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Fig. 3. Hydrochemical evolution of karstwaters from spring sites downstream, during successive CO 2 degassing. (a) Westerh¨fer Bach, western Harz Foreland. (b) Deinschwanger
Bach, Franconian Alb. (c) Reinsgraben at the Schillerwiese in G¨ttingen. (d) 'Steinerne Rinne' of the Erasbach rivulet, Franconian Alb. Note that the hydrology of the
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Tufas and Speleothems: Unravelling the Microbial and Physical Controls
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