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The Geography of Phytochemical Races

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3.2 North American Conifers 155<br />

agreement with average values for 20 other conifer species (Hamrick et al., 1981):<br />

78.6% polymorphic loci per population as opposed to 67%; 2.35 alleles per locus<br />

compared to 2.29, and 0.327 for mean individual heterozygosities, compared to<br />

0.207, the mean conifer value. Hiebert and Hamrick (1983) suggested that the latter<br />

value was higher for the bristlecone populations primarily because <strong>of</strong> an even<br />

distribution <strong>of</strong> allele frequencies at the polymorphic loci.<br />

<strong>The</strong>re are two possible explanations for the present distribution <strong>of</strong> P. longaeva<br />

in the eastern Great Basin. In the fi rst, long-distance dispersal <strong>of</strong> a small number<br />

<strong>of</strong> seeds via birds could have established the species’ presence in the area. In this<br />

case, one would predict a relatively low level <strong>of</strong> intrapopulational variation, since<br />

each population would have originated from a very limited sampling <strong>of</strong> the parental<br />

genome and a relatively high level <strong>of</strong> interpopulational variation because the populations<br />

would not, in all probability, have arisen from related parents. In the second<br />

scenario, the present distribution <strong>of</strong> bristlecone pines refl ects fragments <strong>of</strong> a once<br />

continuous distribution individual populations, <strong>of</strong> which became separated from<br />

others through a series <strong>of</strong> climate changes, resulting in extinction <strong>of</strong> lower-elevation<br />

stands associated with Pleistocene glacial advance and retreat. In this situation, one<br />

would expect to see higher levels <strong>of</strong> intrapopulational and lower levels <strong>of</strong> interpopulational<br />

variation. Since most <strong>of</strong> the observed genetic variation occurs within<br />

populations, the second explanation for the present distribution seems the more<br />

likely. This view is supported by paleo-ecological observations, including radiocarbon<br />

dating <strong>of</strong> bristlecone pine needles, 10,000–40,000 years old, found in pack rat<br />

middens at much lower elevations (1900 m) than those at which the trees exist at<br />

the present time. It was also noted by the authors that, since glacial periods tend to<br />

be longer than interglacials, it is likely that bristlecone pines spent a considerable<br />

amount <strong>of</strong> time in large, continuous populations. <strong>The</strong> low level <strong>of</strong> genetic variation<br />

observed by Hiebert and Hamrick (1983) suggests that bristlecone pine populations<br />

in this area have not lived in isolation from one another for a long time.<br />

Pinus torreyana C. Parry ex Carrière, the Torrey pine, occurs in southern<br />

California and exhibits an interesting natural distribution consisting <strong>of</strong> two disjunct<br />

populations, one on Santa Rosa Island, which lies about 50 km south <strong>of</strong> Santa<br />

Barbara (Santa Barbara County), and one on the mainland immediately south <strong>of</strong> the<br />

town <strong>of</strong> Del Mar on the northern edge <strong>of</strong> San Diego (San Diego County). <strong>The</strong>y are<br />

separated by about 280 km. <strong>The</strong> relationships and taxonomy <strong>of</strong> Torrey pine were<br />

discussed in detail by Haller (1966, 1986), who described the two populations as<br />

two subspecies, P. torreyana subsp. torreyana <strong>of</strong> the mainland, and P. torreyana<br />

subsp. insularis Haller from the island. Features upon which the distinction was<br />

made included crown shape, needle color, cone features, seed width, and seed color.<br />

A further distinction between the two forms came from a study <strong>of</strong> the composition<br />

<strong>of</strong> their turpentines (Zavarin et al., 1967). Table 3.2 summarizes their results. Two<br />

qualitative differences can be noted; n-decylaldehyde (ten-carbon hydrocarbon aldehyde)<br />

and cineole [41] were present in small amounts in the mainland material, but<br />

were not seen in material from the island. Concentration differences were observed<br />

with all components but most were not statistically signifi cant. Two quantitative differences<br />

that were judged signifi cant by statistical tests involved limonene [24] and

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