The distribution of oxygen (O 2 ) at the oxic/ anoxic interface in the water column of two Swiss lakes was measured with sub-micromolar sensitivity, high precision, and high spatial resolution. The O 2 distribution was found to be highly variable and it is shown that N-cycling and the redox gradients of Mn, Fe and CH 4 are controlled by O 2 distributions down to the nanomolar concentration range. The profiles reveal that apparent gaps between the oxic zone and the sites of CH 4 and Mn oxidation are bridged by zones with 0.01-1 lmol L -1 O 2 concentrations and thus CH 4 and Mn oxidation clearly occur at oxic conditions. Directly below the steep oxycline of Lake Rot a broad low O 2 zone in the depth range of 6-7.5 m was now detectable. The O 2 increase during daylight in this zone was comparable to the O 2 flux along the oxycline. Here photosynthesis could be responsible for a substantial part of the chemotrophic oxidation processes. An even broader zone (0.8-3.8 m) with sub-micromolar O 2 and evidence for methanotrophic and lithotrophic activities found at 160 m depth in the deep, dark hypolimnion of Lake Zug was maintained by transport, reaction-and mixing processes. The submicromolar zones could not have been resolved with traditional CTD-profiles. Their existence expands the oxic zone downwards and implies that substantial parts of ''suboxic zones'' characterized by the absence of both O 2 and H 2 S may actually belong to the realm of oxic processes if more sensitive measurement techniques are used for their characterization.