433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia

The Eocene EsmeraldasFormation isa very importantoil reservoir intheMiddle Magdalena ValleyBasin, Colombia, which is a preduct of the fragmentatienof a Cenozoic forelandbasinby the uplift of the Northem Andes. Ihe lateralcentinuity of the formation,as well as its correlations with lithostratigraphic...

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Fecha de publicación:
2012
Institución:
Universidad del Rosario
Repositorio:
Repositorio EdocUR - U. Rosario
Idioma:
eng
OAI Identifier:
oai:repository.urosario.edu.co:10336/27276
Acceso en línea:
https://doi.org/10.24524/jjpal.58.Special_196_2
https://repository.urosario.edu.co/handle/10336/27276
Palabra clave:
South America
Cenozoic
Ccontinental
Corros
Palynology
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id EDOCUR2_ebef8f2b3a2a3b1b97b7393872023f11
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network_acronym_str EDOCUR2
network_name_str Repositorio EdocUR - U. Rosario
repository_id_str
spelling 15d090b1-1154-4efe-b6d0-c21e42693437-1cefd0e5b-5ef0-4aac-b40f-ab5058caf81f-179d77a02-c1bd-4545-8d0e-0964ecf4d0a9-16bf5be9a-5604-4841-88d0-4124b75c58c8-1882350066002020-08-19T14:41:35Z2020-08-19T14:41:35Z2012The Eocene EsmeraldasFormation isa very importantoil reservoir intheMiddle Magdalena ValleyBasin, Colombia, which is a preduct of the fragmentatienof a Cenozoic forelandbasinby the uplift of the Northem Andes. Ihe lateralcentinuity of the formation,as well as its correlations with lithostratigraphic units inadjacent basins isnot clearly understood. The Los CorrosFossilHorizon,a molluscan horizonin the upper partof the Esmeraldas Formation,has been used to tracethe top of the formation, Thishorizonisnot laterallycontinuous over thebasinand its age is still debatable. Some of the key palynostratigraphic events inNorthernSouth America are net present inthepalynological record of the Esmeraldas, Palynologicaldata from 82 samples from an eutcrop section intheNuevo Mundo Synclinearea and from seven previouslystudied wells have been integratedwith a palynologicalzonation of nonhem South America inorder to datctheEsrneraldasForrnation.The age ranges from the lateEarly Eocene to the Late Eocene. The Esmeraldas Forrnationiscorrelative withthe upper Picacho ForTnation and the lowerpartof the ConcentracionForrnationin the EasternCoTdillera, and theupper Mirador Forrnationand thebaseof theCarboneraFormationintheLlanosFeothills. [[heLos Corros FossilHorizon is Late Eocene and is time-correlative with a marine transgression inthe central Llanos Foothills,A non-menic multidimensional scaling analysis suggests that florasfrom the Middle Magdalena Valleywere differentfromthe Llanos Foothillsarea during the Middle to Late Eocene. This is apparently due to taphonomic effects. The results efthis study conuibute to a betterunderstanding of theoverall evolution ef the Middle Magdalena ValleyBasin and the evolution of thenonhem Andes.application/pdfhttps://doi.org/10.24524/jjpal.58.Special_196_2ISSN: 0387-1851EISSN: 2433-0272https://repository.urosario.edu.co/handle/10336/27276engPalynological Society of Japan197No. Special196Japanese Journal of PalynologyVol. 58Japanese Journal of Palynology, ISSN: 0387-1851;EISSN: 2433-0272, Vol.58, No.Special (2013); pp. 196-197 https://www.jstage.jst.go.jp/article/jjpal/58/Special/58_KJ00008443174/_pdf/-char/enAbierto (Texto Completo)http://purl.org/coar/access_right/c_abf2Japanese Journal of Palynologyinstname:Universidad del Rosarioreponame:Repositorio Institucional EdocURSouth AmericaCenozoicCcontinentalCorrosPalynology433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia433 Palinoestratigrafía de la formación eoceno esmeraldas, Cuenca del Valle del Magdalena Medio, ColombiaarticleArtículohttp://purl.org/coar/version/c_970fb48d4fbd8a85http://purl.org/coar/resource_type/c_6501Rodriguez, GuillermoOboh-Ikuenobe, FranciscaJaramillo, CarlosRueda, MiltonCadena, Edwin Alberto10336/27276oai:repository.urosario.edu.co:10336/272762021-06-03 00:50:09.014https://repository.urosario.edu.coRepositorio institucional EdocURedocur@urosario.edu.co
dc.title.spa.fl_str_mv 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
dc.title.TranslatedTitle.spa.fl_str_mv 433 Palinoestratigrafía de la formación eoceno esmeraldas, Cuenca del Valle del Magdalena Medio, Colombia
title 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
spellingShingle 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
South America
Cenozoic
Ccontinental
Corros
Palynology
title_short 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
title_full 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
title_fullStr 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
title_full_unstemmed 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
title_sort 433 Palynostratigraphy of the eocene esmeraldas formation, middle Magdalena Valley Basin, Colombia
dc.subject.keyword.spa.fl_str_mv South America
Cenozoic
Ccontinental
Corros
Palynology
topic South America
Cenozoic
Ccontinental
Corros
Palynology
description The Eocene EsmeraldasFormation isa very importantoil reservoir intheMiddle Magdalena ValleyBasin, Colombia, which is a preduct of the fragmentatienof a Cenozoic forelandbasinby the uplift of the Northem Andes. Ihe lateralcentinuity of the formation,as well as its correlations with lithostratigraphic units inadjacent basins isnot clearly understood. The Los CorrosFossilHorizon,a molluscan horizonin the upper partof the Esmeraldas Formation,has been used to tracethe top of the formation, Thishorizonisnot laterallycontinuous over thebasinand its age is still debatable. Some of the key palynostratigraphic events inNorthernSouth America are net present inthepalynological record of the Esmeraldas, Palynologicaldata from 82 samples from an eutcrop section intheNuevo Mundo Synclinearea and from seven previouslystudied wells have been integratedwith a palynologicalzonation of nonhem South America inorder to datctheEsrneraldasForrnation.The age ranges from the lateEarly Eocene to the Late Eocene. The Esmeraldas Forrnationiscorrelative withthe upper Picacho ForTnation and the lowerpartof the ConcentracionForrnationin the EasternCoTdillera, and theupper Mirador Forrnationand thebaseof theCarboneraFormationintheLlanosFeothills. [[heLos Corros FossilHorizon is Late Eocene and is time-correlative with a marine transgression inthe central Llanos Foothills,A non-menic multidimensional scaling analysis suggests that florasfrom the Middle Magdalena Valleywere differentfromthe Llanos Foothillsarea during the Middle to Late Eocene. This is apparently due to taphonomic effects. The results efthis study conuibute to a betterunderstanding of theoverall evolution ef the Middle Magdalena ValleyBasin and the evolution of thenonhem Andes.
publishDate 2012
dc.date.created.spa.fl_str_mv 2012
dc.date.accessioned.none.fl_str_mv 2020-08-19T14:41:35Z
dc.date.available.none.fl_str_mv 2020-08-19T14:41:35Z
dc.type.eng.fl_str_mv article
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
dc.type.spa.spa.fl_str_mv Artículo
dc.identifier.doi.none.fl_str_mv https://doi.org/10.24524/jjpal.58.Special_196_2
dc.identifier.issn.none.fl_str_mv ISSN: 0387-1851
EISSN: 2433-0272
dc.identifier.uri.none.fl_str_mv https://repository.urosario.edu.co/handle/10336/27276
url https://doi.org/10.24524/jjpal.58.Special_196_2
https://repository.urosario.edu.co/handle/10336/27276
identifier_str_mv ISSN: 0387-1851
EISSN: 2433-0272
dc.language.iso.spa.fl_str_mv eng
language eng
dc.relation.citationEndPage.none.fl_str_mv 197
dc.relation.citationIssue.none.fl_str_mv No. Special
dc.relation.citationStartPage.none.fl_str_mv 196
dc.relation.citationTitle.none.fl_str_mv Japanese Journal of Palynology
dc.relation.citationVolume.none.fl_str_mv Vol. 58
dc.relation.ispartof.spa.fl_str_mv Japanese Journal of Palynology, ISSN: 0387-1851;EISSN: 2433-0272, Vol.58, No.Special (2013); pp. 196-197
dc.relation.uri.spa.fl_str_mv https://www.jstage.jst.go.jp/article/jjpal/58/Special/58_KJ00008443174/_pdf/-char/en
dc.rights.coar.fl_str_mv http://purl.org/coar/access_right/c_abf2
dc.rights.acceso.spa.fl_str_mv Abierto (Texto Completo)
rights_invalid_str_mv Abierto (Texto Completo)
http://purl.org/coar/access_right/c_abf2
dc.format.mimetype.none.fl_str_mv application/pdf
dc.publisher.spa.fl_str_mv Palynological Society of Japan
dc.source.spa.fl_str_mv Japanese Journal of Palynology
institution Universidad del Rosario
dc.source.instname.none.fl_str_mv instname:Universidad del Rosario
dc.source.reponame.none.fl_str_mv reponame:Repositorio Institucional EdocUR
repository.name.fl_str_mv Repositorio institucional EdocUR
repository.mail.fl_str_mv edocur@urosario.edu.co
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