Factors Controlling Extremely Productive Heterotrophic Bacterial Communities in Shallow Soda Pools A. Eiler, 1 A.H. Farnleitner, 2 T.C. Zechmeister, 3 A. Herzig, 4 C. Hurban, 5 W. Wesner, 5 R. Krachler, 5 B. Velimirov, 1 A.K.T. Kirschner 1 1 Institute of Medical Biology, Vienna University, Waehringerstr. 10, A-1090 Vienna, Austria 2 Institute of Chemical Engineering, Technical University, A-1060 Vienna, Austria 3 Institute of Bacteriology, Mycology, and Hygeine, University of Veterinary Medicine, A-1210 Vienna, Austria 4 Biological Research Institute Burgenland, A-7142 Illmitz, Austria 5 Institute of Inorganic Chemistry, Vienna University, A-1090 Vienna, Austria Received: 20 June 2002; Accepted: 23 December 2002; Online publication: 13 May 2003 A B S T R A C T Dilute soda lakes are among the world’s most productive environments and are usually domi- nated by dense blooms of cyanobacteria. Up to now, there has been little information available on heterotrophic bacterial abundance, production, and their controlling factors in these eco- systems. In the present study the main environmental factors responsible for the control of the heterotrophic bacterial community in five shallow soda pools in Eastern Austria were investi- gated during an annual cycle. Extremely high cyanobacterial numbers and heterotrophic bac- terial numbers up to 307 · 10 9 L )1 and 268 · 10 9 L )1 were found, respectively. Bacterial secondary production rates up to 738 lgCL )1 h )1 and specific growth rates up to 1.65 h )1 were recorded in summer and represent the highest reported values for natural aquatic ecosystems. The combination of dense phytoplankton blooms, high temperature, high turbidity, and nutrient concentration due to evaporation is supposed to enable the development of such extremely productive microbial populations. By principal component analysis containing the data set of all five investigated pools, two factors were extracted which explained 62.5% of the total variation of the systems. The first factor could be interpreted as a turbidity factor; the second was assigned to as concentration factor. From this it was deduced that bacterial and cyanobacterial abundance were mainly controlled by wind-induced sediment resuspension and turbidity stabilized by the high pH and salinity and less by evaporative concentration of salinity and dissolved organic carbon. Bacterial production was clustered with temperature in factor 3, showing that bacterial growth was mainly controlled by temperature. The concept of describing the turbid water col- umns of the shallow soda pools as ‘‘fluid sediment’’ is discussed. Correspondence to: A.K.T. Kirschner; E-mail: alexander.kirschner@univie.ac.at Microb Ecol (2003) 46:43–54 DOI: 10.1007/s00248-002-2041-9 Ó 2003 Springer-Verlag New York Inc.