Net primary production and respiration were estimated in a hypersaline cyanobacterial mat colonizing a gypsum crust in the Eilat salterns, Israel. Two different approaches were used: in situ microprofiling with Clark-type O 2 sensors and application of optode sensor spots in incubation chambers. The net O 2 release rates of the mat phototrophs was high, with a maximum of 3.4 nmol O 2 cm -2 min -1 measured by microprofiling and 4.4 nmol O 2 cm -2 min -1 determined in the incubation chambers. The upper 2 layers of the mat as well as the overlying water quickly became O 2 saturated during the day. The respiration of the whole gypsum crust was also very intensive and corresponded to the O 2 produced by photosynthesis on a diurnal basis, which prevented most of the evolved O 2 from reaching the water. The results presented show that optode sensor spots are useful tools providing additional information about export and photosynthetic production rates of O 2 in hypersaline microbial mats.KEY WORDS: Hypersaline · Gypsum crust · Microbial mat · Net production and respiration · Microelectrode · Optode
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Contribution to AME Special 2 'Progress and perspectives in aquatic primary productivity'OPEN PEN