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Is Lake Erie a resilient ecosystem?
M. Munawar, I. F. Munawar, R. Dermott, H.
Niblock, S. Carou
1Great
Lakes Laboratory for Fisheries and Aquatic Sciences.
Department of Fisheries and Oceans Canada.
867 Lakeshore Rd. Burlington, Ontario, L7R 4A6 Canada.
2Plankton
Canada, 685 Inverary Road, Burlington, Ontario, L7L 2L8 Canada.
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Abstract
Lake Erie has a long history of natural
and cultural perturbations ranging from glacial origins, arrival
of Europeans, exploration-early colonization, degradation, exotic
invasion, and phosphorus reduction to its recent recovery. Is Lake
Erie a resilient ecosystem responding to phosphorus abatement and
exotic invasion? It is believed that Erie was an oligotrophic system
when glaciers receded followed by a long period of mesotrophic conditions.
It has been classified from mesotrophic to eutrophic ecosystem during
the past three decades. In the 1970s the Great Lakes Water Quality
Agreement was signed between Canada and the United States and steps
were taken to reduce the phosphorus loading to the Great Lakes including
Lake Erie. Total phosphorus and chlorophyll a levels in the eutrophic
west have dropped from 41 µg L-1
and 13.8 µg L-1 M the 1970s
to <20 µg L-1 and 5.6
µg L-1 in the 1990s. Similarly
a sign significant decrease in phytoplankton biomass was recorded
from 1970 to 1992 in the western basin. During the same period Diatomeae
decreased markedly from 55% to 10% whereas Chlorophyta increased
from 8% to 55%. Similar trends were evident in the other biota.
Primary production rates in the 1990s were dominated by small sized
organisms (Pico plankton and nanoplankton) similar to Lake Superior-a
pristine oligotrophic ecosystem. Based on several criteria such
as reduction of biomass and primary production, high species diversity,
decrease of eutrophic and increase of mesotrophic-oligotrophic species
and prevalence of picoplankton-nanoplankton, Lake Erie appears to
be a rapidly changing and resilient ecosystem altering from eutrophic
to meso-oligotrophic conditions. These observations are also supported
by the response of other biota such as zooplankton and benthos.
For example during 1993 the non-zebra mussel benthic biomass in
the western basin had returned to a similar composition observed
earlier in 1952 including the recovery of the mayfly. On the other
hand eastern basin benthos has not shown the same extent of recovery
as the west Fish community trends are very complex, but the return
of the walleye and whitefish in the western and eastern basins respectively
are encouraging signs of recovery. The changes observed at various
trophic levels are indicative of a meso-oligotrophic environment.
Keywords: recovery, phosphorus, phytoplankton, species,
exotics, zebra mussels
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