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The Geography of Phytochemical Races

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2.7 North and Central America 89<br />

those studies however, which prompted an examination <strong>of</strong> a larger number <strong>of</strong> individuals<br />

from as many <strong>of</strong> the species’ respective ranges as possible.<br />

<strong>The</strong> presence <strong>of</strong> variable pigment pr<strong>of</strong>i les in several other species was noted in a<br />

survey <strong>of</strong> populations (Saleh et al., 1971; Ornduff et al., 1974) and on a study <strong>of</strong> fl avonoids<br />

<strong>of</strong> artifi cial hybrids in the genus (Ornduff et al., 1973a). In an effort to arrive<br />

at a better appreciation <strong>of</strong> how extensive fl avonoid pigment variation is in the genus,<br />

the most widely ranging species, L. californica DC. ex Lindley [= L. chrysostoma<br />

(Fisch. and Mey.) Greene, in the earlier literature] was subjected to a more detailed<br />

examination. Lasthenia californica is not only geographically the most widely distributed<br />

taxon in the genus, but it is also known to occur on a variety <strong>of</strong> substrates,<br />

which suggested that this system might provide some insight into how the species<br />

responds to different edaphic situations. <strong>The</strong> site chosen for detailed study was<br />

the Jasper Ridge Biological Preserve <strong>of</strong> Stanford University (referred to simply as<br />

Jasper Ridge below), which lies south <strong>of</strong> San Francisco in San Mateo County in<br />

the Santa Cruz Mountains (ca. 37°25′N, 122°2.5′W). One <strong>of</strong> the features <strong>of</strong> Jasper<br />

Ridge is the presence <strong>of</strong> a serpentine outcrop that harbors an extensive population<br />

<strong>of</strong> L. californica. Initial sampling was done along a transect approximately 1 km in<br />

length running along the spine <strong>of</strong> the serpentine ridge. In addition to the anthochlors<br />

that characterize this species, which were observed in all individuals, differences<br />

in the nonanthochlor fl avonoid pr<strong>of</strong>i les were observed. Race A was distinguished<br />

by the presence <strong>of</strong> fl avonol diglycoside sulfates and the fl avanone eriodictyol<br />

7-O- glucoside (eriodictyol is the fl avanone equivalent to luteolin), whereas race C<br />

exhibited only the basic array <strong>of</strong> anthochlor pigments. A third variant, called race<br />

B in earlier papers, was observed in a few plants but is now included within race<br />

C. Race B is characterized by the presence <strong>of</strong> luteolin 7-O-glucoside, in addition to<br />

the basic array <strong>of</strong> anthochlors. Plants were also collected along several other transects,<br />

each between 50 m and 65 m long, that lie at right angles to the ridge. Since<br />

no additional pigment variants were observed in these shorter transects, no further<br />

collections were made along the original long transect. We focus our attention, at<br />

least for the moment, on a single transect.<br />

Individual plants were collected at meter intervals, starting at a fi re-access road<br />

near the crest <strong>of</strong> the ridge progressing downslope for a distance <strong>of</strong> 65 m. Elevation<br />

change over this distance is approximately 5 m, which defi nes the drainage pattern<br />

on this part <strong>of</strong> Jasper Ridge. Analysis <strong>of</strong> the individual plants showed that race C<br />

plants occurred in the range 0–45 m after which only race A plants were observed<br />

(Fig. 2.55). This pattern was closely approximated in plants collected along other<br />

parallel transects on either side <strong>of</strong> the main transect. <strong>The</strong> site was visited each year<br />

for a period <strong>of</strong> 6 years during which the distribution pattern <strong>of</strong> race A and race C<br />

plants remained essentially unchanged (a race B plant was observed in the upper<br />

portion <strong>of</strong> the transect during one season). <strong>The</strong>se observations have been described<br />

in a paper (Bohm et al., 1989) where it was pointed out that this was, at least to the<br />

best <strong>of</strong> the authors’ knowledge, the only report <strong>of</strong> a fl avonoid distribution pattern<br />

remaining constant over a period <strong>of</strong> years. Subsequent collections along the same<br />

transect have shown the pattern to have remained constant for a period <strong>of</strong> 15 years<br />

(N. Rajakaruna & B. A. Bohm, unpublished observations). Greenhouse studies

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