The charophyte fossil record on the Iberian peninsula: A synthesis

dc.contributor.authorMartı́n-Closas, Carles
dc.contributor.authorVicente, Alba
dc.contributor.authorVillalba-Breva, Sheila
dc.contributor.authorSanjuan, Josep
dc.contributor.departmentDepartment of Geology
dc.contributor.facultyFaculty of Arts and Sciences (FAS)
dc.contributor.institutionAmerican University of Beirut
dc.date.accessioned2025-01-24T11:24:08Z
dc.date.available2025-01-24T11:24:08Z
dc.date.issued2016
dc.description.abstractIberia was first an island and then a European peninsula during most of the Earth's history. This along with a long-lasting non-marine record has determined that fossil charophytes are wellrepresented and show significant particularities. As a matter of fact, the Iberian Peninsula is one of the best suited regions of Europe in which to study the charophyte fossil record from the Jurassic to the present. Middle and Late Jurassic charophyte assemblages are represented in the Lusitanian basin (Portugal). They show dominance of the family Porocharaceae in many of the environments available for charophytes. Lower Cretaceous charophytes, dominated by clavatoraceans, have been more studied in the Iberian Chain, where this family achieved high diversity. Also, many European charophyte biozones of this interval are based on Iberian clavatoraceans and have their stratotypes in the Iberian Chain. Upper Cretaceous charophytes of the Iberian Peninsula have been more studied in the Campanian of the Southwestern Iberian Chain (Serrania de Cuenca) and in the Maastrichtian of the south-Pyrenean basins (Catalonia). The floras show important affinity with those from southern France, which is not surprising since both regions were part of the so-called Ibero-Armorican Island. The Upper Cretaceous charophyte record from the southern Pyrenees is significant because it contains a reference section enabling us to define the Cretaceous-Palaeogene boundary based on charophytes in the Ager basin. Palaeogene charophytes from Iberia are best known from studies devoted to the Ebro foreland basin, where a detailed biozonation of the Eocene and Oligocene has been proposed. The charophyte assemblages were composed of a mixture of fossil and present-day genera and included both typical European species as well as endemic taxa. Neogene charophytes from Iberia are poorly known, but a number of studies have been performed, mainly in Central Spain and in the Ebro basin. © 2016 Institute of Botany and Botanical Garden Jevremovac, Belgrade.
dc.identifier.doihttps://doi.org/10.5281/zenodo.162219
dc.identifier.eid2-s2.0-85001831591
dc.identifier.urihttp://hdl.handle.net/10938/25908
dc.language.isoen
dc.publisherInstitute of Botany and Botanical Garden Jevremovac, University of Belgrade
dc.relation.ispartofBotanica Serbica
dc.sourceScopus
dc.subjectCenozoic
dc.subjectCharophyta
dc.subjectMesozoic
dc.subjectPortugal
dc.subjectSpain
dc.titleThe charophyte fossil record on the Iberian peninsula: A synthesis
dc.typeArticle

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