|
Aquatic Ecosystem Topics
Biodiversity
"The normal functioning
of our diverse ecosystems depends on the biodiversity of all
species, including fish. Fish need a healthy habitat to survive,
declining fish populations reflect an unhealthy and unstable
ecosystem." MOELP Fisheries website
History of People and Water in the
Columbia Basin
1500 BC to the
1990s
When the first inhabitants
migrated to the Columbia Basin, 3,500 years ago, they found
jagged mountain ranges and valleys full of moist, dense cedar,
hemlock and fir forests laced with streams, rivers and lakes.
The diversity of plants, animals and geography formed the
foundation of a rich native culture. Anadromous (migratory)
chinook and sockeye salmon, steelhead trout and white sturgeon
migrated up the Columbia River from the Pacific Ocean to spawn
in the River's upper reaches, providing food for the forest
animals and replenishing the nutrients in the waterways. The
culture of the Kootenai Indians evolved around these migratory
fish runs which provided food for them and other wildlife
in the area (see Earliest
Beginnings). They also
fished for the rainbow trout, burbot, whitefish and bull trout
which flourished in the lakes.
The waterways of the Columbia
Basin provided transportation up and down the valleys for
the native populations and later for the early explorers.
One of the first recorded exploration trips up the Columbia
River into Arrow Lakes is Emilius Simpson's 1826 trip. He
noted "The Arrow Rock, so named on account of a round
hole in the face full of Arrows, said to have been fired at
it by the Indians when practicing the Bow and Arrow before
a war excursion." (Journal of Emilius Simpson, HBC Archives
B223/a/3 1826 Folio 39D-41). This wall of arrows is the source
of the name "Arrow Lakes".
Non-native settlement in the
Columbia Basin was established when the industrial value was
realized, with mining and logging attracting many people to
the area. Transportation was the most recognized value of
the waterways, with paddlewheelers hauling people and goods
up and down the networks of lakes and rivers. Many communities
flourished in the valley bottoms, where fertile soil provided
great farming. Later, in the 1900s, the hydroelectric potential
of rivers of the Columbia Basin led to the damming of several
lakes and rivers (see Aquatic
Ecosystem Structure). The area's
biodiversity began to falter with the intense industrial pressure
from forestry, mining, manufacturing and hydroelectric power
production.
By the
early 1990s, people began to grasp the full impact of human
intervention on the aquatic ecosystems of the Columbia Basin.
Not only were the large lakes and rivers in a state of ecosystem
collapse as a result of being dammed, but small streams and
entire watersheds were in jeopardy, also, from the intrusions
of industry. Indeed, the rich aquatic biodiversity of the
region currently rests in a precarious state, and residents,
researchers, governments and industry agents are working together
to ensure the waterways of the Columbia Basin flourish again
(see Aquatic
Ecosystem Management).
The
Arrow Lakes Kokanee Connection
Figure
1. Kokanee Spawning (BC Environment, data)
Kokanee salmon are an important
sports fish throughout the Kootenays and a critically important
food source for the larger sport fish: bull trout, rainbow
trout and burbot. An alarming downward trend in kokanee numbers
was noted by anglers and fisheries biologists throughout the
1990s, similar to the observations leading to the fertilization
of Kootenay Lake. Although it was known that damming the Columbia
River at Castlegar, Revelstoke and Mica (see Ecosystem
Structure) eliminated 30% of the Arrow Lakes' kokanee
spawning and rearing habitat, as well as a good proportion
of the rainbow trout and bull trout spawning habitat, it didn't
explain the precipitous drop in populations well after the
dams were built.
Figure 2. Kokanee
Out-migration and Fry Survival (BC Environment data)
Suspicions
that something was wrong with Arrow Lakes itself, rather than
the hatchery or some other problem, were fueled by the discovery
that the survival of fry (baby fish) counted migrating out
from the hatchery and again returning as adults was also declining
precipitously (Figure 2, left). This suggested that, once
in the lake, the fish were not getting enough to eat to grow
and to escape their predators. Possible alternative explanations,
such as a marked increase in predator populations or a disease,
were ruled out by intensive research that began in cooperation
with the University of British Columbia, the Ministry of Environment,
Lands and Parks, BC Hydro and Columbia Basin Fish and Wildlife
Compensation Program.
The research, which includes
studies of water quality, bathymetry, limnology, nutrient
sources, phytoplankton (below), zooplankton (below), mysis
shrimp and kokanee, demonstrated Arrow Lakes was in a state
of ecosystem collapse. After discussing these results in a
series of scientific and public workshops and meetings, fertilizing
began in Arrow Lake in the spring of 1999 to stimulate production
in the troubled aquatic ecosystem.
Sport
Fishing
Sport fishing has always been
popular in the Columbia Basin. While trophy fishing for bull
trout and rainbow trout provides great adventure and eating;
other species including burbot, kokanee and whitefish are
desirable catches also. Almost all accessible small lakes
in the area are stocked with Cutthroat, rainbow or brook trout
raised in the Kootenay Trout Hatchery, which, in 1996, provided
1.25 million fish for release into 174 different lakes (Thorp,
BC MOELP, personal communication). Some small, glacially-fed
alpine lakes in the area are currently being assessed for
suitability for stocking to provide an even broader range
of fishing opportunities (Bray, CBFWCP, personal communication).
Fly fishing is popular in the streams and smaller lakes, while
trolling the lakes for the big fish is rewarding year-round,
whether in the icy cold of winter or summer's lush heat. Fishing
attracts tourists from all over the region, country and world,
many of whom make annual pilgrimmages to Columbia Basin lakes.
It is not just the draw of "food in your belly"
that brings locals and tourists out onto the water but something
deeper and less definable, more spiritual and far more nourishing.
As Glen Olson, third generation angler and Arrow Lakes fishing
charter operator said, "It's kind of hard to explain,
but they're so beautiful it's almost a shame to kill them.
Sometimes they look like rainbows lying in the bottom of your
boat." (from Welcome Home, Stuart McLean, 1992).
For more information, link to http://www.fishbc.com
or http://www.bcadventure.com
Phytoplankton - The Foundation of
Aquatic Life
The
entire food chain in lakes is based on algae. The algae found
in the aquatic ecosystem are more technically known as phytoplankton,
meaning plants suspended in water. Phytoplankton are photosynthetic,
meaning they use the energy of the sun to convert carbon dioxide
into high-energy carbohydrates. When consumers graze upon
algae, the energy held in the carbohydrates is transferred
to the consuming animal, which are then consumed by the next
level of the food chain, and the energy is passed on again.
Algae thus provide the energy for all other growth in the
lakes and streams.
Phytoplankton are autotrophic
photosynthesizers, creating their own food by converting sunlight
into sugars. Because they need to be where the sunlight can
penetrate, phytoplankton spend at least some of their time
in the light-filled limnetic zone. Some of them are able to
move around by using flagella. Phytoplankton also feed the
insects, crustaceans and decomposers living in the profundal
zone of the lake by sinking to the lower levels when they
die.
All phytoplankton need carbon,
potassium, sulfur, calcium, nitrogen and phosphorus molecules
to help build their proteins and other growth molecules; they
cannot make their own nutrient molecules and must therefore
get them from the water in which they live. Potassium, calcium,
and sulfur are in ample supply in aquatic ecosystems; nitrogen
and phosphorus often aren’t. Therefore, phytoplankton
growth in lakes and streams is based on the amount of phosphorus
(P) and nitrogen (N) present in the water. When nutrient shortage
limits plankton growth in an aquatic ecosystem, the system
is called “oligotrophic” (Greek for ‘poorly
nourished’). N and P are used by plankton to build proteins
in an average ratio of 7 N atoms for every P atom. N is 20
times more abundant in most aquatic systems. It is most often
P which is the limiting nutrient in aquatic ecosystems. Dams
and reservoirs alter the natural nutrients available in aquatic
ecosystems (see Aquatic
Ecosystem Structure), affecting the phytoplankton
first and then the rest of the aquatic food chain.
Because algae are so responsive
to their environment, their population diversity and abundance
can be a measure of the general health of the aquatic ecosystem.
Overall, the extremely low abundance and biomass of the phytoplankton
in the Arrow Lakes and the lack of seasonal blooms indicate
an ultra-oligotrophic lake. The same phytoplankton are found
throughout the lake. The most abundant belong to the phyla
Cyanobacteria or blue green algae (>15,000 cells/mL during
a September peak in the Lower Arrow), mainly represented by
various species of Synechococcus. The next most abundant
belong to the phyla Chrysophyta, represented by the nanoflagellate
class Chrysophyceae and the diatom class Bacillariophyceae,
and to the phyla Pyrrhophyta, represented by the dinoflagellate
class Dinophyceae and the flagellate class Cryptophyceae.
An algal bloom is a great burst of phytoplankton population
growth following seasonal nutrient influxes in well nourished
ecosystems. Algal blooms are no longer observed in Arrow Lakes,
although phytoplankton populations do increase seasonally.
The great numbers of the blue-green algae Synechococcus
sp. coupled with the diverse and abundant array of Chrysophyceae
and Cryptophyceae are clear and unambiguous indicators of
the ultra-oligotrophic condition of Arrow Lake. Without healthy
phytoplankton populations, the food web has no foundation
to build upon, ultimately threatening unique stocks of fish.
In Kootenay Lake, the Dinophyceae
(diatoms) have traditionally dominated, with Cryptophyceae
and Chrysophyceae present and Cyanobacteria making up a very
small part of the picture. A five year artificial fertilization
experiment began in 1992 on Kootenay Lake, supplying phosphorus
to phytoplankton, and they have increased in abundance since
then (see Aquatic
Ecosystem Management). The diatoms have responded
particularly well, with Tabellaria, a species indicative
of moderate nutrient availability, experiencing a large bloom
in 1994. The following table demonstrates the positive impact
fertilization has had on Kootenay Lake phytoplankton:
|
Year
|
Annual phytoplankton biomass (mg/mm3)
|
| |
Station
2 (fertilized) |
Station
6 (control) |
| 1992 |
445 |
359 |
| 1993 |
658 |
364 |
| 1994 |
900 |
477 |
Arrow Lakes is now being fertilized
also in the hopes of stimulating the food chain and preserving
the trophy rainbow and bull trout stocks for which the Arrow
Lake is renowned.
Zooplankton
Copepod zooplankton
with egg sacs
Zooplankton
are microscopic animals suspended in water. Zooplankton are
heterotrophic which means they cannot make their own food
and must, therefore, consume plants (herbivores) or animals
(carnivores). Zooplankton are able to move about minimally
to secure food or to migrate diurnally through the water column
(moving up and down daily), occupying both the limnetic zone
where sunlight penetrates and the dark profundal zone. Zooplankton
are consumed in the light-filled limnetic zone by larger zooplankton,
insects, and kokanee, which hunt visually, or in the profundal
zone by crustaceans such as Mysis shrimp, decomposers and
bottom feeders living there.
- Daphnia, a Cladoceran zooplankton
- drawings by Heather MacKay
-
- All of the zooplankton
discussed are greater than 150 um in size, as that was
the pore size in the Clarke-Bumpus sampling net researchers
used in the Kootenay and Arrow Lakes fertilization experiments.
-
Zooplankton
abundance indicates that Arrow Lakes is less productive
than Kootenay Lake, with 7 individuals/L as compared with
19 individuals/L, respectively. There was a greater proportion
of cladocerans, the preferred food of kokanee and mysids,
in the Arrow system. The Lower Arrow had an especially
healthy population of water fleas, or Daphnia (see drawing),
the cladoceran making up about 90% of kokanee’s
diet.
-
-
Water flea, a Cladoceran
zooplankton
Mysids
In 1949, mysid shrimp (Mysis
relicta) were introduced into Kootenay Lake as an intermediate
food source for rainbow trout as they grew and switched from
eating Daphnia (zooplankton) to eating kokanee fry. An increase
in the number and size of kokanee in the 1960’s was
mistakenly attributed to the introduction of the mysid shrimp,
which were thought to be acting as a food source for the kokanee.
This resulted in the unfortunate introduction of mysids to
hundreds of lakes in North America and Scandinavia. The mysids
can be detrimental because, although some are eaten by kokanee,
they also compete with the kokanee for plankton, their primary
source of food.
Mysid shrimp, Mysis relicta
When
fertilizing, mysid shrimp were an ecological wild card, leaving
scientists unable to predict whether the shrimp would out-compete
the kokanee for the new zooplankton food source expected.
It is now believed that the shrimp graze on the zooplankton
in the productive limnetic layer at night and then migrate
down in the water column during the day where the kokanee
are less able to hunt them. Kokanee hunt by sight in the limnetic
layer during the day. The mysids show no growth trend as of
yet, but they are being carefully monitored lest they suddenly
upset the ecological apple cart.
Average annual mysid density
in the Upper and Lower Arrow were 32 and 63 individuals per
square meter, respectively, while Kootenay Lake had a density
of 120 individuals per square meter. Although the mysid shrimp
competition did not cause the collapse of the Arrow Lakes
ecosystem, it could have been a direct contributor to the
decline of the kokanee populations.
Fish
The Columbia Basin supports
27 native species of fish including rainbow trout, bull trout,
kokanee, mountain whitefish, burbot and white sturgeon, as
well as a number of smaller fish, some of which are now officially
endangered (see Endangered Species).
Changes to the physical structure
of the system have eliminated the spawning migrations of several
of these and caused other changes that have diminished the
productive capacity of aquatic systems (see above). Consequently,
many of the fish populations are currently in a state of stress
(not to say crisis), and this is occupying considerable management
attention (see Ecosystem
Management).
The Columbia and its tributaries
contain one of the most distinctive fish faunas in North America
(Miller, 1965, in McPhail and Carveth, 1992), all of which
probably survived the Pleistocene glaciations (see Earliest
Beginnings) somewhere within the Columbia system. Nine Columbia
species (35%) are endemic, i.e., they evolved within the system.
No other drainage system in British Columbia contains this
number of endemic species, and it is these Columbia endemics
that set the B.C. freshwater fish fauna apart from that in
the rest of Canada (McPhail and Carveth, 1992).
Because of the mountainous
terrain, there are barriers (falls and rapids) on most upper
Columbia tributaries, above which only trout or char occur.
In the lower Columbia and Kootenay system, where the gradient
lessens, the environment is more benign and the number of
species increases until, near the U.S. border, all 27 native
species and numerous exotics (see below) are present, either
in the main rivers or their tributaries (McPhail and Carveth,
1992). However, the upstream distribution of a number of species
of dace and sculpins has been limited by Bonnington Falls,
on the Kootenay River below Kootenay Lake, and the 3-5 metre
vertical drop where the Pend d'Orielle River enters the Columbia
River (McPhail and Carveth, 1992).
In addition to the native
species, some 16 exotic species
(37%) now occur in the Columbia Basin. This is a higher proportion
of introduced species than in any other river system in British
Columbia (McPhail and Carveth, 1992). Most exotics (brook
trout, brown trout, lake trout, broad whitefish, carp, goldfish,
tench, brown catfish, black catfish, pumpkin seeds, black
crappie, largemouth bass, smallmouth bass, yellow perch and
walleye) are found in the lower Columbia and Okanagan drainages.
One of these, largemouth bass, has become a sports fish (for
example, at Duck Lake in the East Kootenay), but the others
are mainly pests, or potential pests.
Brief notes on the major sports
fish follow:
Kokanee (Oncorhynchus merka)
Kokanee, landlocked sockeye
salmon, are present in large lakes and rivers throughout the
Columbia Basin. They have small mouths and eat mainly zooplankton,
preferring a diet of about 90% Daphnia. Kokanee feed
during the day, hunting their food by sight. They will prey
on mysid shrimp if possible, but the mysids feed in the dark
and migrate down during the day to where no light penetrates
and kokanee can't see them. In their night feedings, mysids
are competitors for the limited zooplankton prey. Kokanee
are a popular sport fish, and the main prey item for bull
trout and large rainbow trout.
Kokanee show the first response
to a decrease in lake productivity, so their numbers reflect
the health of the ecosystem (Ney, 1996). The trend in Kootenay
Lake kokanee numbers echoes dam construction, mysid introduction,
fertilizer plant operations and lake fertilization, increasing
in the1960s when the Kimberley fertilizer plant was fully
operational, peaking in the early 1970s, dropping in the 1980s
and declining steadily from 1986 to 1991. In 1991 kokanee
numbers were about 150 fish per hectare. Research indicated
a worsening crisis and convinced scientists and fisheries
managers to proceed with fertilization on a trial basis. Since
fertilization began in 1992, kokanee numbers have increased
to their 1998 population density of 600 - 1000 fish per hectare,
totalling 25 - 30 million kokanee in Kootenay Lake. There
are roughly five million kokanee in the Arrow Lakes. They
are found at depths between five and 35 m and preferably at
temperatures between seven and 13.5 degrees C.
Bull Trout (Salvelinus confluentus)
Formerly called Dolly Varden
trout (actually a char), bull trout are now recognized as
a separate species. A consumate predator,
bull trout have a large head, sharp teeth, and a relatively
small, narrow body. They are blue-listed in British Columbia
("vulnerable") and are of management concern for
various threats, including logging and hydroelectric development.
For example, an estimated 4,000 adult spawners were lost to
the Revelstoke dam alone (Pieters et al., 1998).
By providing more food (kokanee)
for the resident Gerrard rainbow and bull trout populations
in Kootenay Lake, fertilization has resulted in larger and
more numerous stocks, benefiting the local sports fishery.
Overall, both rainbow and bull trout in Kootenay Lake have
been increasing by two pounds per year since fertilization
began in 1992, with anglers now recording rainbow and bull
trout as large as 29 pounds. A similar trend is hoped for
in Arrow Lakes.
Bull trout raised at the Hill
Creek Hatchery are released in Arrow Lakes at the mouths of
various creeks. In 1996, for example, 29,077 bull trout were
released into Snow, Illecillewaet, Hill and St. Leon Creeks.
This program has been scaled back until fertilization has
proven successful.
Cutthroat Trout (Oncorhynchus
clarki lewisi)
Isolated populations of Westside
cutthroats, a separate subspecies, occupy specific parts of
the Columbia drainage. Blocked from migration by impassable
falls, they have become so distinct that another species designation,
O. c. alpestris, has been proposed (but not widely
accepted) for those in the Revelstoke area, such as those
in Akokolex Creek (McPhail and Carveth, 1992). Sometime after
BC's last Ice Age, they occupied extensive ranges in the Columbia
Basin in the absence of vigorous predators (such as bull trout).
As the ice melted, the water level dropped, and natural dams,
formed by massive ice chunks or terminal moraines, washed
out. This isolated certain populations behind falls, while
the rest occupied the lower elevation water ways. Later, predators
accessed the system from downstream and eliminated all the
fish below the falls. Thus, the populations above the falls
diverged, evolving to succeed in their unique habitat. Thus,
a legacy of variety remains in our native fish species, including
unique ones like these relic populations of cutthroat trout.
Kootenay Trout Hatchery raises
Westslope (Yellowstone) cutthroat trout to stock the area's
smaller lakes. In 1996, for example, 33 lakes, primarily in
the East Kootenays, were stocked with a total of 119,500 cutthroats
for sport fishing.
Gerrard Rainbow Trout
(a race of Oncohyrnchys mykiss)
22 pound (below)
and 15 pound (right) Gerrard Rainbow Trout caught on Arrow
Lakes Photos coutesy of Glen Olson Fishing Charters
The Gerrards, named for an
abandoned mining town near their spawning grounds at the outlet
of Trout Lake, are a giant race of rainbows that made Kootenay
Lake famous for its fishing. However, fishing, nutrient overloading
from a fertilizer plant, nutrient starvation because of power
dams (Duncan, Libby) and the inappropriate introduction of
an exotic crustacean (mysid shrimp) brought them to the edge
of extinction, with only a few hundred breeding females observed
from the early 1980s and onwards. The Gerrard rainbow trout
have responded well to the fertilization of Kootenay Lake,
achieving sizes of up to 29 pounds in 1998 and returning to
spawn in greater numbers every year. Kootenay Trout Hatchery
raises the Gerrard stock to release into smaller lakes in
the East and West Kootenays and other parts of BC. In 1996,
16 lakes were stocked with 183,465 Gerrard rainbow trout.
That year, a total of 1,002,628 rainbow trout (various stocks)
were raised at the Kootenay Trout Hatchery and used to stock
113 different systems.
Yellowfin Rainbow Trout
(a race of Oncohyrnchys mykiss)
The yellowfins, native only
to Arrow Lakes, began disappearing soon after construction
of the Keenleyside, Mica and Revelstoke dams, apparently having
lost spawning habitat and nutrients. An estimated 3,000 adult
were lost following dam construction (Pieters et al., 1998).
They may be further threatened by the introduction of Gerrard
rainbows into Arrow Lakes in the 1980s. These fish were large,
up to 14 kg, with distinctive yellow colouration on their
bellies, pectoral, pelvic and anal fins (Pieters et al., 1998).
According to local anglers, a remnant population remains,
yet they have proven elusive to fisheries biologists. Thus,
attempts to preserve and enhance the stock have been unsuccessful
so far.
Burbot or Ling Cod (Lota lota)
Ling
cod caught on Arrow Lakes
Ling
cod are considered primarily a coarse fish, although they
are sought for food periodically. They are fished by jigging
in ling holes where they swarm in small groups. They have
elongated bodies, brown/yellow colouration and wide flat heads.
Ling are predatory, with a diet consisting mostly of other
fish. Ling cod are common in lakes throughout the Columbia
Basin and all of North America.
-
White Sturgeon (Acipenser
transmontanus)
White sturgeon are huge, long-lived
fish, up to 800 kg in weight and over 100 years old (Cannings,
1993). A resident of large, cool rivers, they formerly occurred
in the entire Columbia River, migrating from the ocean to
spawn in its upper reaches. Until recently, because of dams,
they are only found below Keenleyside Dam below Corra Linn
Dam in the Kootenay system. In 1999, however, a small population
has been found spawning in the Columbia River below Revelstoke
Dam. They formed the basis of a commercial fishery for caviar
in the early 1900s, and they still provide excellent eating
where it is legal to catch them. They are not known to have
spawned in these systems "...since the construction of
the hydroelectric dams" altered their spawning habitat
(Haas, 1996), and they may be further challenged by toxic
chemicals and overfishing. According to Larson, 1998, "...construction
and operation of hydropower systems have severely impacted
white sturgeon populations in the Columbia River basin. Dams
have not only blocked upstream spawning and feeding migrations,
but they have also altered and/or destroyed much of the spawning
habitat. Dams and their associated reservoirs have also altered
food availability, natural flow patterns, and water temperatures."
For more information: http://www.worldstar.com/~dlarson/SturgeonoftheColumbia.htm
References
- Ashley et al., 1996. Fisheries
Project Report No. RD 49, 1996.
Cannings, S., 1993. Rare Freshwater fish of British
Columbia. B.C. Conservation Data Centre Report No. 1.
Haas, G.R., 1996. Categorization and assessment
of indigenous fish species at risk in British Columbia,
with recommendations and prioritizations for research,
inventory and conservation. Fisheries Management and Environment
Report, Ministry of Environment Lands and Parks.
Larson, D., 1998. Notes posted at http://www.worldstar.com/~dlarson/SturgeonoftheColumbia.htm
- McLean, Stuart, 1992. Welcome Home. McGraw-Hill,
Toronto.
McPhail, J.D. and R. Carveth, 1992. A foundation
for conservation: The nature and origin of the freshwater
fish fauna of British Columbia. Univ. of B.C.
Ney, 1996.
- Pieters, R., L.C. Thompson, L. Vidmanic,
S. Pond, J. Stockner, P. Hamblin, M. Young, K. Ashley,
B. Lindsay, G. Lawrence, D. Sebastian, G. Scholten and
D. L. Lombard, 1998. Arrow Reservoir limnology
and trophic status - Year 1 (1997/98) Report. B.C. Ministry
of Environment, Lands and Parks.
-
-
-
- Aquatic Ecosystem Topics
-
|