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1 Introduction Benthic deep-sea foraminifera are a diverse group of shell-bearing unicellular eukaryotes adapted to a wide range of marine microhabitats (e.g., Sen Gupta, 2002). Their distribution is largely determined by the interplay of organic carbon influx, physical and chemical properties of major water masses, and the hydrodynamic regime at the sediment-water interface (Mackensen et al., 1995; Schmiedl et al., 1997; Gooday and Jorissen, 2012).
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