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2018 SOUTHEASTERN NATURALIST 17(3):476–483
Movement of Southern Brook Charr in a North Carolina
Headwater Stream
Zachary W. Anglin1 and Gary D. Grossman1,*
Abstract - Little is known about the genetically distinct southern strain of Salvelinus fontinalis
Mitchell (Brook Charr), a species that is likely to be negatively affected by global
climate change at the southern extent of its range. We tagged 35 Southern Brook Charr
between March and October of 2011 and sampled for movements in May and October 2011
and May 2012. The study site in Ball Creek, NC, was 330 m long, and we sampled 2 ancillary
50-m sites located 300 m above and below the site boundaries. We recaptured a total
of 12 fish: 10 fish once, 1 fish twice, and another fish 3 times for a total of 15 recaptures.
Individuals recaptured in spring 2011 moved an average of 9 m downstream, whereas fish
recaptured in autumn 2011 moved an average of 7 m upstream. Fish recaptured in spring
2012 moved an average of 6 m upstream from their locations in autumn 2011. There was no
relationship between fish length or growth and either distance or direction moved. In addition,
there were no significant differences in length or mass of fish that were recaptured and
those that were not. The maximum distance moved by a single fish was 49 m downstream.
Our results suggest that Southern Brook Charr in headwater streams may have relatively
small home ranges (less than 20 m), although our conclusions were limited by small sample sizes
and a 34% recapture percentage based on individual fish. Given that most populations of
Southern Brook Charr occur in small streams above barriers, limited movements suggest
that population persistence will depend on satisfactory foraging, shelter, and reproductive
habitat types within a relatively small area. These requirements should be a concern for
managers given that global climate change will affect ambient temperatures and these populations
have limited opportunity for movement and emigration.
Introduction
The native distribution of Salvelinus fontinalis Mitchell (Brook Charr) encompasses
nearly the entire length of the Appalachian Mountain system. In streams
within their native range, especially within the Southern Appalachian region, native
Brook Charr populations generally are restricted to habitats above barriers that
prevent invasion by Salmo trutta L. (Brown Trout) and Oncorhynchus mykiss Walbaum
(Rainbow Trout), species introduced in eastern North America in the late 19th
century (Behnke 2002, Galbreath et al. 2001). Brook Charr occur in 2 genetically
distinct strains, i.e., Northern and Southern Brook Charr (Habera and Moore 2005,
Stoneking et al. 1981), and these forms likely justify the reclassification of Brook
Charr into separate subspecies or species. Despite strong genetic differentiation,
there is little published ecological information that can be used for management
or conservation of Southern Brook Charr (but see Anglin and Grossman 2013,
1Warnell School of Forestry and Natural Resources, University Of Georgia, Athens GA
30602. *Corresponding author - grossman@uga.edu.
Manuscript Editor: Nathan Franssen
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Grossman et al. 2010, Habera and Moore 2005). The need for ecological information
is particularly critical because the abundance and distribution of Brook Charr
in general and Southern Brook Charr specifically, has decreased substantially in the
past 3 decades primarily due to habitat degradation, invasive trout, and widespread
stocking of Northern Brook Charr (Hudy et al. 2008). In addition, given that Southern
Brook Charr exist at the southernmost extent of the species’ natural range, they
are likely to be affected by temperature increases and increasingly variable precipitation
produced by global climate change in the Southern Appalachian Mountains
(Flebbe et al. 2006, Ford et al. 2011, Laseter et al. 2012).
Although movement studies on Northern Brook Charr are not uncommon (Davis
et al. 2015, Petty et al. 2012), there appears to be little or no published information
on movements of Southern Brook Charr. Data for the northern strain demonstrate a
range of movement patterns, with headwater mountain populations demonstrating
relatively low movements (2 m/d) and main-stem or riverine populations displaying
substantial movements (Davis et al. 2015, Hartman and Logan 2010, Petty et
al. 2012). Given the lack of information on movement patterns of Southern Brook
Charr, coupled with the small population sizes and restricted distribution of this
species (Anglin and Grossman 2013, Grossman et al. 2010), we quantified movement
of Southern Brook Charr in a North Carolina headwater stream via passive
integrated transponder (PIT) tagging over 14 months. Grossman et al. (2010)
demonstrated that this population displays: (1) small maximum sizes (less than 15 cm SL),
(2) low maximum ages (3+), (3) low densities, and (4) population regulation via
density-dependent processes, although high winter flows affect growth of youngof-
the-year. We hypothesized that movements of Southern Brook Charr would be
affected by season, and that older (larger) fish would move greater distances than
younger (smaller) fish.
Methods and Materials
Study site
The study site consisted of a 330-m section of stream located within a third-order
stretch of Ball Creek, located on the USDA Forest Service Coweeta Hydrologic
Laboratory (35°11'N; 83°23'W) in Otto, NC. This site is typical of many relatively
undisturbed small streams in the Southern Appalachian region, especially those
occupied by Southern Brook Charr (Grossman et al. 2010). The study site was
bisected by a small natural waterfall, a possible barrier to fish movement. We used
this natural separation to split the site into upper and lower segments, each measuring
~150 m in length. The upper and lower sections were further sub-divided
and marked off at 10-m benchmark increments for movement estimates. The entire
330-m site was called the main site.
The main site was composed of riffle–pool geomorphology with little variation
in width (mean wetted width = 5.2 m ± 0.3 m 95% CI; measurements made
every 5 m of linear bank). The surrounding mixed hardwood–conifer forest provided
dense canopy cover, shading the stream during the growing season. Riparian
vegetation was dominated by Rhododendron maximum (Rhododendron), typical
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of headwater streams in the Blue Ridge Province of the southern Appalachian
Mountains. The fish assemblage within the site is composed of only 3 species: pure
Southern Brook Charr (T. King, United States Geological Survey, Leetown, WV,
now deceased, pers. comm.) and occasional Cottus bairdi Girard (Mottled Sculpin)
and Rainbow Trout (G.D. Grossman, pers. observ.).
Movement
We quantified movement patterns of Southern Brook Charr using electrofishing
and mark–recapture techniques with 12.0-mm PIT (Biomark) tags. These tags have
minimal effects after insertion (Acolas et al. 2007, Ombredane et al. 1998); however,
it was logistically infeasible to measure tag loss given the low density of the
population (see Grossman et al. 2010) and small number of fish tagged. We used a
seasonal sampling regime, and on 25 March 2011, we made a 1-pass electrofishing
sweep, starting 50 m above the downstream border of the main site and ending 50 m
below the upstream border of the main site (the middle 230 m). Southern Brook
Charr in this population can be aged (0+, 1+, 2+) by their lengths, which show little
overlap (Grossman et al. 2010), and we tagged all fish longer than 7 cm (standard
length [SL]). We did not tag smaller fish were for fear of internal injuries or negative
behavioral effects from handling stress and the size of tags, and so just returned
them to their point of capture. In addition, we did not tag fish in the upper- and
lowermost 50-m sections of the site because of the possibility that these fish would
move out of the sampled area; although these 50-m sections always were sampled
subsequently for tagged fish.
Tagging consisted of injecting a uniquely coded PIT tag into the body cavity
using a syringe tipped with a 12-gauge hypodermic needle. We weighed (digital
scale, ± 0.01 g), and measured (SL, straight edge, ± 1.0 mm) each tagged fish and
held them for a 30-minute recovery period prior to release at the site of capture. We
observed neither mortality nor aberrant behavior in fish during the recovery period.
All fish-capture locations were recorded to the nearest meter using maps drawn of
the main site. We calculated movement as the linear distance between capture and
recaptures, or between sequential recaptures for fish recaptured multiple times. All
subsequent seasonal samples (19 May 2011, 25 October 2011, and 25 May 2012)
employed this sampling methodology. We did not sample during summer because
the combination of high water temperatures, the disturbance from handling, and the
procedure of tagging unmarked fish likely would have stressed fish substantially.
We used a hand-held PIT tag reader to identify recaptured fish. To detect fish that
may have moved long distances (e.g., out of the site), we also sampled two 50-m
sites both 300 m below and above the borders of the site just after the 25 October
2011 sample. We used Wilcoxon rank sum tests to examine whether SL and mass
differed significantly between recaptured fish and unrecaptured fish. We also tested
for significant differences in movement based on length and sampling date using
analysis of variance (ANOVA). Given that fish can be aged based on their lengths,
we report results as length/age.
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Results
During sampling, we captured a total of 56 Southern Brook Charr (March 2011:
12 fish, May 2011: 23 fish, October 2011: 16 fish, and May 2012: 4 recaptures) of
which 12 fish were recaptured out of a total of 35 fish tagged (10 single recaptures,
1 double recapture, and 1 triple recapture). Twenty-one untagged fish were captured
and released: 3 were either too small (less than 70 mm, SL) to tag, and 18 were
captured in either the upper- or lowermost 50-m sections of the site. Recapture
rates based on individual fish and total recaptures were 34% and 43%, respectively.
Recaptured fish varied in size from 112 to 169 mm SL and represented mostly 2+
fish (Fig. 1). Of the 10 Southern Brook Charr recaptured once, 1 remained at the
initial position of capture, 6 moved an average of 18.2 (SD = 11.6) m upstream,
2 moved an average of 6.5 (SD = 2.1) m downstream, and 1 individual moved
49 m downstream. Although sample sizes were too small for statistical testing, the
6 individuals recaptured on 19 May 2011 moved an average of 9 (SD = 20.3) m
downstream and grew an average of 25 (SD = 5.0) mm SL over a 55-day period.
The 5 individuals recaptured on 25 October 2011, moved an average of 11.4 (SD
= 13.2) m upstream and grew an average of 13 (SD = 14.7) mm SL over a 159-day
period. The 3 individuals recaptured on 25 May 2012 grew an average of 10 (SD
=15.0) mm SL and moved an average of 6 (SD = 22.8) m upstream from their locations
on 25 October 2011, nearly a 7-month period. The double recapture displayed
only downstream movement (7 m and 2 m), whereas the triple recapture moved
upstream (7 m), maintained position (0 m), and moved downstream (8 m) over the
course of sampling. We did not observe either upstream or downstream movement
Figure 1. Movement data for age 1+ (<120 mm) and age 2+ (>125 mm) Southern Brook
Trout in Ball Creek for all sampling seasons. Negative x-values indicate downstream movement
whereas positive x-values indicate upstream movement. Demographic data on this
population can be found in Grossman et al. (2010).
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of fish over the waterfall. Movement data suggest that home ranges of Southern
Brook Charr in upper Ball Creek may be less than 20 m. There were no significant
differences in either length (W = 94.5, P = 0.11) or mass (W = 109.0, P = 0.27)
between recaptured and unrecaptured fish. In addition, fish length/age (F1, 11 = 0.46,
P = 0.51) or growth in length (F1, 11 = 0.21, P = 0.66) did not significantly affect
upstream or downstream movement or total distance moved. No tagged individuals
were recaptured in the sites 300 m below or above the main site.
Discussion
To our knowledge, these are the first published estimates of movements of
Southern Brook Charr, a species that is likely to be strongly affected by increases
in water temperature and precipitation variability predicted to occur with global
climate change (Flebbe et al. 2006, Ford et al. 2011, Laseter et al. 2012). Although
most Southern Brook Charr displayed some movement in all seasons,
total distances moved frequently were fairly limited (generally less than 20 m).
However, our design was biased against fish that moved long distances (e.g., out
of the study site), although sampling of 2 sites 300 m above and below the study
site boundary yielded no recaptures. Given that most populations of Southern
Brook Charr are confined to headwater streams above barriers, it is fortuitous that
at least some individuals in Ball Creek possess home ranges sufficiently small to
complete their life-cycles and maintain a persistent population in this restricted
habitat (see Grossman et al. 2010). Nonetheless, most Southern Brook Charr populations
are isolated and subject to genetic drift and inbreeding because of limited
genetic exchange among populations.
A variety of factors could have affected our analysis including the small number
of fish marked and recaptured. Nonetheless, recapture success (recapture rate =
34%) was similar to several other salmonid tagging studies (Creswell 1981, Deiterman
and Hoxmeier 2009, Turek et al. 2010). Regardless, the fate of individuals that
were not recaptured (i.e., a majority of fish sampled) remains unknown. Some may
have moved long distances that took them out of the study site and adjacently sampled
areas, others may have shed tags, and still others may have perished (Meyer
et al. 2011). Nonetheless, Meyer et al. (2011) suggested that salmonids of similar
size tagged with PIT tags should not experience high mortality. Finally, logistical
constraints prevented extensive upstream and downstream sampling aside from
the two 50-m sites, located 300 m from the upstream and downstream border of the
study site, and we may not have been able to detect many large-scale movements.
Finally, our data indicate that some 1+ and 2+ older Southern Brook Charr display
relatively restricted movements (sensu Gerking 1959), but it is unclear whether this
conclusion can be extrapolated to the population as a whole. Petty et al. (2012) also
found restricted movement of Northern Brook Charr in headwater streams.
All but 2 recaptured Southern Brook Charr were at least 2 years old. This may
be an artifact of electrofishing (i.e., older larger individuals are easier to capture
with electrofishing; Hense et al. 2010). Consequently, our movement data may
only be valid for larger and older Southern Brook Charr, although in a previous
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study older Northern Brook Charr were shown to be the most mobile segment of
the population (Petty et al. 2005). However, our data are from a 14-month period,
without summer sampling, and should be used with caution in years with differing
environmental conditions (i.e., low flows). Our results also were affected by the
low numbers of Southern Brook Charr present in the main site when compared to
previous years (Grossman et al. 2010).
Previous studies of Brook Charr movement have shown that a variety of factors
may affect movement, including gradient, water quality, reproduction, and resource
competition (Fausch and Young 1995, Petty et al. 2005, Riley et al. 1992). Roghair
and Dolloff (2005) observed Brook Charr recolonization of a Virginia stream after
natural defaunation, noting that 1.9 km of defaunated stream was recolonized from
upstream to downstream in 2.5 to 3.0 years (average = 0.69 km-1year-1). Brook
Charr in some populations display limited movement (e.g., less than 100 m; Adams et al.
2000, Hartman and Logan 2010, Hudy et al. 2010), whereas others from invasive
populations outside the native range show large-scale movements (e.g. >3000 m;
Gowan and Fausch 1996, Gowan et al. 1994).
Habitat degradation is a major problem for salmonids in North America (Elser
1968, Elwood and Waters 1969, Mortensen 1977), and global climate change will
likely exacerbate this problem via changes in physico-chemical factors such as
temperature, flow, and sedimentation. Our movement data should assist in the conservation
and management of Southern Brook Charr, the only salmonid native to
the Southern Appalachians. Our data suggest that management plans may need to
maintain all essential habitat types (spawning and foraging habitat) within a relatively
small area if populations of Southern Brook Charr are to persist.
Acknowledgments
Many individuals aided in tasks required for completion of this research. Specifically,
we thank J. and A. Anglin, G. Sundin, D. Elkins, C. Gatrell, G. Mitchell, S. Thomas, J.
James, R. Ratajczak, A., R., and B. Grossman, Jittery Joe’s and Michters Single Barrel. The
comments of both R. Bringolf and N. Nibbelink, and 2 anonymous referees improved the
manuscript. This project was supported by USDA Forest Service McIntire-Stennis program
grants GEO-00144-MS and GEO-00176-MS and the D.B. Warnell School of Forestry and
Natural Resources.
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