Brook Trout (Salvelinus fontinalis) Habitat Use and
Dispersal Patterns in New York Adirondack Mountain
Headwater Streams
Justin Ecret and Timothy B. Mihuc
Northeastern Naturalist, Volume 20, Issue 1 (2013): 19–36
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2013 NORTHEASTERN NATURALIST 20(1):19–36
Brook Trout (Salvelinus fontinalis) Habitat Use and
Dispersal Patterns in New York Adirondack Mountain
Headwater Streams
Justin Ecret1,* and Timothy B. Mihuc2
Abstract - Minimal research has been conducted involving Salvelinus fontinalis
(Brook Trout) habitat use and dispersal patterns within Adirondack Mountain
headwater streams. Hence, fishery managers are left with information gaps regarding
the specific habitat conditions characteristic of sustainable Brook Trout populations in
Adirondack flowing waters. Through the use of single-pass electrofishing and markrecapture
techniques, size-class specific microhabitat use and reach-scale movement
patterns for Brook Trout were examined within two northern Adirondack streams. Water
depth, water velocity, and substrate-size use were observed to be similar among two
Brook Trout size classes. Both size classes exhibited use patterns within deeper slowermoving
pool habitats; however, larger Brook Trout were found to be associated with
smaller-sized substrates within one of our study sites. These habitat-use patterns were
also supported by comparison of stream hydrologic condition, including Froude number.
Brook Trout movement patterns were found to be dependent on both size class and
season. Smaller-sized trout exhibited increased movement during the spring, whereas
larger trout were found to be more mobile and move more frequently during early fall.
Lastly, we examined the proportion of Brook Trout moving upstream/downstream and
found a greater frequency of smaller Brook Trout moving upstream during late summer.
Introduction
Of the factors that influence the presence, abundance, and distribution of biota
in the environment, habitat conditions are known to carry the greatest influence
(Reyjol et al. 2001). Fish habitat use is an important component of their biology,
especially for stream-resident (non-diadromous) fish, which endure extensive
hydrologic variation in stream channels. As a result of deficiencies in literature
and scientific research involving Salvelinus fontinalis (Mitchill) (Brook Trout ) in
Adirondack streams, it is essential to classify Brook Trout habitat use within these
systems. Studies have observed habitat shifts among varying age-classes of streamresident
salmonids, and have suggested that younger individuals typically occupy
shallow, slow-flowing stream habitats, while the larger individuals reside at greater
depths (Mäki-Petäys et al. 1997). Under natural stream conditions, Brook Trout
have also been found to predominantly use pool habitats (Hansbarger 2005).
The long-term debate over the movement patterns associated with streamresident
fish has been closely examined since Gerking’s (1959) seminal
research. The early concept of restricted movement was later termed the restricted
movement paradigm (RMP) (Gowan et al. 1994). According to the
1US Fish and Wildlife Service Region 5, 3817 Luker Road, Cortland, NY 13045. 2Department
of Earth and Environmental Science, State University of New York, 101 Broad
Street, Plattsburgh, NY 12901. *Corresponding author - Justin_Ecret@fws.gov.
20 Northeastern Naturalist Vol. 20, No. 1
RMP, stream-resident fish are primarily sedentary, or immobile. As a result,
these fish exhibit minimal movement and reside in natal pools. Consequently,
these fish remain within, or in proximity to, their initial capture site during
mark-recapture and movement studies. In subsequent research, the RMP has
been challenged, as a result of findings proposing that stream fish populations
are not exclusively homogenous in their movement patterns, but rather are comprised
of both sedentary and mobile individuals (Penzcak 2006). Subsequent
studies have also provided evidence that individual stream-resident salmonids
exhibit dual movement behavior and “switch” between sedentary and mobile
movements between seasons (Hilderbrand and Kershner 2000, Morrissey and
Ferguson 2011, and Smithson and Johnston 1998). Long-range movement patterns
exhibited by salmonids have been well documented (Hilderbrand and
Kershener 2000, Peterson and Fausch 2003, Sorensen et al. 1995). Furthermore,
riverine fish species populations have been suggested to be comprised of both
static (i.e., sedentary) and highly mobile individuals (Penczak 2006).
Salmonids have been closely studied by federal and state agencies, as well as
among local anglers, as they are of great local conservation importance within
the Adirondacks (EBTJV 2006). Recent assessments of Brook Trout populations
have been conducted in response to the growing concern of the above-mentioned
stakeholders with the rapid decline in native Brook Trout populations. The distribution
of self-sustaining Brook Trout populations has been greatly reduced from
its natal range, once extending from the Appalachian Mountains to the Carolinas
and as far north as Atlantic Canada and west to the Great Lakes regions (Hudy
et al. 2008). Extensive research and monitoring has illustrated the physical,
chemical, and biological watershed-level changes over the past 200 years and
has demonstrated that Brook Trout respond negatively to such changes across the
eastern United States (Hudy et al. 2008).
Furthermore, the spread of non-native coldwater fishes, as well as habitat
fragmentation via dams, road crossings, and extensive channelization, have all
contributed to the decline in self-sustaining Brook Trout populations (Hudy et
al. 2008). Understanding the habitat use and movement patterns associated with
Brook Trout , as well as other stream-resident fish, is crucial in order to provide
future protection and commence restoration. Species-specific and age-class
movement data could assist in land-management policies that promote the enhancement
of threatened Brook Trout populations.
Methods
Field-site description
Both study streams are within the True Brook watershed in Clinton County,
which is located in the Adirondack Park in northern New York. The larger of the
two streams, Fall Brook is a total of 24.5 km and drains a catchment area of approximately
10.8 km2, while the smaller un-named stream (TB10) is a total of
5.03 km in length and drains a catchment area of approximately 1.9 km2. The
study site (44°39.21'N, 73°49.5'W) was selected on the basis of preliminary examination
of potential fish passage impediments by various crossing structures
2013 J. Ecret and T.B. Mihuc 21
within 9 sub-watersheds (including True Brook) in Essex and Clinton counties
(Mihuc et al. 2008). Both TB10 and Fall Brook contain a minimum of one crossing
structure, all of which were assessed and evaluated and showed varying rates
of fish passage (Mihuc et al. 2008). In addition, Salmo trutta L. (Brown Trout )
were observed within the lower reaches of both streams during the sampling portion
of this study. The local landscape mostly consists of heavily forested areas
that are moderately fragmented by rural residences (Fig. 1).
Study design
Fish were captured using a DC backpack electrofisher (300–400 volts, 30-cm
anode) using a single-pass technique and were individually tagged with a small
(1-mm) individually numbered aluminum tag (National Band and Tag Co., Newport,
KY) within the two major tributaries. The smaller of the two tributaries,
TB10, was sampled in its entirety, and consisted of a total study reach of approximately
1600 m extending from the mainstream of True Brook to its associated
headwater. Contrastingly, the larger tributary, Fall Brook, was only sampled from
the mainstream of True Brook approximately 900 m upstream, due to restricted
stream access. The first fish-tagging event was conducted in June 2010, followed
by three subsequent sampling sessions and fish-tagging events during July, August,
and October. Selection for sampling sessions was not based on any specific
criteria; however, we did expect fish movements to be greatest during early June
and July as a result of elevated stream discharge (i.e., snowmelt runoff) and again
during October during spawning (Peterson and Fausch 2003).
Following Bond and Lake (2003), an anchored float was placed within the
stream indicating the fish’s initial location in order to record habitat variables.
Throughout all four sampling events, habitat variables were measured and recorded,
and fish were identified and tagged within the peduncle region, just
anterior to the lower portion of the caudal fin, prior to release at point of capture
(Fig. 2). Trout total length (cm) and mass (g) were also recorded, enabling us
to provide size-class-specific microhabitat assessments for Brook Trout. Again,
following Bond and Lake (2003), fish sampling-point microhabitats (e.g., stream
depth [cm], water velocity [m/s], and substrate size [cm]), from the initially
marked bobber and sinker, were measured and recorded within an approximate
1-m quadrat around the bobber and sinker. Stream depth was measured from
streambed bottom to water surface; substrate size was measured by recording the
longest axes of a randomly selected substrate within the quadrat. Additionally,
two supplementary depth and velocity measurements were taken within the quadrat.
All velocity measurements were recorded at approximately 0.4 x [depth],
measured upward from the streambed (Gore 2006).
During the first sampling session, researchers delineated and marked with
flags 25-m sub-reaches within both streams. The reach location (distance [m]
from the main confluence of True Brook) where each tagged trout was captured
during each sampling event was recorded. Sub-reach delineation followed that
of earlier research conducted on dispersal patterns of stream-dwelling salmonids
(Hutchings and Gerber 2002, Morrissey and Ferguson 2011, Wilson et al. 2004).
22 Northeastern Naturalist Vol. 20, No. 1
Figure 2. Photograph depicting placement of individually numbered aluminum tags,
placed within the penducle region of successfully captured and tagged Brook Trout.
Figure 1. True Brook (Clinton County, NY). The two study streams are Fall Brook and
TB10. Each study reach began at the main confluence of the study stream with True
Brook and extended a minimum of 0.9 km upstream.
2013 J. Ecret and T.B. Mihuc 23
Three subsequent sampling events allowed us to collect both microhabitat
and seasonal movement data for Brook Trout in these streams using point
abundance estimates. This method permits both microhabitat variables and fish
movement patterns to be accounted for within the system. In order to compare
trout habitat variables to overall stream habitat, we also recorded randompoint
sampling of each of the microhabitat variables previously mentioned
throughout the entire study stream during all sampling events. There were approximately
10 random points to record habitat variables per 25-m sub-reach;
these points were randomly selected simply by identifying stream habitats
where trout were not observed or captured.
In order to determine size-class-specific variation among fish microhabitat use,
we used a Mann-Whitney U test to compare microhabitat use between two fish size
classes to habitat availability in two headwater streams (SPSS v.16.0) (P = 0.05).
We compared the medians of habitat variables among both size classes of Brook
Trout, as well as random variables using a non-parametric test. Stream hydraulic
habitat conditions (e.g., Froude number) were also compared using the same analysis
techniques among fish size classes and random-point sampling. All variables
were tested for correlation using Pearson’s correlation (2 -tailed), and positive correlations
existed between random depth, Froude number, and substrate size (P less than
0.001). Random velocity did not correlate with any of the other random variables
or any of the measured fish variables in either fish size class (SC1, SC2).
Hydraulic habitat assessments facilitate proficient habitat representation
in that they incorporate multiple habitat use. Froude number (v/[dg]0.5) is a
dimensionless value that characterizes open channel flow based on a ratio of
velocity (v) to hydraulic depth (d) and the acceleration due to gravity (g =
9.81m/s2). A Froude number greater than 1.0 represents fast rapid flow conditions
(supercritical flow), whereas a Froude number less than 1.0 represents slow or
tranquil hydraulic conditions (subcritical flow). For the purpose of this study, we
substituted stream depth for hydraulic depth in order to calculate Froude number
for both fish and random sampling points. Additionally the proportion of Brook
Trout found in pool and riffle habitats was also determined. Jowett (1993) classifies
a Froude number less than 0.18 as pools and greater than 0.41 as riffles. This
study used a modification of Jowett (1993) classification of pool and riffles, in
that pools were determined by a Froude number less than 0.18 and riffles by a
Froude number greater than 0.18 due to the low sample size of riffle features.
The location within the reach (number of meters from stream outlet) of each successfully
recaptured Brook Trout was recorded in order to determine approximate
distance and direction moved between sampling events. Habitat use and movement
data was only collected for Brook Trout; however, total length and weight
for successfully captured Brown Trout was also recorded.
Results
During each sampling event, stream and fish sampling consistently began at
TB10 and continued until the stream was sampled in its entirety (approximately
24 Northeastern Naturalist Vol. 20, No. 1
1600-m study reach), followed by the same sampling protocols at Fall Brook
(approximately 900 m). The entire research study occurred over a total of 28
sampling days (18 and 10 days at TB10 and Fall Brook, respectively). The mean
and median water depth, velocity, and substrate size was calculated from all fish,
random, and supplementary locations for both TB10 and Fall Brook for each
sampling session.
Overall, there was a greater number of successfully captured Brook Trout at
TB10 (n = 736) compared to Fall Brook (n = 273), both sites combined constituted
a total of 173 recaptured marked Brook Trout upon study completion within
the two major tributaries (Table 1). Overall, there was consistently a greater
proportion of Brook Trout captured and tagged among the smaller size class
within both study streams. However, there was a greater number of larger trout
Table 1. Capture and tagging data per sampling event for Brook Trout size class within TB10 (top)
and Fall Brook (bottom). Brook Trout length is expressed as the mean ± SD.
SC1 SC2 Total
TB10
June NCaptured 239 84 323
NTagged 211 80 291
NRecapture 0 0 0
Mean length (cm) 12.1 ± 1.3 17.1 ± 3.2
July NCaptured 144 64 208
NTagged 23 7 30
NRecapture 17 24 41
Mean length (cm) 12.4 ± 1.1 17.4 ± 4.2
August NCaptured 94 35 129
NTagged 9 5 14
NRecapture 37 22 59
Mean length (cm) 12.4 ± 1.0 17.0 ± 4.0
October NCaptured 60 16 76
NTagged 0 0 0
NRecapture 12 15 27
Mean length (cm) 10.0 ± 2.3 16.7 ± 2.3
Fall Brook
June NCaptured 50 25 75
NTagged 49 25 74
NRecapture 0 0 0
Mean length (cm) 12.4 ± 1.4 17.0 ± 2.3
July NCaptured 51 38 89
NTagged 21 35 56
NRecapture 6 9 15
Mean length (cm) 12.5 ± 1.1 15.5 ± 2.5
August NCaptured 29 21 50
NTagged 4 20 24
NRecapture 13 14 27
Mean length (cm) 13.0 ± 0.7 17.7 ± 2.9
October NCaptured 46 13 59
NTagged 0 0 0
NRecapture 3 1 4
Mean length (cm) 9.6 ± 3.2 18.7 ± 7.1
2013 J. Ecret and T.B. Mihuc 25
recaptured compared to smaller trout as the study progressed (Table 1). There
was a total of 43 Brook Trout that exhibited tag loss with both study streams,
and smaller-size Brook Trout had a higher percentage of tag loss (SC1 = 69.8%,
SC2 = 30.2%) within both study streams. However, tagged Brook Trout did not
exhibit any noticeable impairment of swimming abilities, nor was there any immediate
mortality observed.
Other observed fish species consisted of Brown Trout , Cottus cognatus Richardson
(Slimy Sculpin), Rhinichthys atratulus (Hermann) (Blacknose Dace), and
Catostomus commersoni (Lacepède) (White Sucker). Although Brown Trout were
observed within both study streams, habitat and movement data were not collected.
The frequency and size of both Brook and Brown Trout was collected and showed
that theses streams were predominantly inhabited by Brook Trout among the 13.5–
14.5-cm size range, with a fewer number of Brown Trout (Table 2).
Habitat data
In order to evaluate Brook Trout microhabitat use, all measured Brook Trout
were placed into two major size classes (SC), where SC1 and SC2 represented
Brook Trout less than and greater than 14.5 cm in total length, respectively.
Length-frequency data were compiled for both study sites; the smaller stream,
TB10, was composed of predominately Brook Trout within the 11–12 cm length
range, while Fall Brook consisted mostly of Brook Trout in the 13–14 cm range.
The median seasonal water depth, velocity, and substrate size were compared
between Brook Trout size classes, as well as between random sampling
points, in order to determine fish size-class-specific microhabitat use. Overall,
water depth appeared to be the most definitive microhabitat variable influencing
Brook Trout of both size classes within both study streams. A greater
proportion of Brook Trout among both size classes was found in pool habitats
(Fr < 0.18), as compared to riffle habitats (Fr > 0.18) in both TB10 and Fall
Brook (Fig. 3).
Microhabitat use
With the exception of median substrate size, microhabitat use did not significantly
differ between the two Brook Trout size classes in TB10 (Table 3). The
median substrate size associated with Brook Trout of SC1 (15.0 cm) was significantly
larger than the median substrate size of SC2 (12.0 cm) (Table 3, Fig. 4B).
Both the median water depth and water velocity use did not significantly differ
between SC1 and SC2 (Table 3; Fig. 4A, C). However, both size classes greatly
differed for multiple microhabitat use in relation to overall habitat availability
(random points). Median water depth for SC1 (20.0 cm) and SC2 (21.3 cm) were
Table 2. Mean length ± SD for brook and Brown Trout in TB10 and Fall Brook.
TB10 Fall Brook
Species n Length (cm) n Length (cm)
Brook Trout 736 13.4 ± 2.5 273 14.4 ± 3.3
Brown Trout 8 13.4 ± 2.6 1 19.5
26 Northeastern Naturalist Vol. 20, No. 1
significantly greater than the median water depth at random stream locations
(14.0 cm) (Table 3, Fig. 4A). Additionally, both size classes exhibited different
microhabitat use within regions of stream with lower water velocities, where
SC1 (0.10 m/s), and SC2 (0.09 m/s) were more prevalent in stream habitats with
significantly lower water velocities in relation to their habitat availability (0.24
m/s) (Table 3, Fig. 4C). Lastly, the median substrate size of SC2 (10.0 cm) within
TB10 was significantly smaller than the median substrate size at random stream
locations (16.0 cm) (Table 3, Fig. 4B).
The only microhabitat variable that significantly differed between Brook
Trout size classes within Fall Brook was median water depth, where the median
water depth for SC2 (26.0 cm) was significantly deeper compared to the
median depths of SC1 (22.0 cm) (Table 4, Fig. 5A). There was no statistical
difference in median water velocity and median substrate-size use between
size classes within Fall Brook (Table 4; Fig. 5B, C). Similar to TB10, both size
classes differed in their median water-depth use in relation to their overall
habitat availability. The median depth for SC1 (22.0 cm) and SC2 (26.0 cm)
were both significantly deeper compared to median random depth locations
(18.0 cm) (Table 4, Fig. 5A). There were also statistical differences between
Figure 3. The number of Brook Trout that were found in pools and riffles at (A) TB10 and
(B) Fall Brook throughout the study duration. Pools and riffle classifications derivation
after Jowett (1993).
Table 3. Mann Whitney U test for the effects of Brook Trout size-class on the habitat use among
three microhabitat characteristics at study site TB10. Ns = not significant (P > .05).
Size class Depth Velocity Sub Froude No
SC1 vs. SC2 ns ns 0.01* ns
SC1 vs. Random <0.001** <0.001** 0.05* <0.001**
SC2 vs. Random <0.001** <0.001** <0.001** <0.001**
2013 J. Ecret and T.B. Mihuc 27
Figure 4. The median water depth (A), substrate size (B), water velocity (C), , and Froude
number (D) at TB10. Error bars display standard error.
size classes and random points within Fall Brook in terms of median water
velocity, where the median water velocity for SC1 (0.20 m/s) and SC2 (0.16
m/s) were significantly lower than the median water velocity at random points
(0.30 m/s) (Table 4, Fig. 5C). There was no statistical difference in regards to
median substrate size within study site Fall Brook (Table 4, Fig. 5B).
Table 4. Mann Whitney U test for the effects of Brook Trout size-class on the habitat use among
three microhabitat characteristics at study site Fall Brook. Ns = not significant (P > .05).
Size class Depth Velocity Sub Froude No
SC1 vs. SC2 <0.001** ns ns <0.05*
SC1 vs. Random <0.001** <0.001** ns <0.001**
SC2 vs. Random <0.001** <0.001** ns <0.001**
28 Northeastern Naturalist Vol. 20, No. 1
Hydrologic habitat classification
Brook Trout habitat was also evaluated among Brook Trout size classes and
random points by comparing the median Froude number. Both study sites showed
similar trends, such that Brook Trout among both size classes were observed in
stream conditions with lower than median Froude number as compared to that of
random stream locations (Tables 3, 4; Figs. 4D, 5D).
There was no statistical difference in mean Froude number between Brook
Trout size classes; however, microhabitat use for both size classes showed significant
differences in comparison to random stream habitats. The median Froude
number for SC1 (0.08) was significantly lower than the median Froude number
(0.21) associated with random stream locations. Additionally, the median Froude
number of SC2 (0.12) was significantly lower than the median Froude number at
random locations (0.23) (Table 3, Fig. 4D).
There were greater differences between Brook Trout size classes in Fall Brook
as compared to those of TB10. Specifically, Brook Trout of SC1 were observed
more often in stream habitats with higher median Froude number as compared
Figure 5. The median water depth (A), substrate size (B), water velocity (C), and Froude
number (D) at Fall Creek. Error bars display standard error.
2013 J. Ecret and T.B. Mihuc 29
to SC2. The median Froude number for SC1 (0.12) showed no statistical significance
when compared to the median Froude number for SC2 (0.12) (Table 4, Fig.
5D). Finally, there was no statistical distinction between the median Froude number
of Brook Trout size classes and random stream locations within Fall Brook
(Table 4, Fig. 5D).
Fish Movement
It was assumed that fish immigration derived exclusively from the mainstem
of True Brook in TB10 due to it being sampled in its entirety (1600 m), whereas
fish immigration could derive from both the mainstream of True Brook as well
as upstream reaches in Fall Brook because Fall Brook was not sampled to its
headwater. The average distance moved, directional movement patterns (i.e., upstream
or downstream), and percent of movement were determined for both size
classes within both TB10 and Fall Brook. There was a greater number of recaptured
Brook Trout in TB10; however, both sites were composed of both sedentary
and mobile individuals. The majority of the recaptured Brook Trout made short
distance movements (<100 m) in both TB10 and Fall Brook, while 28% and
24% of recaptured Brook Trout, in TB10 and Fall Creek respectively, exhibited
no movement and remained at their initial point of capture throughout the duration
of the study (Table 5). SC1 (n = 72) in TB10 and SC1 (n = 25) in Fall Creek
moved a greater mean distance during July compared to SC2; furthermore, SC2
(n = 51) in TB10 and SC2 (n = 23) in Fall Creek moved a greater distance during
August and October compared to SC1 (Fig. 6A, B) However, both size classes
in TB10 exhibited the most movement during October (Fig. 6A). In Fall Brook,
the longest average distance moved by Brook Trout was observed by SC1 in July
(Fig. 6B). In addition, smaller sized Brook Trout within both study streams exhibited
a greater mean distance moved upstream during July, and a greater mean
distance moved downstream during August and October (Fig. 7).
Both TB10 and Fall Brook were composed of sedentary and mobile Brook
Trout. Overall, the majority of Brook Trout in both streams showed small-scale
movement patterns and remained close to or at their initial capture location.
However, individual Brook Trout did move distances greater than 600 m. In both
study streams, SC1 Brook Trout displayed increased movement patterns (>200
m) compared to SC2 Brook Trout both upstream and downstream (Fig. 7). Despite
moving distances greater than 100 m, a greater proportion of SC2 Brook
Trout displayed shorter movement patterns (<100 m) (Table 5) compared to SC1
Table 5. Percent of movement for Brook Trout size classes at TB10 and Fall Brook. (Percents are
based on the number of recaptured trout upon study completion.)
SC1 SC2
% short % long % short % long
% no movement movement % no movement movement
Stream movement (<100 m) (>100 m) movement (<100 m) (>100 m)
TB10 28% 54% 18% 26% 62% 12%
Fall Brook 24% 68% 8% 26% 61% 13%
30 Northeastern Naturalist Vol. 20, No. 1
Figure 7. Seasonal mean distance moved for Brook Trout of SC1 at TB10 (A), SC2 at
TB10 (B), SC1 at Fall Brook (C), and SC2 at Fall Brook(D). Distance moved was between
previous point of capture and final recapture location. Negative values indicate
Brook Trout that moved downstream.
Figure 6. Mean distance moved for Brook Trout at TB10 (A) and Fall Brook (B).
2013 J. Ecret and T.B. Mihuc 31
Brook Trout in both TB10 and Fall Creek. Brook Trout in SC1, in both TB10 and
Fall Brook, exhibited greatest movement downstream (>200 m) during October
(Fig. 7A, C).
Discussion
The initial aim of this research study was to define and quantify Brook Trout
habitat use within Adirondack headwater streams, as well as to examine the
seasonal movement patterns among different age-classes of Brook Trout. We hypothesized
that habitat use would vary between Brook Trout size classes, where
smaller-sized Brook Trout would occupy shallow, slow-moving stream areas and
larger Brook Trout would occupy deeper stream regions. We also theorized that
smaller Brook Trout would exhibit greater movement patterns, and move larger
distances, in contrast to larger Brook Trout, which would remain sedentary.
Research has shown that salmonid fishes are not uniform in their habitat selection;
rather they vary habitat selection based on seasonal variation, fish size, diel
variation, food availability, and presence of intra-and interspecfic competitors
(Huusko and Yrjana 1997, Mäki-Petäys et al. 1997).
Water depth was the most prominent habitat variable exhibited for Brook
Trout habitat use. Both size classes were more prevalent in pool habitats
(Fig. 3) and were also found to occupy significantly deeper stream areas when
compared to overall habitat availability. Within both study streams, largersized
Brook Trout were observed in significantly deeper stream habitats than
younger fish demonstrating varying habitat use among different size-classes of
Brook Trout (Tables 3, 4; Figs. 4A, 5A). Fausch and White (1986) suggest that
stream-resident salmonids choose focal points in streams with low velocities in
order to minimize energy expenditure from actively swimming; furthermore,
stream-resident salmonids remain close to currents to maximize energetic gains
by feeding on invertebrate drift. This finding could suggest that larger-sized
Brook Trout demonstrate competitive dominance for favorable habitat conditions.
These results provide support for Mäki-Petäys et al.’s (1997) findings
that showed statistical differences in habitat use among trout age classes in
northern Finland. Mäki-Petäys et al. (1997) illustrated preference for deeper
stream habitats among larger-sized Brown Trout, as compared to smaller trout.
These results could in part be attributed to intercohort competitive interactions,
whereby larger trout exclude smaller trout from more favorable stream habitat
areas (Fausch and White 1986).
Water velocity has been shown to be a strong influential factor contributing
to habitat selection for stream-resident salmonids (Reyjol et al. 2001).
However, we observed water velocity and substrate size to be secondary
factors contributing to Brook Trout habitat use. There were no statistical differences
between fish size classes in either study stream in regards to water
velocity. However, in both study streams, both fish size classes were found in
significantly slower habitats as compared to overall habitat availability (Tables
3, 4; Figs. 4C, 5C). Likewise, there was no significant difference in substratesize
selection between trout size classes at Fall Brook; however, Brook Trout
32 Northeastern Naturalist Vol. 20, No. 1
of SC2 within TB10 were found at stream regions with significantly smaller
substrates compared to SC1 (Table 3, Fig. 4B). Witzel and MacCrimmon (1983)
showed that Brook Trout selected habitats with significantly smaller-sized substrates,
as compared to Brown Trout, in a series of southwestern Ontario stream
systems, successfully demonstrating the varying habitat use among salmonid
species. Water velocity has also been shown to be interdependent with substrate
size because larger substrates typically are associated with higher velocities
(Armstrong et al. 2003). These two coupled habitat parameters may play a more
focal role for stream-resident salmonids during spawning seasons (Shirvell and
Dungey 1983). Larger reproductive Brook Trout may select for stream areas
with higher velocities in order to adequately ventilate redds during embryo
development, or may choose to spawn in stream regions with larger substrates
to improve redd structure and stability, or a combination of both. Shirvell and
Dungey (1983) suggest that stream-resident salmonids select for water velocity
as a surrogate for substrates during spawning.
Froude number is a useful descriptor of the hydraulic habitat conditions at
stream regions because it is a dimensionless value that can be used to compare
habitat conditions between small-scale streams and larger river systems as well
as among different fish species (Armstrong et al. 2003). Similarly with water
velocity and substrate size, both Brook Trout size classes within TB10 were
found in stream habitats with significantly lower Froude numbers as compared
to that of random locations (Table 3, Fig. 4D). In-stream enhancement structures
were found to increase habitat availability and trout density by creating a more
spatially complex microhabitat with reduced water velocity and Froude number
values (Huusko and Yrjana 1997).
Overall, Brook Trout populations in our study were composed of both immobile
and mobile individuals. Brook Trout of SC1 within both TB10 and Fall
Creek showed increased upstream movement (>200 m) during July and increased
downstream movement during August and October. The only increased movement
displayed by SC2 was during October, in which larger Brook Trout moved
larger distances upstream (> 100 m) compared to the other two sampling events
during July and August. (Fig. 7). These Brook Trout movement patterns have
been well documented, showing an increase in movements during early spring
and early fall due to increased flow events (Gowan and Fausch 1996, Jackson
and Zydlewski 2009, and Peterson and Fausch 2003). The reduction in movement
during summer months has been attributed to Brook Trout seeking thermal refuge
in deeper pool habitats. Moreover, we also observed minimal trout movements
(<50 m) during the summer. Our stream and fish sampling methods could have favored
capturing Brook Trout in pool habitats due to their reduction in movement
during summer months. Brook Trout have been shown to migrate to deeper pond
or lake areas, and remain in these areas and exhibit little movement (Jackson and
Zydlewski 2009). Peterson and Fausch (2003) suggested that during the summer,
Brook Trout move more frequently upstream seeking colder water conditions.
Movement and habitat selection may work in conjunction, causing smaller
Brook Trout to move to more suitable foraging sites. Riffle habitats have been
2013 J. Ecret and T.B. Mihuc 33
shown to have higher densities of some aquatic macoinvertebrates that occupy
the interstitial spaces within the substratum; these habitats provide both
food resources and protection from fish predators. Also, the larvae of other
suspension-feeding macroinvertebrates are more common in stream habitats
with reduced flow. Likewise, riffle habitats serve to assist in dispersal for
aquatic macroinvertebrates (Malmqvist 2002). Mäki-Petäys et al. (1997) suggest
that riffle margins may constitute the more profitable habitat conditions for
stream-resident Brown Trout.
This study shows that smaller Brook Trout utilize riffle habitats more frequently
than pool habitats, as compared to larger trout in both study streams (Fig. 3). This
finding may suggest that younger Brook Trout utilize riffle habitats as foraging
sites more often, while larger trout inhabit pools to forage. Differential feeding
behavior exhibited by Brook Trout may constitute varying habitat selection based
on foraging efficacy. In addition, preference for deeper habitats could be related
to stream cover, as these two habitat variables are highly correlated. Canopy cover
has been well recognized as a crucial habitat requirement for Brook Trout as a
means to control stream temperature, as well as providing allochthonous inputs
(Raleigh 1982). Selection for deeper habitats with increased canopy cover may
also be attributed to predator avoidance by stream fishes (Power 1987). However,
the absence of canopy cover as a habitat parameter within this study may be limiting
our interpretation of differential habitat use among difference size classes of
Brook Trout within our study streams.
The absence of Brown Trout habitat use and movement data within this
study may also be limiting the validity and understanding of Brook Trout habitat
selection, as well as their seasonal dispersal patterns within these stream
systems. The European Brown Trout has been widely introduced into stream/
river systems in the eastern United States and has been partially attributed to
the reduction and alteration of Brook Trout populations (Grant et al. 2002).
Although these two salmonid species differ in their natural habitat range, they
have been shown to share several biological and ecological characteristics,
which facilitate their overlap within stream habitats. Both sympatric Brook
and Brown Trout share similarities in life-history events, including fall spawning.
However, advantages in growth and foraging behavior exhibited by Brown
Trout may contribute to their competitive advantage and potential displacement
of Brook Trout (Dewald and Wilzback 1992). The reproductive and behavioral
activities of sympatric Brook and Brown Trout have been examined in natural
and laboratory settings, both of which have suggested a negative response of
Brook Trout when interacting with the nonnative Brown Trout (DeWald and
Wilzback 1992, Grant et al. 2002, Sorensen et al. 1995).
The sampling methods utilized in our study allowed us to measure Brook
Trout movement, but not without bias. Some factors of our study design, including
timing and spacing between sampling sessions, as well as tag loss, may
have influenced results. We did not observe any impairment of fish movement
or mortality, but external tags have been shown to significantly influence movement
by penetrating and impairing swimming muscles when inserted (Gowan
34 Northeastern Naturalist Vol. 20, No. 1
and Fausch 1996). Electrofishing may have also influenced Brook Trout habitat
data by causing Brook Trout to move further upstream during stream sampling
sessions. Studies have examined the potential impacts of electrofishing on rates
of fish injury and also the influence on fish movement (Gowan and Fausch 1996).
Although we marked Brook Trout habitat at first detection, fish may have shifted
their habitat use in response to our sampling methods.
Consequences for management
The influence and underlying dynamic nature of lotic systems has led
authors to overgeneralize stream-resident fish habitat-use patterns. Habitat
suitability and availability are often regarded as the most significant factors affecting
populations; thus, characterizing fish habitat is fundamental in restoring
threatened populations (Armstrong et al. 2003, Bond and Lake 2003). Factors
that influence habitat availability include dispersal barriers (i.e., road crossings)
and introduced species that restrict target species’ response to restoration
efforts (Bond and Lake 2003).
Managers have utilized in-stream structures, including road crossings and
barriers, to isolate and prevent threatened salmonid communities from non-native
competitors. However, modifications to a stream or river channel, such as
a road crossing, change physical habitat components (e.g., depth, velocity, and
substrate) and greatly alter fish populations. Research on the ecological impacts
of road crossings on stream-resident fish demonstrates that many species
are negatively impacted; moreover, dispersal barriers such as road crossings
have been shown to be major threats to both stream fish abundance and diversity;
furthermore, habitat fragmentation has been shown to drastically increase
the rate of extinction in stream networks (Letcher et al. 2007). However, understanding
individual salmonid species behavioral movement patterns, based
on varying life-history stages, must be considered prior to barrier construction.
Land-management agencies may be inadvertently trading the risk of extirpation
from invading fish species for other risks including restricted movement
to available stream habitats, as well as overall habitat fragmentation (Gowan
et al. 1994, Gowan and Fausch (1996). Our study demonstrates that native
Brook Trout share stream habitats with non-native Brown Trout, and preceding
studies have successfully illustrated behavioral and reproductive interactions
between these sympatric species (DeWald and Wilzback 1992, Grant et
al. 2002, Sorensen et al. 1995). Additionally, these results show that Brook
Trout populations are not homogenous in their movement patterns within Adirondack
headwater streams; rather, they are comprised of both sedentary and
highly mobile individuals. Understanding individual fish species movements
and habitat-use patterns will ultimately lead to a better comprehension of the
dynamic behavior of stream fish ecology allowing us to preserve and enhance
threatened fish populations.
Acknowledgments
A great deal of thanks to my graduate committee, Dr. Timothy Mihuc, Dr. Danielle
Garneau, and Dr. Edwin Romanowicz. I would also like to thank the faculty and staff
2013 J. Ecret and T.B. Mihuc 35
members of SUNY Plattsburgh and The Lake Champlain Research Institute for their time
and effort in completing this research. This work was funded by the United States Fish
and Wildlife Service, Trout Unlimited, and The Lake Champlain Research Institute.
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