We studied on an isolation of chlorophyll
a for determination of stable isotope ratios of carbon (δ
13C) and nitrogen (δ
15N) and applied it to determine in
Microcystis spp. from Suwa lake, Japan. The algae were collected four times between June and September, 1987 by using a 20l plankton net (40μm, mesh size). Collected freezed-samples (7.320.6 g, wet base) ground with anhydrous Na
2SO
4 using a mortor and a pestle were extracted with acetone (200 ml). The extracts were precipitated with 1, 4-dioxane (crude chlorophyll) and consequently purified chlorophyll
a (2.38.1 mg) was obtained quantitatively by successive chromatography with DEAE-Toyopearl 650 M (2288μm) and Sepharose CL6B (45165μm) packed in glass tubings. The ratio, (δ
13C, ‰ ) of chlorophyll
a in the algae had changed from -33.8±0.05 in June 19 to -27.5±0.3 September with different growth. Difference (Δ
13C) between δ
13C of chlorophyll
a and that of a whole body of the algae had also changed from -9.4±0.05 to -3.4±0.1.Comparing to the carbon ratios, the both ratios of δ
15N and Δ
15N slightly changed from 22.0 to 23.5 and 12.9 to 16.0, respectively. The change of heavy isotopes in Δ
13C and Δ
15N was reverse: The heavy carbon was depleted and heavy nitrogen was enriched.
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