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                  <text>The research in this publication was partially or fully funded by Colorado Parks and Wildlife.

Dan Prenzlow, Director, Colorado Parks and Wildlife • Parks and Wildlife Commission: Marvin McDaniel, Chair • Carrie Besnette Hauser, Vice-Chair
Marie Haskett, Secretary • Taishya Adams • Betsy Blecha • Charles Garcia • Dallas May • Duke Phillips, IV • Luke B. Schafer • James Jay Tutchton • Eden Vardy

�American Fisheries Society Symposium 9:49-64. 1991

Interactions of Zooplankton, Mysis relicta, and Kokanees in
Lake Granby, Colorado
PATRICK J. MARTINEZ
Colorado Division of Wildlife, 317 West Prospect, Fort Collins, Colorado 80526. USA
ERIC P. BERGERSEN
U.S. Fish and Wildlife Service. Colorado Cooperative Fish and Wildlife Research Unit'
Room 201 Wagar Building, Colorado State University. Fort Collins, Colorado 80523, USA
Abstract. In studies of zooplankton and kokanees Oncorhynchus nerka in Lake Granby,
Colorado, conducted from 1981 to 1983, we investigated the suspected role of introduced Mysis
relicta in the decline of the kokanee sport fishery and egg take. Mysis relicta entered surface waters
at night and preyed on zooplankton, except when summer temperatures above 14°C excluded it
from the epilimnion and created a temporary refuge for cladocerans. We attributed the disappearance of hypolimnetic Daphnia longiremis to predation by mysids, and the virtual elimination of
Daphnia pulex (once the preferred item in the kokanee diet) to the effects of intense selective
predation by abundant M. relicta and to kokanee overstocking. Daphnia galeata mendotae,
historically the most abundant daphnid, has replaced D. pulex as the principal item in the kokanee
diet. Premysid populations of Daphnia spp. appeared by late May and peaked by late July, whereas
postmysid populations appeared in late June and peaked in late August or early September. Mysis
relicta appeared more frequently in stomachs of large kokanees ( 21)0 mm in total length) and
sometimes contributed substantially to the biomass of the kokanee diet. However, actual numbers
of mysids and their frequency of occurrence in individual kokanee stomachs remained low. The
disappearance or persistence of Daphnia spp. in other Colorado waters containing mysids appears
to be explained by thermal conditions. It is clear that the introduced M. relicta has not adequately
substituted for the diminished daphnid populations that were used heavily by planktivorous fishes.

Mysis relicta has been introduced in many
western lakes and reservoirs (Gosho 1975), including 50 in Colorado (Martinez and Bergersen
1989), to enhance forage bases for coldwater fish.
Its establishment in Kootenay Lake, British Columbia (Sparrow et al. 1964), and the subsequent
increased growth of kokanees Oncorhynchus
nerka (Northcote 1972a, 1972b), provided impetus
for further mysid introductions to benefit kokanee
(Rieman and Falter 1981; Leathe and Graham
1982; Brown 1984).
Unfortunately, kokanees have not responded as
positively in other lakes where M. relicta has been
established as they did in Kootenay Lake. The
deleterious effects of introduced mysids on daphnid populations have caused kokanee population
declines in Lake Tahoe, California—Nevada (Morgan et al. 1978), Pend Oreille Lake, Idaho (Rieman and Falter 1981), and Whitefish Lake, Montana (G. Anderson and D. Domrose, Montana
Department of Fish, Wildlife, and Parks, unpublished), and poor kokanee growth in Dillon Reservoir, Colorado (Nelson 1981).

Kokanees in Lake Granby, Colorado, have
supported a major sport fishery and served as the
source of several million eggs annually. In the late
1970s, the numbers of kokanees harvested and
eggs collected declined considerably (Table I).
Sealing and Bennett (1980) attributed the declines
to predation by lake trout Salvelinus namaycush,
reservoir drawdown that reduced survival of kokanee fry, overstocking of kokanees, and the
negative effect of introduced mysids on daphnid
populations.
The loss of all Daphnia spp. in Lake Granby
would be detrimental to the kokanee sport fishery
and to the statewide stocking program dependent
on the lake's kokanees for eggs (Nelson 1981).
The objective of this study was to determine the
interactions of zooplankton, M. relicta, and kokanees in Lake Granby.
Study Area
Lake Granby is 160 km northwest of Denver
near the headwaters of the Colorado River (Figure
I). Constructed in 1949, the impoundment is a
major source of irrigation water for northeastern
Colorado via transmountain water diversion. It
has a surface area of 2,938 hectares, a depth of
61 m, a mean depth of 22.6 m, and 64.4 km of

'The Unit is jointly sponsored by the U.S. Fish and
Wildlife Service, the Colorado Division of Wildlife, and
Colorado State University.
49

�50

MARTINEZ AND BERGERSEN

TABLE 1.-Summary

of Lake Granby kokanee fishery statistics, 1975-1987 (Sealing and Bennett 1980; Martinez

and Wiltzius 1991).

Year
1975
1976
1977
1978
1979
1980
1981
1982
1983
1984
1985
1986
1987

Total
fishing
hours•
(thousands)

•

Kokanee
Number
stocked°
(millions)

Boat
harvest'
(thousands)

1.4
1.3
1.8
1.7
1.2
1.3
1.1
1.0
1.0
1.0
0.9
0.5
0.5

69
45
43
23
21

228
171
131
151
130
126
141
141
135
137
99
75

16
39
44
24
16
5
3

Spawning
fund
(thousands)

Egg
take'
(millions)

Mean total length
of spawners
(mm)

88
29
30
11
32
33
104
134
154
149
80
37
39

10.1
1.9
5.5
2.4
4.6
6.8
16.4
12.3
10.2
13.0
6.8
4.0
6.1

330
378
399
394
356
295
312
306
304
295
269
274
287

*Includes effort expended by both boat and shore anglers.
°All stocked kokanee were fry until 1981. Larger sizes have been stocked experimentally in recent years.
'Includes all fish species; however, boat anglers caught kokanees primarily.
°Number of mature kokanees estimated to ascend the Colorado River.
'Numbers of kokanee eggs artificially stripped and fertilized at the Colorado River spawn-taking site.

shoreline at maximum elevation of 2,524 m above
mean sea level. It is subject to wide surface-level
fluctuation and can be drawn down as much as
28.7 m (Timm and Seeley 1970). In past investigations, the reservoir has been classified as oligotrophic (PHS 1963), oligomesotrophic (Timm
and Seeley 1970), mesoeutrophic (USEPA 1977),
and mesotrophic (Nelson 1982).
Mysis relicta, which was introduced in Lake
Granby in 1971 (Finnell 1977), developed a relatively dense population by 1978 (Nelson 1981).
Five fish species in addition to kokanee are abundant in Lake Granby: rainbow trout Oncorhynchus mykiss, brown trout Salmo trutta, lake trout,
longnose sucker Catostomus catostomus, and
white sucker Catostomus commersoni. Less common species are cutthroat trout Oncothynchus
clarki, brook trout Salvelinus fontinalis, johnny
darter Etheostoma nigrum, and mottled sculpin
Coitus bairdi.
Methods
Crustacean zooplankton was sampled in the
entire water column at a single deep station and
down to 10 m at several shallow stations (Figure
1). Midday samples were collected at monthly
intervals from June to December. In l983, samples were collected only once (deep station on 27
August) to confirm findings of the previous years.
From June to October 1982, diel samples (midday,
dusk, darkness, and dawn) were collected at the

deep station to monitor vertical movements of
zooplankton.
Quantitative collections of zooplankton were
made with an opening-closing Clarke-Bumpus
metered plankton sampler (0.12-mm-aperture netting) towed obliquely through the water column in
nonoverlapping strata of 5, 10, and 20 m. While
being towed, the sampler was opened at the
stratum upper limit, lowered to the stratum lower
limit, and then closed during retrieval at the
stratum upper limit. Qualitative collections also
were made through the ice at the deep station in
January, March, and April 1982 by drawing a
Wisconsin plankton net (0.12-mm-aperture netting) upward through the entire water column.
We periodically monitored the contribution of
daphnids to Lake Granby from surrounding impoundments from June to December 1982 by
collecting samples with a Clarke-Bumpus sampler
held in the current of major inlets near their
confluences with the reservoir.
Diel vertical distributions of M. relicta and
kokanees were recorded with an echo sounder in
1982. Soundings were taken concurrently with our
diel zooplankton sampling at the deep station
from June to September.
The relative abundance of M. relicta in shallow
water (3-7 m) was determined at monthly intervals from June to December 1982. Midday samples were collected at stations 1-6 (Figure 1) with

�51

MYSIDS IN LAKE GRANBY

N

Colorado
Granby -4. River
Pump
Canal

Colorado
Study
Area
Denver

7
•

(

7Continental
Divide

Willow
Creek-se
Canal
olorado
River
1.0km
1-1

Arapaho
Creek

FIGURE 1.—Lake Granby, Colorado, showing sampling stations. Stations A (deep) and a, b, c, and d (shallow) are
sampling sites for crustacean zooplankton; stations 1-6 are shallow-water sites used for epibenthic trawling for
Mysis relicta. Broken line in inset denotes Continental Divide.

an epibenthic trawl fitted with 0.71-mm-aperture
netting (Gregg 1976).
Kokanees were captured with a large midwater
trawl (mouth 6-m square) towed just after dark in
June, August, and October 1982 and in July,
August, and October 1983, at depths of 10-20 m
(Martinez and Wiltzius 1991). More than 1,400
stomachs were collected for food analyses. Gill
nets were occasionally set overnight to collect
kokanees in 1981 (N = 63) and 1982 (N = 119) for
cursory examination of stomach contents to compare with other food data.
Water temperature and dissolved oxygen were
measured on zooplankton sampling dates at the
deep station in 1981 and 1982. Dissolved oxygen
in water samples taken at 0, 5, 10, 20, 30, 40, and
50 m was measured by the Winkler method.
Mysids were removed from Clarke-Bumpus
samples before the crustacean zooplankton was
counted. Total counts of all species in three 1-mL
aliquots were made in a Sedgwick-Rafter counting chamber. Copepod nauplii were not counted.
In random subsamples, mysids were measured to

the nearest 1.0 mm and zooplankters to the nearest 0.01 mm.
The consumption of zooplankton by mysids
was studied by examining pooled stomach contents of 20-60 adult M. relicta each month from
June to December 1982. Three to five stomachs
were teased open into a Palmer-Maloney counting cell and all zooplankters were identified and
counted. Ingested rotifers appeared to remain
intact; cladocerans and copepods were identified
by specific structures; Bosmina longirostris by the
antennules, Daphnia galeata mendotae by the
postabdominal claw, and Diacyclops bicuspidatus
thomasi2 by the urosome.
Mysids in kokanee stomachs were picked out
and counted. Intact mysids were measured to the
nearest 1.0 mm. An average length of ingested

mysids was determined for estimating dry weight
from a length-weight equation established for M.

2Called Cyclops bicuspidatus thomasi by other authors.

�52

MARTINEZ AND RERGERSEN

relicta in Lake Tahoe by Morgan (1979). After the
mysids were removed, the remaining stomach
contents were pooled, by date, for kokanees in
10-mm-length categories. The number of zooplankters in a pool was estimated by counting all
individuals in three l-mL aliquots in a SedgwickRafter chamber. Average lengths of zooplankters
were used to calculate wet weights from established length—weight equations (Edmondson
1971). Dry weight was estimated by multiplying
wet weights by 0.1 (Rieman and Bowler 1980).
Once the numbers and dry weights of zooplankters were estimated, stomach contents with large
numbers of insects were filtered and dried at 60°C
for 12 h. After these materials were weighed, the
calculated zooplankton dry weight in the dilution
was subtracted from the dried sample weight to
estimate the dry weight of insects in the pooled
samples.
Abundance and Distribution of Zooplankton,
Mysis relicla, and Kokanees
Daphnid Population Changes
Studies conducted by Finnell and Reed (1969)
and Nelson (1971) focused on three daphnids
eaten by fish: Daphnia longiremis, D. pulex, and
D. g. mendotae. Finnell and Reed reported that
the daphnid population, in order of abundance,
was composed of D. g. mendotae, D. pulex, and
D. longiremis. Finnell and Reed (1969) and Nelson (1971) showed that D. longiremis was most
abundant below 10 m, D. pulex was concentrated
above 9-10 m, and D. g. mendotae was concentrated above 10 m. Maximum densities (number
per liter) reported by Nelson (1971) from 1%3 to
1965 were 18.4 for D. g. mendotae, 16.7 for D.
longiremis, and 3.9 for D. pulex.
The composition of the Lake Granby daphnid
community changed after the introduction of M.
relicta. Daphnia longiremis, which formerly appeared in the kokanee diet (Finnell and Reed
1969), was not seen during the current study.
Nelson (1971) suggested that predation on this
species may have been slight because it was small
(0.48-1.26 mm long; modal peaks at 0.61 and 0.81
mm) and concentrated in deep water. Although D.
pulex was extremely rare during our study, it was
once the species most heavily used by kokanees,
composing 85% of all organisms ingested in 1965
and 92% in 1966 (Finnell and Reed 1969).
Seasonal Zooplankton Densities
Daphnia g. mendotae and Bosmina longirostris
essentially composed the cladoceran community

during our study. Both appeared in small numbers
by late June. Although bosminids outnumbered
daphnids in July in 1981 and 1982, daphnids
surpassed bosminids for the rest of the year
(Table 2). Daphnia g. mendotae flourished in all
years of our study and its density peaked from late
August to early September (Martinez 1986).
Daphnia ptdex, which appeared in October and
November 1981 and in October and December
1982, never exceeded a mean density of 0.1/L
(Martinez 1986). L. M. Finnell (Colorado Division
of Wildlife, unpublished report) reported small
numbers of cladocerans and copepods in Lake
Granby in May and indicated that zooplankton
concentrations in the upper strata peaked by late
June or early July. He noted peak cladoceran
numbers in July or August. Nelson (1971) suggested that densities of daphnids were greatest
from late July to early August. Apparently, the
seasonal abundance of daphnids in Lake Granby
shifted after the establishment of mysids, as was
reported for cladocerans in Pend Oreille Lake by
Rieman and Bowler (1980), Rieman and Falter
(1981), and Bowles et al. (1986). These investigators also reported seasonal shifts in abundance of
B. longirostris. Unfortunately, no similar comparisons can be made for Lake Granby because
historical data on bosminid abundance are lacking. The highest daphnid density seen during our
study, in November 1982 (Table 2), may or may
not have reflected typical population dynamics of
D. g. mendotae in Lake Granby; however, it
showed that substantial numbers of daphnids persisted in the presence of an established mysid
population.
The cyclopoid copepod Diacyclops bicuspidaIns thomasi was the most abundant crustacean
zooplankter seen throughout our study (excluding
nauplii), and was present in all collections (Table
2). It was virtually the only crustacean zooplankter in samples collected through the ice (Martinez
1986). The calanoid copepod Diaptomus nudes,
rare throughout our study, appeared to be best
represented from October to December (Martinez
1986).
Temporal and Spatial Distribution
Generally, all species of zooplankton were most
abundant at depths above 10 m. Typically, Daphnia g. mendotae was concentrated above 10 m
with peak densities above 5 m. Nelson (1971)
found this species concentrated above 10-13 m in
other Colorado lakes and reservoirs. The greatest
density of D. g. mendotae observed in the main
lake during our study exceeded 60/L at 0-5 m at

�MYSIDS IN LAKE GRANBY

53

TABLE 2.-Mean midday densities of dominant crustacean zooplankton above 10 m in Lake Granby, 1981 and

1982.

Density (number/L) of

Date
1981
Jun 18
Jul 7
Aug 23
Sep 6
Sep 26
Oct 18
Nov 21
Dec 20
1982
Jun 1-2
Jun 28-29
Jul 27-28
Sep 3-4
Oct 10-11
Nov 14
Dec 4

Number of
samples

alumina
langimstris

Daphnia
galeaia
mendatae

2
2
7
7
7
7
7
5

&lt;0.1
29.5
14.4
10.6
5.4
1.9
3.0
0.5

&lt;0.1
0.8
38.0
31.7
17.3
6.4
18.3
3.6

12
12
12
12
12
12
8

&lt;0.1
1.2
16.4
4.3
1.8
6.0
1.1

&lt;0.1
&lt;0.1
3.1
27.7
14.1
64.9
9.9

the deep station in November 1982. Daphnia
pulex, when present, showed no distinct distribution pattern; however, Finnell and Reed (1969)
and Nelson (1971) found this species occasionally
more abundant at depths of 5-20 m than at 0-5 m.
Diacyclops b. thomasi occurred in all strata and
was the most abundant crustacean below 10 m.
Diaptomus nudus, which rarely exceeded a density of 0.2/L, was most abundant above 20 m
(Martinez 1986).
Diet-stratified sampling in 1982 did not clearly
demonstrate vertical migrations by zooplankton.
Although densities within the same stratum differed among the four diel sampling periods (daylight, dusk, darkness, and dawn), the strata may
not have been narrow enough to define vertical
movements (Martinez 1986). Finnell and Reed
(1969) did not observe diet vertical distribution
trends in Lake Granby daphnids. In nearby Grand
Lake, Pennak (1944) found no vertical migrations
of Diacyclops b. thomasi and only moderate diet
vertical movement (5.8 m) of Daphnia longispina.
Diet movements of M. relicta were clearly
evident. Changes in mysid densities in the water
column were closely correlated with echograms of
mysid distributions (Martinez 1986). Typically,
mysids were near the bottom or in deep water
during daylight and migrated upward at night. At
dawn, they returned to deep water. These downward migrations were rapid. Echograms indicated
that the M. relicta population, pelagic at 10-20 m
before dawn, descended to 40-50 m within 15-20
min. The upward migration at dusk appeared to be
slower, requiring 30-40 min regardless of the

Daphnia
pules

&lt;0.1
&lt;0.1

&lt;0.1
&lt;0.1
&lt;0.1

Diacyclops
bicuspidatus
Ihamast

Diaptomus
audios

34.8
70.7
31.5
24.4
12.1
11.0
68.5
50.4

&lt;0.1
&lt;0.1
&lt;0.1
&lt;0.I
0.1
0.4
&lt;0.1

3.5
9.7
23.2
29.3
19.0
38.5
46.6

&lt;0.1
&lt;0.1
&lt;0.1
0.3
0.6
0.1

vertical distance. These rates were similar to
those reported by Rybock (1978) for ascents (48
m/h) and descents (100 m/h) of M. relicta in Lake
Tahoe.
Finnell and Reed (1969) reported that kokanees
in Lake Granby occupied the upper 9 m by day
and migrated downward at night, when they concentrated between 9 and 18 m. Observations of
kokanee movements during our study differed
slightly. Echograms showed that kokanees were
primarily above 10 m by day but occurred down to
20 m. They began descending at dusk, were
concentrated between 10 and 20 m at night, and
returned into surface waters at dawn (Figure 2).
Crustacean zooplankton appeared to be the
organisms least affected by seasonal changes in
iimnological conditions. However, water circulation during the fall turnover distributed zooplankters (usually concentrated in the upper 10 m)
throughout the water column.
The vertical extent of the diet mysid migration
appeared to be restricted by temperature. Mysis
relicta occurs in cold water, down to -2°C
(Holmquist 1963), and has a strong preference for
waters less than 14°C (Morgan 1979; Pennak
1989). It can withstand temperatures up to 20°C
only through very gradual acclimation (Holmquist
1959; Smith 1970; DeGraeve and Reynolds 1975).
Although M. relicta can endure high temperatures
for short periods, DeGraeve and Reynolds (1975)
demonstrated that mortality increased rapidly at
temperatures above 13°C.
Mysids in Lake Granby did not enter surface
waters when thermal stratification developed and

�54

MARTINEZ AND DERGERSEN
0
10

&gt;-

•
•

20

• • •
•

•
•

.

•

7
•

•
•

•

KOKANEE

•

/

•

•• •
•

•••

• "j/.

./• 1

•

•
. • • •• „

l

30
40-

•

MYSIS

I

50

0
I0
I— 20-

•

•

•

•

Z
— 30-

I
40-

I

Temperature
— —Disolved
Oxygen

50

,

JUN 27
5

10

15

JUL 28
20

0

5

10

15

20

0

5

0

2.5

1114/11

SEP 3
10
15

20

5.0

10.0

TEMPERATURE (°C)
2.5

5.0 • 7.5

10.0

0

2.5

5.0

7.5

10.0

7.5

DISOLVED OXYGEN (mg/ L)
FIGURE 2.—Diurnal and nocturnal echogram depictions of vertical distribution of kokanees and Mysis relicta in
Lake Granby at station A on 27 June, 28 July, and 3 September 1982. Solid line shows temperature profile; dotted
line shows dissolved oxygen profile.

epilimnetic temperatures exceeded 14°C (Figure
3). As the epilimnion thickness increased, the
upward limit of the vertical migration of M. relicta
progressed downward. Beeton (1960) demonstrated not only that light was the most important
factor governing timing of these vertical migrations, but that high epilimnetic temperatures were
important in limiting vertical distribution. When
thermal stratification was pronounced in Lake
Granby during late July to mid-September,
mysids were effectively excluded from the upper
10-11 m of the reservoir. It appeared that most of
the population did not enter the upper water
column where temperatures exceeded I4°C. Similarly, Rieman and Falter (1981) found that M.
relicta in Pend Oreille Lake was seasonally isolated from the upper 10 m of the water column in
August and September by increasing thermal
stratification.
Mysis relicta also requires well-oxygenated wa-

ter and can tolerate conditions of less than 2 mg/L
for only short periods (Juday and Birge 1927;
Brownell 1970; Sandeman and Lasenby 1980).
Despite its ability to reduce oxygen consumption
as ambient temperatures and oxygen concentrations decrease, it remains intolerant of oxygen
below 2-3 mg/L (Sandeman and Lasenby 1980).
Declining ,dissolved oxygen in Lake Granby
during late summer and fall was correlated with
both vertical and horizontal movements of the
mysid population. Hypolimnetic oxygen depletion
began soon after the spring turnover. By late
August or early September, dissolved oxygen
below 40 m fell to less than 2 mg/L and the entire
mysid population was suspended off the bottom
(Figure 2). This avoidance of hypoxic conditions
by mysids was evident in stratified Clarke—Bumpus net collections and in echograms (Martinez
1986). By October, dissolved oxygen concentrations at depths greater than 20 m fell below 2 mg/L

�55

MYSIDS IN LAKE GRANBY

n Kokanee
containing
mysids

JUN 15-17
11+

1+

n=229

w
fr

co
O

20 60 100 140 180 220 260 300 340 380

Length Imml
FIGURE

3.—Kokanee length-frequencies and occurrences of Mysis relicta in kokanee stomachs in Lake Granby,

1982.

(Martinez 1986). Instead of suspending in the
water column above 20 m, most of the mysid
population moved horizontally in the reservoir.
They were scarce or absent in stratified zooplankton samples (Martinez 1986), absent in pelagic
echogram records, and very abundant in epibenthic
trawl collections taken in water 3-7 m deep (Table
3). Horizontal migrations of mysids from deep to
shallow water in response to low dissolved oxygen in deeper portions of lakes have been documented by other investigators (Tattersal and Tattersal 1951; Holmquist 1959; Lasenby 1971;

Morgan and Threlkeld 1982). In Lake Granby, M.
relicta reappeared in open-water zooplankton

samples below 20 m by late November, after fall
turnover had replenished dissolved oxygen in
deeper waters (Martinez 1986). Lasenby (1971)
reported similar timing for the return of mysids to
the depths of Stony Lake, Ontario, after the fall
turnover. The abundance of M. relicta in inshore
areas appeared to diminish as ice formation began
in December (Table 3).
The persistence of large numbers of mysids in
shallow water at station 1 (Table 3) may be

�MARTINEZ AND BERGERSEN

56

TABLE 3.-Occurrence of Mysis relicta in shallow
water (3-7 m) in Lake Granby in 1982. A = abundant; P
= present; 0 = absent. Stations are shown in Figure 1.

Station
Date
Jun I
Jun 27
Jul 274
Sep 3
Oct 10
Nov 14
Dec 4

A
A

0

A
A

2

3

4

5

6

A

P

A
P

P
0
0
0

A

A
A
Ice

A
A

0
A
A

P

P

0
0
0

0
0
0

A
A

A
A

P

P

0
0

0
0

explained by age composition. Station 1 was in a
large, relatively shallow part of the reservoir
(Figure 1). All mysids collected in epibenthic
trawls in this area during summer were young of
the year. The summer occurrence of predominantly juvenile mysids in deeper water near station 1 was also noted by W. C. Nelson (Colorado
Division of Wildlife, personal communication).
Morgan and Threlkeld (1982) described horizontal
migrations of newly hatched juvenile mysids into
shallow water during summer in Lake Tahoe and
nearby lakes. Juvenile mysids appeared less sensitive to light and temperature (Gosho 1975),
which would explain their tolerance of summer
conditions in shallower waters.
Water temperatures also appeared to influence
the vertical distribution of kokanees. Generally,
kokanees migrated to the lake surface during the
day and to deeper waters at night (Finnell and
Reed 1969). From late July to early September,

when surface water temperatures were highest,
kokanees did not appear to enter the upper few
meters of water in the reservoir during daylight
(Figure 2). Water temperatures at 0-3 m often
exceeded 18°C during this period. This observation of kokanees avoiding near-surface waters
was consistent with Brett's (1971) finding that the
natural occurrence of the anadramous, conspecific sockeye salmon is limited to temperatures at
or below 18°C, despite its ability to tolerate 24°C.
Similarly, Finnell and Reed (1969) found kokanees in Lake Granby to be most abundant at
depths of 4.5-13.5 m during the day from late July
to mid-September. Because kokanees lived in the
upper 20 m of the reservoir, oxygen depletion
probably had no direct effect on their distribution.
Trophic Relations of Zooplankton,
Mysis relicta, and Kokanees

Zooplankton in Mysid Diet
In June and July, rotifers (primarily Kellicottia
longispina and a few Keratella cochlearis) composed the bulk of the zooplankters in the mysid
diet (Table 4). The large rotifer Asplanchna sp.,
which appeared to be abundant in spring and early
summer, was not detected in mysid guts. Either it
was not eaten or we failed to recognize its parts
among other zooplankton fragments. Rybock
(1978) found positive selection for K. longispina
by M. relicta in Lake Tahoe; however, Cooper
and Goldman (1980) and Langeland (1981) showed
that mysids fed on larger prey when available. As

TABLE 4.-Numbers and percentages (in parentheses) of zooplankton prey in pooled stomach contents of Mysis

relicta (10-18 mm long) collected in Lake Granby, 1982.
Date and sample size

Prey type

Jun l•
N 49

Bosmina
longirostris

Jun 2T
N .= 46

Jul 27•
N = 62

Aug 11°
N 35

Sep 3•
N = 28

Oct 116
N = 25

Nov 14°
N = 30

Dec 4°
N= 20

2
(0.5)

143
(23.7)

238
(52.8)

37
(60.7)

12
(21.8)

IS
(26.9)

4
(16.0)

58
(12.9)

21
(34.4)

37
(67.2)

9
(16.0)

'5
(20.0)

32
(57.1)

16
(64.0)

Daphnia
galeata
mendotae
Diacyclops
bicuspidatus
thomasi

27
(4.5)

6
(1.3)
149
(33.0)

Kellicottia
longispina

345
(98.0)

334
(90.8)

424
(70.3)

Keratella
cochlearis

7
(2.0)

32
(8.7)

9
(1.5)

3
(5.5)
3
(4.9)

"Mysis relicta from Clarke-Rumpus collections.
°Mysis relicta from epibenthic trawl collections.
`Mysis relicta from Clarke-Rumpus and epibenthic trawl collections combined.

3
(5.5)

�57

MYSIDS IN LAKE CRANBY '

TABLE 5.-Frequency of occurrence of food items in stomachs of kokanees collected at night with a midwater
trawl in Lake Granby, 1982 and 1983.

Date
1982
Jun 15-17
Aug 11-13
Oct 5-6
1983
Jul 11-12
Aug 23-24
Oct 13
"Includes

Number (%) of food items

Number of
kokanees
captured

Number of
stomachs
examined

Crustacean
zooplankton"

249
353
326

229
345
322

201 (87.8)
343 (99.4)
294 (91.4)

88 (38.4)
50 (14.5)

276
354
72

273
353
71

264 (96.7)
351 (99.4)
62 (87.3)

250 (91.6)
17 (4.8)
8 (11.3)

Insects°

0

Mysis
relkta
42 (18.3)
172 (49.9)
52 (17.7)

4 (1.7)

12 (4.4)
84 (23.8)
17 (23.9)

2 (0.7)
I (0.2)
5 (7.0)

Bosmina longirostris, Daphnia galeata mendotae, Daphnia palm Diacyclops biatspidatus thomasi,

nudus; however, not all species were consumed on all dates.

Number (%)
of empty
stomachs

0

4 (1.2)

and

Diaptomus

b lneludes chironomids (pupae and adults) and hypmenopterans (ants).

cladoceran abundance and their consumption by
mysids increased in August, fewer rotifers were
eaten. Although rotifer densities were not determined, rotifers appeared to be relatively abundant
throughout the open-water season. As cladoceran
numbers diminished in late fall, K. longispina
again became prevalent in the mysid diet (Table
4).
Daphnia spp. and Bosmina spp. are preferred
prey of M. relicta (Lasenby and Langford 1973;
Langeland 1981; Lasenby and Furst 1981), but
daphnids are preferred over other zooplankters
(Grossnickle 1978; Cooper and Goldman 1980).
Bosmina longirostris, appearing before Daphnia
g. mendotae in early summer in Lake Granby,
also appeared earlier in mysid stomachs and continued to be eaten in relatively large numbers for
the rest of the year (Table 4). Even after July,
when daphnids were more numerous at all depths,
mysids in Lake Granby appeared to select B.
longirostris as preferred prey. Daphnia g. mendotae was abundant and was eaten by mysids in
August and September, but it did not compose the
highest percentage of ingested zooplankters until
October. Although B. longirostris and D. g. mendome were most abundant above 10 m, both
occurred in deeper water and were available to M.
relicta even during summer when it was isolated
from surface waters.
Despite its abundance and occurrence at all
depths, few Diacyclops bicuspidatus thomasi appeared in mysid stomachs (Table 4). Lasenby
(1971) found that mysids in Stony Lake also fed
almost exclusively on cladocerans in summer,
even in the presence of abundant copepods.
Lasenby and Fiirst (1981) suggested that mysids
eventually would feed on copepods if cladoceran
numbers remained low. Diaptomus nudus was not

found in mysid guts, perhaps because of its scarcity, although mysids elsewhere have shown low
(Grossnickle 1978) to negative (Rybock 1978) selection for Diaptomus spp.
Kokanee Food Habits
Kokanees in Lake Granby fed on crustacean
zooplankton and insects (chironomid pupae and
larvae and ants). Only a few rotifers and a single
small kokanee were seen in kokanee stomachs.
Crustacean zooplankton (cladocerans and copepods) appeared in 87-99% of the kokanee stomachs examined during all sampling periods (Table
5). The frequency of insect occurrence in kokanee
stomachs ranged widely among the six sampling
dates-from 0 to almost 92%. Mysis relicta occurred in 4-50% of the kokanees. The incidence of
empty stomachs was low, ranging from 0 in July
1982 to 7% in October 1983.
The use of Bosmina longirostris, Diacyclops
bicuspidatus thomasi, and insects by kokanees in
Lake Granby was greatest in spring and early
summer. Relatively few B. longirostris appeared
in kokanee stomachs and (partly because of their
small size) they contributed little to the biomass of
the kokanees' diet (Table 6). Although D. b.
thomasi was eaten by kokanees during all sampling periods, it contributed most to the diet
biomass early in the year (Table 6). In Lake
Chelan, Washington, Brown (1984) reported
heavy, selective use of Bosmina spp. by kokanees. In Pend Oreille Lake, Bosmina spp. was
an important kokanee food during spring and
early summer, but it was little used when cyclopoids were extremely abundant (Rieman and
Bowler 1980). Finnell (unpublished) reported
heavy consumption of copepods and light use of
aquatic and terrestrial insects by Lake Granby

�58

MARTINEZ AND BERGERSEN

TABLE 6.-Numbers and dry weight (mg) of food items in pooled stomach contents of age-0, age-1, and age-2
kokanees collected at night with a midwater trawl in Lake Granby, 1982 and 1983. N is the number of stomachs with
food.

Date

Food
item*

Age 0

Age 1
Weight

Number

1982
Jun 15-17

75)
33
105

89
1
5
138

(N = 70)
191,034
1,356
80
1
3.720
16
14
67
39
262

(N = 217)
449,048
3,188
132
8,381
37
233
1,111
1,114
7.613

267
2

(N = 99)
117.244
3,113

1,278
17

(N = 186)
538.897
5,874
3,750
21
1.865
11,827

1
15
145

(N = IS)
300
1,460
8,423
437

2
3
46
1,926

(N = 235)
2,523
18
2.707
6
135,253
730
1.205
5,311
298
47

(N= 65)
145,810
1,341
1,420
7
3
13
14
89
(N= 18)
3,598
37
130
1,230
26
8
35

(N = 250)
640,880
5,896
3,030
15
27
119
227
1,440
(N = 43)
2,615
27
215
1,860
39

12,518
133
1,051
29

Daphnia
Diacyclops
Mysis

24,526
327

Daphnia
Bosmina
Diacyclops
Insects
Mysis

120
188
2.710
33

Daphnia
Diacyclops
Insects
Mysis

11,795
40
7

Daphnia
Diacyclops
Diaptomus
Insects
Mysis

160
200

2
1

5
4

22
25

(N= 58)

(N = 33)

= 21)

(N = 37)

Aug 23-24

Oct 13

109
1
31
(N

Weight

(N = 65)
605
2
31,241
172
2,995
628
265
1,586

Daphnia
Bosmina
Diacyclops
Insects
Mysis

1983
Jul 11-12

Number

12
384
448
191

5,998
22

Oct 5-6

Age 2
Weight

(N = 85)
4,718
69,873
94
32

Bosmina
Diacyclops
Insects
Mysis
Aug 11-13

Number

5)

43

273

Insects include chironomids (pupae and adults) and hymenopterans (ants).

kokanees in early spring. In contrast, during the
earliest sampling periods in 1982 and 1983, insects
composed the bulk of the biomass ingested by
kokanees of all ages (Table 6). Because of the
comparatively large size of insects, relatively few
made up a large percentage of the diet biomass.
Daphnia g. mendotae was the most used food
of kokanees of all sizes after July, usually outnumbering all other organisms combined. Information on diet obtained from kokanees captured
in gill nets also showed this (Martinez 1986).
Clearly, the species composition of the kokanee
diet has changed since Finnell and Reed (1969)
reported that D. pulex was the most heavily used
and preferred food of Lake Granby kokanees in
the 1960s. Kokanee preference for daphnids is
well documented (Rieman and Bowler 1980;
Leathe and Graham 1982; Vinyard et al. 1982). As

one of the larger crustacean zooplankters in the
reservoir, D. g. mendotae also contributed significantly to the kokanees' diet biomass (Table 6).
The limited use of Daphnia pulex and Diaptomus nudus, the largest limnetic entomostracans,
was probably due to their scarcity. Diaptomus
nudus was absent from all kokanee stomachs
examined except in October 1983, when it appeared in the stomachs of 1- and 2-year-old kokanees (Table 6). Large numbers of Daphnia
pulex were found in the stomachs of 12 kokanees
collected in a gill net on December 4, 1982. The
net was set in the vicinity of zooplankton sampling station A (Figure I). Zooplankton samples
collected nearby at station A on the same day
contained high densities of Daphnia g. mendotae
and very few Daphnia pulex. These observations
corroborate the strong selection for Daphnia

�MYSIDS IN LAKE GRANBY

pulex by kokanees in Lake Granby reported by
Finnell and Reed (1969), even when the density of
this daphnid is very low.

59

predation. Because this cladoceran occurred in
the hypolimnion (Finnell and Reed 1969), it was
available to M. relicta as prey. Threlkeld et al.
(1980) and Morgan et al. (1981) suggested that
Use of Mysids by Kokanees
cladoceran species inhabiting deep water in lakes
Although other food items were seasonally im- typically disappear after mysids are introduced.
Because daphnids were concentrated above 10
portant to kokanees, there was no distinct peak in
m,
they were spatially separated from M. relicta
use of mysids. They appeared in nearly 50% of the
for
nearly 2 months (late July to mid-September).
kokanee stomachs examined in August 1982 (Th.;
This
seasonal exclusion of mysids from surface
ble 6), and some stomachs contained mysids
almost exclusively, but overall, few kokanees fed waters provided a thermal sanctuary for daphon them. Only 29% (N = 896) of the stomachs nids. Threlkeld et al. (1980) and Morgan et al.
examined contained mysids in 1982 and 16% (N = (1981) stressed the importance of thermal refugia
697) in 1983. Rieman and Bowler (1980) found M. in the coexistence of daphnids and mysids, and
recta in 19-23% of the kokanee stomachs exam- they proposed such refugia as the principal mechanism that allows cladocerans to persist in lakes
ined in Pend Oreille Lake in 1977-1978.
Rieman and Bowler (1980) reasoned that the containing natural mysid populations.
Temporal shifts in the development of daphnid
contribution of mysids to the kokanee diet was
populations
have been attributed to intense selecless than such percentages indicated. Mysis
tive
predation
by mysids (Rieman and Falter
relicta typically is not available to kokanees dur1981). A similar pattern was evident in Lake
ing the day (when kokanees often feed). If stomachs for food analysis came from kokanees col- Granby in the spring when mysids inhabited the
lected just after dusk, the samples would tend to entire water column during their vertical migraoverrepresent the actual contribution of mysids to tion and, in the upper strata, preyed selectively on
the daily kokanee ration (Rieman and Bowler daphnids at night, severely depressing numbers of
1980). Because kokanees in Lake Granby feed daphnids and inhibiting population development.
diurnally (Finnell and Reed 1969) and the stom- As the thermal refuge developed in the summer,
achs examined in this study were from kokanees the daphnid population recovered rapidly and
collected just after dusk, the same bias probably attained premysid densities, despite the presence
applies. In the gut samples, M. relicta appeared to of fewer species (Figure 5).
The importance of a thermal refuge in limiting
be the last item ingested, which further supports
mysid
predation on epilimnetic daphnids is further
this contention.
supported
by the scarcity of Daphnia spp. in
As with insects, mysids (because they are large)
Grand
Lake,
Dillon Reservoir, and Lower Twin
contributed substantially to the biomass of the
Lake
(Table
7).
These waters formerly contained
were
kokanee diet, even when comparatively few
ingested. Overall, however, the numbers of in- thriving populations of daphnids and also supgested mysids were low. Individual kokanees ported kokanee fisheries. Because Daphnia spp.
contained up to 176 mysids, but most contained became scarce after M. relicta was established,
only 1-5 (Martinez 1986). There appeared to be a these lakes are no longer managed for kokanees.
trend in Lake Granby toward higher mysid use by The stocking of juvenile rainbow trout has been
larger ( �200 mm) kokanees (Figures 3 and 4). discontinued in Dillon Reservoir because the trout
This trend was reported also for kokanees in Lake was suspected of competing with stunted koTahoe (Morgan et al. 1978) and Pend Oreille Lake kanees for extremely limited cladoceran forage
(Rieman and Bowler 1980). The smallest kokanee (Stuber et al. 1985)—a situation apparently aggrato contain mysids during this study was 87 mm vated by a dense mysid population.
Thermal conditions appear to be the most imlong. Rieman and Bowler (1980) reported M.
portant factor in the coexistence of daphnids and
relicta in kokanees as short as 40-45 mm.
introduced mysids. In Colorado waters, where
low epilimnetic temperatures allow M. relicta to
and
Interactions of Daphnids, Mysids,
enter surface waters almost year-round, daphnids
Kokanees
can be expected to become scarce (Nester 1986).
Daphnids versus Mysids
Although surface temperatures exceed 14°C in
The disappearance of Daphnia longiremis in Grand and Lower Twin lakes (Table 7), subsurLake Granby probably was caused by mysid face water temperatures are lower, and the short-

�60

MARTINEZ AND BERGERSEN

20

n Kokanee
JUL 11-12
0+

1+

II+

containing
mysids

10

n = 273

20
AUG 23-24

0

Y
0

1+

0+

II+

10

n =353

20

OCT 13
0+

1+

10-

n = 71

20

i

610 100 1d0 180 220 260 300 340 1 380
Length imml

F IGURE 4.—Kokanee length-frequencies and occurrences of Mysis relicta in kokanee stomachs in Lake Granby,
1983.
ness of the warmwater period apparently does not
exclude mysids long enough to allow daphnid
populations to develop. In Lake Granby, where
mysids are excluded from surface waters for
nearly 2 months, daphnids persist.
The small numbers of M. relicta in Green
Mountain Reservoir suggest that thermal regimes
also may be important in establishing dense mysid
populations. Green Mountain Reservoir does not
stratify pronouncedly in summer (Table 7); instead, because of the reservoir's low retention
time, water temperatures decrease gradually from

top to bottom (Nelson 1981). Such thermal conditions apparently are not conducive to proliferation
of M. relicta, because most of the reservoir exceeds 14°C during summer. Nelson (1981) suggested that inflow-outflow conditions in Green
Mountain Reservoir did not favor development of
a mysid population. This appears to have held
true in the 15 years following the M. relicta
introduction in the reservoir, where it is now rare
to absent and daphnids remain abundant (Table
7).
Daphnia g. mendotae

remained the dominant

�MYSIDS IN LAKE GRANBY

30-

Pre - Mysis

61

D. g. mendotae
D. longiremis
D. putex

20-

0
_a

30-,

E

Post- Mysis

z
Z 2010-

A

M

J

J

A

S

O

N

D

J

FIGURE 5.—Trends in composition and abundance for three species of Daphnia before and after the establishment
of Mysis relicta in Lake Granby.

cladoceran in Lake Granby after mysids fed on
the daphnid population. Rieman and Falter (1981)
wrote that it replaced D. thorata as the dominant
daphnid after M. relicta became established in
Kootenay and Pend Oreille lakes. These investigators suggested that the helmet spikes of D. g..
mendotae gave it a survival advantage over
round-helmeted D. thorata. Because M. relicta
must seize and manipulate larger prey for ingestion (Cooper and Goldman 1980), the helmet
spikes might foil mysid attacks by impeding such

manipulation. This feature alone, which can develop in several Daphnia species including D.
longiremis (Zaret 1980), is not sufficient to avert
mysid predation—as evidenced by the disappearance of the spike-forming species in several Col-

orado lakes. It may, however, preserve greater
numbers of D. g. mendotae, whose populations
can rebound more quickly once mysid predation
is curbed by thermal stratification.
Typically, D. ptdex was concentrated above 10
m in Lake Granby (Finnell and Reed 1969; Nelson

TABLE 7.—Comparison of Mysis relicta introduction dates and current status, mean August temperature profiles,
and current status of daphnid populations in five Colorado lakes.
Species
and
variable
Mysis relicta
Year introduced
Status 1983'
Water temperature MP
Surface
10-m depth
20-m depth
40-m depth
Daphnia spp.
Status 1983'

Lake
Granby

Grand
Lake

Green
Mountain
Reservoir

Dillon
Reservoir

Lower
Twin
Lake

1971
A

1969
A

1974
RA

1970
A

1962
A

18
15
9
8

15
10
7
5

16
16
14
12

14
13

16
13
8

A

RA

A

'A abundant; RA = rare to absent.
°Temperature data for all lakes except Lower Twin Lake are from Nelson (1981).

6
RA

RA

�62

MARTINEZ AND BERGERSEN

1971) and should have received the same sanctuary in warm surface waters enjoyed by D. g.
mendotae. That it did not indicates selective fish
predation was responsible for the suppression of
D. pulex numbers.
Daphnids versus Kokanees

The' virtual elimination of D. pulex in Lake
Granby probably was among the chief causes of
the kokanee fishery's decline. Ironically, the scarcity of D. pulex in 1981-1983 apparently resulted
from intense kokanee predation that followed
kokanee overstocking. Despite its addition to the
reservoir from surrounding impoundments (Martinez 1986), D. pulex has been unable to recolonize the reservoir.
Suppression of particular daphnid species,
however, depends not only on selective removal
of larger members of the population, but on
whether the fish consume both mature and immature forms (Galbraith 1967). If fish feed primarily
on mature daphnids, adequate numbers of reproducing females usually survive to sustain the
population; this tends not to be the case if fish
consume immature as well as mature daphnids
(Galbraith 1967). Obviously, size at maturity becomes an important factor in the capacity of
different daphnid species to withstand fish predation. Daphnia g. mendotae typically matures at
about 1 mm and D. pulex at 2 mm (Zaret 1980). In
Lake Granby, kokanees preyed primarily on D. g.
mendotae longer than 1 mm, whereas most of the
D. pulex in kokanee stomachs were shorter than 2
mm (Martinez 1986). Consistent with Galbraith's
(1967) findings, D. pulex appeared unable to sustain a viable population when faced with intense
predation by kokanees.
This suppression of D. pulex implies that the
rate of kokanee predation on limnetic daphnids
has increased since the kokanee harvest and egg
take went into decline in the late 1970s. At that
time, larger kokanees appeared in fishermen's
creels and in spawning runs. In the early 1980s,
the Lake Granby kokanee fishery was characterized by low harvest of small kokanees and record
numbers of smaller and older spawners (Table 1).
Brown (1984) reported a negative relation between mean size of kokanees and angler catch
rate. This negative relation seemingly developed
in Lake Granby (Martinez and Wiltzius 1991). The
reduced catch rate and harvest meant that thousands of kokanees were not removed by fishermen and remained in the lake. These trends
toward smaller kokanees, lower harvests, and
numerous spawners led to stunting due to over-

stocking (Martinez and Wiltzius 1991). Stunting
undoubtedly increased intraspecific competition
between all age-classes of kokanees that rely on •
the same pelagic foods. It seems reasonable to
presume that this competition intensified predation on all available prey, particularly on preferred items.
Daphnia g. mendotae may have an additional
survival advantage over D. pulex because of its
extreme transparency, which conceivably protects it from sight-feeding kokanees. Transparency in zooplankton is believed to be an effective
adaptation against sight-feeding predators (Kerfoot 1980). Nelson (1971) suggested that D. g.
mendotae may have been protected from fish
predation by its ability to produce small, helmeted
morphs during summer. Both helmeted and unhelmeted forms occurred in Lake Granby during
our study. Possibly transparency and smaller
morphs both contributed to the persistence of D.
g. mendotae by making detection by kokanees
more difficult.
Mysids versus Kokanees

It appears that the decline of the Lake Granby
kokanee fishery can be attributed to changes in
the daphnid populations resulting from the joint
effects of intense selective predation by introduced mysids and overabundant kokanees, particularly kokanees. Although thermal conditions
allow daphnids to persist in the reservoir, the
temporal shift of the daphnid population may
effectively shorten the season of optimum kokanee growth. Kokanees now appear to grow only
during a 2-month period from late August to late
October (W. J. Wiltzius, Colorado Division of
Wildlife, personal communication).
Because kokanee growth is strongly density
dependent (Goodlad et al. 1974; Leathe 1984),
stunting of the kokanee population before Mysis
became established could have been easily corrected by a reduction in stocking rate. However,
the postmysid situation may be more complex. It
does not appear that the inclusion of other zooplankton, insects, or even M. relicta in the kokanee diet has adequately compensated for the
diminished daphnid forage. The reduction in annual growth may mean that the reservoir can no
longer support the kokanee density that produced
exceptional kokanee fishing (Table 1).
Martinez and Wiltzius (1991) noted an increased frequency of occurrence of M. relicta in .
Lake Granby kokanees and rainbow trout in September 1981. Because hypolimnetic oxygen became depleted by August (Martinez 1986), many

�r
MYSIDS IN LAKE GRANBY

mysids may have been trapped between hypoxic
conditions in deeper waters and high temperatures in the epilimnion, which could have increased their availability to the fish.
Despite the trend toward higher use of mysids
by larger kokanees, the consumption of M. relicta
in populations containing more large kokanees
would probably remain low. Simply put, M.
relicta typically is available to kokanees only at
night when the fish cease feeding (Finnell and
Reed 1969; Doble and Eggers 1978). Myth relicta
has not enhanced kokanee growth in Lake Granby
and probably will not benefit kokanees in other
Colorado lakes where it has become established.
Acknowledgments

We thank Wes Nelson, Bill Wiltzius, Jake Bennett, and Clee Sealing of the Colorado Division of
Wildlife for their involvement and cooperation in
this study. We gratefully acknowledge Anita Martinez and Beverly Klein for their assistance in
producing this manuscript.
References
Beeton, A. M. 1960. The vertical migration of Mysis
relicta in Lakes Huron and Michigan. Journal of the
Fisheries Research Board of Canada 17:517-540.
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Edmondson, W. T. 1971. Methods for processing samples and developing data. IBP (International Biological Programme) Handbook 17:127-169.
Finnell, L. M. 1977. Fryingpan-Arkansas fish research

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              <text>Abstract. In studies of zooplankton and kokanees &lt;em&gt;Oncorhynchus nerka&lt;/em&gt; in Lake Granby, Colorado, conducted from 1981 to 1983, we investigated the suspected role of introduced &lt;em&gt;Mysis relicta&lt;/em&gt; in the decline of the kokanee sport fishery and egg take. &lt;em&gt;Mysis relicta&lt;/em&gt; entered surface waters&lt;br /&gt;at night and preyed on zooplankton, except when summer temperatures above 14°C excluded it from the epilimnion and created a temporary refuge for cladocerans. We attributed the disappearance of hypolimnetic &lt;em&gt;Daphnia longiremis&lt;/em&gt; to predation by mysids, and the virtual elimination of &lt;em&gt;Daphnia pulex&lt;/em&gt; (once the preferred item in the kokanee diet) to the effects of intense selective predation by abundant &lt;em&gt;M. relicta&lt;/em&gt; and to kokanee overstocking. &lt;em&gt;Daphnia galeata mendotae&lt;/em&gt;, historically the most abundant daphnid, has replaced &lt;em&gt;D. pulex&lt;/em&gt; as the principal item in the kokanee diet. Premysid populations of &lt;em&gt;Daphnia&lt;/em&gt; spp. appeared by late May and peaked by late July, whereas postmysid populations appeared in late June and peaked in late August or early September. &lt;em&gt;Mysis relicta&lt;/em&gt; appeared more frequently in stomachs of large  kokanees ( 21)0 mm in total length) and sometimes contributed substantially to the biomass of the kokanee diet. However, actual numbers of mysids and their frequency of occurrence in individual kokanee stomachs remained low. The disappearance or persistence of &lt;em&gt;Daphnia&lt;/em&gt; spp. in other Colorado waters containing mysids appears to be explained by thermal conditions. It is clear that the introduced &lt;em&gt;M. relicta&lt;/em&gt; has not adequately substituted for the diminished daphnid populations that were used heavily by planktivorous fishes.</text>
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              <text>&lt;a href="https://cpw.state.co.us/Documents/Research/Aquatic/pdf/Publications/InteractionsOfZooplankton1991.PDF" target="_blank" rel="noreferrer noopener"&gt;Martinez, P. J., and E. P. Bergersen. 1991. Interactions of zooplankton, Mysis relicta, and Kokanees in Lake Granby, Colorado. American Fisheries Society Symposium 9:49–64.&lt;/a&gt;</text>
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              <text>&lt;em&gt;Mysis relicta&lt;/em&gt;</text>
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