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Full text: North Sea Summer Survey 2002

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GAUSS 385 
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Longitude [°W/E] 
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shallow areas off Sylt and the coast of Jutland (Fig. 4, vertical temperature sections) 
the bottom water layer is only a few metres thick, so that in calm weather conditions, 
with continued depletion, the plant biomass still available in that area for bacterial 
decomposition could have led to an even stronger depletion of oxygen.
	        
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