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Grass diversification in Madagascar: In situ radiation of two large C 3 shade clades and support for a Miocene to Pliocene origin of C 4 grassy biomes
Author(s) -
Hackel Jan,
Vorontsova Maria S.,
Nanjarisoa Olinirina P.,
Hall Russell C.,
Razanatsoa Jacqueline,
Malakasi Panagiota,
Besnard Guillaume
Publication year - 2018
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.13147
Subject(s) - endemism , range (aeronautics) , biology , ecology , biogeography , biological dispersal , taxon , clade , grassland , lineage (genetic) , habitat , geography , phylogenetics , population , materials science , demography , sociology , composite material , biochemistry , gene
Abstract Aim Grasses (Poaceae) are found in all major habitats of Madagascar and have a particular importance in C 4 grasslands, whose origins are controversial. We aimed to estimate the number, age and origins of endemic grass lineages in the Madagascar region, and to compare the diversification of C 3 and C 4 taxa. Location Madagascar and the surrounding Indian Ocean islands, integrated within a global dataset. Methods We estimated 11 time‐calibrated molecular phylogenies including 73% of Madagascar's known grass flora (65% of endemics), using two calibration scenarios. Integrating the available sequences from worldwide grass species, a total of 1928 accessions were analysed. We tested range evolution models, estimated ancestral ranges, and compared the patterns of lineage accumulation between endemic C 3 and C 4 grasses. Results We recovered 69 lineages endemic to or with an estimated origin in the Madagascar region, 25 of them C 3 and 44 C 4 . Range evolution analysis suggests widespread distance‐scaling of dispersal and strongest historical links to Africa. Extant grass diversity largely accumulated since the Miocene, with parallel increases in C 3 and C 4 taxa. Two large C 3 groups in the “Forest shade clade” (Paniceae: Boivinellinae) and the bamboos (subtribe Hickeliinae) have an estimated origin in the Madagascar region. Divergences and crown ages of endemic C 4 lineages largely coincide with the Miocene grassland expansion. Main conclusions Madagascar's extant grass flora is the result of multiple overseas dispersals, predominantly from Africa, and diversified from the Miocene onwards. C 3 grasses are characterized by two large presumed in situ radiations of shade grasses in the Paniceae and bamboos. Endemic C 4 lineages result from twice as many immigration events, resulting in smaller clades. Ages of C 4 lineages are consistent with a Pliocene or Late Miocene origin of grasslands in Madagascar, but estimating the nature and expanse of such early grasslands will require further research.