NEW RECORDS OF FERNS AND CONIFERS FROM THE LOWER CRETACEOUS IN THE UPPER MAGDALENA VALLEY BASIN, COLOMBIA

dc.contributor.authorCamila Monje-Dussán
dc.contributor.authorCamila Martínez
dc.contributor.authorIgnacio Escapa
dc.contributor.authorSantiago Madriñán
dc.coverage.spatialBolivia
dc.date.accessioned2026-03-22T20:05:19Z
dc.date.available2026-03-22T20:05:19Z
dc.date.issued2016
dc.description.abstractDescriptions of new plant macrofossils from the Lower Cretaceous (Aptian-Albian) of Colombia are presented. The studied material was collected in the Upper Magdalena Valley Basin in three exposing levels from the Yaví and Caballos formations. The fossil remains are associated to filicopsids and conifers. Within the ferns, the family Marsileaceae, constitutes an important group identified in the fossil flora because it is proposed as the first record of aquatic ferns for the Lower Cretaceous of Colombia. Additionally, abundant sterile bipinnate fronds with lanceolate pinnule and pecopteridea venation remains were included in the morphogenus Cladophlebis sp. The studied conifers presented vegetative structures associated to reproductive organs. The most abundant sterile fragments were included within the morphogenus Brachyphyllum sp. and ovuliferous scales of Araucarites sp. (Araucariaceae) type. Together these new findings represent a key aspect to understand the biogeography of the mentioned groups and, simultaneously, contribute to the knowledge of the Cretaceous plant fossils from Colombia.  
dc.identifier.urihttps://andeanlibrary.org/handle/123456789/79914
dc.language.isoes
dc.relation.ispartofUniversidad Industrial de Santander
dc.sourceSmithsonian Tropical Research Institute
dc.subjectCretaceous
dc.subjectMacrofossil
dc.subjectFrond
dc.subjectPaleontology
dc.subjectFlora (microbiology)
dc.subjectFossil Record
dc.subjectPollen
dc.subjectPaleobotany
dc.subjectKey (lock)
dc.subjectBiology
dc.titleNEW RECORDS OF FERNS AND CONIFERS FROM THE LOWER CRETACEOUS IN THE UPPER MAGDALENA VALLEY BASIN, COLOMBIA
dc.typearticle

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