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168<br />

Figure 3 middle trace). Therefore, the differential response of these two organisms to<br />

the presence of ginsenosides in their growth medium is coincident with differences in<br />

the profile of ginsenosides that can be recovered from their spent medium.<br />

Interestingly, preliminary observations also show that the recovery of ginsenosides<br />

from the spent broth of Py. irregulare is dependent on the presence of sucrose in the<br />

original culture medium, since significantly smaller amounts of ginsenosides were<br />

recovered from a spent broth lacking sucrose (Yousef and Bernards, unpublished<br />

data). This observation implies that Py. irregulare is using ginsenosides as a source<br />

for carbon. However, the additional observation that mineral broth supplemented with<br />

a concentration of glucose equimolar to that expected to be released into the medium<br />

by ginsenoside de-glycosylation, does not support the same degree of growth increase<br />

in Py. irregulare biomass observed when the same broth is supplemented with<br />

ginsenosides (Yousef and Bernards, unpublished data), argues against a simple carbon<br />

source mechanism. Since Pythium spp. have been reported to incorporate sterols into<br />

their membranes (Olsen, 1973a) and because sterols are known to mediate growth<br />

(Nes, 1987), we now hypothesize that Py. irregulare secretes saponinases to (partially)<br />

deglycosylate ginsenosides, the latter of which are then incorporated as “sterol”<br />

triterpenoids into its membrane. It is further assumed that under the experimental<br />

conditions employed, this incorporation favours growth.<br />

5.1. RETS and Soil Analysis<br />

MARK A. BERNARDS, LINA F. YOUSEF, ROBERT W. NICOL<br />

5. GINSENOSIDES IN THE RHIZOSPHERE<br />

When the soil associated with three-year-old ginseng roots was extracted and analysed<br />

by HPLC, six major ginsenosides were tentatively identified by co-elution with<br />

standards. While much of the soil chemical HPLC profile remains unidentified, HPLC-<br />

MS analysis confirmed the presence of the six major ginsenosides (Rb 1 , Rb 2 , Rc, Rd,<br />

Re and Rg 1 ) plus pseudoginsenoside F 11 and another protopanaxadiol ginsenoside in<br />

the soil extracts (Nicol et al., 2003). The amount of ginsenosides as percent weight of<br />

dry soil was calculated to range from 0.02% to 0.098% (average 0.06%).<br />

In order to confirm that ginsenosides were present in the exudate of intact ginseng<br />

roots, (and not isolated from residual root tissue in our soil preparations) root exudates<br />

were collected from pot-grown ginseng plants using a root exudate trapping system,<br />

or RETS (Tang and Young, 1982). HPLC analysis of the trapped exudate revealed<br />

the presence of peaks that had the same retention times as the ginsenoside standards.<br />

These peaks were not present in the exudate collected from control pots (no ginseng<br />

plants) and were taken as evidence of ginsenosides in the exudate of pots containing<br />

ginseng plants. HPLC-MS analysis of the trapped exudate confirmed the presence of<br />

the same suite of ginsenosides as found in the soil (Nicol et al., 2003). After<br />

quantification of the ginsenoside content of the root exudates, the individual ginseng<br />

plants were determined to be losing approximately 25 µg of ginsenosides per day<br />

(i.e., amount of recovered ginsenoside / number of plants / number of days the<br />

experiment ran).

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