Phylogeographical Analyses of a Relict Fern of Palaeotropical Flora (Vandenboschia speciosa): Distribution and Diversity Model in Relation to the Geological and Climate Events of the Late Miocene and Early Pliocene Ben-Menni Schuler, Samira Blanca López, Gabriel Romero García, Ana Teresa Suárez Santiago, Víctor Fern phylogeography gapCp gene Palaeotropical flora Plastid DNA Refugia Relict fern Species distribution modelling Tertiary Vandenboschia speciosa Samira Ben-Menni Schuler was granted a predoctoral grant (F.P.U. program) from the Spanish Government. Hammadi Hamza was granted by a postdoctoral fellowship (Erasmus Mundus-Al Idrisi II scholarship) from the European Union. The authors thank all those people and institutions that facilitated or helped in the collection of samples (in alphabetical order: angel Banares, Antonio Delgado, Brother Anthony, Government of Ireland, Elizabeth Ojeda, Emer Ni Dhuill, Gobierno de Canarias, Ibai Olariaga-Ibarguren, Inaki Sanz-Azkue, Junta de Andalucia, Kristyna Hanuova, Miguel Perez-Gutierrez, Parque Nacional de Garajonay, Ranger Brian Duffy, Sito Chinea, Yves Krippel). We also thank Ana Garcia-Garcia for technical assistance in SDM analysis. This research was funded by the Regional Andalusian Government, grant number P10-RNM-6198. Fern phylogeographic studies have mostly focused on the influence of the Pleistocene climate on fern distributions and the prevalence of long-distance dispersal. The effect of pre-Pleistocene events on the distributions of fern species is largely unexplored. Here, we elucidate a hypothetical scenario for the evolutionary history of Vandenboschia speciosa, hypothesised to be of Tertiary palaeotropical flora with a peculiar perennial gametophyte. We sequenced 40 populations across the species range in one plastid region and two variants of the nuclear gapCp gene and conducted time-calibrated phylogenetic, phylogeographical, and species distribution modelling analyses. Vandenboschia speciosa is an allopolyploid and had a Tertiary origin. Late Miocene aridification possibly caused the long persistence in independent refugia on the Eurosiberian Atlantic and Mediterranean coasts, with the independent evolution of gene pools resulting in two evolutionary units. The Cantabrian Cornice, a major refugium, could also be a secondary contact zone during Quaternary glacial cycles. Central European populations resulted from multiple post-glacial, long-distance dispersals. Vandenboschia speciosa reached Macaronesia during the Pliocene–Pleistocene, with a phylogeographical link between the Canary Islands, Madeira, and southern Iberia, and between the Azores and northwestern Europe. Our results support the idea that the geological and climate events of the Late Miocene/Early Pliocene shifted Tertiary fern distribution patterns in Europe. 2022-05-04T08:42:09Z 2022-05-04T08:42:09Z 2022-03-22 info:eu-repo/semantics/article Ben-Menni Schuler, S... [et al.]. Phylogeographical Analyses of a Relict Fern of Palaeotropical Flora (Vandenboschia speciosa): Distribution and Diversity Model in Relation to the Geological and Climate Events of the Late Miocene and Early Pliocene. Plants 2022, 11, 839. [https://doi.org/10.3390/plants11070839] http://hdl.handle.net/10481/74687 10.3390/plants11070839 eng http://creativecommons.org/licenses/by/3.0/es/ info:eu-repo/semantics/openAccess Atribución 3.0 España MDPI