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The regulation of phytoplankton population dynamics in the
world's largest lakes
Colin S.Reynoldsa, Simon N.Reynoldsa,
I. F. Munawarb, M. Munawarb
aNERC
Institute of Freshwater Ecology, Windermere Laboratory, Ambleside,
LA22 0LP, UK;
bGreat Lakes Laboratory for Fisheries and Aquatic Sciences,
Fisheries and Oceans Canada, P.O.Box 5050, Burlington, L7R 4A6,
Canada |
Abstract
The world's largest lakes, really inland seas, are
characterised by long retention times, and are dominated by internal
physical forcing, generally low nutrient loadings and predominantly
internal recycling. Most are oligotrophic. Many are severely phosphorus
deficient. Certainly few ever support large crops of phytoplankton.
Horizontal heterogeneity sometimes permits enhanced production in
shallow bays or behind thermal bars and occasional blooms develop
under conditions of near-surface stratification.
An assessment of published information on the composition
and seasonality of phytoplankton in the open water habitats of these
lakes confirms the oligotrophic nature of the world's great lakes.
There is a predominance of diatoms at all latitudes; chrysophytes
are seasonally prominent in some lakes at high latitude; other flagellates,
including dinoflagellates, and species of cyanobacteria represent
increasing proportions of the pelagic biomass towards the equator.
There is an indication that species composition is influenced by
underwater light availability and a positive correlation between
Microcystis plankton and relatively higher concentrations of total
phosphorus (TP>30 µg l-1) is suggested. Picoplankton is
apparently abundant during periods of relatively high insolation
of the water column. Although the carrying-capacity of the nutrients
available is scarcely large, the production of biomass is strongly
related to seasonal variability in the intensity and extent of water-
column mixing and its relation to the periodicity and underwater
penetration of photosynthetically- active radiation. Attainment
of nutrient-limited crops generally coincides with shallow mixing
whereas deep circulation suppresses production. The
differential effects of latitude, local climate and salinity upon
this general deduction are also evaluated. The role of grazing,
its contribution to nutrient recycling, and its contribution to
sustaining pelagic food webs, is also considered. The paper makes
some deductions about the threats placed on large-lake ecosystems
by pollution, eutrophication and acidification and upon how their
ecosystem health might be monitored and conserved in the future.
Keywords: Great Lakes; Phytoplankton; Population dynamics
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