Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean

Autores
Houben, Alexander J. P.; Bijl, Peter K.; Guerstein, Gladys Raquel; Sluijs, Appy; Brinkhuis, Henk
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
The Eocene-Oligocene Transition (EOT, ~. 34. Ma) represents the culmination of Eocene cooling by the initiation of large-scale Antarctic glaciation. Recognition and correlation of the EOT in Southern Ocean sedimentary successions have been difficult as a result of the general lack of well-calibrated biostratigraphic markers. Here we describe an unusual hypnozygotic organic walled dinoflagellate cyst (dinocyst) that originated in the Southern Ocean in conjunction with the onset of major Antarctic glaciation as reflected by 'oxygen isotope event 1' (Oi-1).We restudied samples from Deep Sea Drilling Program (DSDP) Site 511 using Light Microscopy and Scanning Electron Microscopy and found that a taxon previously known as Forma T constitutes a new protoperidinioid dinocyst genus and species that we name Malvinia escutiana. Published and re-evaluated data from other Southern Ocean sites show that M. escutiana did not occur before the Oi-1 (33.7. Ma), emphasizing its potential as a useful biostratigraphic marker for this key interval in the Southern Ocean's Cenozoic climate history.
Fil: Houben, Alexander J. P.. Utrecht University; Países Bajos
Fil: Bijl, Peter K.. Utrecht University; Países Bajos
Fil: Guerstein, Gladys Raquel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Sluijs, Appy. Utrecht University; Países Bajos
Fil: Brinkhuis, Henk. Utrecht University; Países Bajos
Materia
Antarctic Glaciation
Dinoflagellate Cysts
Eocene
Oligocene
Peridinioid
Southern Ocean
Nivel de accesibilidad
acceso abierto
Condiciones de uso
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
Repositorio
CONICET Digital (CONICET)
Institución
Consejo Nacional de Investigaciones Científicas y Técnicas
OAI Identificador
oai:ri.conicet.gov.ar:11336/73205
Acceder
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repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern OceanHouben, Alexander J. P.Bijl, Peter K.Guerstein, Gladys RaquelSluijs, AppyBrinkhuis, HenkAntarctic GlaciationDinoflagellate CystsEoceneOligocenePeridinioidSouthern Oceanhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1The Eocene-Oligocene Transition (EOT, ~. 34. Ma) represents the culmination of Eocene cooling by the initiation of large-scale Antarctic glaciation. Recognition and correlation of the EOT in Southern Ocean sedimentary successions have been difficult as a result of the general lack of well-calibrated biostratigraphic markers. Here we describe an unusual hypnozygotic organic walled dinoflagellate cyst (dinocyst) that originated in the Southern Ocean in conjunction with the onset of major Antarctic glaciation as reflected by 'oxygen isotope event 1' (Oi-1).We restudied samples from Deep Sea Drilling Program (DSDP) Site 511 using Light Microscopy and Scanning Electron Microscopy and found that a taxon previously known as Forma T constitutes a new protoperidinioid dinocyst genus and species that we name Malvinia escutiana. Published and re-evaluated data from other Southern Ocean sites show that M. escutiana did not occur before the Oi-1 (33.7. Ma), emphasizing its potential as a useful biostratigraphic marker for this key interval in the Southern Ocean's Cenozoic climate history.Fil: Houben, Alexander J. P.. Utrecht University; Países BajosFil: Bijl, Peter K.. Utrecht University; Países BajosFil: Guerstein, Gladys Raquel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; ArgentinaFil: Sluijs, Appy. Utrecht University; Países BajosFil: Brinkhuis, Henk. Utrecht University; Países BajosElsevier Science2011-06info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/73205Houben, Alexander J. P.; Bijl, Peter K.; Guerstein, Gladys Raquel; Sluijs, Appy; Brinkhuis, Henk; Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean; Elsevier Science; Review of Palaeobotany and Palynology; 165; 3-4; 6-2011; 175-1820034-6667CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0034666711000340info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2011.03.002info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-10-22T11:04:15Zoai:ri.conicet.gov.ar:11336/73205instacron:CONICETInstitucionalhttp://ri.conicet.gov.ar/Organismo científico-tecnológicoNo correspondehttp://ri.conicet.gov.ar/oai/requestdasensio@conicet.gov.ar; lcarlino@conicet.gov.arArgentinaNo correspondeNo correspondeNo correspondeopendoar:34982025-10-22 11:04:16.196CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
title Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
spellingShingle Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
Houben, Alexander J. P.
Antarctic Glaciation
Dinoflagellate Cysts
Eocene
Oligocene
Peridinioid
Southern Ocean
title_short Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
title_full Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
title_fullStr Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
title_full_unstemmed Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
title_sort Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean
dc.creator.none.fl_str_mv Houben, Alexander J. P.
Bijl, Peter K.
Guerstein, Gladys Raquel
Sluijs, Appy
Brinkhuis, Henk
author Houben, Alexander J. P.
author_facet Houben, Alexander J. P.
Bijl, Peter K.
Guerstein, Gladys Raquel
Sluijs, Appy
Brinkhuis, Henk
author_role author
author2 Bijl, Peter K.
Guerstein, Gladys Raquel
Sluijs, Appy
Brinkhuis, Henk
author2_role author
author
author
author
dc.subject.none.fl_str_mv Antarctic Glaciation
Dinoflagellate Cysts
Eocene
Oligocene
Peridinioid
Southern Ocean
topic Antarctic Glaciation
Dinoflagellate Cysts
Eocene
Oligocene
Peridinioid
Southern Ocean
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv The Eocene-Oligocene Transition (EOT, ~. 34. Ma) represents the culmination of Eocene cooling by the initiation of large-scale Antarctic glaciation. Recognition and correlation of the EOT in Southern Ocean sedimentary successions have been difficult as a result of the general lack of well-calibrated biostratigraphic markers. Here we describe an unusual hypnozygotic organic walled dinoflagellate cyst (dinocyst) that originated in the Southern Ocean in conjunction with the onset of major Antarctic glaciation as reflected by 'oxygen isotope event 1' (Oi-1).We restudied samples from Deep Sea Drilling Program (DSDP) Site 511 using Light Microscopy and Scanning Electron Microscopy and found that a taxon previously known as Forma T constitutes a new protoperidinioid dinocyst genus and species that we name Malvinia escutiana. Published and re-evaluated data from other Southern Ocean sites show that M. escutiana did not occur before the Oi-1 (33.7. Ma), emphasizing its potential as a useful biostratigraphic marker for this key interval in the Southern Ocean's Cenozoic climate history.
Fil: Houben, Alexander J. P.. Utrecht University; Países Bajos
Fil: Bijl, Peter K.. Utrecht University; Países Bajos
Fil: Guerstein, Gladys Raquel. Consejo Nacional de Investigaciones Científicas y Técnicas. Centro Científico Tecnológico Conicet - Bahía Blanca. Instituto Geológico del Sur. Universidad Nacional del Sur. Departamento de Geología. Instituto Geológico del Sur; Argentina
Fil: Sluijs, Appy. Utrecht University; Países Bajos
Fil: Brinkhuis, Henk. Utrecht University; Países Bajos
description The Eocene-Oligocene Transition (EOT, ~. 34. Ma) represents the culmination of Eocene cooling by the initiation of large-scale Antarctic glaciation. Recognition and correlation of the EOT in Southern Ocean sedimentary successions have been difficult as a result of the general lack of well-calibrated biostratigraphic markers. Here we describe an unusual hypnozygotic organic walled dinoflagellate cyst (dinocyst) that originated in the Southern Ocean in conjunction with the onset of major Antarctic glaciation as reflected by 'oxygen isotope event 1' (Oi-1).We restudied samples from Deep Sea Drilling Program (DSDP) Site 511 using Light Microscopy and Scanning Electron Microscopy and found that a taxon previously known as Forma T constitutes a new protoperidinioid dinocyst genus and species that we name Malvinia escutiana. Published and re-evaluated data from other Southern Ocean sites show that M. escutiana did not occur before the Oi-1 (33.7. Ma), emphasizing its potential as a useful biostratigraphic marker for this key interval in the Southern Ocean's Cenozoic climate history.
publishDate 2011
dc.date.none.fl_str_mv 2011-06
dc.type.none.fl_str_mv info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
http://purl.org/coar/resource_type/c_6501
info:ar-repo/semantics/articulo
format article
status_str publishedVersion
dc.identifier.none.fl_str_mv http://hdl.handle.net/11336/73205
Houben, Alexander J. P.; Bijl, Peter K.; Guerstein, Gladys Raquel; Sluijs, Appy; Brinkhuis, Henk; Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean; Elsevier Science; Review of Palaeobotany and Palynology; 165; 3-4; 6-2011; 175-182
0034-6667
CONICET Digital
CONICET
url http://hdl.handle.net/11336/73205
identifier_str_mv Houben, Alexander J. P.; Bijl, Peter K.; Guerstein, Gladys Raquel; Sluijs, Appy; Brinkhuis, Henk; Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean; Elsevier Science; Review of Palaeobotany and Palynology; 165; 3-4; 6-2011; 175-182
0034-6667
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/http://www.sciencedirect.com/science/article/pii/S0034666711000340
info:eu-repo/semantics/altIdentifier/doi/10.1016/j.revpalbo.2011.03.002
dc.rights.none.fl_str_mv info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-sa/2.5/ar/
dc.format.none.fl_str_mv application/pdf
application/pdf
dc.publisher.none.fl_str_mv Elsevier Science
publisher.none.fl_str_mv Elsevier Science
dc.source.none.fl_str_mv reponame:CONICET Digital (CONICET)
instname:Consejo Nacional de Investigaciones Científicas y Técnicas
reponame_str CONICET Digital (CONICET)
collection CONICET Digital (CONICET)
instname_str Consejo Nacional de Investigaciones Científicas y Técnicas
repository.name.fl_str_mv CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicas
repository.mail.fl_str_mv dasensio@conicet.gov.ar; lcarlino@conicet.gov.ar
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score 12.982451

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