Aquatic Ecosystem
Topics
Introduction
to Aquatic Ecosystems
As with all ecosystems, aquatic
ecosystems are complex, natural self-sustaining systems made
u of physical and living elements. The interconnected web
they create fluidly spans time and space, with each component
connected in some way to every other component. The connections
within an ecosystem are so profound that any occurrence within
that ecosystem will affect every member in some way, at some
time. The aquatic ecosystems of the Columbia Basin have been
altered by changes to their physical
structure, additions to and deletions from their biological
components, and introduction of toxic compounds.
Water is the most prominent physical
component of an aquatic ecosystem, interacting with the biota,
geography and climate of an area to produce a specific kind
of environment. 99.99% of the Earth’s water is in the
oceans, the remaining 0.01% may take the form of lakes and
ponds or rivers and streams. Geography and climate affect
the behaviour of the water, whether it will stand still or
flow, freeze or evaporate, stagnate or circulate. The water’s
interaction with its environment determines its physical and
chemical properties which in turn affects the productivity,
biodiversity and complexity
of the aquatic community formed therein. Because they are
all connected, the life forms which will flourish depend on
the combined characteristics of the aquatic ecosystem.
Columbia
Basin
In the Columbia Basin there are
lakes and rivers of various sizes. Streams collect fresh water from
extensive watersheds where the forests harbour the annual rain and
snowfall and funnel it downward through pristine valleys into large
rivers and lakes in the valley bottoms. Glacial melt from the high
alpine flows into small alpine lakes or joins the downhill flow.
The water collected in the lakes and rivers holds the nutrients
which will support the first tier of the aquatic food chain: phytoplankton.
Phytoplankton creates food using the sun’s energy and the water’s
nutrients. Tiny microscopic animals will eat the phytoplankton,
and then small fish and other animals eat the zooplankton. Larger
fish will eat the small fish, and mammals of all sorts, including
humans, will feed on the fish. Decomposition will occur at all stages
of the chain and serve to replenish the lake’s nutrient.
The following map shows the major
river and lake networks in the Columbia River Basin.

Macleans magazine recognized
the damming of the Columbia River, a result of the Columbia
River Treaty negotiated between Canada and the USA in 1964,
as one of the 25 major nation-shaping events of the twentieth
century, ranking it as equally significant to giving women
the vote, incorporating Newfoundland and Nunavut into Canada,
creating medicare and the CBC, and the Free Trade Agreement.
In the Columbia Basin, alterations to the physical
structure by hydroelectric dams, and the resulting challenges
to biodiversity have
affected kokanee and trout populations, with consequent effects
on the social, cultural and economic viability of the region.
The following sections outline the biological, structural
and managerial
elements of the aquatic systems in the region.