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The Geography of Phytochemical Races

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188 4 Intercontinental Disjunctions<br />

Western Australia, as one might have expected. This observation was in agreement<br />

with conclusions drawn on the basis <strong>of</strong> morphological differences (Ornduff, 1974).<br />

4.2.4 Icacinaceae<br />

One <strong>of</strong> the most serious contributors to chemical ecology-chemical geography has<br />

been the Brazilian natural product chemist Otto Gottlieb (see Gottlieb and Kubitzki,<br />

1983; Gottlieb, 1986, 1990). It has been his goal to examine chemical pr<strong>of</strong>i les <strong>of</strong><br />

target taxa, not just from the point <strong>of</strong> view <strong>of</strong> presence or absence <strong>of</strong> a suite <strong>of</strong><br />

compounds, but rather to investigate the levels <strong>of</strong> complexity involved in the processes<br />

by which the compounds are elaborated. Among other things, his work has<br />

involved searches for regular changes in oxidation level <strong>of</strong> a set <strong>of</strong> compounds, or<br />

for situations where there has been a switch between different biochemical pathways<br />

(e.g., shikimate to acetate/malonate), or differences in the way plants protect<br />

component compounds from degradation. Following these analyses is not always<br />

easy, with point scores being tallied for certain structural aspects within each class<br />

<strong>of</strong> compounds and the calculation <strong>of</strong> various indices <strong>of</strong> evolutionary advancement.<br />

Detailed consideration is given to the steps involved in forming end products,<br />

with recognition given not only to compounds that are specialized or “advanced”<br />

because they have had substituents added to the base structure, but also to those that<br />

have been modifi ed in ways that make them appear simpler then the base structure,<br />

that is, the loss <strong>of</strong> a functional group originally present. An example <strong>of</strong> this is seen<br />

below, where loss <strong>of</strong> a carbon atom through oxidation leads to a derived (advanced)<br />

molecule.<br />

<strong>The</strong> example to be described, admittedly one whose chemistry is diffi cult, is,<br />

nonetheless, typical <strong>of</strong> the approach. In the case <strong>of</strong> Icacinaceae, Kaplan et al. (1991)<br />

studied the increase in complexity <strong>of</strong> terpenoid compounds <strong>of</strong> selected members <strong>of</strong><br />

the family as a function <strong>of</strong> where, in the geographic range <strong>of</strong> the family, the various<br />

genera occur. Although the work was set in a taxonomic context—using chemical<br />

features to assess the proper placement <strong>of</strong> the family—our interest lies in the chemical<br />

changes that appear to be associated with geography.<br />

Icacinaceae are a moderate-sized, primarily tropical family consisting <strong>of</strong> 52<br />

genera, many <strong>of</strong> which are monotypic, and 300 species. Additional background on<br />

taxonomic problems surrounding the family can be found in the 1991 paper by<br />

Kaplan et al. Chemical data have been used by Dahlgren (1980) to assess these<br />

relationships with related families, but the application involved simple presence or<br />

absence data (iridoids) and did not touch upon the dynamic nature <strong>of</strong> the pathways<br />

involved.<br />

<strong>The</strong> genera and relevant chemistry <strong>of</strong> Icacinaceae involved in this example are<br />

given in Fig. 4.8, using the format <strong>of</strong> Kaplan et al. (1991) wherein the four sets <strong>of</strong><br />

genera, grouped according to chemical similarity, are listed according to geographic<br />

areas. <strong>The</strong> geographic areas represented range from eastern Australia (Queensland)<br />

westward through Melanesia, southeastern Asia, India, and Africa to South America.

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