Plant palaeoecology of the latest Eocene flora from the Saint-Chaptes and Alès basins of Gard, southern France

dc.contributor.authorTosal Alcobé, Aixa
dc.contributor.authorTanrattana, Mélanie
dc.contributor.authorFournier, François
dc.contributor.authorDe Franceschi, Dario
dc.contributor.authorDel Rio, Cédric
dc.contributor.authorMartín-Closas, Carles
dc.contributor.authorLettéron, Alexandre
dc.contributor.authorSemmani, Nazim
dc.contributor.authorBoura, Anaïs
dc.date.accessioned2025-03-12T14:16:39Z
dc.date.available2025-03-12T14:16:39Z
dc.date.issued2023-07-22
dc.date.updated2025-03-12T14:16:39Z
dc.description.abstractRapid cooling during the Eocene-Oligocene transition resulted in a vegetation shift in southern France, fromwarm, humid vegetation to open savannah-like vegetation; however, the precise nature of this shift is uncertain.In this paper, we study the latest Eocene flora from the Saint-Chaptes and Al`es basins (southern France) andcompare it with other well-known southern European localities to evaluate vegetation changes near the Eocene-Oligocene boundary. Five plant communities are recognised: 1) hydrophytic vegetation dominated by water liliesand a Limnobiophyllum-like plant; 2) reeds that formed a palustrine belt around the lake; 3) ferns with Osmundaaff. parschlugiana and Pronephrium stiriacum, conifers with Doliostrobus taxiformis, a Sequoia-like plant, angiospermswith Daphnogene sp., Byttneriopsis sp., Myrica sp., Comptonia difformis and palms, which inhabited the lakeshores and constituted the riparian vegetation; 4) Tetraclinis, which grew just behind the riparian vegetation butnot far from watercourses, forming open landscapes and 5) Zizyphus ziziphoides, Fabaceae, and probably Ailanthussp. and Tetraclinis forming an open woodland distal to the lake. The flora of the Saint-Chaptes and Al`es basinsresembles coeval floras from Sarral (Catalonia, Spain) that are characteristic of Southern Europe, although riparianvegetation is more diverse in the Saint-Chaptes and Al`es basins, and Fabaceae diversity is higher at Sarral.We hypothesise that vegetation composition was mainly controlled by (1) basin architecture, allowing for avariety of wetland habitats and (2) climate. The coexistence of genera that are restricted to Central Europe (e.g.,Byttneriopsis or Doliostrobus), together with genera more typical of Southern Europe (e.g., diversity of Fabaceae,C. difformis and Z. ziziphoides) suggests that the Saint-Chaptes and Al`es basins contain latest Priabonian florasthat are transitional between these two regions.
dc.format.extent18 p.
dc.format.mimetypeapplication/pdf
dc.identifier.idgrec746028
dc.identifier.issn0031-0182
dc.identifier.urihttps://hdl.handle.net/2445/219659
dc.language.isoeng
dc.publisherElsevier B.V.
dc.relation.isformatofReproducció del document publicat a: https://doi.org/10.1016/j.palaeo.2023.111740
dc.relation.ispartofPalaeogeography Palaeoclimatology Palaeoecology, 2023, vol. 627, 111740
dc.relation.urihttps://doi.org/10.1016/j.palaeo.2023.111740
dc.rightscc-by-nc-nd (c) The Author(s), 2023
dc.rights.accessRightsinfo:eu-repo/semantics/openAccess
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/
dc.sourceArticles publicats en revistes (Dinàmica de la Terra i l'Oceà)
dc.subject.classificationPaleoecologia
dc.subject.classificationSediments lacustres
dc.subject.classificationBiogeografia
dc.subject.classificationPaleogen
dc.subject.classificationPaleobotànica
dc.subject.classificationPaleoclimatologia
dc.subject.classificationDinàmica de la vegetació
dc.subject.otherPaleoecology
dc.subject.otherLake sediments
dc.subject.otherBiogeography
dc.subject.otherPaleogene
dc.subject.otherPaleobotany
dc.subject.otherPaleoclimatology
dc.subject.otherVegetation dynamics
dc.titlePlant palaeoecology of the latest Eocene flora from the Saint-Chaptes and Alès basins of Gard, southern France
dc.typeinfo:eu-repo/semantics/article
dc.typeinfo:eu-repo/semantics/acceptedVersion

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