Validation of Annulus Formation in Otoliths of Notchlip
Redhorse (Moxostoma collapsum) and Brassy Jumprock
(Moxostoma sp.) in Broad River, South Carolina, with
Observations on their Growth and Mortality
Jason M. Bettinger and John S. Crane
Southeastern Naturalist, Volume 10, Issue 3 (2011): 443–458
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2011 SOUTHEASTERN NATURALIST 10(3):443–458
Validation of Annulus Formation in Otoliths of Notchlip
Redhorse (Moxostoma collapsum) and Brassy Jumprock
(Moxostoma sp.) in Broad River, South Carolina, with
Observations on their Growth and Mortality
Jason M. Bettinger1.* and John S. Crane1
Abstract - Moxostoma collapsum (Notchlip Redhorse) and the undescribed Moxostoma
sp. (Brassy Jumprock) form a large component of the fish assemblage in the Broad River,
SC, but little is known about their population characteristics, nor has an aging method
been validated for either species. We validate that one annulus is formed each year in the
lapillus otolith of the two species and identify spring as the period of annulus formation,
using chemical marking and marginal increment analyses, respectively. Notchlip Redhorse
and Brassy Jumprock are long-lived, with observed maximum estimated ages of 17
and 21, respectively. Both species grow quickly during their first few years; little growth
occurs after age 7. Instantaneous total mortality of each species was low (Z ≤ 0.35), suggesting
there is little exploitation of either species in the Broad River, SC.
Suckers (Pisces: Catostomidae) represent an important component of the
Broad River, SC, fish assemblage, accounting for more than 51% of total fish biomass
(Bettinger et al. 2003). Two species, Moxostoma collapsum Cope (Notchlip
Redhorse) and an undescribed Moxostoma sp. (Brassy Jumprock) (Jenkins and
Burkhead 1994), are among the most abundant fishes in the river, accounting for
more than 12% and 5%, respectively, of the relative abundance of all fish species,
and together comprising nearly 90% of the relative abundance of all catostomids
(Bettinger et al. 2003). Yet little is known about their age structure, growth, and
mortality within the Broad River or in other systems throughout their range.
In fact, there is limited published life-history information for catostomids in
general. Cooke et al. (2005) suggested that the paucity of available life-history
information has hampered conservation efforts for this diverse and ecologically
Notchlip Redhorse was recently removed from synonymy with Moxostoma
anisurum Rafinesque (Silver Redhorse) (Nelson et al. 2004), which only occurs
in the Mississippi basin and northward (Lee et al. 1980). Notchlip Redhorse is an
Atlantic Slope species ranging from Georgia to Virginia; its distribution in Lee et
al. (1980) is shown as the “southeastern race” of M. anisurum. Published information
on age and growth of Silver Redhorse is restricted to studies conducted in
the Mississippi basin (Hackney et al. 1971, Meyer 1962). Grabowski et al. (2007)
estimated the growth of four catostomid species, including Notchlip Redhorse, in
the Savannah River, South Carolina–Georgia.
1South Carolina Department of Natural Resources, 1921 Vanboklen Road, Eastover, SC
29044. *Corresponding author - BettingerJ@dnr.sc.gov.
444 Southeastern Naturalist Vol. 10, No. 3
Brassy Jumprock was formerly known as Moxostoma robustus Cope
(Smallfin Redhorse). However, Jenkins and Burkhead (1994:491 [footnote])
determined that the species was never described or validly named. While the
species remains undescribed at the time of publication, there is general consensus
that its common name is Brassy Jumprock (Jenkins and Burkhead 1994).
Brassy Jumprock is also an Atlantic Slope species ranging from Georgia to Virginia
(Lee et al. 1980:432). We were unable to find any published information
on the growth and longevity of either Smallfin Redhorse or Brassy Jumprock.
Several structures have been used to age catostomid species, including scales,
fin rays, opercle bones, and otoliths. However, the use of scales and fin rays has
been shown to be an unreliable estimator of age in older, mature Moxostoma
erythrurum Rafinesque (Golden Redhorse; Curry and Spacie 1984) and Catostomus
commersoni Lacepède (White Sucker; Sylvester and Berry 2006), though
fin rays were comparable to otoliths when estimating the ages of Catostomus
discobolus Cope (Bluehead Sucker), Catostomus latipinnis Baird and Girard
(Flannelmouth Sucker), and White Sucker in a Wyoming stream (Quist et al.
2007). Otoliths have been used and validated as an appropriate structure for estimating
the ages of Moxostoma carinatum Cope (River Redhorse; Hutson 1999),
Moxostoma duquesnei Lesueur (Black Redhorse), Golden Redhorse (Howlett
1999), and White Sucker (Thompson and Beckman 1995). Of the three otolith
pairs present, lapilli are preferred for age estimation of catostomids because they
are generally larger, more durable, and more readable than sagittae or asterisci
(Hoff et al. 1997).
The objectives of this study were to validate yearly annulus formation in the
otoliths of Notchlip Redhorse and Brassy Jumprock, determine the season of
annulus deposition, and describe the growth, longevity, and mortality of the two
species in the Broad River, SC.
The Broad River basin is a major division of the Santee River drainage. It
originates in North Carolina and dominates the central Piedmont of South Carolina
(Fig. 1). Within South Carolina, the Broad River basin encompasses 9819
square km; the river flows approximately 170 km until it merges with the Saluda
River, near Columbia, SC, to form the Congaree River. Average annual discharge
during 1999–2009, based on mean daily averages, of the Broad River approximately
11 km downstream from the North Carolina state line was 1546 cfs, while
average discharge 16 km below Parr Reservoir, near Columbia, SC, was 3912
cfs. Average annual water temperature at Carlisle, SC (mid-length of the river),
based on mean daily average was 17.9 ºC during 1999 through 2009, and average
annual minimum and maximum water temperatures for that period were 2.7 ºC
and 32.1 ºC, respectively.
The Broad River is relatively shallow with few unimpounded areas deeper
than 3 m. The majority of the habitat in the river is shallow sand-filled pools
2011 J.M. Bettinger and J.S. Crane 445
separated by bedrock shoals and gravel riffles. The river is interrupted by seven
hydroelectric dams with run-of-the-river impoundments ranging in size from 101
ha to 1781 ha.
During October 2001, 91 Brassy Jumprock (mean total length [TL] = 321
mm; range = 190–445 mm) and 33 Notchlip Redhorse (mean TL = 399 mm;
range = 217–475 mm) were collected from the lower Broad River, below Parr
Shoals Reservoir, with boat-mounted electrofishing gear. Each fish was measured
Figure 1. Broad River drainage in South Carolina, location of impoundments, and sites
sampled for catostomids during 2001 and 2006–2007.
446 Southeastern Naturalist Vol. 10, No. 3
to the nearest mm TL and received an intraperitoneal or intramuscular injection
of 0.5 cc of oxytetracycline (OTC, Liquamycin® LA-200®, Pfizer) to produce a
chemical mark on its otoliths that could be used later to document single annulus
formation per year. The fish were then transferred to the Cheraw State Fish
Hatchery, SC, and placed in grow-out ponds.
During November 2002, Brassy Jumprock and Notchlip Redhorse were harvested
from grow-out ponds and measured to the nearest mm TL. The lapillus
otoliths were removed from each fish, cleaned of connective tissue, dried with
paper towels, and placed in vials for storage. One otolith from each fish was then
placed in a mold and embedded in an epoxy resin (Araldite®). A 1–2 mm-thick section
was cut from the transverse plane of each embedded otolith with an Isomet®
low speed saw (Buehler LTD, Lake Bluff, IL) equipped with a diamond wafering
blade. Sections were mounted with an adhesive (Crystalbond™ 509, Electron
Microscopy Sciences) onto numbered microscope slides, sanded with 400–1500
grit sandpaper to remove saw marks, and polished on a felt pad with a 0.3-μm
polishing compound. Prepared sections were viewed at various magnifications
with a compound microscope and transmitted light. Otoliths were read independently
by two experienced readers, who estimated the age of each fish by counting
the number of opaque bands (annuli) (Fig. 2). Disagreements were resolved by
concurrence between the original readers and a third experienced reader when
disputed otoliths were reread simultaneously and discussed. Age agreement could
not be reached for one Brassy Jumprock and one Notchlip Redhorse. Otolith sections
were examined for fluorescent OTC marks with a JenaLumar compound
microscope (Zeiss Microscopy Group, Germany) equipped with a 50-W mercury
arc light source, and a filter set consisting of a 475-nm excitation filter, a 505-nm
dichroic mirror, and a 535-nm emission filter.
Based on the results of the OTC study, a subsequent study was initiated to
determine when annulus formation occurred. Notchlip Redhorse and Brassy
Jumprock were collected from one site on the lower Broad River near Columbia,
SC at least once every two months from September 2006 through June 2007.
Otoliths were prepared for age estimation as previously described, and marginal
increment analysis was used to determine the season of annulus formation. The
marginal increment ratio (MIR) was calculated as:
MIR = (R - Rn) / (Rn - Rn -1),
where R is the distance from the nucleus to the outer margin of the lapillus, Rn is
the distance from the nucleus to the outer edge of the last opaque band, and Rn-1
is the distance to the outer edge of the second to last complete opaque band. MIR
was only calculated for fish with two or more complete annuli.
Notchlip Redhorse and Brassy Jumprock were collected with boat-mounted
electrofishing gear from 10 sites along the Broad River during spring (April and
May) and fall (October and November) 2001 (Fig. 1). Fish were measured to the
nearest mm TL and weighed to the nearest gram. Lapillus otoliths were removed
during fall from up to four fish selected randomly from predetermined 25-mm
2011 J.M. Bettinger and J.S. Crane 447
length groups, and processed for age estimation as described previously. Because
we assumed fish caught in October and November had completed nearly all of
their growth for the year, we counted the margin as an annulus when estimating
fish age. This convention allowed for easier comparisons with growth studies that
relied on back-calculated ages, or that estimated ages using spring-caught fish.
Precision in age estimates between readers was assessed with the coefficient of
variation (CV), estimated as:
where Xij is the ith estimated age of the jth fish, Xj is the mean age estimate of the
jth fish, and R is the number of age estimates for each fish (Campana et al. 1995).
Since not all collected fish were aged, un-aged fish within 25-mm length groups
were assigned an age using a computerized age-length key (Isermann and Knight
2005) designed for that purpose. Growth of each species was estimated with a
Von Bertalanffy growth equation,
Figure 2. Sectioned lapillus otoliths from a 7-year-old (A) and 3-year-old (B) Brassy
Jumprock. Scale bar = 1 mm.
CVj = 100 x (√ΣR
i =1[(Xij -Xj)2) / (R - 1)] ) / Xj ,
448 Southeastern Naturalist Vol. 10, No. 3
= L∞ (1 - e-k (t - t0)),
where Lt = length at time t, L∞ = asymptotic length, k = growth coefficient, and
t0 = the theoretical age where Lt = 0 (Von Bertalanffy 1938). Instantaneous total
mortality (Z) of each species was estimated with a catch-curve based on the age
frequency data for fall-caught age 3 to age 13 Notchlip Redhorse and age 3 to
age 10 Brassy Jumprock (Ricker 1975). Instantaneous natural mortality was estimated
with the equation suggested by Hoenig (1983),
M = 4.22 (Tmax)-0.982,
where Tmax = maximum observed age in the population. Linear regression was
used to describe the relationship between log10 transformed TL and log10 transformed
weight for Notchlip Redhorse and Brassy Jumprock collected during
spring and fall. Observations having studentized residuals with absolute values
greater than 2.5 were considered outliers and were eliminated from regression
analysis. Analysis of covariance (ANCOVA) was used to test for seasonal differences
in regression parameters for each species.
On 5 November 2002, 12 Brassy Jumprock and 14 Notchlip Redhorse were harvested
from ponds at the Cheraw State Fish Hatchery. Survival of Brassy Jumprock
(13%) was poor, while that of Notchlip Redhorse was moderate (43%). Estimated
ages of OTC-injected Brassy Jumprock and Notchlip Redhorse ranged from 3 to 13
and 4 to 13, respectively. OTC marking efficacy was 100%, with each of the 26 otoliths
examined having an OTC mark on or just before the last fully formed annulus.
Based on distances between earlier annuli, we determined that the space between
the last annulus and the margin represented a year’s growth.
One hundred forty Brassy Jumprock (mean TL = 304 mm, range = 97–447
mm) and 107 Notchlip Redhorse (mean TL = 411 mm, range = 157–567 mm)
were collected for marginal increment analysis. Age was estimated for 57
Brassy Jumprock and 62 Notchlip Redhorse. Ages of Brassy Jumprock ranged
from 1 to 14, and ages of Notchlip Redhorse ranged from 0 to 21. Fifty-five
Brassy Jumprock and 46 Notchlip Redhorse between age 2 and age 12 were
included in the marginal increment analysis. The mean marginal increment
ratio increased from September through April for each species, then decreased
sharply between May and June, indicating that annulus formation occurred during
that period (Fig. 3).
Two hundred fifteen Brassy Jumprock (mean TL = 296 mm, range = 76–424
mm) and 429 Notchlip Redhorse (mean TL = 357 mm. range = 143–518 mm)
were collected from ten sites along the Broad River during 2001 (Table 1, Fig. 4).
For Notchlip Redhorse and Brassy Jumprock, the spring and fall TL-Wt regression
slopes were significantly different (ANCOVA, P < 0.0001), indicating that
the two species have different trends in weight relative to length between spring
2011 J.M. Bettinger and J.S. Crane 449
and fall. The TL-Wt relationship was significant for Notchlip Redhorse and
Brassy Jumprock during both seasons (P < 0.0001; Table 1).
Lapilli were removed from 75 Brassy Jumprock and 121 Notchlip Redhorse
and aged. Agreement between readers was 77% and 72% for Brassy Jumprock
and Notchlip Redhorse, respectively. For Brassy Jumprock, reader differences
ranged from 1 to 3 years, with the majority (94%) being 1 year (Fig. 5). For
Figure 3. Mean (± 2SE) marginal increment ratio by date for Notchlip Redhorse and Brassy
Jumprock collected from the Broad River near Columbia, SC during 2006 and 2007.
450 Southeastern Naturalist Vol. 10, No. 3
Notchlip Redhorse, reader differences ranged from 1 to 4 years, with the majority
(86%) being 1 year (Fig. 5). Most disagreements in estimated age were due
to differences identifying the first annulus. Mean CV in age estimates between
readers was 5.05 for Brassy Jumprock and 4.28 for Notchlip Redhorse.
Estimated ages for Brassy Jumprock ranged from 1 to 17. For Notchlip Redhorse,
they ranged from 1 to 19; an age-21 Notchlip Redhorse was collected
during our marginal increment study. Plots of age-class frequency distribution
(Fig. 6) indicated that both species become fully vulnerable to boat electrofishing
gear in their 3rd year when they attain lengths near 300 mm TL. Age-3 fish
accounted for 28% of Brassy Jumprock collected, while age-6 fish dominated
Notchlip Redhorse, accounting for 37% of those fish collected. Age-4 and age-
5 Notchlip Redhorse were grossly underrepresented in our samples, potentially
indicating poor recruitment of those year classes and variable recruitment in general
for the species. There is little if any exploitation of catostomids in the Broad
River drainage, which likely contributes to their longevity.
There was large variation in length at age for Notchlip Redhorse and Brassy
Jumprock (Fig. 7). Notchlip Redhorse and Brassy Jumprock grew quickly during
their first four years, attaining an average length of 336 mm TL and 319 mm
TL at age 4, respectively. After age 4, growth of both species slowed considerably,
and neither species grew much, if at all, with regard to length beyond
age 7. Von Bertalanffy growth model parameters were L∞ = 435.1 mm TL (SE =
7.9), t0 = -0.12 (SE = 0.25), and k = 0.36 (SE = 0.04) for Notchlip Redhorse, and
L∞ = 400.3 mm TL (SE = 8.6), t0 = 0.29 (SE = 0.14), and k = 0.43 (SE = 0.04) for
Brassy Jumprock. Estimated total instantaneous mortality Z of Notchlip Redhorse
was 0.27 (r2 = 0.51, P < 0.05); estimated instantaneous natural mortality
M was 0.21. Estimated Z for Brassy Jumprock was 0.35 (r2 = 0.70, P < 0.05);
estimated M was 0.26.
Based on our finding that one annulus is formed each year in lapillus otoliths
of Notchlip Redhorse and Brassy Jumprock, we conclude that otoliths are
Table 1. Length-weight regression coefficients, standard errors in parentheses, for Brassy Jumprock
and Notchlip Redhorse collected from the Broad River, SC during 2001.
Species n (mm) TL (mm) Wt (g) Age Slope Intercept r2
Spring 95 277 76–411 4–882 3.07 (0.02) -5.12 (0.04) 0.99
Fall 112 311 103–424 9–829 1–17 3.17 (0.02) -5.42 (0.05) 0.99
Combined 208 296 76–424 4–882 3.07 (0.01) -5.15 (0.04) 0.99
Spring 225 351 143–518 34–1424 2.90 (0.02) -4.73 (0.06) 0.99
Fall 190 365 157–485 45–1217 1–19 3.01 (0.02) -5.01 (0.06) 0.99
Combined 417 357 143–518 34–1424 2.93 (0.02) -4.81 (0.04) 0.99
2011 J.M. Bettinger and J.S. Crane 451
appropriate structures to use for age estimation in these species. Otoliths have
been shown to be reliable for estimating the ages of catostomids studied in different
locales (e.g., Hutson 1999, Sylvester and Berry 2006, Quist et al. 2007).
The May–June timing of annulus formation for Notchlip Redhorse and Brassy
Jumprock in the Broad River agrees with that of the closely related Silver Redhorse,
which forms its annulus during June–August in the Des Moines River,
IA (Meyer 1962) and, at lower latitude, late April–May in the Flint River, AL
Figure 4. Length-frequency distributions for Notchlip Redhorse and Brassy Jumprock
collected from the Broad River, SC during spring and fall 2001.
452 Southeastern Naturalist Vol. 10, No. 3
(Hackney et al. 1971). Other North American sucker species (Howlett 1999,
Hutson 1999), and indeed, most north latitude temperate fishes (Beckman and
Wilson 1995) undergo annulus formation during the same general time period in
The position of the OTC mark on or just before the last fully formed annulus
was unexpected. Our initial interpretation of this result was that annulus
formation occurred during fall, which would have been unusual. An alternative
explanation was that the stress associated with handling, marking, and transporting
the fish caused an anomalous growth check on the otoliths that was incorrectly
interpreted as an annulus. However, the spacing of annuli, including the putative
last annulus, on the otoliths was consistent with yearly growth. Our uncertainty
lead to the marginal increment analysis that demonstrated little growth occurred
Figure 5. Age-bias graphs for two readers of Brassy Jumprock and Notchlip Redhorse
otoliths. Numbers indicate sample size. Dashed line represents agreement between reader-
estimated age and final estimated age as determined by a concert read.
2011 J.M. Bettinger and J.S. Crane 453
in the otoliths of either species between November and May and that most otolith
growth (roughly 70%), and presumably fish growth, occurred between July and
September. Similarly, Meyer (1962) showed that most Silver Redhorse growth in
the Des Moines River, IA, occurred in late July, August, and September.
In both Notchlip Redhorse and Brassy Jumprock, fish collected during
spring were slightly heavier on average than fall-collected fish of similar
length; however, the disparity in weight decreased with increasing length, and
in Notchlip Redhorse, fall-collected fish larger than 350 mm TL were heavier
than spring-collected fish of similar size. The seasonal disparity in weight
for fish greater than 250 mm TL was less than 4% and less than 13% for Notchlip Redhorse
Figure 6. Age-class frequency distributions of Notchlip Redhorse and Brassy Jumprock
collected from the Broad River, SC during fall 2001.
454 Southeastern Naturalist Vol. 10, No. 3
and Brassy Jumprock, respectively. Whether the differences in weight relative
to length are of biological significance or the result of sampling error is
unknown; it is suggested that the combined equation be used to estimate
weight from length in these species.
Figure 7. Von Bertalanffy growth curves based on otolith-estimated age of Notchlip Redhorse
and Brassy Jumprock collected from the Broad River, SC during fall 2001.
2011 J.M. Bettinger and J.S. Crane 455
Notchlip Redhorse and Brassy Jumprock are long-lived in the Broad River,
SC. Notchlip Redhorse in the Broad River attained considerably older ages than
those reported in the Savannah River, SC–GA (Grabowski et al. 2007) or for the
closely related Silver Redhorse in the Flint River, AL (Hackney et al. 1971) and
the Des Moines River, IA (Meyer 1962), where the oldest captured fish were age
10 or less. However, those studies used only scales to estimate age; scales have
been shown to underestimate the age of older catostomids (Beamish and Harvey
1969, Quist et al. 2007, Sylvester and Berry 2006) as well as other species. Reid
(2009), using fin ray sections, estimated the maximum ages of Black Redhorse
and Moxostoma macrolepidotum Lesueur (Shorthead Redhorse) in Ontario to
be 17, comparable to our maximum estimated ages for Notchlip Redhorse and
The diminished growth in length of Notchlip Redhorse and Brassy
Jumprock after age 4 was likely due to maturation. Growth in fish length
is typically fastest before maturation. Once fish reach maturity, more energy
is invested in gonadal tissues than somatic tissues, which likely explains the
reduced growth in both species after age 4. The closely related Silver Redhorse,
as well as other moderate- and large-sized catostomids, are known to
spawn by age-5 (Jenkins and Burkhead 1994). Although growth in length of
both species slowed considerably after age 4, mature catostomids are heavier
per unit length than immature fish, and relatively small increases in length can
result in large increases in weight.
The large variation in length at age for Notchlip Redhorse and Brassy Jumprock
in the Broad River could be due to several factors. First, the fish were
collected from sections of river that span over 170 km, where average flows and
water temperatures vary considerably from the uppermost to the lowermost sampling
sites. Based on limited available data, mean annual water temperatures in
the uppermost portion of the river average roughly 17 ºC, while those in the lower
river, below Parr Shoals Reservoir, average roughly 19 ºC. Additionally, based on
average annual discharge, the river at the lowermost sample site is roughly 2.5
times the size of the river at our uppermost sample site. It is possible that growth
varied among sites, but limited samples from each site precluded meaningful
statistical comparisons. Second, we did not determine the sex of the fish we collected,
so we could not account for the possible influence of sex on the growth
rates of either species. Although there was no apparent difference in growth between
male and female Notchlip Redhorse in the Savannah River (Grabowski et
al. 2007), older female Silver Redhorse appeared to grow faster than males in the
Flint River, AL (Hackney et al. 1971), and other catostomids have been found to
have differential growth based on sex (Grabowski et al. 2007).
Growth of Notchlip Redhorse in the Broad River was slower than that reported
in the Savannah River (Grabowski et al. 2007). For example, an age-4 Notchlip
Redhorse in the Savannah River averaged 399 mm TL, compared to 336 mm in
the Broad River. Because Notchlip Redhorse from the Savannah River were aged
with scales, and scales typically underestimate the ages of older fish, the slower
456 Southeastern Naturalist Vol. 10, No. 3
growth could be explained by the choice of aging structure. However, for fish less
than age 5, scale ages typically have high agreement with otolith ages (e.g., Quist
et al. 2007); since fish less than age 5 in the Savannah River grew faster than
those in the Broad River, it is likely that growth differences for Notchlip Redhorse
between the two rivers were real, at least for younger fish. Length ranges of
Brassy Jumprock observed in the Broad River, SC were similar to those reported
from Lake Norman, NC (Jenkins and Burkhead 1994), the only other published
length information we found for Brassy Jumprock.
Mortality rates of Brassy Jumprock and Notchlip Redhorse in the Broad River
were very low. There was qualitative agreement between the catch-curve derived
estimates and estimates of natural mortality using the equation of Hoenig (1983).
The low mortality rates suggest there is very little exploitation of either species
in the Broad River, SC. Mortality estimates for Notchlip Redhorse in the Broad
River were much lower than in the Savannah River, where Z was between 0.51
and 0.85; however, those high mortality estimates may have resulted in part from
underestimating the age of older fish due to scale-estimated ages (Grabowski et
al. 2007). Mortality estimates for Black Redhorse (Z = 0.26) and Shorthead Redhorse
(Z = 0.24), other moderate-sized catostomids, in Ontario (Reid 2009) were
comparable to those we observed in the Broad River.
Populations of Notchlip Redhorse and Brassy Jumprock in the Broad River,
SC, appear to be secure and relatively stable, as evidenced by their high relative
abundance and long life spans. Notchlip Redhorse was able to overcome
the potentially detrimental effects of two consecutive poor year classes—aided,
perhaps, by the particularly strong year class that preceded them. Apparently,
both Notchlip Redhorse and Brassy Jumprock have been generally tolerant of
a wide spectrum of human activities that are known to adversely affect more
sensitive species. On the Broad River, these activities include dam construction
and operation, riparian agriculture and forestry, in-stream sand mining,
wastewater discharges, and creeping urbanization. The population characteristics
of Notchlip Redhorse and Brassy Jumprock presented in this study are
important tools for the development of management strategies in other locales
where these populations may be negatively impacted by high exploitation and/
or habitat degradation.
We thank South Carolina Department of Natural Resources staff, Drew Robb, Robert
Stroud, Richard Bassett, and Treye Byars for assisting in the collection of fish for
this study. Rick Slack at the Cheraw Sate Fish Hatchery maintained study fish in growout
ponds for OTC evaluation. Treye Byars was also responsible for sectioning and
aging fish otoliths. Funding for this project was provided by the Broad River Mitigation
Trust Fund, the members of which include Duke Energy, South Carolina Electric
and Gas, and Lockhart Power Company. The manuscript benefited greatly from the
constructive comments and suggestions of Robert E. Jenkins, Timothy B. Grabowski,
and one anonymous reviewer.
2011 J.M. Bettinger and J.S. Crane 457
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