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The Geography of Phytochemical Races

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280 6 Oceanic Islands<br />

Fuerteventura, and Lanzarote. <strong>The</strong> islands are volcanic and range in age from less<br />

than 1 million to about 21 million years (Carracedo, 1994). Two recent papers<br />

present detailed accounts <strong>of</strong> the geologic history <strong>of</strong> the Canary Islands along with<br />

extensive literature reviews (Anguita and Hernan, 2000; Dañobeitia and Canales,<br />

2000). <strong>The</strong> Cape Verde archipelago consists <strong>of</strong> several small islands centered at<br />

16°00′ N, 24°00′ W, to the west <strong>of</strong> Senegal. <strong>The</strong> Madeira archipelago consists <strong>of</strong><br />

two main islands, Madeira (32°45′N, 17°W) and the much smaller Porto Santo<br />

(33°04′N, 16°20′W). <strong>The</strong> Selvagens Islands, among the smallest <strong>of</strong> the Macaronesian<br />

group, consist <strong>of</strong> two small landmasses at ca. 30°00′N, 16°00′W, which puts<br />

them roughly one-third <strong>of</strong> the way between the Canary Islands and the island <strong>of</strong><br />

Madeira.<br />

6.9.1 Anomalographis madeirensis (Graphidaceae)<br />

Differences in the depsidone chemistry <strong>of</strong> the lichen Anomalographis madeirensis<br />

(Tav.) Kalb. have been noted by González et al. (1999), who reported identifi cation<br />

<strong>of</strong> stictic (see Fig. 5.4 for structures), norstictic, and cryptostictic acids from a specimen<br />

collected on Tenerife. In contrast, Kalb and Hafellner (1992) reported stictic<br />

and norstictic acids from material <strong>of</strong> this species collected on Madeira, but did not<br />

fi nd cryptostictic acid. <strong>The</strong>y did fi nd two other depsidones, however, that is, constictic<br />

and connorstictic acids. It would be interesting to know if plants from these<br />

two sites respond to differences in localized microhabitats by synthesizing different<br />

arrays <strong>of</strong> compounds similar to the case with Ramalina siliquosa in Wales, which<br />

was commented upon above.<br />

6.9.2 Dactylis glomerata (Poaceae)<br />

Dactylis is a small genus thought by some to be monotypic, consisting only <strong>of</strong><br />

D. glomerata L. (cock’s-foot), a Eurasian native now widely naturalized in other<br />

parts <strong>of</strong> the world. That the species is complex can be seen in the recognition <strong>of</strong><br />

15 diploid (2n = 14) members as subspecies (Stebbins and Zohary, 1959; Lumaret,<br />

1988). In Macaronesia, several morphologically and chromosomally distinct entities<br />

are restricted to single islands, and some islands support different subspecies<br />

in different habitats. Dactylis has also been divided into three climatic groups,<br />

mesic-temperate, Mediterranean, and subtropical (Lumaret, 1988), each <strong>of</strong> which<br />

may have both diploid and tetraploid members.<br />

In order to gain a better understanding <strong>of</strong> the relationships and evolutionary<br />

history <strong>of</strong> Dactylis, Lumaret and colleagues have undertaken extensive studies <strong>of</strong><br />

various biochemical markers. <strong>The</strong> fi rst <strong>of</strong> these that can be examined is the fl avonoid<br />

analysis <strong>of</strong> the Atlantic part <strong>of</strong> the subtropical group (Jay and Lumaret, 1995). In all,

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