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The Geography of Phytochemical Races

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4.1 Across the Atlantic Ocean 181<br />

caused by some combination <strong>of</strong> the nitrogenous components <strong>of</strong> the species, ephedrine<br />

derivatives taken as a case in point. A recent paper by Caveney et al. (2001)<br />

surveyed 26 species <strong>of</strong> Ephedra for nitrogenous compounds. Several interesting<br />

differences among different groups <strong>of</strong> species were observed, but the observation<br />

<strong>of</strong> interest to us here is the presence <strong>of</strong> ephedrine [(–)-1-phenyl-1-hydroxy-2-Nmethylaminopropane]<br />

and pseudo-ephedrine [the ( + )-isomer] in Eurasian species<br />

and their nearly total absence from New World species. <strong>The</strong> only exception was the<br />

detection <strong>of</strong> a trace <strong>of</strong> pseudo-ephedrine (>0.01% wet mass) in E. californica.<br />

4.1.6 Cactaceae and Aizoaceae<br />

An early review <strong>of</strong> chemistry <strong>of</strong> disjunct (allojunct in the paper) taxa was that <strong>of</strong><br />

Turner (1972), one <strong>of</strong> the strongest proponents <strong>of</strong> the chemotaxonomic school <strong>of</strong><br />

the 1960s and 1970s. One <strong>of</strong> the subjects he discussed was the disjunct family<br />

pair Cactaceae and Aizoaceae. His story started with a reference to a much earlier<br />

paper by Vierhapper (1919) that suggested that these two families were disjuncts.<br />

Both are succulents, with Aizoaceae predominantly South African in distribution,<br />

whereas Cactaceae is predominantly New World. As emphasized by Turner,<br />

Vierhapper’s suggestion was remarkably prescient considering that plate tectonic<br />

theory lay well in the future and, in line with our concerns in this review, nothing<br />

was yet known about the unusual secondary chemistry that links these families and<br />

ties them together with others in Caryophyllalles (Centrospermae) (Wohlpart and<br />

Mabry, 1968). <strong>The</strong> chemistry to which we refer here, <strong>of</strong> course, is the presence <strong>of</strong><br />

betacyanins (betalains is the more general term) as fl oral pigments in place <strong>of</strong> the<br />

more common anthocyanins. Figure 4.5 illustrates the two compound types, with<br />

betanin [312] representing the betacyanins and cyanidin [313] representing the typical<br />

anthocyanins.<br />

Fig. 4.5 Compounds 312 and 313, typical betacyanin and anthocyanin, respectively. Compounds<br />

314 and 315 from Trachylobium

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