Pollen-and diatom based environmental history since the Last Glacial Maximum from the Andean core Fúquene-7, Colombia

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dc.citation.journalTitleJournal Of Quaternary Science
dc.contributor.authorVélez, Maria Isabelspa
dc.contributor.authorHooghiemstra, Henryspa
dc.contributor.authorMetcalfe, Sarahspa
dc.contributor.authorMartínez, Ignaciospa
dc.contributor.authorMommersteeg, Hermanspa
dc.contributor.departmentUniversidad EAFIT. Departamento de Geologíaspa
dc.contributor.researchgroupCiencias del Marspa
dc.date.accessioned2021-03-23T20:20:22Z
dc.date.available2021-03-23T20:20:22Z
dc.date.issued2003-01-01
dc.description.abstractThe late Pleistocene-Holocene ecological and limnological history of Lake Fúquene (2580 m a.s.l.), in the Colombian Andes, is reconstructed on the basis of diatom, pollen and sediment analyses of the upper 7 m of the core Fúquene-7. Time control is provided by 11 accelerator mass spectrometry (AMS) 14C dates ranging from 19 670 ± 240 to 6040 ± 60 yr BP. In this paper we present the evolution of the lake and its surroundings. Glacial times were cold and dry, lake-levels were low and the area was surrounded by paramo and subparamo vegetation. Late-glacial conditions were warm and humid. The El Abra Stadial, a Younger Dryas equivalent, is reflected by a gap in the sedimentary record, a consequence of the cessation of deposition owing to a drop in lake-level. The early Holocene was warm and humid; at this time the lake reached its maximum extension and was surrounded by Andean forest. The onset of the drier climate prevailing today took place in the middle Holocene, a process that is reflected earlier in the diatom and sediment records than in the pollen records. In the late Holocene human activity reduced the forest and transformed the landscape. Climate patterns from the Late-glacial and throughout the Holocene, as represented in our record, are similar to other records from Colombia and northern South America (the Caribbean, Venezuela and Panama) and suggest that the changes in lake-level were the result of precipitation variations driven by latitudinal shifts of the Intertropical Convergence Zone. © 2003 John Wiley and Sons, Ltd.eng
dc.identifierhttps://eafit.fundanetsuite.com/Publicaciones/ProdCientif/PublicacionFrw.aspx?id=1180
dc.identifier.doi10.1002/jqs.730
dc.identifier.issn02678179
dc.identifier.issn10991417
dc.identifier.otherWOS;000180962300003
dc.identifier.otherSCOPUS;2-s2.0-0037282908
dc.identifier.urihttp://hdl.handle.net/10784/26865
dc.language.isoengeng
dc.publisherJOHN WILEY & SONS LTD
dc.relation.urihttps://www.scopus.com/inward/record.uri?eid=2-s2.0-0037282908&doi=10.1002%2fjqs.730&partnerID=40&md5=392956bffe7dd69b47dc88d644c1ef7c
dc.relation.urihttps://onlinelibrary.wiley.com/doi/10.1002/jqs.730
dc.rightshttps://v2.sherpa.ac.uk/id/publication/issn/0267-8179
dc.rights.accessrightsinfo:eu-repo/semantics/openAccesseng
dc.rights.localAcceso abiertospa
dc.sourceJournal Of Quaternary Science
dc.subject.keyworddiatomeng
dc.subject.keywordlake evolutioneng
dc.subject.keywordLast Glacial Maximumeng
dc.subject.keywordpaleoenvironmenteng
dc.subject.keywordpalynologyeng
dc.subject.keywordQuaternaryeng
dc.subject.keywordColombiaeng
dc.subject.keywordAbraeng
dc.subject.keywordBacillariophytaeng
dc.titlePollen-and diatom based environmental history since the Last Glacial Maximum from the Andean core Fúquene-7, Colombiaeng
dc.typeinfo:eu-repo/semantics/articleeng
dc.typearticleeng
dc.typeinfo:eu-repo/semantics/publishedVersioneng
dc.typepublishedVersioneng
dc.type.localArtículospa

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