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Late Cretaceous–Early Eocene origin of yams ( Dioscorea , Dioscoreaceae) in the Laurasian Palaearctic and their subsequent Oligocene–Miocene diversification
Author(s) -
Viruel Juan,
SegarraMoragues José Gabriel,
Raz Lauren,
Forest Félix,
Wilkin Paul,
Sanmartín Isabel,
Catalán Pilar
Publication year - 2016
Publication title -
journal of biogeography
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.7
H-Index - 158
eISSN - 1365-2699
pISSN - 0305-0270
DOI - 10.1111/jbi.12678
Subject(s) - pantropical , land bridge , biogeography , paleontology , biological dispersal , dioscorea , biology , western palaearctic , cretaceous , late miocene , range (aeronautics) , genus , ecology , population , demography , alternative medicine , pathology , sociology , composite material , structural basin , medicine , materials science
Abstract Aim Dioscorea (Dioscoreaceae) is a predominantly pantropical genus (< 600 species) that includes the third most important tropical tuber crop and species of pharmacological value. Fossil records from both the Northern and Southern Hemispheres were used to test hypotheses about the origin of the genus Dioscorea , and to examine potential macroevolutionary processes that led to its current distribution. Location Pantropical distribution. Methods Divergence times were estimated using the most comprehensive phylogeny of the group published to date based on plastid sequences and fossil calibrations, applying a relaxed‐clock model approach. Ancestral areas and range shifts were reconstructed using time‐stratified likelihood‐based models, reflecting past continental connectivity and biogeographical models incorporating the spatial range of fossils. Results Fossil‐informed biogeographical analysis supported colonization of the Nearctic by ancient yam lineages from the western Palaearctic and subsequent migration to the South. Most of the pantropical South American, African and Southeast Asian lineages experienced a relatively recent diversification in the Oligocene–Miocene. Long‐distance dispersals were inferred for the colonizations of the New World, Africa and Madagascar. Main conclusions Dioscorea likely originated between the Late Cretaceous and the Early Eocene in the Laurasian Palaearctic, followed by possible dispersal to South America via the Eocene North Atlantic Land Bridge.