Description: Greifensee is a small lake in north-eastern switzerland which has become progressively eutrophic during the last 100 years, as a consequence of higher rates of organic productivity facilitated by an increased nutrient supply. Mckenzie (1982) demonstrated that annual changes in the surface water productivity of greifensee could be followed using the carbon-isotop signal of the desorbed bicarbonate. This integrated study allows us to evaluate the significance of our geochemical signals (i.e. How do the signals respond to productivity changes), to quantitatively model the carbon cycle in a highly productive lake, hence to extrapolate our results to ancient anoxic basins.
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Origins: /Bund/UBA/UFORDAT
Tags: Bicarbonat ? Zürich ? Eutrophierung ? Kohlenstoff ? Nährstoff ? Seensediment ? Schweiz ? Hydrochemie ? Nährstoffkreislauf ? Sediment ? Greifensee ? Isotop ? See [Binnengewässer] ? carbone ? elements nutritifs ? elements radioactifs ? eutrophisation ? lac ?
License: cc-by-nc-nd/4.0
Language: Deutsch
Time ranges: 1983-01-01 - 1985-12-31
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