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The varying radiocarbon activity of some recent submerged Estonian plants grown in the early 1990s.

Ingrid U Olsson, Enn Kaup

Abstract


Eleven samples of aquatic plants from three Estonian lakes were analyzed for their radiocarbon content in a collaboration between the laboratories in Tallinn and Uppsala. delta (super 13) C values for the actual species were compiled to allow normalization of activities measured in Tallinn without delta (super 13) C values. The range for well determined species is usually a few per mil and the statistical uncertainty > or =1 per mil delta (super 13) C values vary considerably for different Potamogeton species and Myriophyllum spp. Lake Antu Sinijarv and Lake Paidre are hard-water lakes containing 300 and 200 mg HCO (sub 3) -/L, respectively. One sample consisted of a carbonate crust deposited on a Ceratophyllum demersum plant in L. Antu Sinijarv. Its delta (super 14) C value was -147.3+ or -6.7 per mil in 1990, whereas the plant had a value of -74.1+ or -8.0 per mil (delta (super 13) C = -35.0 per mil). The same species in L. Paidre had a delta (super 14) C value of +8.0+ or -8.8 per mil (delta (super 13) C = -25.2 per mil) in 1992. Other species in L. Paidre contained more (super 14) C, from a delta (super 14) C value of about +30 per mil to about +155 per mil, the latter value measured in Tallinn on floating leaves of Nuphar lutea, close to that of the contemporaneous atmospheric CO (sub 2) . In the third lake, Lake Punso, containing >30 mg HCO (sub 3) -/L, the stems of Nuphar lutea exhibited in 1990 a memory effect: the activity, delta (super 14) C = 209.6+ or -10.3 per mil, significantly exceeded that of the contemporaneous atmospheric CO (sub 2) . However, the floating leaves of the same plant had the delta (super 14) C value 143.1+ or -10.0 per mil, close to the atmospheric (super 14) C level in 1990. The memory is explained by nutrients stored in the root stock, used when the growth starts.

Keywords


species diversity;activity;modern;aquatic environment;lake sediments;lacustrine environment;Baltic region;Estonia;Tallinn Estonia;C 14 C 12;atmosphere;isotope ratios;Holocene;upper Holocene;Plantae;biochemistry;Europe;sediments;Cenozoic;Quaternary;C 14;carbon;isotopes;radioactive isotopes;carbon dioxide;C 13 C 12;stable isotopes;geochemistry

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