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epilimnion

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epilimnion [‚ep·ə′lim·nē‚än]
(hydrology)
A fresh-water zone of relatively warm water in which mixing occurs as a result of wind action and convection currents.


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Maximum temperature difference ([DELTA]T) between the epilimnion and the hypolimnion was attained on 15 June 2006, at all but the deepest location (#6), where maximum AT of 1.
Therefore, as the lake water is stratified nearly all the year round and the water in the epilimnion is oxygen-depleted, it seems that the conditions in the deeper water layers are unfavourable for the bottom fauna and their role in the early diagenesis is modest.
 
 
 
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