Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography

Autores
Bijl, Peter K.; Pross, Jörg; Warnaar, Jeroen; Stickley, Catherine E.; Huber, Matthew; Guerstein, Gladys Raquel; Houben, Alexander J. P.; Sluijs, Appy; Visscher, Henk; Brinkhuis, Henk
Año de publicación
2011
Idioma
inglés
Tipo de recurso
artículo
Estado
versión publicada
Descripción
Despite warm polar climates and low meridional temperature gradients, a number of different high-latitude plankton assemblages were, to varying extents, dominated by endemic species during most of the Paleogene. To better understand the evolution of Paleogene plankton endemism in the high southern latitudes, we investigate the spatiotemporal distribution of the fossil remains of dinoflagellates, i.e., organic-walled cysts (dinocysts), and their response to changes in regional sea surface temperature (SST). We show that Paleocene and early Eocene (∼65-50 Ma) Southern Ocean dinocyst assemblages were largely cosmopolitan in nature but that a distinct switch from cosmopolitan-dominated to endemic-dominated assemblages (the so-called "transantarctic flora") occurred around the early-middle Eocene boundary (∼50 Ma). The spatial distribution and relative abundance patterns of this transantarctic flora correspond well with surface water circulation patterns as reconstructed through general circulation model experiments throughout the Eocene. We quantitatively compare dinocyst assemblages with previously published TEX86-based SST reconstructions through the early and middle Eocene from a key locality in the southwest Pacific Ocean, ODP Leg 189 Site 1172 on the East Tasman Plateau. We conclude that the middle Eocene onset of the proliferation of the transantarctic flora is not linearly correlated with regional SST records and that only after the transantarctic flora became fully established later in the middle Eocene, possibly triggered by large-scale changes in surface-ocean nutrient availability, were abundances of endemic dinocysts modulated by regional SST variations.
Fil: Bijl, Peter K.. Utrecht University; Países Bajos
Fil: Pross, Jörg. Goethe Universitat Frankfurt; Alemania
Fil: Warnaar, Jeroen. Utrecht University; Países Bajos
Fil: Stickley, Catherine E.. University Of Norway; Noruega
Fil: Huber, Matthew. Purdue University; Estados Unidos
Fil: Guerstein, Gladys Raquel. Universidad Nacional del Sur; Argentina. 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: Houben, Alexander J. P.. University of Utrecht; Países Bajos
Fil: Sluijs, Appy. Utrecht University; Países Bajos
Fil: Visscher, Henk. Utrecht University; Países Bajos
Fil: Brinkhuis, Henk. Utrecht University; Países Bajos
Materia
dinoflagellate cysts
Paleogene
Paleoceanography
Paleoproductivity
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:11336/73207
Acceder
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oai_identifier_str oai:ri.conicet.gov.ar:11336/73207
network_acronym_str CONICETDig
repository_id_str 3498
network_name_str CONICET Digital (CONICET)
spelling Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeographyBijl, Peter K.Pross, JörgWarnaar, JeroenStickley, Catherine E.Huber, MatthewGuerstein, Gladys RaquelHouben, Alexander J. P.Sluijs, AppyVisscher, HenkBrinkhuis, Henkdinoflagellate cystsPaleogenePaleoceanographyPaleoproductivityhttps://purl.org/becyt/ford/1.5https://purl.org/becyt/ford/1Despite warm polar climates and low meridional temperature gradients, a number of different high-latitude plankton assemblages were, to varying extents, dominated by endemic species during most of the Paleogene. To better understand the evolution of Paleogene plankton endemism in the high southern latitudes, we investigate the spatiotemporal distribution of the fossil remains of dinoflagellates, i.e., organic-walled cysts (dinocysts), and their response to changes in regional sea surface temperature (SST). We show that Paleocene and early Eocene (∼65-50 Ma) Southern Ocean dinocyst assemblages were largely cosmopolitan in nature but that a distinct switch from cosmopolitan-dominated to endemic-dominated assemblages (the so-called "transantarctic flora") occurred around the early-middle Eocene boundary (∼50 Ma). The spatial distribution and relative abundance patterns of this transantarctic flora correspond well with surface water circulation patterns as reconstructed through general circulation model experiments throughout the Eocene. We quantitatively compare dinocyst assemblages with previously published TEX86-based SST reconstructions through the early and middle Eocene from a key locality in the southwest Pacific Ocean, ODP Leg 189 Site 1172 on the East Tasman Plateau. We conclude that the middle Eocene onset of the proliferation of the transantarctic flora is not linearly correlated with regional SST records and that only after the transantarctic flora became fully established later in the middle Eocene, possibly triggered by large-scale changes in surface-ocean nutrient availability, were abundances of endemic dinocysts modulated by regional SST variations.Fil: Bijl, Peter K.. Utrecht University; Países BajosFil: Pross, Jörg. Goethe Universitat Frankfurt; AlemaniaFil: Warnaar, Jeroen. Utrecht University; Países BajosFil: Stickley, Catherine E.. University Of Norway; NoruegaFil: Huber, Matthew. Purdue University; Estados UnidosFil: Guerstein, Gladys Raquel. Universidad Nacional del Sur; Argentina. 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: Houben, Alexander J. P.. University of Utrecht; Países BajosFil: Sluijs, Appy. Utrecht University; Países BajosFil: Visscher, Henk. Utrecht University; Países BajosFil: Brinkhuis, Henk. Utrecht University; Países BajosAmerican Geophysical Union2011-03-04info:eu-repo/semantics/articleinfo:eu-repo/semantics/publishedVersionhttp://purl.org/coar/resource_type/c_6501info:ar-repo/semantics/articuloapplication/pdfapplication/pdfhttp://hdl.handle.net/11336/73207Bijl, Peter K.; Pross, Jörg; Warnaar, Jeroen; Stickley, Catherine E.; Huber, Matthew; et al.; Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography; American Geophysical Union; Paleoceanography; 26; 1; 4-3-2011; 1-120883-8305CONICET DigitalCONICETenginfo:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2009PA001905info:eu-repo/semantics/altIdentifier/doi/10.1029/2009PA001905info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/2.5/ar/reponame:CONICET Digital (CONICET)instname:Consejo Nacional de Investigaciones Científicas y Técnicas2025-09-03T10:04:17Zoai:ri.conicet.gov.ar:11336/73207instacron: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:34982025-09-03 10:04:17.484CONICET Digital (CONICET) - Consejo Nacional de Investigaciones Científicas y Técnicasfalse
dc.title.none.fl_str_mv Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
title Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
spellingShingle Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
Bijl, Peter K.
dinoflagellate cysts
Paleogene
Paleoceanography
Paleoproductivity
title_short Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
title_full Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
title_fullStr Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
title_full_unstemmed Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
title_sort Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography
dc.creator.none.fl_str_mv Bijl, Peter K.
Pross, Jörg
Warnaar, Jeroen
Stickley, Catherine E.
Huber, Matthew
Guerstein, Gladys Raquel
Houben, Alexander J. P.
Sluijs, Appy
Visscher, Henk
Brinkhuis, Henk
author Bijl, Peter K.
author_facet Bijl, Peter K.
Pross, Jörg
Warnaar, Jeroen
Stickley, Catherine E.
Huber, Matthew
Guerstein, Gladys Raquel
Houben, Alexander J. P.
Sluijs, Appy
Visscher, Henk
Brinkhuis, Henk
author_role author
author2 Pross, Jörg
Warnaar, Jeroen
Stickley, Catherine E.
Huber, Matthew
Guerstein, Gladys Raquel
Houben, Alexander J. P.
Sluijs, Appy
Visscher, Henk
Brinkhuis, Henk
author2_role author
author
author
author
author
author
author
author
author
dc.subject.none.fl_str_mv dinoflagellate cysts
Paleogene
Paleoceanography
Paleoproductivity
topic dinoflagellate cysts
Paleogene
Paleoceanography
Paleoproductivity
purl_subject.fl_str_mv https://purl.org/becyt/ford/1.5
https://purl.org/becyt/ford/1
dc.description.none.fl_txt_mv Despite warm polar climates and low meridional temperature gradients, a number of different high-latitude plankton assemblages were, to varying extents, dominated by endemic species during most of the Paleogene. To better understand the evolution of Paleogene plankton endemism in the high southern latitudes, we investigate the spatiotemporal distribution of the fossil remains of dinoflagellates, i.e., organic-walled cysts (dinocysts), and their response to changes in regional sea surface temperature (SST). We show that Paleocene and early Eocene (∼65-50 Ma) Southern Ocean dinocyst assemblages were largely cosmopolitan in nature but that a distinct switch from cosmopolitan-dominated to endemic-dominated assemblages (the so-called "transantarctic flora") occurred around the early-middle Eocene boundary (∼50 Ma). The spatial distribution and relative abundance patterns of this transantarctic flora correspond well with surface water circulation patterns as reconstructed through general circulation model experiments throughout the Eocene. We quantitatively compare dinocyst assemblages with previously published TEX86-based SST reconstructions through the early and middle Eocene from a key locality in the southwest Pacific Ocean, ODP Leg 189 Site 1172 on the East Tasman Plateau. We conclude that the middle Eocene onset of the proliferation of the transantarctic flora is not linearly correlated with regional SST records and that only after the transantarctic flora became fully established later in the middle Eocene, possibly triggered by large-scale changes in surface-ocean nutrient availability, were abundances of endemic dinocysts modulated by regional SST variations.
Fil: Bijl, Peter K.. Utrecht University; Países Bajos
Fil: Pross, Jörg. Goethe Universitat Frankfurt; Alemania
Fil: Warnaar, Jeroen. Utrecht University; Países Bajos
Fil: Stickley, Catherine E.. University Of Norway; Noruega
Fil: Huber, Matthew. Purdue University; Estados Unidos
Fil: Guerstein, Gladys Raquel. Universidad Nacional del Sur; Argentina. 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: Houben, Alexander J. P.. University of Utrecht; Países Bajos
Fil: Sluijs, Appy. Utrecht University; Países Bajos
Fil: Visscher, Henk. Utrecht University; Países Bajos
Fil: Brinkhuis, Henk. Utrecht University; Países Bajos
description Despite warm polar climates and low meridional temperature gradients, a number of different high-latitude plankton assemblages were, to varying extents, dominated by endemic species during most of the Paleogene. To better understand the evolution of Paleogene plankton endemism in the high southern latitudes, we investigate the spatiotemporal distribution of the fossil remains of dinoflagellates, i.e., organic-walled cysts (dinocysts), and their response to changes in regional sea surface temperature (SST). We show that Paleocene and early Eocene (∼65-50 Ma) Southern Ocean dinocyst assemblages were largely cosmopolitan in nature but that a distinct switch from cosmopolitan-dominated to endemic-dominated assemblages (the so-called "transantarctic flora") occurred around the early-middle Eocene boundary (∼50 Ma). The spatial distribution and relative abundance patterns of this transantarctic flora correspond well with surface water circulation patterns as reconstructed through general circulation model experiments throughout the Eocene. We quantitatively compare dinocyst assemblages with previously published TEX86-based SST reconstructions through the early and middle Eocene from a key locality in the southwest Pacific Ocean, ODP Leg 189 Site 1172 on the East Tasman Plateau. We conclude that the middle Eocene onset of the proliferation of the transantarctic flora is not linearly correlated with regional SST records and that only after the transantarctic flora became fully established later in the middle Eocene, possibly triggered by large-scale changes in surface-ocean nutrient availability, were abundances of endemic dinocysts modulated by regional SST variations.
publishDate 2011
dc.date.none.fl_str_mv 2011-03-04
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/11336/73207
Bijl, Peter K.; Pross, Jörg; Warnaar, Jeroen; Stickley, Catherine E.; Huber, Matthew; et al.; Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography; American Geophysical Union; Paleoceanography; 26; 1; 4-3-2011; 1-12
0883-8305
CONICET Digital
CONICET
url http://hdl.handle.net/11336/73207
identifier_str_mv Bijl, Peter K.; Pross, Jörg; Warnaar, Jeroen; Stickley, Catherine E.; Huber, Matthew; et al.; Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography; American Geophysical Union; Paleoceanography; 26; 1; 4-3-2011; 1-12
0883-8305
CONICET Digital
CONICET
dc.language.none.fl_str_mv eng
language eng
dc.relation.none.fl_str_mv info:eu-repo/semantics/altIdentifier/url/https://agupubs.onlinelibrary.wiley.com/doi/10.1029/2009PA001905
info:eu-repo/semantics/altIdentifier/doi/10.1029/2009PA001905
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 American Geophysical Union
publisher.none.fl_str_mv American Geophysical Union
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 13.13397

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