During the Arctic Expedition ARK 8/3 (August to October 1991) with RV
'Polarstern', sediment samples from 13 staions with water depths of be
tween 258 and 4,427 m were taken along a transect from the Barents Sea
slope across the deep Arctic Eurasian Basins and the Gakkel Ridge to
the Lomonosov Ridge to determine bacterial biomasses and organic carbo
n contents. Bacterial abundance dropped along the transect from 3.03 t
o 0.63 x 10(8) cells/cm(3), and correspondingly bacterial biomass decr
eased from 17.35 to 3.43 mu g C/cm(3) sediment. Positve correlations w
ere only found between total organic carbon concentrations of surface
sediment layers and biomasses of small coccoid cells and small rods. T
he ridges and slopes seem to be sedimentation areas for the larger coc
coid cells, presumably cyanobacteria.