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Porewater advection stimulates nutrient exchange and microbial activity in shallow marine sediments, whereas element cycling in deeper diffusion-dominated sediments is comparatively slow due to limited nutrient supply. We studied the vertical distribution of microbial communities and organic matter (OM) cycling in these contrasting porewater regimes down to 5m depth at an intertidal flat of the southern...
A novel approach was developed to follow the successive utilization of organic carbon under anoxic conditions by microcalorimetry, chemical analyses of fermentation products and stable‐isotope probing (SIP). The fermentation of 13C‐labeled glucose was monitored over 4 weeks by microcalorimetry in a stimulation experiment with tidal‐flat sediments. Based on characteristic heat production phases, time...
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