Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences
Autor(a) principal: | |
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Data de Publicação: | 2019 |
Outros Autores: | , |
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/28468 |
Resumo: | A detailed palynological analysis was conducted on 29 samples obtained from the Cretaceous interval of the well Campos-01, drilled in the Northern portion of the offshore Campos Basin. The main objectives of this study were to precise the age the rocks and to perform an analysis and interpretation of the depositional environment of the interval. The material consists of mainly shales, marls, calcareous mudstones and sandstones deposited in a deep marine environment. The palynological analysis consisted on identification and counting of all palynomorphs. The paleoenvironmental and paleoecological investigations were supported by cluster analysis, ecological indices (e.g. diversity, dominance) and ratios (e.g. continental:marine) were used. A total of 97 taxa was identified, which included 46 genera of dinoflagellates cysts, 25 genera of spores, 21 genera of pollen grains, 2 genera of freshwater algae and microforaminiferal linings. The recorded assemblage (e.g. Trichodinium castanea, Dinogymnium acuminatum, Zlivisporis blanensis) was assigned to a late Campanian—late Maastrichtian age for the studied section. The interval is clearly dominated by the dinoflagellate cysts that reach 90.7% of total of palynomorphs. On the basis of cluster analysis (r-mode) three dinoflagellate associations were recognized: Systematophora, Areoligera and Spiniferites. The stratigraphic distribution of dinoflagellates associations indicates three intervals (I1-I3). The intervals I1 and I2, dominated by Systematophora and Spiniferites respectively, are interpreted as open marine environment. In the interval I3, the dominance of Areoligera Association indicates a nearshore environment, also supported by the large amount of continental elements, including the genus Callialasporites, which is attributed to high altitude flora, suggesting the presence of highland feeding areas. |
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Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental InferencesPalynology; Paleoenvironment; Cretaceous; Campos BasinA detailed palynological analysis was conducted on 29 samples obtained from the Cretaceous interval of the well Campos-01, drilled in the Northern portion of the offshore Campos Basin. The main objectives of this study were to precise the age the rocks and to perform an analysis and interpretation of the depositional environment of the interval. The material consists of mainly shales, marls, calcareous mudstones and sandstones deposited in a deep marine environment. The palynological analysis consisted on identification and counting of all palynomorphs. The paleoenvironmental and paleoecological investigations were supported by cluster analysis, ecological indices (e.g. diversity, dominance) and ratios (e.g. continental:marine) were used. A total of 97 taxa was identified, which included 46 genera of dinoflagellates cysts, 25 genera of spores, 21 genera of pollen grains, 2 genera of freshwater algae and microforaminiferal linings. The recorded assemblage (e.g. Trichodinium castanea, Dinogymnium acuminatum, Zlivisporis blanensis) was assigned to a late Campanian—late Maastrichtian age for the studied section. The interval is clearly dominated by the dinoflagellate cysts that reach 90.7% of total of palynomorphs. On the basis of cluster analysis (r-mode) three dinoflagellate associations were recognized: Systematophora, Areoligera and Spiniferites. The stratigraphic distribution of dinoflagellates associations indicates three intervals (I1-I3). The intervals I1 and I2, dominated by Systematophora and Spiniferites respectively, are interpreted as open marine environment. In the interval I3, the dominance of Areoligera Association indicates a nearshore environment, also supported by the large amount of continental elements, including the genus Callialasporites, which is attributed to high altitude flora, suggesting the presence of highland feeding areas.Universidade Federal do Rio de JaneiroAzevedo, Sergio Martins Lopes deCarvalho, Marcelo de AraujoRios-Netto, Aristóteles de Moraes2019-09-09info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionapplication/pdfhttps://revistas.ufrj.br/index.php/aigeo/article/view/2846810.11137/2018_2_332_343Anuário do Instituto de Geociências; Vol 41, No 2 (2018); 332-343Anuário do Instituto de Geociências; Vol 41, No 2 (2018); 332-3431982-39080101-9759reponame:Anuário do Instituto de Geociências (Online)instname:Universidade Federal do Rio de Janeiro (UFRJ)instacron:UFRJenghttps://revistas.ufrj.br/index.php/aigeo/article/view/28468/15499Copyright (c) 2019 Anuário do Instituto de Geociênciashttp://creativecommons.org/licenses/by/4.0info:eu-repo/semantics/openAccess2022-10-06T17:22:23Zoai:www.revistas.ufrj.br:article/28468Revistahttps://revistas.ufrj.br/index.php/aigeo/indexPUBhttps://revistas.ufrj.br/index.php/aigeo/oaianuario@igeo.ufrj.br||1982-39080101-9759opendoar:2022-10-06T17:22:23Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ)false |
dc.title.none.fl_str_mv |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences |
title |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences |
spellingShingle |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences Azevedo, Sergio Martins Lopes de Palynology; Paleoenvironment; Cretaceous; Campos Basin |
title_short |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences |
title_full |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences |
title_fullStr |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences |
title_full_unstemmed |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences |
title_sort |
Upper Cretaceous Palynology of the Campos-01 Well, Northern Campos Basin: Paleoenvironmental Inferences |
author |
Azevedo, Sergio Martins Lopes de |
author_facet |
Azevedo, Sergio Martins Lopes de Carvalho, Marcelo de Araujo Rios-Netto, Aristóteles de Moraes |
author_role |
author |
author2 |
Carvalho, Marcelo de Araujo Rios-Netto, Aristóteles de Moraes |
author2_role |
author author |
dc.contributor.none.fl_str_mv |
|
dc.contributor.author.fl_str_mv |
Azevedo, Sergio Martins Lopes de Carvalho, Marcelo de Araujo Rios-Netto, Aristóteles de Moraes |
dc.subject.none.fl_str_mv |
|
dc.subject.por.fl_str_mv |
Palynology; Paleoenvironment; Cretaceous; Campos Basin |
topic |
Palynology; Paleoenvironment; Cretaceous; Campos Basin |
description |
A detailed palynological analysis was conducted on 29 samples obtained from the Cretaceous interval of the well Campos-01, drilled in the Northern portion of the offshore Campos Basin. The main objectives of this study were to precise the age the rocks and to perform an analysis and interpretation of the depositional environment of the interval. The material consists of mainly shales, marls, calcareous mudstones and sandstones deposited in a deep marine environment. The palynological analysis consisted on identification and counting of all palynomorphs. The paleoenvironmental and paleoecological investigations were supported by cluster analysis, ecological indices (e.g. diversity, dominance) and ratios (e.g. continental:marine) were used. A total of 97 taxa was identified, which included 46 genera of dinoflagellates cysts, 25 genera of spores, 21 genera of pollen grains, 2 genera of freshwater algae and microforaminiferal linings. The recorded assemblage (e.g. Trichodinium castanea, Dinogymnium acuminatum, Zlivisporis blanensis) was assigned to a late Campanian—late Maastrichtian age for the studied section. The interval is clearly dominated by the dinoflagellate cysts that reach 90.7% of total of palynomorphs. On the basis of cluster analysis (r-mode) three dinoflagellate associations were recognized: Systematophora, Areoligera and Spiniferites. The stratigraphic distribution of dinoflagellates associations indicates three intervals (I1-I3). The intervals I1 and I2, dominated by Systematophora and Spiniferites respectively, are interpreted as open marine environment. In the interval I3, the dominance of Areoligera Association indicates a nearshore environment, also supported by the large amount of continental elements, including the genus Callialasporites, which is attributed to high altitude flora, suggesting the presence of highland feeding areas. |
publishDate |
2019 |
dc.date.none.fl_str_mv |
2019-09-09 |
dc.type.none.fl_str_mv |
|
dc.type.driver.fl_str_mv |
info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion |
format |
article |
status_str |
publishedVersion |
dc.identifier.uri.fl_str_mv |
https://revistas.ufrj.br/index.php/aigeo/article/view/28468 10.11137/2018_2_332_343 |
url |
https://revistas.ufrj.br/index.php/aigeo/article/view/28468 |
identifier_str_mv |
10.11137/2018_2_332_343 |
dc.language.iso.fl_str_mv |
eng |
language |
eng |
dc.relation.none.fl_str_mv |
https://revistas.ufrj.br/index.php/aigeo/article/view/28468/15499 |
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 41, No 2 (2018); 332-343 Anuário do Instituto de Geociências; Vol 41, No 2 (2018); 332-343 1982-3908 0101-9759 reponame:Anuário do Instituto de Geociências (Online) instname:Universidade Federal do Rio de Janeiro (UFRJ) instacron:UFRJ |
instname_str |
Universidade Federal do Rio de Janeiro (UFRJ) |
instacron_str |
UFRJ |
institution |
UFRJ |
reponame_str |
Anuário do Instituto de Geociências (Online) |
collection |
Anuário do Instituto de Geociências (Online) |
repository.name.fl_str_mv |
Anuário do Instituto de Geociências (Online) - Universidade Federal do Rio de Janeiro (UFRJ) |
repository.mail.fl_str_mv |
anuario@igeo.ufrj.br|| |
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1797053544603320320 |