná (UNIOESTE)instacron:UNIOESTEORIGINALKarina de Cássia Gazola - 2020.pdfKarina de Cássia Gazola - 2020.pdfapplication/pdf6854007http://tede.unioeste.br:8080/tede/bitstream/tede/4843/5/Karina+de+C%C3%A1ssia+Gazola+-+2020.pdfbaa7767039357a5e49f29b88639b9917MD55CC-LICENSElicense_urllicense_urltext/plain; charset=utf-849http://tede.unioeste.br:8080/tede/bitstream/tede/4843/2/license_url4afdbb8c545fd630ea7db775da747b2fMD52license_textlicense_texttext/html; charset=utf-80http://tede.unioeste.br:8080/tede/bitstream/tede/4843/3/license_textd41d8cd98f00b204e9800998ecf8427eMD53license_rdflicense_rdfapplication/rdf+xml; charset=utf-80http://tede.unioeste.br:8080/tede/bitstream/tede/4843/4/license_rdfd41d8cd98f00b204e9800998ecf8427eMD54LICENSElicense.txtlicense.txttext/plain; charset=utf-82165http://tede.unioeste.br:8080/tede/bitstream/tede/4843/1/license.txtbd3efa91386c1718a7f26a329fdcb468MD51tede/48432020-07-20 09:25:04.008oai:tede.unioeste.br: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Biblioteca Digital de Teses e Dissertaçõeshttp://tede.unioeste.br/PUBhttp://tede.unioeste.br/oai/requestbiblioteca.repositorio@unioeste.bropendoar:2020-07-20T12:25:04Biblioteca Digital de Teses e Dissertações do UNIOESTE - Universidade Estadual do Oeste do Paraná (UNIOESTE)false |
dc.title.por.fl_str_mv |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio |
dc.title.alternative.eng.fl_str_mv |
Hillslopes dynamics in compartment dissected from the surface of the Pinhão / Guarapuava in the upper quaternary |
title |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio |
spellingShingle |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio Gazola , Karina de Cássia evolução do relevo critérios estratigráficos paleossolo hidromórfico, colúvi co-alúvio evolution of relief stratigraphic criteria hydromorphic paleosol colluvium co-aluvium CIÊNCIAS HUMANAS: GEOGRAFIA |
title_short |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio |
title_full |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio |
title_fullStr |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio |
title_full_unstemmed |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio |
title_sort |
Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio |
author |
Gazola , Karina de Cássia |
author_facet |
Gazola , Karina de Cássia |
author_role |
author |
dc.contributor.advisor1.fl_str_mv |
Paisani , Julio Cesar |
dc.contributor.advisor1Lattes.fl_str_mv |
http://lattes.cnpq.br/1104080942110403 |
dc.contributor.referee1.fl_str_mv |
Paisani , Julio Cesar |
dc.contributor.referee1Lattes.fl_str_mv |
http://lattes.cnpq.br/1104080942110403 |
dc.contributor.referee2.fl_str_mv |
Pontelli, Marga Eliz |
dc.contributor.referee2Lattes.fl_str_mv |
http://lattes.cnpq.br/5909311662921266 |
dc.contributor.referee3.fl_str_mv |
Sordi, Michael Vinicius de |
dc.contributor.referee3Lattes.fl_str_mv |
http://lattes.cnpq.br/6233886021337527 |
dc.contributor.referee4.fl_str_mv |
Camargo Filho , Mauricio |
dc.contributor.referee4Lattes.fl_str_mv |
http://lattes.cnpq.br/1455869486742599 |
dc.contributor.authorLattes.fl_str_mv |
http://lattes.cnpq.br/7682899684035616 |
dc.contributor.author.fl_str_mv |
Gazola , Karina de Cássia |
contributor_str_mv |
Paisani , Julio Cesar Paisani , Julio Cesar Pontelli, Marga Eliz Sordi, Michael Vinicius de Camargo Filho , Mauricio |
dc.subject.por.fl_str_mv |
evolução do relevo critérios estratigráficos paleossolo hidromórfico, colúvi co-alúvio |
topic |
evolução do relevo critérios estratigráficos paleossolo hidromórfico, colúvi co-alúvio evolution of relief stratigraphic criteria hydromorphic paleosol colluvium co-aluvium CIÊNCIAS HUMANAS: GEOGRAFIA |
dc.subject.eng.fl_str_mv |
evolution of relief stratigraphic criteria hydromorphic paleosol colluvium co-aluvium |
dc.subject.cnpq.fl_str_mv |
CIÊNCIAS HUMANAS: GEOGRAFIA |
description |
The present work aimed to characterize a hillslopes dynamics in compartment dissected from the surface of the pinhão / guarapuava in the upper quaternary, based on the description of the surface formations by the litho-; alo- and chronostratigraphic criteria. The study object consists of a stratigraphic section in a context of paleovalleyhead located in the dissected border of Pinhão/Guarapuava-PR surface, individualized from a cross section of highway. To reach the objective, it was necessary to identify and describe the stratigraphic section; characterization of stratigraphic records; the chronology for the process recorded in the superficial formations; and the verification and correlation of the pedostratigraphic records of studies of the region with global paleoclimatic variations. The records found on the slope were individualized, being a paleosol buried with hydromorphic characteristics and cut by a linear incision, stratigraphic deposits of co-aluvium, an intermediate colluvial sequence of granular structure and na upper colluvial sequence. The last three records were responsible for the filling the gully, and the presence of alterite was identified throughout the slope base. These sedimentary records are the results of morphogenesis that favored the filling the gully, generating an inversion of relief in the area. Twenty-four pedostratigraphic horizons were characterized, the micromorphological description revealed that the records submitted to the method are of allochthonous origin and were transported by different processes, being channeled surface runoff (co-alluvial sequence), surface runoff (intermediate colluvial sequence) and earth flow (upper colluvial sequence). The data obtained by isotopic carbon analysis, suggest that the records follow an isotopic variation, consisting of C3 plants (shrubs and trees) and mixture (C3 + C4). From the LOE and 14C dating it was possible to establish the geochronological records 6Cb (18,850 ± 2,350 ky BP), 13Cb (24,750 ± 2,780 ky BP) and 16CAb (25,495 ± 25,013 ky BP), which were established between the Last Interstate ( EIM3) and the Last Glacial Maximum (EIM2). The phases of pedogenesis and morphogenesis identified in the Pinhão / Guarapuava summit surface are similar to those identified in the Planalto de Palmas / Caçador. |
publishDate |
2020 |
dc.date.accessioned.fl_str_mv |
2020-07-20T12:25:03Z |
dc.date.issued.fl_str_mv |
2020-02-28 |
dc.type.status.fl_str_mv |
info:eu-repo/semantics/publishedVersion |
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/masterThesis |
format |
masterThesis |
status_str |
publishedVersion |
dc.identifier.citation.fl_str_mv |
GAZOLA, Karina de Cássia. Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio. 2020.124f. Dissertação( Mestrado em Geografia) - Universidade Estadual do Oeste do Paraná,Francisco Beltrão, 2020. |
dc.identifier.uri.fl_str_mv |
http://tede.unioeste.br/handle/tede/4843 |
identifier_str_mv |
GAZOLA, Karina de Cássia. Dinâmica de encosta em compartimento dissecado da superfície de cimeira de Pinhão/Guarapuava no quaternário tardio. 2020.124f. Dissertação( Mestrado em Geografia) - Universidade Estadual do Oeste do Paraná,Francisco Beltrão, 2020. |
url |
http://tede.unioeste.br/handle/tede/4843 |
dc.language.iso.fl_str_mv |
por |
language |
por |
dc.relation.program.fl_str_mv |
5677331228603424138 |
dc.relation.confidence.fl_str_mv |
600 600 600 |
dc.relation.department.fl_str_mv |
1964243308973517033 |
dc.relation.sponsorship.fl_str_mv |
2075167498588264571 |
dc.rights.driver.fl_str_mv |
http://creativecommons.org/licenses/by-nc-nd/4.0/ info:eu-repo/semantics/openAccess |
rights_invalid_str_mv |
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 |
Universidade Estadual do Oeste do Paraná Francisco Beltrão |
dc.publisher.program.fl_str_mv |
Programa de Pós-Graduação em Geografia |
dc.publisher.initials.fl_str_mv |
UNIOESTE |
dc.publisher.country.fl_str_mv |
Brasil |
dc.publisher.department.fl_str_mv |
Centro de Ciências Humanas |
publisher.none.fl_str_mv |
Universidade Estadual do Oeste do Paraná Francisco Beltrão |
dc.source.none.fl_str_mv |
reponame:Biblioteca Digital de Teses e Dissertações do UNIOESTE instname:Universidade Estadual do Oeste do Paraná (UNIOESTE) instacron:UNIOESTE |
instname_str |
Universidade Estadual do Oeste do Paraná (UNIOESTE) |
instacron_str |
UNIOESTE |
institution |
UNIOESTE |
reponame_str |
Biblioteca Digital de Teses e Dissertações do UNIOESTE |
collection |
Biblioteca Digital de Teses e Dissertações do UNIOESTE |
bitstream.url.fl_str_mv |
http://tede.unioeste.br:8080/tede/bitstream/tede/4843/5/Karina+de+C%C3%A1ssia+Gazola+-+2020.pdf http://tede.unioeste.br:8080/tede/bitstream/tede/4843/2/license_url http://tede.unioeste.br:8080/tede/bitstream/tede/4843/3/license_text http://tede.unioeste.br:8080/tede/bitstream/tede/4843/4/license_rdf http://tede.unioeste.br:8080/tede/bitstream/tede/4843/1/license.txt |
bitstream.checksum.fl_str_mv |
baa7767039357a5e49f29b88639b9917 4afdbb8c545fd630ea7db775da747b2f d41d8cd98f00b204e9800998ecf8427e d41d8cd98f00b204e9800998ecf8427e bd3efa91386c1718a7f26a329fdcb468 |
bitstream.checksumAlgorithm.fl_str_mv |
MD5 MD5 MD5 MD5 MD5 |
repository.name.fl_str_mv |
Biblioteca Digital de Teses e Dissertações do UNIOESTE - Universidade Estadual do Oeste do Paraná (UNIOESTE) |
repository.mail.fl_str_mv |
biblioteca.repositorio@unioeste.br |
_version_ |
1801124568011636736 |