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Phylogenetic relationships between disjunctly occurring groups of Tristicha trifaria (Podostemaceae)
Author(s) -
Kita Yoko,
Kato Masahiro
Publication year - 2004
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/j.1365-2699.2004.01047.x
Subject(s) - biology , phylogenetic tree , phylogeography , botany , intergenic region , disjunct , disjunct distribution , chloroplast dna , clade , evolutionary biology , genetics , gene , genome , population , demography , sociology
Aim  To reveal the phylogeographic relationship of disjunct specimens of Tristicha trifaria (Bory ex Willd.) Spreng., a member of the Podostemaceae river‐weed family, which is distributed exceptionally widely, but disjunctly, in Africa and the Americas. Location  Brazil, Mexico, Ghana, Tanzania and Madagascar. Methods  The chloroplast mat K and rbc L genes, a trn K intron, the trn S‐ trn G intergenic spacer (IGS), the two IGSs of trn T‐ trn L‐ trn F, a trn L intron, and nuclear ribosomal ITS regions were sequenced and analysed. Phylogenetic analyses were conducted using maximum likelihood and maximum parsimony methods. Results  The T. trifaria samples analysed were separated into two groups in a rooted tree based on a combined mat K/ rbc L/ITS dataset; one contained the West African and all of the American samples, and the other contained the East African and Madagascan samples. An unrooted tree obtained from a combined analysis of all the chloroplast DNA and nuclear ITS data showed that a sample from West Africa was sister to an American T. trifaria group. Main conclusions  The American and West African T. trifaria are closely related, despite the great distance between their locations. This observation, along with a tree of the whole Tristichoideae subfamily and estimated divergence times, suggests that an ancestor of T. trifaria migrated from Asia to Africa during the early Tertiary, and that this was followed by further westward migration to the Americas at the end of the Miocene or in the early Pliocene.

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