Marko Lipka

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In this study, we analysed metagenomes along with biogeochemical profiles from Skagerrak (SK) and Bothnian Bay (BB) sediments, to trace the prevailing nitrogen pathways. NO3 − was present in the top 5 cm below the sediment-water interface at both sites. NH4 + increased with depth below 5 cm where it overlapped with the NO3 − zone. Steady-state modelling of(More)
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