Temporal Stability Patterns in Fish Species Richness,
Diversity, and Evenness in Otter Creek, Vigo County, IN
Thomas P. Simon, Charles C. Morris, and John O. Whitaker, Jr.
Northeastern Naturalist, Volume 21, Issue 2 (2014): 174–191
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T.P. Simon, C.C. Morris, and J.O. Whitaker, Jr.
22001144 NORTHEASTERN NATURALIST 2V1(o2l). :2117,4 N–1o9. 12
Temporal Stability Patterns in Fish Species Richness,
Diversity, and Evenness in Otter Creek, Vigo County, IN
Thomas P. Simon1,*, Charles C. Morris1, and John O. Whitaker, Jr.1
Abstract - We used abundance data from fish-population studies (1962–2010) on Otter
Creek at Markle’s Dam, Vigo County, IN, to examine temporal variation in stream-fish assemblages.
Species-richness variation showed a declining trend during the 50 year study
period with a mean of 49 ± 8.8 species per decade (range = 39–62 species). Cumulative
study species richness comprised 76 fish species with a mean of 21.3 ± 6.1 species collected
per sampling event. Dominant species, based on relative abundance during the 50 year
period, included Cyprinella spiloptera (Spotfin Shiner), Pimephales notatus (Bluntnose
Minnow), Hybognathus nuchalis (Mississippi Silvery Minnow), and Luxilus chrysocephalus
(Striped Shiner). Relative abundance of Spotfin Shiner showed an increasing trend
during the 50-year study period, whereas Bluntnose Minnow relative abundance showed
a decreasing trend. Cumulative frequency-distribution of species richness normalized by
decade showed no significant difference, with the exception of the 1970s, which showed a
steep decline in the number of species. Repeated-measures analysis of variance showed no
significant differences in species diversity (H') or evenness (Pielou’s J) over the 5-decade
study period. Eleven cool-water species including Chrosomus erythrogaster (Southern Redbelly
Dace), Perca flavescens (Yellow Perch), Catostomus commersonii (White Sucker),
and Ambloplites rupestris (Rock Bass), and lithophilic spawning species such as Nocomis
micropogon (River Chub) and Hybopsis amblops (Bigeye Chub) were extirpated during the
study period. Potential changes in sedimentation and thermal gradients may have contributed
to these observed extirpations.
Introduction
Spatially heterogeneous environments offer the potential for spatial segregation
of species and provide refugia from harsh physical environmental conditions
(Schlosser 1991). Temporal variation in the physical environment can influence
growth, survival, immigration, and emigration (Karr and Freemark 1985). Spatial
and temporal variation alter species richness indirectly by altering nutrients and
organic cycling, production, processes at lower trophic levels, resource and habitat
availability, and resource use (Fisher et al. 1982, Poff et al. 1997, Probst et al.
2008). Annual species-richness variation is lower in more-diverse stream assemblages
(Franssen et al. 2011).
Long-term studies (>30 years) of fish-assemblage structure are few; however,
regionally important data sets include large midwestern rivers and the Great Lakes,
such as the Illinois River (1957–), Wabash River (1966–), and Lake Michigan
(1972–) (Beugly and Pyron 2010, Brunnell et al. 2005, Gammon and Simon 2000,
1Department of Biology, 600 Chestnut Street, Science Building, Indiana State University,
Terre Haute, IN 47809. *Corresponding author - thomas.simon@indstate.edu.
Manuscript Editor: Glen Mittelhauser
Northeastern Naturalist Vol. 21, No. 2
T.P. Simon, C.C. Morris, and J.O. Whitaker, Jr.
2014
175
Koehl and Sparks 2002, Pegg and McClelland 2004, Probst et al. 2008). Trends
in stable physical environments show that neither species richness nor diversity
change temporally (Greenfield and Bart 2005). Physical environmental disturbances
within streams and rivers over the last 40 years include increased sedimentation
(Beugly and Pyron 2010), habitat fragmentation (Taylor et al. 2008), decline of current
velocities (Poff and Allan 1995, Poff et al. 1997), and nutrient-cycle increases
(Bunnell et al. 2005, Pegg and McClelland 2004).
The Otter Creek study, which began in the late 1870s, is one of a few continuous
long-term studies of fish assemblages in small streams, (Blatchley 1938, Gerking
1945, Jordan 1877). Surveys of the stream documented 63 species between 1885
and 1886 (Hay 1894, Jenkins 1887, Jordan 1890). Whitaker and Wallace (1973)
sampled 321 sites in Vigo County, including 60 sites in the Otter Creek watershed.
Forty-seven fish species (46.5% of the 101 species collected in the entire study)
were collected at Markle’s Dam, a site located on Otter Creek in Markle Mill Park.
This single site had the highest species richness recorded in the study. Whitaker
(1976) reported 57 species within the Otter Creek Markle’s Dam site (1962–1974)
based on his 12-year continuous seining study.
The concept of stream stochasticity, i.e., response to unpredictable environmental
change, is based on study of Otter Creek at Markle’s Dam (Grossman et al.
1982, 1985). Using data collected over 12 years at the site, Grossman et al. (1982)
conducted a trait analysis of the 10 most common fish species to rank species by
abundance and trophic group, and concluded that the fish assemblage at Otter Creek
at Markle’s Dam was determined by stochastic factors; however, these conclusions
were not unanimous (Herbold 1984, Rahel et al. 1984, Yant et al. 1984).
The current study evaluates temporal changes in species richness, species diversity,
and evenness at Markle’s Dam. Our objectives were to assess temporal patterns
and identify temporal shifts in fish assemblages over a 5-decade period. Temporal
shifts are particularly interesting given the lack of management manipulations at
the site, and our results provide some insight into fish-assemblage response over the
latter half of the 20th century.
Methods
Study area and design
Otter Creek is a third-order stream draining 326 km2 in Vigo, Clay, and Parke
counties in west-central Indiana (Hoggatt 1975). The mainstem of Otter Creek
originates near the town of Carbon and flows westward for 38.6 km before entering
the Wabash River 4 km North of Terre Haute (Weinman 2007). The Otter Creek
watershed is located entirely within the Interior River Lowland ecoregion, an area
that is characterized by undulating plains with wide, shallow valleys that were covered
by pre-Wisconsian glaciers (Melhorn 1997, Woods et al. 1998). The majority
of the land area in the Otter Creek watershed is used for agriculture (41.7%) or is
forested (41.4%); residential areas (7.9%) and grass and pastureland (7.6%) account
for much of the remaining area (Choi et al. 2005). The qualitative habitat evaluation
index (QHEI) for this stream reach ranges from 87–90 QHEI points with a
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T.P. Simon, C.C. Morris, and J.O. Whitaker, Jr.
2014 Vol. 21, No. 2
mean of 88.5 ± 0.89 based on 1990–2010 sample events. No habitat measures were
completed during the 1960–1989 time period because the QHEI index was not developed
until 1989 (Rankin 1989).
The Otter Creek Markle Dam reach averages 12.4 m wide and originates 150 m
downstream (39.529027oN, 87.346958oW) of the Mill Dam in Markle’s Mill Park
(39.527934o N, 87.345928oW), Otter Creek Township (Fig. 1). The Mill Dam is
Figure 1. Geographic
location of
the Markle Dam
reach on Otter
Creek, Vigo County,
IN. Bottom:
photograph of Mill
Dam in Markle’s
Mill Park.
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2014
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a national historic landmark originally constructed in 1817, rebuilt in 1938 after
burning, and reconstructed in 1984. Limited details of the reconstruction are available,
but the dam was dismantled during the mill reconstruction and then rebuilt to
the original specifications in 1984. We assume that sediment behind the dam was
released during dam removal and that upstream dam pool habitat transitioned into
free-flowing run habitat; however, we do not know how long this situation persisted.
The dam is a hydrologically stabilizing structure that acts as a sediment trap
and mitigates flow downstream and restricts fish passage.
We conducted sampling in Otter Creek at the same reach annually (n = 54) during
June–August from 1962 to 2010. We grouped data based on annual, 3-yr, 5-yr,
and 10-yr periods to evaluate patterns. Because some years had more effort, and
to statistically avoid bias of the results by differentially weighting those years that
had more effort, we selected 10-yr periods for presentation. Annual analysis increases
data resolution, but also increases beta error. We chose time periods for our
analysis to balance alpha against beta error; our choice is based on convenience and
normal statistical convention. We compiled data into 5 study periods—1962–1970,
1971–1980, 1981–1990, 1991–2000, and 2001–2010. We used a random sample (n
= 5) drawn from each decade to perform evaluations and make comparisons. We
used cumulative-frequency distribution to determine the number of samples based
on distribution of pooled data, to show accumulation of species with increasing
number of sample events. To ensure consistency, the same crew leader (J. Whitaker)
supervised sampling throughout the entire study period, 1962–2010. Crews
conducted sampling during stable flow periods with a minimum of 7 days between
events. Researchers avoided sampling immediately after storm events, instead
waiting until water clarity and flow rates returned to normal levels, based on the
average streamflow that occurred over 7 consecutive days and had a 10-year reoccurrence-
interval–period (i.e., 7Q10) discharge mean. We vouchered and deposited
fish specimens at the Indiana State University Zoology Collection, Department of
Biology, Terre Haute, IN.
Field survey methods
Each sampling event consisted of 3600 s of seining effort using a 4.5-m seine
and a 9-m seine with 6.25-mm standard mesh during daylight hours. We sampled in
an upstream direction within a 150-m reach (Whitaker 1976). The reach included
a single habitat cycle of riffle, run, and pool habitats. Sampling within the reach
included all available instream cover and substrate types. Seining crews included
groups of 5 or 6 students. We positioned each seine with a student on each brail.
Three to four crew members went upstream a distance equivalent to the width of the
seine and then kicked the substrate vigorously to dislodge individual fish by moving
in unison in a downstream direction towards the stationary seine. We placed all
fish collected into a live-well for later identification. We identified individual fish
to species, counted and batch-weighed them by species, and recorded minimum
and maximum length for each species. We made our identifications using regional
identification manuals (Gerking 1955, Simon 2011, Smith 1973, Trautman 1981).
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2014 Vol. 21, No. 2
Data analysis
We tested for significant differences between decade-long periods using Kruskal
Wallis ANOVA, α = 0.05, with a post hoc Tukey’s honest significant difference
(HSD) test (Zar 2009). Cumulative frequency distributions included an analysis of
decade-delimited fish-collection events in order to compare the number of sample
events that maximized the number of species. We standardized these data based
on a total of 5 sampling events so that equal numbers of samples were statistically
selected to avoid differential weighting of decades (Fig. 2).
We measured species α-diversity using the Shannon-Weiner (H') diversity based
on the formula,
R
H' = -Σpi ln pi ,
i = 1
where pi is the proportion of individuals belonging to the ith species (Shannon
1948). Evenness is a measure of the distribution of individuals over species (Pielou
1975). Pielou’s J is measured based on the formula
J = H' ,
(ln S)
where H' is the Shannon-Weiner diversity index and S is the number of species.
Figure 2. Standardized cumulative-frequency distribution of species richness from each of 5
decades of sampling at Markle’s Dam on Otter Creek, Vigo County, IN, limited to 5 random
observations (1960s = thick black line, 1970s = black dashed line, 1980s = thick gray line,
1990s = gray dashed line and 2000s = thin black line).
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2014
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Results
During our cumulative study-period sampling (n = 54 events) at the Otter Creek
Markle’s Dam site between 1962 and 2010, we collected and identified 203,742
individuals representing 76 species (Appendix 1). The species richness per sample
event averaged 21.3 ± 6.1 species (range = 9–33 species).
During the 1960s, numerically dominant species included Pimephales notatus
(Bluntnose Minnow), Luxilus chrysocephalus (Striped Shiner), and Cyprinella spiloptera
(Spotfin Shiner), which comprise 29%, 22%, and 13% of the total decade
relative-abundance, respectively. During this decade, we collected 9 species that
have not been collected since— Ichthyomyzon unicuspis (Silver Lamprey), Macrhybopsis
hyostoma (Shoal Chub), Luxilus cornutus (Common Shiner), Carpiodes
velifer (Highfin Carpsucker), Moxostoma macrolepidotum (Shorthead Redhorse),
Noturus eleutherus (Mountain Madtom), Pylodictis olivaris (Flathead Catfish),
Morone chrysops (White Bass), and Lepomis gulosus (Warmouth).
Collections during the 1970s were numerically dominated by Spotfin Shiner and
Hybognathus nuchalis (Mississippi Silvery Minnow) comprising 43% and 20%
of the total relative abundance for the decade, respectively (Appendix 1). Spotfin
Shiner dominance was consistent with the previous decade, while the Mississippi
Silvery Minnow increased an order of magnitude compared to the 2% relative abundance
it comprised during the 1960s. Bluntnose Minnow and Striped Shiner showed
a declining trend in the 1970s collections. We collected 7 species for the first time
during the 1971–1979 period: Lepisosteus platostomus (Shortnose Gar), Cyprinus
carpio (Common Carp), Erimyzon oblongus (Creek Chubsucker), Moxostoma
anisurum (Silver Redhorse), Ictiobus cyprinellus (Bigmouth Buffalo), Lepomis
microlophus (Redear Sunfish), and Perca flavescens (Yellow Perch). We failed to
collect 8 other native species after the 1970s including River Chub, Notropis boops
(Bigeye Shiner), Southern Redbelly Dace, Ameiurus melas (Black Bullhead), Lepomis
humilis (Orangespotted Sunfish), Etheostoma spectabile (Orangethroat Darter),
Creek Chubsucker, and Yellow Perch. These species are considered cool-water species
(Frimpong and Angermeier 2009).
Numerically dominant species from 1980 to 1989 included Spotfin Shiner and
Gizzard Shad, which comprised 67% and 15% of the total decade relative abundance,
respectively. The numerical dominance of Gizzard Shad contrasts with its
relative abundance in the 1960s (less than 1%) and 1970s (7%). We collected two species,
Amia calva (Bowfin) and Rhinichthys obtusus (Western Blacknose Dace), for the
first time during 1980–1989, but did not collect them in subsequent decades. We
collected White Sucker, River Carpsucker, and Rock Bass for the last time during
the 1980s (Appendix 1).
Spotfin Shiner and Gizzard Shad were numerically dominant during 1990–1999,
comprising 54% and 16% of the total decade catch, respectively (Appendix 1). We
collected Bigeye Chub and Ameiurus natalis (Yellow Bullhead) for the first time
during 1990–1999; during this period, Notropis volucellus (Mimic Shiner), Ictiobus
niger (Black Buffalo), and Percina sciera (Dusky Darter) returned for the first time
since the 1960s.
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2014 Vol. 21, No. 2
During 2001–2010, Spotfin Shiner dominated collections with Notropis atherinoides
(Emerald Shiner), which comprised the second most abundant species. We
collected Gambusia affinis (Western Mosquitofish), an invasive species, Cyprinella
whipplei (Steelcolor Shiner), and Cottus bairdii (Mottled Sculpin) for the first time
during the 2000s. Pimephales vigilax (Bullhead Minnow) returned for the first time
since the 1960s.
We used our decade-long datasets to compare number of species and number of
individuals in each collection and their means and standard deviations. Sampling
events from 1962 to 1970 (n = 23) resulted in a total of 173,349 individuals representing
62 fish species (Appendix 1). Species richness per sample event averaged
21 ± 5 species (range = 9–33 species). During 1971–1980 we collected a total of
10,750 individuals (n = 10 sample events; Appendix 1) representing 53 species with
an average species richness of 25 ± 2 species (range = 22–29 species) collected
during each sampling event. Sampling events from 1981 to 1990 resulted in 14,301
individuals (n = 10 sample events) representing 46 species with an average species
richness of 22 ± 4 species collected per event (range - 17–32 species; Appendix 1).
During 1991–1999 we collected a total of 2947 individuals (n = 6 sampling events;
Appendix 1) representing 45 species with an average species richness of 18 ± 2
species collected per event (range = 16–21). Sampling events from 2001 to 2010
included 2395 individuals (n = 5 sampling events; Appendix 1). We collected a total
of 39 species with an average species richness of 18 ± 4 species collected per event
(range = 14–24 species).
Species richness adjusted for sampling effort by decade (n = 5 sampling events)
declined over the five decades of sampling at Markle’s Dam by an average of 5.75
± 2.99 species per decade (Fig. 3). We observed the maximum net loss during the
1970s (net loss = 9 species), and the smallest species net loss was during the 1990s
(net loss = 2 species). We found a significant difference (ANOVA, F = 3.47, P =
0.014) in average number of species collected within year by decade during the
1970s (Tukey HSD = 0.021; Table 1). No other decade showed a significant difference
in species richness, H', or J (Table 1).
Table 1. Repeated-measures ANOVA with Tukey HSD post hoc test for Shannon-Weiner (H') species
diversity and Pielou’s (J) Evenness based on decade temporal change for Otter Creek at Markle’s Dam,
Vigo County, IN for 1962 to 2010 (P-values at α = 0.05).
H' Evenness
Decade 1960s 1970s 1980s 1990s 2000s 1960s 1970s 1980s 1990s 2000s
1960s
1970s 0.9999 0.9994
1980s 0.1277 0.0826 0.1277 0.0826
1990s 0.1504 0.0983 0.9999 0.1054 0.0983 0.9999
2000s 0.1177 0.0758 0.9999 0.9999 0.1177 0.0758 0.9999 0.9999
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Discussion
The structural organization of fish-assemblage response is strongly linked
to local habitat variation (Hoeinghaus et al. 2006), which is influenced by hydrologic
regime (Poff et al. 1997). Changes in hydrologic-variation patterns are
responsible for fish-assemblage structure by introducing variation in disturbance
regimes (Poff and Allan 1995). Hydrologically stable sites support specialist species,
while hydrologically variable sites support generalist species (Poff and Allan
1995). Hydrologic alterations result in changes in relative abundance. The Otter
Creek reach at Markle’s Dam is hydrologically stable as a result of the Mill Dam,
Figure 3. Boxand
whiskerp
l o t s b a s e d
on normalized
effort (n = 5
samples) showing
temporal
changes in Otter
Creek at Markle’s
Dam, Vigo
County, IN. A.
Shannon-Weiner
(H') diversity
index, and B.
Pielou’s J evenness.
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2014 Vol. 21, No. 2
and the heterogeneous reach-specific habitat features increase niche complexity
and, with a QHEI of 88.5 ± 0.89, this reach has one of the highest habitat scores in
southwestern Indiana (T.P. Simon, unpubl data). It is possible that this habitat heterogeneity
may have been compromised during the dam reconstruction and events
leading up to this repair.
Our analysis of 50 years of data from 1962–2010 collections resulted in a cumulative
76 fish species collected from this single site (Appendix 1). Otter Creek
at Markle’s Dam species richness represents 75% of the fish fauna known to occur
in Vigo County (Whitaker and Wallace 1973) and 38% of the entire fish fauna of
Indiana (Simon 2011). The mean species richness within decade by sampling event
did not vary significantly (Fig. 2), and normalized effort shows no significant difference
in decade cumulative-frequency distribution. The 1960s data is represented by
a sigmoidal curve in contrast to the much flatter curves from subsequent decades. In
order to detect a decrease in species relative abundance during the 50 years of sampling,
we would have to have sampled more frequently to collect the same number
of species through time.
Our sampling design did not account for seasonality of fish assemblages at this
site; some of the species presented in Appendix 1 may be transient and may have
been present at the Markle’s Dam location only occasionally for reproduction or
refuge and likely would not be collected every event. For example, Dorosoma
cepedianum (Gizzard Shad) is a schooling species that can be patchily distributed
(Simon 2011). This species was among the most dominant by relative abundance
from 1980 to 1999 (Appendix 1).
Based on dominant species, loss of native species, and new species occurrences,
Markle’s Dam species composition showed a general trend toward declining native
species and fewer new native species.
Stream fish-assemblage structure and its relation to patterns associated with
natural variability need to be understood in order to manage abiotic and biotic conditions
in watersheds. Herbold (1984) analyzed Whitaker’s (1976) data and showed
similarity in community composition between years; the pool-dwellers, which are
composed of bottom-feeding species, showed similarity within years but little similarity
between years. Yant et al. (1984) stated that the study site, sampling method,
and within-year replications used by Grossman et al. (1982) emphasized season,
and their data-analysis methods resulted in more variability than equally plausible
alternate choices for those factors. Reanalysis of the data by Yant et al. (1984)
concluded that there was actually very little variation in the fish community at this
location over the course of 12 years. Gorman (1986) proposed that the presence of
Markle’s Dam resulted in more variability in the assemblage compositio n.
Changes in species composition over the 5-decade study period show that fish
assemblages remained diverse based on measures of species diversity and evenness
(Fig. 3); however, species richness and composition of the assemblage were dynamic
with decreasing trends over time (Fig. 2). Diversity indices, such as Shannon-
Weiner and Pielou’s J, should be regarded as a summary of α-diversity, which is the
diversity within a uniform habitat (Whittaker 1972). Both of these measures should
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T.P. Simon, C.C. Morris, and J.O. Whitaker, Jr.
2014
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be considered structural aspects of the assemblage. Spotfin Shiner was among the
dominant 3 species during all 5 decade-long periods, but exhibited the highest relative
abundance during the period from 1970 to 2010.
Many long-term data sets do not include abiotic information for covariate analysis;
however, using data from Frimpong and Angermeier (2009), we completed a
trait analysis based on temperature and habitat factors such as sedimentation. Eleven
species were extirpated during the study period. These species represent cool-water
species like Southern Redbelly Dace, Yellow Perch, White Sucker, and Rock Bass,
and lithophilic spawning species such as River chub and Bigeye Chub (Appendix 1;
Frimpong and Angermeier 2009). Community shifts possibly linked to sedimentation
and thermal gradients may have contributed to these observed changes. Our hypothesis
is that during the reconstruction of the dam in 1984, sediment that accumulated
behind the dam was released downstream. In addition, the river probably returned to
shallow, unrestricted flow regimes resulting in warmer water in the reach while the
dam was being rebuilt. Substrates downstream may have been blanketed with fine
sediments during the removal of the dam. After fish thermally classified as cool-water
species were eliminated from the reach and lithophilic spawning minnow species
were impacted by the elimination of downstream coarse substrates, neither guild
could return. We do not believe that density-dependent predator-prey biotic interactions
or other biotic factors directly contributed to changes at Markle Dam because
predator numbers declined during this study period.
It is important to recognize that factors other than sedimentation and water
temperature might explain changes in species over the 50-year study period. As is
common in long-term studies that lack information, precise determination of cause
and effect is not possible; however, trait analysis may provide some hypotheses for
species change that require further evaluation (Frimpong and Angermeier 2009).
Indirect effects altering nutrients and organic cycling, production, processes at
lower trophic levels from both top-down predator and bottom-up cascading trophic
level changes, resource and habitat availability during the reconstruction of the Mill
dam, and resource use by dominant species might be equally plausible explanations
that either separately or cumulatively may explain patterns.
Acknowledgments
Special thanks to Indiana State University students in the Vertebrate Zoology classes that
assisted in field collection over the years. We especially thank D. Sparks, D.C. Wallace, and
R. Benda for field assistance during the past 20 years. Chris Winslow and an anonymous
reviewer provided constructive comments. Paul D. McMurray provided assistance organizing
an early draft of this manuscript.
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Appendix 1. Species composition, including minimum and maximum relative abundance and percent relative abundance, over 50 years (1960–2010)
segregated into five distinct decade periods for Otter Creek at Markle’s Dam, Vigo County, IN. Number after year is the number of sample events for each
decade period.
Number of Individuals by Species
1960s (n = 23) 1970s (n = 10) 1980s (n = 10) 1990s (n = 6) 2000s (n = 5)
Scientific name/ common name min max %rel min max %rel min max %rel min max %rel min max %rel
Ichthyomyzon unicuspis Hubbs and Trautman 1 1
Silver Lamprey
Lepisosteus platostomus Rafinesque 1 1 15 15 3 3
Shortnose Gar
Amia calva L. 1 1
Bowfin
Dorosoma cepedianum (Lesueur) 1 15 6 300 7% 1 1000 15% 10 200 16% 1 1
Gizzard Shad
Esox americanus vermiculatus Gmelin 1 1 1 4 1 2 1 1
Grass Pickerel
Campostoma anomalum (Rafinesque) 1 570 8% 2 35 1% 1 35 1% 1 100 6% 1 15 1%
Central Stoneroller
Chrosomus erythrogaster (Rafinesque) 1 1 2 2
Southern Redbelly Dace
Cyprinella spiloptera (Cope) 1 576 13% 40 3000 43% 150 3000 67% 30 500 54% 87 500 56%
Spotfin Shiner
Cyprinella whipplei Girard 4 4
Steelcolor Shiner
Cyprinus carpio L. 1 1 1 2 5 5
Common Carp
Hybognathus nuchalis Agassiz 1 70 2% 1 1000 20% 2 350 3% 1 100 4% 2 100 5%
Mississippi Silvery Minnow
Hybopsis amblops (Rafinesque) 1 1
Bigeye Chub
Luxilus chrysocephalus Rafinesque 1 9 1 50 1% 1 50 1% 2 2 1 7
Striped Shiner
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Number of Individuals by Species
1960s (n = 23) 1970s (n = 10) 1980s (n = 10) 1990s (n = 6) 2000s (n = 5)
Scientific name/ common name min max %rel min max %rel min max %rel min max %rel min max %rel
Luxilus cornutus (Mitchill) 3 1693 22%
Common Shiner
Lythrurus umbratilis (Girard) 2 55 2% 1 200 3% 1 15 5 5 1 20 1%
Redfin Shiner
Macrhybopsis storeriana (Kirtland) 16 16 3 3 2 2
Silver Chub
Macrhybopsis hyostoma (Gilbert) 20 20
Shoal Chub
Nocomis micropogon (Cope) 2 4 1 1
River Chub
Notemigonus crysoleucas (Mitchill) 1 5 1 12 7 8 3 3
Golden Shiner
Notropis atherinoides Rafinesque 1 253 7% 1 200 3% 1 100 2% 10 10 8 132 12%
Emerald Shiner
Notropis blennius (Girard) 1 11 3 6 4 4
River Shiner
Notropis boops Gilbert 1 1 2 2
Bigeye Shiner
Notropis buccatus (Cope) 1 87 3% 1 80 2% 1 15 1 25 1% 1 40 5%
Silverjaw Minnow
Notropis rubellus (Agassiz) 1 8 1 4 1 4 1 14 1%
Rosyface Shiner
Notropis stramineus (Cope) 1 34 1% 1 25 1% 1 6 15 15 1% 3 50 2%
Sand Shiner
Notropis volucellus (Cope) 1 3 2 2 1 1
Mimic Shiner
Phenacobius mirabilis (Girard) 1 190 2% 1 15 1 10 1 8 1%
Suckermouth Minnow
Pimephales notatus (Rafinesque) 7 3317 29% 1 250 6% 3 150 2% 3 100 5% 3 20 2%
Bluntnose Minnow
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Number of Individuals by Species
1960s (n = 23) 1970s (n = 10) 1980s (n = 10) 1990s (n = 6) 2000s (n = 5)
Scientific name/ common name min max %rel min max %rel min max %rel min max %rel min max %rel
Pimephales vigilax (Baird and Girard) 9 9 1 1
Bullhead Minnow
Rhinichthys obtusus Agassiz 1 1
Western Blacknose Dace
Semotilus atromaculatus (Mitchill) 2 43 2% 2 15 3 5 10 10 1 15 1%
Creek Chub
Catostomus commersonii (Lacepède) 1 2 1 20 1 2
White Sucker
Carpiodes cyprinus (Lesueur) 2 3 1 1 12 12 2 11 1%
Quillback
Carpiodes carpio (Rafinesque) 19 19 1 2
River Carpsucker
Carpiodes velifer (Rafinesque) 20 20
Highfin Carpsucker
Erimyzon oblongus (Mitchill) 1 1
Creek Chubsucker
Hypentilium nigricans (Lesueur) 1 60 1% 3 40 2% 3 25 1% 1 5 1% 1 4
Northern Hogsucker
Ictiobus cyprinellus (Valenciennes in Cuvier 1 1 1 5 1 2
and Valenciennes) Bigmouth Buffalo
Ictiobus niger (Rafinesque) 1 1 10 10
Black Buffalo
Minytrema melanops (Rafinesque) 1 1 1 1 2 2
Spotted Sucker
Moxostoma anisurum (Rafinesque) 1 1 1 4 3 3 2 7
Silver Redhorse
Moxostoma duquesnii (Lesueur) 1 1 1 1 1 1 2 2
Black Redhorse
Moxostoma erythrurum (Rafinesque) 1 12 1 20 1% 1 50 1% 1 5 1 2
Golden Redhorse
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Number of Individuals by Species
1960s (n = 23) 1970s (n = 10) 1980s (n = 10) 1990s (n = 6) 2000s (n = 5)
Scientific name/ common name min max %rel min max %rel min max %rel min max %rel min max %rel
Moxostoma macrolepidotum (Lesueur) 9 9
Shorthead Redhorse
Ameiurus melas (Rafinesque) 1 1 1 2
Black Bullhead
Ameiurus natalis (Lesueur) 4 4
Yellow Bullhead
Ictalurus punctatus (Rafinesque) 5 5 1 4 1 1
Channel Catfish
Noturus eleutherus Jordan 1 1
Mountain Madtom
Noturus miurus Jordan 1 16 1 100 3% 1 2 1 10 1 8
Brindled Madtom
Pylodictis olivaris (Rafinesque) 3 3
Flathead Catfish
Fundulus notatus (Rafinesque) 1 15 2 4 1 4 1 10
Blackstripe Topminnow
Gambusia affinis (Baird and Girard) 1 4
Western Mosquitofish
Labidesthes sicculus (Cope) 2 5 2 9 2 100 2% 1 100 4% 5 117 6%
Brook Silverside
Cottus bairdii Girard 2 2
Mottled Sculpin
Morone chrysops (Rafinesque) 6 6
White Bass
Ambloplites rupestris (Rafinesque) 1 1 1 1 1 1
Rock Bass
Lepomis cyanellus Rafinesque 1 20 1 1 1 1
Green Sunfish
Lepomis gulosus (Cuvier in Cuvier and 1 1
Valenciennes) Warmouth
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Number of Individuals by Species
1960s (n = 23) 1970s (n = 10) 1980s (n = 10) 1990s (n = 6) 2000s (n = 5)
Scientific name/ common name min max %rel min max %rel min max %rel min max %rel min max %rel
Lepomis humilis (Girard) 1 2 1 1
Orangespotted Sunfish
Lepomis macrochirus Rafinesque 1 25 1% 2 10 1 75 1% 1 10 1% 1 15 1%
Bluegill
Lepomis megalotis (Rafinesque) 1 5 3 3 1 3 1 1 1 1
Longear Sunfish
Lepomis microlophus (Günther) 1 5 1 2 3 8 1 1
Redear Sunfish
Micropterus dolomieu Lacepède 1 2 1 3 1 6 5 5 1 1
Smallmouth Bass
Micropterus punctulatus (Rafinesque) 1 1 1 2 3 4 2 4 1 1
Spotted Bass
Micropterus salmoides (Lacepède) 1 3 1 6 1 10 1 1 1 1
Largemouth Bass
Pomoxis annularis Rafinesque 20 20 8 8 1 8 1 2
White Crappie
Pomoxis nigromaculatus (Lesueur in Cuvier 1 1 1 3 2 10 1 5 1 2
and Valenciennes) Black Crappie
Etheostoma spectabile (Agassiz) 1 22 2 2 1 1
Orangethroat Darter
Etheostoma blennioides Rafinesque 1 50 2% 6 50 2% 1 40 1% 1 15 1% 4 26 2%
Greenside Darter
Etheostoma caeruleum Storer 1 50 2% 3 20 1% 3 20 4 20 1% 6 18 1%
Rainbow Darter
Etheostoma flabellare Rafinesque 1 19 1 10 1 2 2 10 5 5
Fantail Darter
Etheostoma nigrum Rafinesque 1 40 1% 1 75 2% 1 15 4 10 1 4
Johnny Darter
Perca flavescens (Mitchill) 1 1
Yellow Perch
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Number of Individuals by Species
1960s (n = 23) 1970s (n = 10) 1980s (n = 10) 1990s (n = 6) 2000s (n = 5)
Scientific name/ common name min max %rel min max %rel min max %rel min max %rel min max %rel
Percina caprodes (Rafinesque) 6 6 1 1 1 1 1 4
Logperch
Percina maculata (Girard) 1 5 1 25 1 3 1 3
Blackside Darter
Percina sciera (Swain) 10 10 1 1
Dusky Darter