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
- Institución
- Consejo Nacional de Investigaciones Científicas y Técnicas
- OAI Identificador
- oai:ri.conicet.gov.ar:11336/73205
Ver los metadatos del registro completo
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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 Técnicas2025-09-29T09:36:11Zoai: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:34982025-09-29 09:36:12.067CONICET 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 |
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CONICET Digital (CONICET) |
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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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1844613132850298880 |
score |
13.070432 |