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The Geography of Phytochemical Races

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204 4 Intercontinental Disjunctions<br />

Fig. 4.13 Compounds 357 and 358 from Castanospermum and Alexa. Compounds 359–364,<br />

diterpenes from Scoparia dulcis<br />

Castanospermum, an Australian genus that consists <strong>of</strong> the single species C. australe<br />

A. Cunn. & C. Fraser ex Hook., and Alexa, a genus <strong>of</strong> eight or so species from<br />

South America (Kaplan, 1995); both belong to the tribe Sophoreae <strong>of</strong> Papilionoideae.<br />

Other, related genera will be commented upon below.<br />

Castanospermine was obtained from Castanospermum australe (Hohenschutz<br />

et al., 1981), while australine was isolated from the same species by Molyneux et al.<br />

(1988). Nash et al. (1988) identifi ed these compounds as components <strong>of</strong> Alexa.<br />

Related compounds that differ in the number <strong>of</strong> hydroxyl groups, and respective<br />

stereochemistries, have been isolated from these taxa as well. It is <strong>of</strong> interest that<br />

swainsonine [359], closely related to castanospermine, has been identifi ed (Colegate<br />

et al., 1979) as a component <strong>of</strong> Swainsona canescens (Benth.) F. Muell. Swainsona<br />

is a genus <strong>of</strong> some 50 species (Mabberley, 1997, p. 692), found only in Australia<br />

and on the south island <strong>of</strong> New Zealand (one species). Swainsonine has also been<br />

isolated from North American species <strong>of</strong> Astragalus and Oxytropis (Colgate et al.,<br />

1979; Molyneux and James, 1982). Neither <strong>of</strong> these genera is represented in the<br />

Australian fl ora. Kaplan (1995) suggested that these chemical data point to a “ . . .<br />

common ancestor thriving on the old South Pangaean continent . . .” from which<br />

Castanospermum and Alexa arose. Kaplan goes on to suggest that ancestors <strong>of</strong><br />

Astragalus and Oxytropis may have occupied the “continent” as well. <strong>The</strong> authors<br />

were not precise in their estimates <strong>of</strong> the time scale involved in these events. Given<br />

that the age <strong>of</strong> the legumes has been reasonably estimated at about 50 million years,<br />

based on fossil evidence, it ought to have been possible to narrow the possibilities<br />

for the time <strong>of</strong> separation <strong>of</strong> the ancestors <strong>of</strong> the taxa involved. In any event, it<br />

seems unlikely that compounds <strong>of</strong> the sort seen in these taxa developed independently<br />

in several unrelated ancestral (or modern) taxa, although one can never rule

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