In coastal waters and the ocean silicic acid (Si(OH) 4 ) is a key nutrient for primary producers ( e.g . diatoms) and other siliceous organisms, because it is required for the formation of frustules and other hard parts made of biogenic silica (bSi). Especially in shallow waters like the southern North Sea, dissolution of bSi in surface sediments and the re fl ux of silicic acid from sediments into the water column is an important feedback mechanism for sustaining primary production. We investigated the temporal variability of benthic silicic acid fl uxes and the recycling ef fi ciency of bSi in surface sediments of the Helgoland Mud Area (southern North Sea). For this purpose we used different methods including a benthic chamber lander system for in situ fl ux studies of Si(OH) 4 , ex situ sediment incubations, pore water studies and sediment analysis. Our in situ measurements revealed considerable temporal variations with low silicic acid fl uxes in winter (0.3 – 1.0 mmol m � 2 d � 1 in March 2013 and 2014), increased fl uxes of 2.0 – 4.0 mmol m � 2 d � 1 in November 2013, and high fl uxes in June and August 2012 (3.6 – 8.3 mmol m � 2 d � 1 ). The relevance of biological mediated transport for the recycling of Si(OH) 4 was underlined by comparing in situ and ex situ sediment incubations, pore water studies, as well as depth pro fi les of benthic macrofauna. Mass budget calculations indicate that about 1.7 – 2.2 mol bSi m � 2 settle annually at the sea fl oor, off which about 60 – 81% are recycled within surface sediments and transported back into the water column