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The Geography of Phytochemical Races

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4.1 Across the Atlantic Ocean 177<br />

Table 4.1 Glucosinolates in seeds <strong>of</strong> Cakile maritima and C. arabica (from Rodman, 1976)<br />

Glucosinolate C. maritima subsp. a C. a.<br />

CMBA CMMW CMMM CMEU CARA<br />

Isopropyl trace 3.7 23.8 0 58.5<br />

Allyl 80.3 12.2 9.0 99.9 23.0<br />

sec-Butyl 16.3 84.8 34.0 0 17.0<br />

3-Butenyl trace 0 2.8 0 trace<br />

3-Methylthiopropyl 1.0 trace 4.9 trace 0<br />

4-Methylthiobutyl 0 0 12.1 0 0<br />

5-Methylthiopentyl 0 0 10.8 0 0<br />

a CMBA = subsp. baltica; CMMW = subsp. maritima from western Europe; CMMM = subsp.<br />

maritima from the Mediterranean; CMEU = subsp. euxima; C. a. = CARA = C. arabica.<br />

Unique among the collections reported in this study was the chemistry <strong>of</strong> subsp.<br />

euxima whose glucosinolate pr<strong>of</strong>i le consisted essentially <strong>of</strong> a single compound,<br />

allyl glucosinolate.<br />

It is interesting, and relevant, to look at Rodman’s views on the evolution <strong>of</strong><br />

Cakile, as discussed in his 1976 paper. Cakile arabica Velen. is seen as the primitive<br />

species in the genus (or most closely resembling the primitive form) based on morphological<br />

considerations, breeding system (it is strongly self-incompatible), and<br />

the capacity to utilize the aliphatic amino acids isoleucine, methionine, and valine<br />

for the production <strong>of</strong> glucosinolates. It is also important to note that C. arabica is<br />

endemic to the deserts around the Persian Gulf and that the evolution <strong>of</strong> the beach<br />

lifestyle in other Cakile species is considered to be an adaptation to the expanding<br />

availability <strong>of</strong> sandy beach habitats associated with the development <strong>of</strong> the<br />

Tethys Sea (proto-Mediterranean Sea). Migration <strong>of</strong> Cakile to new areas in Western<br />

Europe was accompanied by partial relaxation <strong>of</strong> self-incompatibility, simplifi cation<br />

<strong>of</strong> glucosinolate pr<strong>of</strong>i les in terms <strong>of</strong> the number <strong>of</strong> compounds, for example,<br />

C. maritima subspecies euxima and baltica, and in some cases, elongation <strong>of</strong> the<br />

precursor amino acids and oxidation <strong>of</strong> methylthioalkyl glucosinolates to the corresponding<br />

sulfi nyl [308] and sulfonyl derivatives [309].<br />

Colonization <strong>of</strong> the New World, thought to have occurred during late Pliocene<br />

or Pleistocene times, was accompanied by further reduction <strong>of</strong> self-incompatibility<br />

and simplifi cation <strong>of</strong> glucosinolate pr<strong>of</strong>i les. A complicating factor in the overall<br />

chemical simplifi cation trend is the capacity <strong>of</strong> the New World species to utilize<br />

aromatic amino acids as precursors in glucosinolate biosynthesis; phenylalanine is<br />

converted to benzyl glucosinolate [310] and to 2-phenylethyl glucosinolate [311]<br />

after one round <strong>of</strong> elongation. Rodman (1976) pointed out that it is not possible to<br />

distinguish between this new biosynthetic pathway having been developed de novo<br />

in New World taxa, or whether this represents a release <strong>of</strong> a repressed pathway.<br />

It had been suggested by Rodman (1974) that the naturalized C. maritima along<br />

the western coast <strong>of</strong> North America originated from plants growing along the shore<br />

<strong>of</strong> the western Mediterranean. This possibility gained a good deal <strong>of</strong> support from the<br />

discovery that the glucosinolate pr<strong>of</strong>i le <strong>of</strong> the North American plants bears close similarity<br />

to that <strong>of</strong> plants from the western Mediterranean. It also appears that the western

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