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Seasonal dynamics of stable isotopes and element ratios in authigenic calcites during their precipitation and dissolution, Sacrower See (northeastern Germany)

Philipp BLUSZCZ, Andreas LÜCKE, Christian OHLENDORF, Bernd ZOLITSCHKA
2009 Journal of Limnology  
The seasonal evolution of chemical and physical water properties as well as particle fluxes was monitored in Sacrower See (northeastern Germany) during two consecutive years (Oct 2003 -Oct 2005). Additonally, we measured δ 18 O and δ 13 C as well as Sr:Ca and Mg:Ca ratios of authigenic calcites that were collected in sequencing sediment traps in order to disentangle environmental and climatic factors controlling these parameters. In particular, our aim was to find out if element ratios and the
more » ... ent ratios and the isotopic composition of calcites reflect changes in water and air temperatures. Lake water is highly enriched in 18 O (-1.3 to -2.5‰ VSMOW) with an evaporative increase of 0.6‰ during summer. Values are 5-6‰ more positive than groundwater values and 4-5‰ more positive than long-term weighted annual means of precipitation. During spring and summer, high amounts of dissolved phosphate cause eutrophic conditions and calcite precipitation in isotopic disequilibrium. Measured values are depleted in 18 O by 2 to 10‰ compared to calculated equilibrium values. Resuspension and partial dissolution of calcite in the water column contribute to this isotopic divergence in summer and autumn as δ 18 O ca and δ 13 C values increased in the hypolimnion during this time. Mg:Ca and Sr:Ca ratios are altered by dissolution as well. In the hypolimnion these ratios were higher than in the epilimnion. Another reason for the huge deviation between measured and theoretical δ 18 O ca values during summer is the occurrence of large amounts of Phacotus lenticularis in the carbonate fraction. High amounts of Phacotus lead to more negative δ 18 O ca and more positive δ 13 C values. Several characteristics of δ 18 O ca and δ 13 C are also reflected by Mg:Ca and Sr:Ca ratios and isotopic composition of oxygen and carbon were influenced by the onset and stability of stratification. Especially the earlier onset of stratification in 2005 caused higher sediment fluxes and more positive carbon and oxygen isotope values of bioinduced carbonates compared to 2004.
doi:10.4081/jlimnol.2009.257 fatcat:lhccwjk6cjeq3amj2x3z77zs44