The community composition of denitrifying bacteria was studied in the stratified water column of Lake Kinneret. The nitrite reductase genes nirS and nirK were amplified by PCR from water samples taken at 1, 14, 19 and 22 m depth, which represent the epi-, meta-and hypolimnion of the lake. The PCR products were analyzed with terminal restriction fragment length polymorphism (T-RFLP) and clone libraries. The highest diversity of nirS denitrifying communities was observed at 1 m depth. According to the T-RFLP profiles and clone libraries of nirS products, 2 groups of denitrifiers were common to and dominant in all depths. Deduced protein sequences from one of these groups displayed low identity (77%) with other nirS sequences reported in GenBank. Denitrifying bacterial communities with nirK were most diverse at 22 m and showed highest similarity to those at 19 m depth. Sequences unrelated to nirK dominated the clone libraries from 1 m depth, suggesting that denitrifying bacteria with copper-containing nitrite reductase were less frequent at this depth. The results suggest that microorganisms with nirK and those with nirS respond differently to the environmental conditions in the stratified water column of Lake Kinneret.
KEY WORDS: nirS · nirK · T-RFLP · Lake Kinneret
Resale or republication not permitted without written consent of the publisherAquat Microb Ecol 51: [129][130][131][132][133][134][135][136][137][138][139][140] 2008 ment (Nogales et al. 2002), marine sediments (Braker et al. 2000(Braker et al. , 2001, aquifers (Santoro et al. 2006), seawater (Jayakumar et al. 2004, Castro-Gonzalez et al. 2005) and the oxygen minimum zone of the Black Sea (Oakley et al. 2007). In marine environments a shift in the community structure of nirS denitrifying bacteria occurs along the physical-chemical gradient in the stratified water column (Castro-Gonzalez et al. 2005, Oakley et al. 2007. However, similar studies have never been carried out in stratified freshwater lakes.Lake Kinneret is a monomictic subtropical freshwater lake located in the northern part of Israel. The water column shows a distinct seasonal pattern of chemical stratification characterized by changes in the concentration of dissolved oxygen, nitrate and sulfide. During the period of mixing (December to March), the concentrations of oxygen and nitrate are high throughout the water column. With the onset of thermal stratification in April, followed by the degradation and decomposition of the massive bloom of the dinoflagellate Peridinium gatunense in May, oxygen is consumed and gradually depleted in the hypolimnion so that anoxic conditions arise. At the onset of anaerobiosis, the activity of denitrifying bacteria in the anoxic hypolimnion leads to the use of nitrate. After depletion of the nitrate, sulfate reduction becomes the dominant microbial process in this layer (Hadas & Pinkas 1995, Eckert et al. 2002.During stratification, the distribution of denitrifying communities in the water column is unknown, but is probably coupled to nitrifica...