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...
- Autores:
- Tipo de recurso:
- 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
- Rights
- License
- Abierto (Texto Completo)
id |
EDOCUR2_ebef8f2b3a2a3b1b97b7393872023f11 |
---|---|
oai_identifier_str |
oai:repository.urosario.edu.co:10336/27276 |
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 |
_version_ |
1814167670186049536 |