The role of export and retention food chains for pelagic-benthic coupl
ing is considered by evaluating different food chain scenarios and pro
cesses such as aggregation, grazing and zooplankton-mediated fluxes. T
he consequences of grazing of primary production by different zooplank
ton for the vertical export of particulate organic matter from the eup
hotic zone are discussed. Reference is made to existing data and algor
ithms regarding primary production and vertical export of carbon from
the euphotic zone, both on annual and daily time scales. Examples rega
rding the role of nutrient addition, removal of pelagic carnivores and
zooplankton grazing for vertical flux are presented. It is speculated
how variable grazing impact of micro- and mesozooplankton, as well as
herbivorous, omnivorous and carnivorous feeding strategies of mesozoo
plankton could compete with aggregation during phytoplankton blooms an
d influence export fluxes. It is concluded that the transport of parti
culate organic matter to depth not only depends on bottom-up regulatio
n as determined by physical forcing, but also on the structure and fun
ction of the prevailing planktonic food web. Scenarios are presented w
hich indicate that top-down regulation plays a pivotal role for the re
gulation of vertical flux. This conclusion may have crucial consequenc
es for future biogeochemical programmes investigating pelagic-benthic
coupling in the ocean. The endeavours of many research programmes are
dominated by lines of thought where straightforward biogeochemistry an
d bottom-up regulation is the focus. Phyto- and zooplankton as well as
process-oriented research activities have to be the focal point of fu
ture research if the current comprehension of export from and retentio
n in the upper layers is going to make distinct progress.