5th International Symposium and Field Seminar on Karst Waters and Environmental Impacts, Antalya, Türkiye, 10 - 20 Eylül 1995, ss.269-280
Travertines are terrestrial, fresh water carbonate deposits formed by karstic springs and associated streams which are supersaturated with respect to calcite. Field observations from recently travertine depositing karstic springs in the Aladaglar, Eastern Taurids - Turkey indicate that the deposition process is accelerated considerably by the physical and biochemical contribution of algae which mostly belong to classes of Cyanophyceae (blue-green algae), Chlorophyceae (green algae), Bacillariophyceae (diatoms), Euglenophyceae and Xantophyceae.