On the basis of results that largely have been derived from the Norweg
ian research programme Pro Mare (1984-1989), an overview of the distri
bution of biomass and productivity at different trophic levels of the
pelagic Barents Sea ecosystem is presented, with comments on year-to-y
ear and horizontal variations. Average biomasses for the whole Parents
Sea and several years range from 2000 kg of carbon km(-2) for each of
Calanus spp. and phytoplankton stocks, down to 0.1 kg carbon km(-2) f
or the polar bear population. Phytoplankton blooms that deplete the wi
nter nutrients give rise locally to a ''new'' productivity of 40-50 g
C m(-2). Areal differences, however, are pronounced in terms of annual
productivity: the ''new'' fraction is more than twice as high in the
southern (Atlantic) part of the Barents Sea as in the areas north of t
he oceanic Polar Front (90 vs. <40 g C m(-2) yr(-1)). Wind-generated v
ertical mixing (in association with passing atmospheric depressions) a
nd turbulence generated on and around banks in the southern part are c
rucial in accounting for this difference. In the northern half of the
Parents Sea a pronounced upper layer stability caused by the supply of
meltwater from seasonal ice retards mixing so that ''new'' production
is small following the depletion of winter nutrients - high productiv
ity is restricted to the 20-50 km wide ice edge bloom. Year-to-year va
riations in fish stocks are pronounced and have always been so there e
xists no ''ecological balance'' in any meaningful sense. These variati
ons are clearly related to the influx of Atlantic water to the Parents
Sea (i.e. ''warm'' years are high-productive years) and, thus, ultima
tely to the same forcing factors that determine climate variations in
coastal Europe. Thus, sound management may diminish the annual fluctua
tions in fish stock sizes but certainly cannot eradicate them. (C) 199
7 International Council for the Exploration of the Sea.