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Phylogenetic relationships and infrageneric classification of Astragalus tragacantha L. (Fabaceae), inferred from nuclear ribosomal<br />

DNA Internal transcribed spacers data (nrDNA ITS)<br />

nial herb widely spread in Eurasia, takes an<br />

obvious basal place, while Astragalus depressus,<br />

an astragal confined on mountains around<br />

Mediterranean Basin, is located between<br />

clade 2 and the base of the MP tree, supported<br />

by a poor bootstrap value.<br />

Homoplasy of thorny cushion-form<br />

in Mediterranean Astragals<br />

The NJ phylogeny positions the West Mediterranean<br />

Astragalus tragacantha in clade C<br />

(Figure 1), clearly separated from clade D<br />

which includes most of the thorny astragals<br />

(such as all sampled astragals of subgenus Tragacantha<br />

and some species of other subgenera).<br />

In fact, recently, morphological (Zarre &<br />

Podlech 1997) and then molecular analyses<br />

(Kazempour Osaloo et al. 2003) have allowed<br />

gathering many spiny astragals, previously<br />

separated in different subgenera. But the<br />

absence of A. tragacantha in clade D is an evidence<br />

of homoplasy for this character. The<br />

thorny cushion-forming is an adapted structure<br />

to aridity and strong winds of North-West<br />

Mediterranean coasts but also of Mediterranean<br />

mountains. This form exists in other<br />

astragals of the same section (Tragacantha DC<br />

of subgenus Cercidothrix Bunge) as A. genargenteus,<br />

A. gennarii, A. greuteri and A. sirinicus<br />

which are West Mediterranean orophytes<br />

and A. angustifolius, a South-East European<br />

orophyte (Baccheta & Brullo 2006), but none<br />

of these orophytes have been sequenced for<br />

nrDNA ITS. Their geographic proximity, their<br />

morphological similarities and their belonging<br />

to section Tragacantha are serious points<br />

underlining their probable close phylogenetic<br />

relationship with A. tragacantha. Knowing<br />

that South-Western and Sino-Himalayan<br />

regions of Asia are supposed to be the geographic<br />

origin of Astragalus genus, a scenario<br />

of differentiation from Eastern to Western<br />

Europe can be assumed (Nimis 1981).<br />

Based on these observations, no decisive conclusions<br />

can be proposed on Astragalus tragacantha<br />

history or homology with its closest<br />

relatives. In order to set robust hypothesis<br />

about evolution and history of Astragalus tragacantha,<br />

more taxa from clade C (Figure 1)<br />

must be sampled. Further steps of sampling<br />

should focus on other species of section Tragacantha<br />

as A. balearicus, A. genargenteus,<br />

A. sirinicus, A. gennarii, A. greuteri and A.<br />

angustifolius.<br />

ecologia mediterranea – Vol. 36 (1) – 2010<br />

Acknowledgments<br />

The authors thank Martin Wojciechowski for<br />

answering to our questions on a genus widely<br />

studied by his works, Pr Akhani to have provided<br />

us study elements about Astragalus, the<br />

Corsican Environment Office to have allowed<br />

us to sample in Corsica, and the Marseille<br />

municipality which grant funds to this study.<br />

Lastly, the authors would like to acknowledge<br />

the anonymous reviewer of this publication<br />

and Dr Ong’amo for helpful comments on the<br />

manuscript.<br />

References<br />

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105

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