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The Geography of Phytochemical Races

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156 3 After the Ice<br />

Table 3.2 Comparison <strong>of</strong> concentrations <strong>of</strong> selected components from Santa Rosa Island and<br />

mainland (Del Mar) populations <strong>of</strong> Pinus torreyana turpentine (from Zavarin et al., 1967)<br />

Compound Santa Rosa Del Mar<br />

Limonene 73.4 (2.1) a 84.2 (2.2)<br />

β-Phellandrene 8.7 (1.2) 0.1 (0.15)<br />

Cineole nd 0.9 (0.5)<br />

n-Decylaldehyde nd 0.4 (0.2)<br />

a Percentage <strong>of</strong> total terpenes (mean deviation).<br />

ß-phellandrene [130]. <strong>The</strong> ß-phellandrene difference amounts to a factor <strong>of</strong> nearly<br />

90, which represents a signifi cantly different fl ow <strong>of</strong> carbon through that particular<br />

part <strong>of</strong> the terpene biosynthetic pathway.<br />

Land bridges, rafting islands, and long-distance dispersal have all been suggested<br />

as means by which the present distribution became established. Geological<br />

evidence suggests that the island separated from the mainland during the Miocene,<br />

and that it has experienced rotation both northward and westward (Axelrod,<br />

1980). Based on the amount and rate <strong>of</strong> genetic divergence between the mainland<br />

and island populations, however, Ledig and Conkle (1983) tentatively concluded<br />

that Torrey pine reached the island from the mainland more recently by “sweepstakes”<br />

dispersal. Coupled with their genetic information, they cited the absence<br />

<strong>of</strong> a Pleistocene land bridge (Junger and Johnson, 1980) and a disharmonic fauna<br />

(Wenner and Johnson, 1980) as evidence for the “sweepstakes” hypothesis. Haller<br />

(1986), however, pointed out that the fl ora <strong>of</strong> the larger Californian islands is neither<br />

depauperate nor disharmonic relative to areas <strong>of</strong> comparable size and habitat variation<br />

on the mainland. He also noted that P. torreyana is not alone as an endemic<br />

on Santa Rosa; Quercus tomentella Engelm., Prunus lyonii (Eastw.) Sargent, and<br />

Lyonothamnus fl oribundus A. Gray are also relic species that were well known on<br />

the mainland during the Tertiary, and that they have not been known on the mainland<br />

for more than 3 million years (see Haller for citations). Other possibilities<br />

include a formerly much more extensive distribution <strong>of</strong> Torrey pine, including other<br />

islands, and that both current populations are relics. After summarizing the various<br />

sources <strong>of</strong> evidence, Haller (1986) concluded that the island population can be<br />

explained perfectly well by means <strong>of</strong> either past land connections or by “normal”<br />

dispersal (Axelrod, 1952). More recently, Waters and Schaal (1991) added valuable<br />

information from their comparison <strong>of</strong> chloroplast DNA from plants collected at<br />

the two sites. <strong>The</strong> two populations were monomorphic at over 150 restriction sites<br />

(26 enzymes) and the chloroplast genomes were identical in length. Those authors<br />

suggested that P. torreyana has been monomorphic since before the populations<br />

became isolated. It is perhaps unnecessary to note that situations such as the Torrey<br />

pine, which appear simple, are only deceptively so. <strong>The</strong>ir resolution requires all <strong>of</strong><br />

the tools available to the biogeographer.<br />

<strong>The</strong>se examples <strong>of</strong> terpenoid analyses represent only a sampling <strong>of</strong> the information<br />

available on pines. Several other studies involving North American and<br />

Mexican pines are listed in Table 3.3.

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