Deep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currents

dc.citation.journalTitleBoletin De Investigaciones Marinas Y Costeras
dc.contributor.authorPatarroyo, Germanspa
dc.contributor.authorIgnacio Martinez, J.spa
dc.contributor.departmentUniversidad EAFIT. Departamento de Geologíaspa
dc.contributor.researchgroupCiencias del Marspa
dc.date.accessioned2021-03-23T20:20:28Z
dc.date.available2021-03-23T20:20:28Z
dc.date.issued2013-02-01
dc.description.abstractDeep 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.eng
dc.identifierhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=5681
dc.identifier.doi10.1029/2005PA001208
dc.identifier.issn01229761
dc.identifier.otherSCOPUS;2-s2.0-84963758616
dc.identifier.urihttp://hdl.handle.net/10784/26913
dc.language.isospaeng
dc.publisherInstituto de Ivestigaciones Marinas y Costeras-INVEMAR
dc.relation.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-84963758616&doi=10.1029%2f2005PA001208&partnerID=40&md5=0a19b7c9c47a278e01334457c6948241
dc.relation.urihttp://boletin.invemar.org.co/ojs/index.php/boletin/article/view/58
dc.rightshttps://v2.sherpa.ac.uk/id/publication/issn/0122-9761
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesseng
dc.rights.localAcceso abiertospa
dc.sourceBoletin De Investigaciones Marinas Y Costeras
dc.subject.keywordDeep sea bottom currentseng
dc.subject.keywordEcologyeng
dc.subject.keywordPanama basineng
dc.subject.keywordRecent benthic foraminiferaeng
dc.titleDeep sea benthic foraminifera of the Panama basin: Ecology and their possible relation with deep sea currentseng
dc.typeinfo:eu-repo/semantics/articleeng
dc.typearticleeng
dc.typeinfo:eu-repo/semantics/publishedVersioneng
dc.typepublishedVersioneng
dc.type.localArtículospa

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