The Veryhachium "complex": Silurian index species?

Detalhes bibliográficos
Autor(a) principal: Cardoso, Tereza Regina Machado
Data de Publicação: 2005
Outros Autores: Rodrigues, Maria Antonieta da Conceição
Tipo de documento: Artigo
Idioma: por
Título da fonte: Anuário do Instituto de Geociências (Online)
Texto Completo: https://revistas.ufrj.br/index.php/aigeo/article/view/6280
Resumo: Acritarchs are known to be related to cysts of marine microphytoplankton, and are reliable indicators of marine paleoenvironments. The acritarch genus Veryhachium was erected by Deunff (1954) to encompass an entire plexus of microfossils first recorded in Paleozoic strata of England and France. It includes a variety of organic-walled microphytoplanktonic organisms consisting of a smooth or granulated, hollow vesicle with triangular to polygonal shape. The vesicle is provided with up to eight, tapered and long, often bent, unbranched processes, which are hollow and present either smooth or granulated walls. The oldest known representatives of Veryhachium are from the Upper Cambrian, but the genus becomes most abundant and diversified in succeeding Paleozoic intervals. By contrast, post-Paleozoic records include only two species from the Cretaceous, and three Tertiary species which Stancliffe & Sarjeant (1994) regard as anomalous forms. The occurrence of Veryhachium in recent sediments of Bolivia has been attributed by several authors to the reworking of Paleozoic strata. Due to the long stratigraphic range of most of its species, the genus has generally played a secondary role in biostratigraphic zonations. Our palynological study of the Trombetas Group (Amazonas basin, northern Brazil), based on numerous outcrops and Eletronorte shallow core-drills, together with core samples of a single Petrobras well, has recorded such Silurian species as Veryhachium owensii, V. oklahomense, V. pertonense, V. longispinosu, V. rhomboidium and V. lairdii. They occur together with more age-diagnostic Silurian species belonging to the genera Deunffia and Domasia. The diversity of Veryhachium in the Trombetas Group highlights not only its importance as a paleoenvironmental indicator, but also its usefulness in characterizing regional palynomorphs assemblages in Paleozoic basins of Western Gondwana.
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spelling The Veryhachium "complex": Silurian index species?"Complexo" Veryhachium: acritarcos indicativos do Siluriano?"Acritarchs are known to be related to cysts of marine microphytoplankton, and are reliable indicators of marine paleoenvironments. The acritarch genus Veryhachium was erected by Deunff (1954) to encompass an entire plexus of microfossils first recorded in Paleozoic strata of England and France. It includes a variety of organic-walled microphytoplanktonic organisms consisting of a smooth or granulated, hollow vesicle with triangular to polygonal shape. The vesicle is provided with up to eight, tapered and long, often bent, unbranched processes, which are hollow and present either smooth or granulated walls. The oldest known representatives of Veryhachium are from the Upper Cambrian, but the genus becomes most abundant and diversified in succeeding Paleozoic intervals. By contrast, post-Paleozoic records include only two species from the Cretaceous, and three Tertiary species which Stancliffe & Sarjeant (1994) regard as anomalous forms. The occurrence of Veryhachium in recent sediments of Bolivia has been attributed by several authors to the reworking of Paleozoic strata. Due to the long stratigraphic range of most of its species, the genus has generally played a secondary role in biostratigraphic zonations. Our palynological study of the Trombetas Group (Amazonas basin, northern Brazil), based on numerous outcrops and Eletronorte shallow core-drills, together with core samples of a single Petrobras well, has recorded such Silurian species as Veryhachium owensii, V. oklahomense, V. pertonense, V. longispinosu, V. rhomboidium and V. lairdii. They occur together with more age-diagnostic Silurian species belonging to the genera Deunffia and Domasia. The diversity of Veryhachium in the Trombetas Group highlights not only its importance as a paleoenvironmental indicator, but also its usefulness in characterizing regional palynomorphs assemblages in Paleozoic basins of Western Gondwana.Sabe-se que os acritarcos estão relacionados a cistos do fitoplâncton marinho, e que sua importância maior tem conotação paleoambiental. O gênero de acritarco Veryhachium foi proposto por Deunff (1954) para englobar um grupo de microfósseis paleozóicos, descritos em sedimentos da Inglaterra e França. Este gênero abrange microorganismos fósseis planctônicos, compostos de matéria orgânica, com vesícula oca, superfície lisa ou granulada, contorno triangular a poligonal, processos (1-8) ocos, lisos ou granulados, pontiagudos, longos e freqüentemente curvados e sem ramificações, entretanto este gênero torna-se o mais abundante e diversificado nas associações do Paleozóico. Em contraste os registros pós-Paleozóicos incluem apenas duas espécies do Cretáceo, e três do Terciário que são supostamente anômalas segundo Stancliffe & Sarjeant (1994). A ocorrência de espécies de Veryhachium atribuídas a sedimentos recentes da Bolívia é vista com ceticismo pelos especialistas e tem sido considerada por diversos autores como devido a retrabalhamento. A longa amplitude estratigráfica da maioria das espécies de Veryhachium tem lhe relegado um caráter secundário nos zoneamentos bioestratigráficos. Neste trabalho, a partir da análise de amostras de testemunhos de sondagem cedidas pela Petrobras e de sondagens rasas da Eletronorte, pertencentes ao Grupo Trombetas (Bacia do Amazonas, Brasil), registramos ocorrência diversificada desse gênero. As espécies Veryhachium owensii, V. oklahomense, V. pertonense, V. longispinosum, V. rhomboidium e V. lairdii, têm distribuição estratigráfica abrangendo Ordoviciano-Devoniano, sendo específicas do Siluriano Veryhachium owensii, V. oklahomense, V. pertonense. Registramos também espécies diagnósticas tais como Deunffia e Domasia que mundialmente caracterizam o Siluriano. A partir dos dados levantados concluímos que a ocorrência de Veryhachium em sedimentos do Grupo Trombetas além de indicadores de paleoambientes constitui-se como elemento auxiliar na definição de associações bioestratigráficas para o Siluriano das bacias paleozóicas do Gondwana ocidental.Universidade Federal do Rio de Janeiro2005-06-01info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/628010.11137/2005_1_143-157Anuário do Instituto de Geociências; Vol 28, No 1 (2005); 143-157Anuário do Instituto de Geociências; Vol 28, No 1 (2005); 143-1571982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJporhttps://revistas.ufrj.br/index.php/aigeo/article/view/6280/4877Copyright (c) 2005 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccessCardoso, Tereza Regina MachadoRodrigues, Maria Antonieta da Conceição2022-10-13T17:44:47Zoai:www.revistas.ufrj.br:article/6280Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2022-10-13T17:44:47Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false
dc.title.none.fl_str_mv The Veryhachium "complex": Silurian index species?
"Complexo" Veryhachium: acritarcos indicativos do Siluriano?"
title The Veryhachium "complex": Silurian index species?
spellingShingle The Veryhachium "complex": Silurian index species?
Cardoso, Tereza Regina Machado
title_short The Veryhachium "complex": Silurian index species?
title_full The Veryhachium "complex": Silurian index species?
title_fullStr The Veryhachium "complex": Silurian index species?
title_full_unstemmed The Veryhachium "complex": Silurian index species?
title_sort The Veryhachium "complex": Silurian index species?
author Cardoso, Tereza Regina Machado
author_facet Cardoso, Tereza Regina Machado
Rodrigues, Maria Antonieta da Conceição
author_role author
author2 Rodrigues, Maria Antonieta da Conceição
author2_role author
dc.contributor.author.fl_str_mv Cardoso, Tereza Regina Machado
Rodrigues, Maria Antonieta da Conceição
description Acritarchs are known to be related to cysts of marine microphytoplankton, and are reliable indicators of marine paleoenvironments. The acritarch genus Veryhachium was erected by Deunff (1954) to encompass an entire plexus of microfossils first recorded in Paleozoic strata of England and France. It includes a variety of organic-walled microphytoplanktonic organisms consisting of a smooth or granulated, hollow vesicle with triangular to polygonal shape. The vesicle is provided with up to eight, tapered and long, often bent, unbranched processes, which are hollow and present either smooth or granulated walls. The oldest known representatives of Veryhachium are from the Upper Cambrian, but the genus becomes most abundant and diversified in succeeding Paleozoic intervals. By contrast, post-Paleozoic records include only two species from the Cretaceous, and three Tertiary species which Stancliffe & Sarjeant (1994) regard as anomalous forms. The occurrence of Veryhachium in recent sediments of Bolivia has been attributed by several authors to the reworking of Paleozoic strata. Due to the long stratigraphic range of most of its species, the genus has generally played a secondary role in biostratigraphic zonations. Our palynological study of the Trombetas Group (Amazonas basin, northern Brazil), based on numerous outcrops and Eletronorte shallow core-drills, together with core samples of a single Petrobras well, has recorded such Silurian species as Veryhachium owensii, V. oklahomense, V. pertonense, V. longispinosu, V. rhomboidium and V. lairdii. They occur together with more age-diagnostic Silurian species belonging to the genera Deunffia and Domasia. The diversity of Veryhachium in the Trombetas Group highlights not only its importance as a paleoenvironmental indicator, but also its usefulness in characterizing regional palynomorphs assemblages in Paleozoic basins of Western Gondwana.
publishDate 2005
dc.date.none.fl_str_mv 2005-06-01
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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 28, No 1 (2005); 143-157
Anuário do Instituto de Geociências; Vol 28, No 1 (2005); 143-157
1982-3908
0101-9759
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