Abstract

Abstract In the eastern Skagerrak a major discontinuity in distribution of species and larval developmental modes of soft-sediment infauna coincides with the border between two distinct current systems. The shelf area, overflown by coastal currents (composed of North Sea and Baltic water) harbours a diverse fauna of interface-feeding species, and planktotrophic larval development is equally common as lecithotrophic development. The basin area, overflown by a current of Atlantic continental-slope origin, which shows up-welling in the basin, harbours a fauna where the interface-feeding category has low diversity and where the planktotrophic mode of development is uncommon. While subsurface detritivores were positively correlated with the amount of sedimenting degradable organic matter, interface feeders showed no clear correlation, and abundance of this category was less variable spatially than the abundance of subsurface feeders. This suggests that numbers of subsurface detritivores are food-limited in the...

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