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...
Published in: | Review of Palaeobotany and Palynology |
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Main Authors: | , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
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Elsevier Science
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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 |
id | ftconicet:oai:ri.conicet.gov.ar:11336/73205 |
institution | Open Polar |
language | English |
long_lat | ENVELOPE(-56.317,-56.317,-63.467,-63.467) |
op_collection_id | ftconicet |
op_container_end_page | 182 |
op_doi | https://doi.org/10.1016/j.revpalbo.2011.03.002 |
op_relation | 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 |
op_rights | info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by-nc-sa/2.5/ar/ |
publisher | Elsevier Science |
record_format | openpolar |
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 |