R. Maranger et al., VIRAL AND BACTERIAL DYNAMICS IN ARCTIC SEA-ICE DURING THE SPRING ALGAL BLOOM NEAR RESOLUTE, NWT, CANADA, Marine ecology. Progress series, 111(1-2), 1994, pp. 121-127
High virus counts were found in Arctic sea ice samples taken during th
e spring ice algal bloom near Resolute, Northwest Territories, Canada.
Viral abundances in the sea ice ranged from 3.7 x 10(11) viruses m(-2
) (or 9.0 x 10(6) ml(-1)) to 4.9 x 10(12) m(-2) (1.3 x 10(8) ml(-1)) w
hich is 10- to 100-fold greater than the concentration of viruses in t
he underlying water column (1.1 x 10(6) ml(-1)). This increase in vira
l abundance corresponds with the 10- to 100-fold increase in bacterial
abundance in sea ice as compared with the water column. Bacterial abu
ndances ranged from 6.1 x 10(9) bacteria m(-2) (1.5 x 10(5) ml(-1)) to
4.2 x 10(11) m(-2) (1.0 x 10(7) ml(-1)) from early to late spring res
pectively. The virus-to-bacteria ratios (VBR) were among the highest r
eported in natural samples. The greatest viral abundances occurred in
the 0.5 to 1.5 cm layer of the ice profile, where the bacteria were mo
st active. The VBR generally decreased during the spring although viru
ses were increasing in abundance. The disequilibrium between phage and
bacterial growth and abundance maxima during the spring bloom is sugg
ested to be due to (1) a change in the makeup of the bacterial communi
ty, such that phage-resistant bacteria proliferated later in the sprin
g, or (2) an increase in viral lytic activity with higher bacterial ce
ll-specific growth rates; both viral lytic activity and bacterial grow
th rates declined later in the spring as the bacterial population reac
hed its peak.