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

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...

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Published in:Review of Palaeobotany and Palynology
Main Authors: Houben, Alexander J. P., Bijl, Peter K., Guerstein, Gladys Raquel, Sluijs, Appy, Brinkhuis, Henk
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier Science
Subjects:
Online Access:http://hdl.handle.net/11336/73205
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author Houben, Alexander J. P.
Bijl, Peter K.
Guerstein, Gladys Raquel
Sluijs, Appy
Brinkhuis, Henk
author_facet Houben, Alexander J. P.
Bijl, Peter K.
Guerstein, Gladys Raquel
Sluijs, Appy
Brinkhuis, Henk
author_sort Houben, Alexander J. P.
collection CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas)
container_issue 3-4
container_start_page 175
container_title Review of Palaeobotany and Palynology
container_volume 165
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. 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
format Article in Journal/Newspaper
genre Antarc*
Antarctic
Southern Ocean
genre_facet Antarc*
Antarctic
Southern Ocean
geographic Antarctic
Southern Ocean
Argentina
Bajos
geographic_facet Antarctic
Southern Ocean
Argentina
Bajos
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spelling ftconicet:oai:ri.conicet.gov.ar:11336/73205 2025-01-16T19:35:19+00:00 Malvinia escutiana, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean Houben, Alexander J. P. Bijl, Peter K. Guerstein, Gladys Raquel Sluijs, Appy Brinkhuis, Henk application/pdf http://hdl.handle.net/11336/73205 eng eng Elsevier Science 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 http://hdl.handle.net/11336/73205 CONICET Digital CONICET info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ Antarctic Glaciation Dinoflagellate Cysts Eocene Oligocene Peridinioid Southern Ocean https://purl.org/becyt/ford/1.5 https://purl.org/becyt/ford/1 info:eu-repo/semantics/article info:ar-repo/semantics/artículo info:eu-repo/semantics/publishedVersion ftconicet https://doi.org/10.1016/j.revpalbo.2011.03.002 2024-10-04T09:34:04Z 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 Article in Journal/Newspaper Antarc* Antarctic Southern Ocean CONICET Digital (Consejo Nacional de Investigaciones Científicas y Técnicas) Antarctic Southern Ocean Argentina Bajos ENVELOPE(-56.317,-56.317,-63.467,-63.467) Review of Palaeobotany and Palynology 165 3-4 175 182
spellingShingle Antarctic Glaciation
Dinoflagellate Cysts
Eocene
Oligocene
Peridinioid
Southern Ocean
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
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
title 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_short 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
topic Antarctic Glaciation
Dinoflagellate Cysts
Eocene
Oligocene
Peridinioid
Southern Ocean
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
topic_facet Antarctic Glaciation
Dinoflagellate Cysts
Eocene
Oligocene
Peridinioid
Southern Ocean
https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
url http://hdl.handle.net/11336/73205