Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents
Deep sea benthic foraminifera of the Panama basin: ecology and their possible relation with deep sea currents. The relationship between recent benthic foraminifera and bottom currents in the Panama basin (Colombian Pacific) is examined, and the main ecological variables which control the distributio...
- Autores:
-
Patarroyo, German
Ignacio Martinez, J.
- Tipo de recurso:
- Fecha de publicación:
- 2013
- Institución:
- Universidad EAFIT
- Repositorio:
- Repositorio EAFIT
- Idioma:
- spa
- OAI Identifier:
- oai:repository.eafit.edu.co:10784/26913
- Acceso en línea:
- https://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=5681
http://hdl.handle.net/10784/26913
- Palabra clave:
- Deep sea bottom currents
Ecology
Panama basin
Recent benthic foraminifera
- Rights
- License
- https://v2.sherpa.ac.uk/id/publication/issn/0122-9761
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2021-03-23T20:20:28Z2013-02-012021-03-23T20:20:28Zhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=568101229761SCOPUS;2-s2.0-84963758616http://hdl.handle.net/10784/2691310.1029/2005PA001208Deep sea benthic foraminifera of the Panama basin: ecology and their possible relation with deep sea currents. The relationship between recent benthic foraminifera and bottom currents in the Panama basin (Colombian Pacific) is examined, and the main ecological variables which control the distribution of benthic foraminifera are discussed. The benthic foraminiferal study of 24 core top samples and the integration with previous reports, support the view that in upwelling areas or under high terrigenous influx, the assemblages are dominated by infaunal forms such as Uvigerina, Bolivina, Globobulimina, and Chilostomella, beside common forms such as Uvigerina peregrina Cushman and Epistominella spp., which are indicative of high productivity. In contrast, epifaunal forms such as Cibicidoides, Laticarinina, and Hoeglundina are more common on the flanks of the Cocos and CarnegieRidges indicating a lower surface productivity and a larger content of dissolved oxygen on the sea foor. Infaunal foraminifera are dominated by Siphouvigerina proboscidea (Schwager). In addition, several proxy taxa of the intensity of deep sea currents were detected in the analyzed assemblages. From these taxa, Cibicides wuellerstorf (Schwager) has the best proxy potential for the reconstruction of intense bottom currents in sediments from the Cocos and Carnegie Ridges for the Holocene.spaInstituto de Ivestigaciones Marinas y Costeras-INVEMARhttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84963758616&doi=10.1029%2f2005PA001208&partnerID=40&md5=0a19b7c9c47a278e01334457c6948241http://boletin.invemar.org.co/ojs/index.php/boletin/article/view/58https://v2.sherpa.ac.uk/id/publication/issn/0122-9761Acceso abiertohttp://purl.org/coar/access_right/c_abf2Boletin De Investigaciones Marinas Y CosterasDeep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currentsinfo:eu-repo/semantics/articlearticleinfo:eu-repo/semantics/publishedVersionpublishedVersionArtículohttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_6501http://purl.org/coar/resource_type/c_2df8fbb1Deep sea bottom currentsEcologyPanama basinRecent benthic foraminiferaUniversidad EAFIT. Departamento de GeologíaPatarroyo, GermanIgnacio Martinez, J.Ciencias del MarBoletin De Investigaciones Marinas Y CosterasORIGINALAdministrador,+58-221-1-CE.pdfAdministrador,+58-221-1-CE.pdfTexto completoapplication/pdf1931373https://repository.eafit.edu.co/bitstreams/c774588e-2a74-45ea-9d2e-d48052c410b2/download250fc0a0c6b0b5b096fca48414f7fe6fMD5110784/26913oai:repository.eafit.edu.co:10784/269132023-02-28 14:22:09.135open.accesshttps://repository.eafit.edu.coRepositorio Institucional Universidad EAFITrepositorio@eafit.edu.co |
dc.title.eng.fl_str_mv |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents |
title |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents |
spellingShingle |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents Deep sea bottom currents Ecology Panama basin Recent benthic foraminifera |
title_short |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents |
title_full |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents |
title_fullStr |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents |
title_full_unstemmed |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents |
title_sort |
Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents |
dc.creator.fl_str_mv |
Patarroyo, German Ignacio Martinez, J. |
dc.contributor.department.spa.fl_str_mv |
Universidad EAFIT. Departamento de Geología |
dc.contributor.author.spa.fl_str_mv |
Patarroyo, German Ignacio Martinez, J. |
dc.contributor.researchgroup.spa.fl_str_mv |
Ciencias del Mar |
dc.subject.keyword.eng.fl_str_mv |
Deep sea bottom currents Ecology Panama basin Recent benthic foraminifera |
topic |
Deep sea bottom currents Ecology Panama basin Recent benthic foraminifera |
description |
Deep sea benthic foraminifera of the Panama basin: ecology and their possible relation with deep sea currents. The relationship between recent benthic foraminifera and bottom currents in the Panama basin (Colombian Pacific) is examined, and the main ecological variables which control the distribution of benthic foraminifera are discussed. The benthic foraminiferal study of 24 core top samples and the integration with previous reports, support the view that in upwelling areas or under high terrigenous influx, the assemblages are dominated by infaunal forms such as Uvigerina, Bolivina, Globobulimina, and Chilostomella, beside common forms such as Uvigerina peregrina Cushman and Epistominella spp., which are indicative of high productivity. In contrast, epifaunal forms such as Cibicidoides, Laticarinina, and Hoeglundina are more common on the flanks of the Cocos and CarnegieRidges indicating a lower surface productivity and a larger content of dissolved oxygen on the sea foor. Infaunal foraminifera are dominated by Siphouvigerina proboscidea (Schwager). In addition, several proxy taxa of the intensity of deep sea currents were detected in the analyzed assemblages. From these taxa, Cibicides wuellerstorf (Schwager) has the best proxy potential for the reconstruction of intense bottom currents in sediments from the Cocos and Carnegie Ridges for the Holocene. |
publishDate |
2013 |
dc.date.issued.none.fl_str_mv |
2013-02-01 |
dc.date.available.none.fl_str_mv |
2021-03-23T20:20:28Z |
dc.date.accessioned.none.fl_str_mv |
2021-03-23T20:20:28Z |
dc.type.eng.fl_str_mv |
info:eu-repo/semantics/article article info:eu-repo/semantics/publishedVersion publishedVersion |
dc.type.coarversion.fl_str_mv |
http://purl.org/coar/version/c_970fb48d4fbd8a85 |
dc.type.coar.fl_str_mv |
http://purl.org/coar/resource_type/c_6501 http://purl.org/coar/resource_type/c_2df8fbb1 |
dc.type.local.spa.fl_str_mv |
Artículo |
status_str |
publishedVersion |
dc.identifier.none.fl_str_mv |
https://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=5681 |
dc.identifier.issn.none.fl_str_mv |
01229761 |
dc.identifier.other.none.fl_str_mv |
SCOPUS;2-s2.0-84963758616 |
dc.identifier.uri.none.fl_str_mv |
http://hdl.handle.net/10784/26913 |
dc.identifier.doi.none.fl_str_mv |
10.1029/2005PA001208 |
url |
https://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=5681 http://hdl.handle.net/10784/26913 |
identifier_str_mv |
01229761 SCOPUS;2-s2.0-84963758616 10.1029/2005PA001208 |
dc.language.iso.eng.fl_str_mv |
spa |
language |
spa |
dc.relation.uri.none.fl_str_mv |
https://www.scopus.com/inward/record.uri?eid=2-s2.0-84963758616&doi=10.1029%2f2005PA001208&partnerID=40&md5=0a19b7c9c47a278e01334457c6948241 http://boletin.invemar.org.co/ojs/index.php/boletin/article/view/58 |
dc.rights.none.fl_str_mv |
https://v2.sherpa.ac.uk/id/publication/issn/0122-9761 |
dc.rights.coar.fl_str_mv |
http://purl.org/coar/access_right/c_abf2 |
dc.rights.local.spa.fl_str_mv |
Acceso abierto |
rights_invalid_str_mv |
https://v2.sherpa.ac.uk/id/publication/issn/0122-9761 Acceso abierto http://purl.org/coar/access_right/c_abf2 |
dc.publisher.none.fl_str_mv |
Instituto de Ivestigaciones Marinas y Costeras-INVEMAR |
publisher.none.fl_str_mv |
Instituto de Ivestigaciones Marinas y Costeras-INVEMAR |
dc.source.none.fl_str_mv |
Boletin De Investigaciones Marinas Y Costeras |
institution |
Universidad EAFIT |
bitstream.url.fl_str_mv |
https://repository.eafit.edu.co/bitstreams/c774588e-2a74-45ea-9d2e-d48052c410b2/download |
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250fc0a0c6b0b5b096fca48414f7fe6f |
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repository.name.fl_str_mv |
Repositorio Institucional Universidad EAFIT |
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repositorio@eafit.edu.co |
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