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This article was downloaded by: [Central Michigan University]On: 14 November 2014, At: 08:37Publisher: Taylor & FrancisInforma Ltd Registered in England and Wales Registered Number: 1072954 Registeredoffice: Mortimer House, 37-41 Mortimer Street, London W1T 3JH, UK
North American Journal of FisheriesManagementPublication details, including instructions for authors andsubscription information:http://www.tandfonline.com/loi/ujfm20
Comparison of White Sucker AgeEstimates from Scales, Pectoral FinRays, and OtolithsRyan M. Sylvester a & Charles R. Berry Jr. ba South Dakota State University, Department of Wildlife andFisheries Sciences , Brookings, South Dakota, 57007, USAb South Dakota Cooperative Fish and Wildlife Research Unit, U.S.Geological Survey, South Dakota State University, Department ofWildlife and Fisheries Sciences , Brookings, South Dakota, 57007,USAPublished online: 08 Jan 2011.
To cite this article: Ryan M. Sylvester & Charles R. Berry Jr. (2006) Comparison of White SuckerAge Estimates from Scales, Pectoral Fin Rays, and Otoliths, North American Journal of FisheriesManagement, 26:1, 24-31, DOI: 10.1577/M04-147.1
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Comparison of White Sucker Age Estimates from Scales,Pectoral Fin Rays, and Otoliths
RYAN M. SYLVESTER*South Dakota State University, Department of Wildlife and Fisheries Sciences,
Brookings, South Dakota 57007, USA
CHARLES R. BERRY, JR.South Dakota Cooperative Fish and Wildlife Research Unit, U.S. Geological Survey, South Dakota State
University, Department of Wildlife and Fisheries Sciences, Brookings, South Dakota 57007, USA
Abstract.—The ages of 229 white suckers Catostomus
commersonii from six drainages in the upper Missouri River
basin were estimated from scales, pectoral fin ray sections,
and lapilli otolith sections to evaluate the potential bias of age
estimates between structures. Age estimates were compared
by calculating the coefficient of variation, average percent
error, percent agreement, and percent agreement within 1 year,
as well as by constructing age bias plots. Overall, the relative
precision of age estimates from pectoral fin rays and otoliths
was higher than that of age estimates from scales and otoliths,
but neither pair differed in precision from scales and fin rays.
The relative precision of age estimates between pairs of
structures was variable both within and among drainages, and
few trends could be detected. The percent agreement between
structures ranged from 50.0% to 93.8% among drainages, but
9 of 18 pairs had agreement rates greater than 70.0%. Percent
agreement within 1 year was greater than 85.0% for all pairs
of structures in all drainages. Age estimates from scales
underestimated the age estimates from pectoral fin rays and
otoliths beyond age 3, while pectoral fin rays only slightly
underestimated ages from otoliths of fish older than age 6. We
recommend sectioned lapilli otoliths for estimating the age of
white suckers, especially if mature individuals are present in
the population and lethal collection techniques are allowed.
Pectoral fin ray sections are the best nonlethal structure for
estimating the age of white suckers but may underestimate the
ages of fish older than 5 years. Scales remain suitable for
estimating the ages of immature fish, but their use is not
recommended for mature fish. This information will allow
fisheries managers and researchers to select the most
appropriate structure for use in future age assessment studies
of white suckers and other catostomid species.
Estimating the age of fish is a common technique
used to understand fish longevity and the growth and
mortality rates of fish populations; however, obtaining
accurate age information is crucial to an accurate
understanding of these metrics (Campana 2001). Many
structures have been used to estimate age of fishes,
including scales, various fin rays, fin spines, vertebrae,
cleithra, opercles, and otoliths. Otoliths have several
advantages over scales and spines for estimating age
because otoliths are not subject to resorption and their
growth is acellular rather than by ossification (Secor et
al. 1995). Higher precision of age estimates from
otoliths has led several authors to recommended
otoliths over other structures for estimating age
(Boxrucker 1986; Sharp and Bernard 1988; Hoxmeier
et al. 2001). However, higher precision of age
estimates provides no insight into the biases or
accuracy of age estimates among or between structures.
Age-estimating structures such as otoliths, scales,
opercles, and pectoral fin rays have been validated in
many species, including the river redhorse Moxostomacarinatum, rainbow trout Oncorhynchus mykiss, andcommon carp Cyprinus carpio (Hutson 1999; Hining etal. 2000; Brown et al. 2004). Many of these validation
studies found that otoliths were accurate for age
estimation, but validation studies are still needed for
many species (Beamish and McFarlane 1983). Com-
parison of age estimates between structures is an
alterative technique to validation that may provide
useful information on the accuracy and bias of age-
estimating structures. Comparisons of age estimates
from various structures have been performed for many
species, including yellow perch Perca flavescens(Niewinski and Ferreri 1999), river carpsuckers
Carpiodes carpio (Braaten et al. 1999), and white
suckers Catostomus commersonii (Scidmore and Glass
1953; Ovchynnyk 1969; Quinn and Ross 1982).
Early age estimation studies of white suckers relied
on scales (Spoor 1938; Geen et al. 1966), but later
studies evaluated vertebrae, cleithra, opercles, and
pectoral fin ray sections (Scidmore and Glass 1953;
Beamish and Harvey 1969; Ovchynnyk 1969; Beamish
1973). Many of these studies agreed that scales did not
provide accurate age estimates for mature fish, and
some authors recommended the use of pectoral fin ray
sections to estimate age. Despite such recommenda-
tions, Quinn and Ross (1982) questioned the reliability
* Corresponding author: [email protected]
Received August 31, 2004; accepted July 28, 2005Published online December 19, 2005
24
North American Journal of Fisheries Management 26:24–31, 2006� Copyright by the American Fisheries Society 2006DOI: 10.1577/M04-147.1
[Management Brief]
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of age estimates from pectoral fin rays in fish older
than 7 years because of the lack of annulus formation
and the difficulty in interpreting fin ray sections.
Comparisons of white sucker age estimates from scales
and pectoral fin ray sections are common (Scidmore
and Glass 1953; Beamish and Harvey 1969; Beamish
1973; Barton 1980; Quinn and Ross 1982), but other
comparisons are rare. Ovchynnyk (1969) evaluated 20
structures for estimating age of white suckers and
found fewer annuli on scales than on other structures;
however, otoliths were not used in that study. Bond
(1972) compared white sucker age estimates from
scales and otoliths, saw general agreement between age
estimates, and proposed that scales were accurate up to
age 9. Otoliths (lapilli) were later determined to be
a reliable age-estimating structure for white suckers
(Thompson and Beckman 1995).
To date, no published studies have compared white
sucker age estimates from scales, pectoral fin ray
sections, and sectioned otoliths. Our objectives were
(1) to compare age estimates between three pairs of
age-estimating structures (i.e., scales versus pectoral
fin rays, scales versus otoliths, and pectoral fin rays
versus otoliths) and (2) to quantify potential biases
between pairs of age-estimating structures for white
suckers sampled in the upper Missouri River basin.
We considered age estimates from otoliths to be
accurate, because Thompson and Beckman (1995)
previously validated otoliths as a reliable estimator of
age for 2–18-year-old white suckers from Lake
Taneycomo, a coldwater reservoir in southwestern
Missouri.
Methods
White suckers were collected in August 2002 and
June and July 2003 from six drainages in the upper
Missouri River basin. Drainages included the Nowood
River drainage in north-central Wyoming; the Beaver
Creek drainage in south-central North Dakota; the Elm
River drainage on the border between North Dakota
and South Dakota; the Rock Creek and Frenchman
River drainages, located in southwestern Saskatche-
wan, Canada, and north-central Montana; and the
Sweet Grass River drainage, located in southwestern
Montana (Figure 1). Fish were collected by electro-
fishing with Smith-Root model 15-B and LR-24
backpack units (Smith-Root, Inc., Vancouver, Wash-
ington) and by seining (4.6- or 9.2-m length; 1.2-m
height; 4.88-mm mesh). The total length (mm) and
weight (g) of each fish were measured to the nearest
unit in the field. Scales (N ¼ 10–20 per fish) were
collected in the field below the dorsal fin and above the
lateral line on the left side of the fish (Beamish 1973).
The left pectoral fin was excised as close to the body as
possible (Quinn and Ross 1982). The scales and
a pectoral fin were placed in a scale envelope to dry
before further preparation. Each fish was preserved in
70% ethanol for later collection of lapilli and sagittal
otoliths.
Scales were cleaned if necessary and pressed onto
acetate slides (0.3 mm) by use of an Ann Arbor roller
press. Scales were then projected on a microfiche
projector at 103 magnification or were viewed under
a compoundmicroscope at 1003magnification by use of
transmitted light. Scale annuli were distinguished as
areas of crowding or crossing over of circuli (Spoor
1938). Regenerated scales were not used to estimate age.
Whole or proximal portions of pectoral fin rays were
set in epoxy and sectioned (0.5–0.7 mm) on the
transverse plane using an Isomet slow-speed saw
(Buehler, Lake Bluff, Illinois). Fin ray sections were
wet or dry sanded with 600-grit sandpaper if necessary.
Fin ray sections were viewed with transmitted light on
a compound microscope at 1003 magnification or
a dissecting microscope at 10–633 magnification
(Scidmore and Glass 1953). We used transmitted light
to distinguish pectoral fin ray annuli as light bands on
a dark background (Cuerrier 1951; Ovchynnyk 1969;
Beamish 1973).
FIGURE 1.—Locations of the six drainages in the upper
Missouri River basin where white suckers were collected in
August 2002 and June and July 2003 for comparisons between
age-estimating structures.
MANAGEMENT BRIEF 25
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Lapilli otoliths were collected, cleaned, allowed to
dry, set in epoxy, and sectioned (0.5–0.7 mm) on the
transverse plane through the focus using an Isomet
slow-speed saw (Secor et al. 1992; Thompson and
Beckman 1995). Otolith sections were wet sanded with
600-grit sandpaper if necessary. Sections were then
viewed under a dissecting microscope with a fiber optic
light source and a black background at 10–633
magnification. Annuli were identified as transparent
bands adjacent to opaque bands, and age was estimated
as the number of opaque bands. Sagittal otoliths were
used as backups if poor sections of both lapilli otoliths
occurred. Sagittal otoliths were prepared, sectioned,
and viewed by the same methods as used for lapilli
otoliths.
Fish were selected from across the entire range of
collected fish within each of the six drainages. Three
ages for each fish (N ¼ 229) were estimated (scale,
pectoral fin ray, otolith) by one experienced reader.
The relative precision between ages estimated from
scales, pectoral fin rays, and otoliths for each fish was
quantified as the average percent error (APE; Beamish
and Fournier 1981) and coefficient of variation (CV;
Chang 1982) between structures, as calculated by the
following formulas:
APE ¼ ½ð1=RÞ3XR
i
ðjXij � Xjj=XjÞ�3 100
CV ¼ ðSD=XjÞ3 100 ;
where R¼ the number of times each fish was aged; Xj¼
the average age calculated for the jth fish; and Xij¼ the
ith age determination of the jth fish. Percent agreement
was calculated as the percentage of estimated ages that
agreed between each pair of structures. The overall CV
between age estimates from scales, fin rays, and
otoliths was calculated for each age-class and structure
to assess which age-classes were responsible for most
of the variation in age estimates. Percent agreement
within 1 year was calculated as the percentage of
FIGURE 2.—Length frequency distributions of white suckers
collected from six drainages in the upper Missouri River basin
in 2002 and 2003.
FIGURE 3.—Length frequency distributions of white suckers
for which ages were estimated from scales, pectoral fin ray
sections, and sectioned lapilli otoliths. Fish were collected
from six drainages in the upper Missouri River basin in 2002
and 2003.
26 SYLVESTER AND BERRY
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estimated ages that were within 1 year of each other.
The mean CV and APE values with 95% confidence
intervals were used to compare precision between pairs
of structures in each of the six drainages and for the
combined samples.
Age bias plots (Campana et al. 1995) were
constructed to quantify the bias between age-estimating
structures. Linear regression was fitted to the observed
data of the mean estimated age of one structure versus
the age of another structure. The slope and intercept of
the observed regression line were compared to the
slope and intercept of a theoretical 1:1 line (indicating
complete agreement between structures) by use of
analysis of covariance (ANCOVA). The hypotheses
tested were that (1) the slope was equal to 1.0 and (2)
the intercept was equal to zero. Rejection of either or
both hypotheses (P � 0.05) was interpreted as bias
between structures. A slope that was not equal to 1.0 or
an intercept that was not equal to zero provided
evidence for age estimate bias between structures.
Types of potential bias include reader bias, systematic
bias (i.e., not recognizing the first annulus in fin rays,
causing age estimates to be low by 1 year), true bias
between structures, or a combination of all three types
of bias. We considered ages estimated from otoliths to
be accurate based on the validation of otolith age
estimates by Thompson and Beckman (1995); howev-
er, no known-age fish were used in this study.
Results
Ages were estimated for 229 white suckers across
the entire length range of fish collected in each of the
six drainages (Figures 2, 3). Most white sucker
populations were dominated by shorter length-groups
(,25 cm), but longer groups (.30 cm) were collected
in the Nowood River, Rock Creek, and Frenchman
River drainages. Most fish were less than 6 years of age
based on scales, but fish older than 6 years were
present based on sections of pectoral fin rays and
sectioned otoliths (Table 1). Age differentials for pairs
of structures generally increased with age; the
maximum estimated age difference was 5 years
between a scale and otolith and 3 years between
a pectoral fin ray and otolith (Table 1; Figure 4).
Overall, the relative precision (i.e., CV and APE) of
ages estimated from pectoral fin ray sections and
sectioned otoliths was higher than the precision of ages
estimated from scales and otoliths; neither pair differed
from scales and pectoral fin rays in terms of precision
(Table 2). The relative precision of age estimates
among pairs of structures was not different within each
of the six drainages, but the relative precision of age
estimates between scales and pectoral fin rays was
different among several drainages (Table 2). Pectoral
fin ray and otolith age estimates had the highest percent
agreement (78.6%) for the combined sample and had
the highest percent agreement within 1 year (97.8%).
Percent agreement between structures ranged from
50.0% to 93.8% among drainages, but the percent
agreement for 9 of the 18 pair–drainage combinations
was greater than 70.0% (Table 2). Percent agreement
within 1 year between structures was greater than
85.0% in all six drainages; agreement within 1 year
TABLE 1.—Age frequency of white suckers collected from six drainages throughout the upper Missouri River basin in 2002
and 2003 and subjected to age estimation based on scales, pectoral fin rays, and lapilli otoliths.
Age
Drainage Fish N Structure 0 1 2 3 4 5 6 7 8 9 10 11
Overall 229 Scale 28 64 59 50 14 11 3 0 0 0 0 0Pectoral 26 59 60 43 18 11 8 1 1 2 0 0Otolith 21 72 58 41 13 12 5 2 3 1 0 1
Nowood River 56 Scale 7 22 11 4 6 5 1 0 0 0 0 0Pectoral 7 21 11 3 5 4 3 0 0 2 0 0Otolith 6 22 11 5 1 6 2 0 1 1 0 1
Beaver Creek 16 Scale 2 0 5 7 2 0 0 0 0 0 0 0Pectoral 2 0 5 6 3 0 0 0 0 0 0 0Otolith 2 2 5 6 1 0 0 0 0 0 0 0
Elm River 16 Scale 8 1 3 4 0 0 0 0 0 0 0 0Pectoral 8 1 4 3 0 0 0 0 0 0 0 0Otolith 8 3 5 0 0 0 0 0 0 0 0 0
Rock Creek 54 Scale 6 11 18 15 1 2 1 0 0 0 0 0Pectoral 2 10 21 15 1 3 2 0 0 0 0 0Otolith 0 13 21 14 2 2 2 0 0 0 0 0
Frenchman River 57 Scale 3 14 14 17 5 3 1 0 0 0 0 0Pectoral 3 11 12 14 8 4 3 1 1 0 0 0Otolith 1 12 13 14 8 4 1 2 2 0 0 0
Sweet Grass River 30 Scale 2 16 8 3 0 1 0 0 0 0 0 0Pectoral 4 16 7 2 1 0 0 0 0 0 0 0Otolith 4 20 3 2 1 0 0 0 0 0 0 0
MANAGEMENT BRIEF 27
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exceeded 90.0% for 16 of the 18 pair–drainage
combinations (Table 2).
Overall, the ages estimated from scales, pectoral fin
rays, and otoliths were the same for ages 0–3,
indicating good precision between structures for
immature fish. Scales began to underestimate ages
from pectoral fin ray sections and sectioned otoliths at
age 4, whereas pectoral fin ray sections began to
underestimate ages from otoliths at about age 6 (Figure
4). Bias in age estimates was present between scales
and pectoral fin ray sections, scales and otoliths, and
pectoral fin rays and otoliths, but most of this bias was
due to older individuals in a few drainages (Table 3;
Figure 4). With the exception of young fish (i.e., ,age
2), the precision of age estimates generally decreased
as the estimated age of fish increased (Figures 4, 5).
Discussion
Prior to this study, we assumed that otoliths would
provide more accurate age estimates than scales or
sections of pectoral fin rays because they had been
indirectly validated (Thompson and Beckman 1995).
After comparing age estimates of the three structures,
we conclude that otoliths may be more accurate for
estimating white sucker age than either scales or
pectoral fin ray sections, as these latter structures
underestimated ages from otoliths. The precision of
ages for individual fish affected differences in precision
between pairs of structures within each drainage.
Young fish that had an age discrepancy of 1 year
between structures had a higher CV and APE than did
older fish with a discrepancy of 1 year because the
relative error was larger. This led to large confidence
intervals for precision metrics for individual pairs of
structures and few differences within or among drain-
ages. The combined sample in our study supports
observations and concerns that were reached by
previous authors regarding the use of scales and
pectoral fin ray sections to estimate the age of mature
white suckers (Beamish and Harvey 1969; Ovchynnyk
1969; Beamish 1973; Quinn and Ross 1982) and
further strengthens support for the use of otoliths to
estimate age.
Scale irregularities, false checks, and false annuli on
scales and fin ray sections were difficult to distinguish
from true annuli and may have contributed to errors in
estimated age (Beamish and Harvey 1969). Scale and
pectoral fin ray sections were often assigned the same
age in some drainages, but both often overestimated the
age from the otolith section; this result suggests the
presence of false annuli or checks on the scales and
pectoral fin ray sections (Beamish and Harvey 1969;
Beamish 1973). These potential false annuli occurred
on individual fish, but the overall trend was the
underestimation of otolith ages by scales and pectoral
fin rays. Despite some age discrepancies, the overall
mean age estimates from all three structures were
equivalent for ages 0–3, indicating that all three
structures may be suitable for estimating the age of
younger fish. Ages estimated from scales underesti-
mated ages from pectoral fin rays and otoliths beyond
age 3, which is similar to findings in other studies that
have reported bias of scales versus pectoral fin rays at
about age 5 (Beamish and Harvey 1969; Beamish
1973; Quinn and Ross 1982). Pectoral fin ray sections
yielded precise ages relative to ages estimated from
otoliths up to age 7, although slight underestimation
occurred in some older fish. If scales or pectoral fin ray
sections are used instead of otoliths to estimate white
sucker age, their potential errors, biases, and limitations
FIGURE 4.—Age bias plots of white suckers collected from
six drainages in the upper Missouri River basin in 2002 and
2003 and subjected to age estimation based on scales, pectoral
fin ray sections, and otoliths. In each panel, the error bars
represent the 95% confidence intervals, the dotted line
indicates the theoretical 1:1 agreement line of age estimates
between structures, and the solid line is the observed
regression line. An asterisk next to an observed slope or
intercept denotes a significant difference from the slope or
intercept of the theoretical 1:1 agreement line and thus
indicates bias between the structures.
28 SYLVESTER AND BERRY
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must be taken into consideration. Differences in age
estimates between structures can have impacts on
population metrics such as growth estimates (Braaten
et al. 1999) and population metrics derived from age
frequencies (e.g., annual mortality and survival rates).
Annuli distinctness and formation on scales varied
among drainages. All drainages had individual fish
with regenerated scales and irregularities. White sucker
populations in the Frenchman River and Rock Creek
drainages grew more slowly than more southerly
populations; scale annuli from these fish were often
indistinct, circuli often did not cross over, and scales
were generally difficult to interpret. These character-
istics have been observed in other slow-growing white
sucker populations (Dence 1948; Geen et al. 1966) and
may have resulted in the lower precision of age
estimates in these drainages.
Pectoral fin ray sections were easy to read, but the
thickness of the section often had to be adjusted for
individual fish. Poor differential light transparency
obscured the annuli if the section was too thick,
whereas too much light transparency made the annuli
TABLE 2.—Comparison of precision and agreement metrics between pairs of age-estimating structures collected from white
suckers in 2002 and 2003 in the upper Missouri River basin (N¼ number of fish, CV¼ coefficient of variation, APE¼ average
percent error, %¼ percent agreement, and 1 year¼ percent agreement within 1 year). Values for CV and APE are means, with
95% confidence intervals in parentheses.
Scale and pectoral fin ray Scale and otolith Pectoral fin ray and otolith
Drainage N CV APE % 1 year CV APE % 1 year CV APE % 1 year
Overall 229 12.6 8.9 71.6 94.8 17.9 12.7 63.8 94.3 9.9 7.0 78.6 97.8(3.7) (2.6) (4.5) (3.2) (3.5) (2.5)
Nowood River 56 4.8 3.4 80.4 94.6 13.5 9.6 71.4 92.9 11.4 8.1 76.8 94.6(2.9) (2.1) (8.8) (6.3) (8.7) (6.1)
Beaver Creek 16 1.3 0.9 93.8 100.0 10.7 7.6 68.8 100.0 12.0 8.5 62.5 100.0(2.7) (1.9) (9.4) (6.6) (9.3) (6.6)
Elm River 16 7.7 5.4 81.3 100.0 18.9 13.3 50.0 100.0 11.2 7.9 68.8 100.0(9.0) (6.4) (11.0) (7.8) (9.6) (6.8)
Rock Creek 54 19.5 13.8 66.7 96.3 23.1 16.3 66.7 98.1 8.0 5.6 87.0 100.0(10.5) (7.4) (12.2) (8.6) (7.6) (5.4)
Frenchman River 57 17.5 12.4 54.4 87.7 17.9 12.7 54.4 86.0 11.2 7.9 75.4 96.5(7.6) (5.4) (7.6) (5.4) (7.6) (5.4)
Sweet Grass River 30 14.0 9.9 80.0 100.0 20.3 14.4 66.7 100.0 6.3 4.4 86.7 100.0(13.8) (9.8) (14.2) (10.1) (6.1) (4.3)
TABLE 3.—Summary of ANCOVA comparisons between the theoretical and observed slopes and intercepts of age bias plots
for three age-estimating structures collected from white suckers in the upper Missouri River basin in 2002 and 2003.
Pair of structures Metric df Statistic P-value
Scale age versus pectoral fin age Model 3 F ¼ 949.17 ,0.0001Error 19Pectoral fin 1 F ¼ 1,646.92 ,0.0001Pectoral fin 3 treatment 1 F ¼ 103.77 ,0.0001Slope t ¼ �10.19 ,0.0001Intercept t ¼ 2.86 0.0099
Scale age versus otolith age Model 3 F ¼ 624.56 ,0.0001Error 20Otolith 1 F ¼ 1,249.68 ,0.0001Otolith 3 treatment 1 F ¼ 128.40 ,0.0001Slope t ¼ �11.33 ,0.0001Intercept t ¼ 3.34 0.0033
Pectoral fin age versus otolith age Model 3 F ¼ 720.63 ,0.0001Error 20Otolith 1 F ¼ 1,919.20 ,0.0001Otolith 3 treatment 1 F ¼ 13.93 0.0013Slope t ¼ �8.73 0.0013Intercept t ¼ 1.50 0.1484
MANAGEMENT BRIEF 29
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indistinguishable if the section was too thin (Scidmore
and Glass 1953). The center of the fin ray may have
obscured the first annulus, and crowding of annuli in
distal portions of fin ray sections may have occurred in
older fish, perhaps leading to errors in the estimated
age (Quinn and Ross 1982; Pehna et al. 2004).
Sections of lapilli otoliths were easy to interpret,
although some crowding of distal annuli occurred in
fish older than 6 years (Thompson and Beckman
1995). Sections of otoliths must contain the nucleus
and may result in age estimation error if this
requirement is not met (DeVries and Frie 1996). It is
possible that the timing of fish collection may have
affected recognition of annuli on otoliths because of
differences in timing of annulus formation (Beckman
and Wilson 1995). Thompson and Beckman (1995)
reported that about 5% of white suckers in Lake
Taneycomo, Missouri, had an annulus at the marginal
edge in June, but the percentage increased to nearly
80% in August. White suckers used for age estimation
in our study were collected in August 2002 (i.e., the
Nowood River, Beaver Creek, and Elm River drain-
ages) and June and July 2003 (i.e., Rock Creek,
Frenchman River, and Sweet Grass River drainages).
The precision estimates and bias between structures
in this study were comparable to those determined in
other studies (Welch et al. 1993; Soupir et al. 1997;
Beckman 2002; Ihde and Chittenden 2002), some of
which recommended otoliths as the preferred age-
estimating structure for a variety of species. Age
validation with the use of known-age fish is still
needed for the white sucker, as recommended by
Beamish and McFarlane (1983). This study is the first
to compare age estimates from scales, pectoral fin ray
sections, and sectioned otoliths in the white sucker.
Sectioned lapilli otoliths are recommended for the best
white sucker age estimates due to underestimation of
age estimates from scales and pectoral fin ray sections.
If nonlethal techniques for estimating age are required,
pectoral fin ray sections provide closer age estimates
for mature fish than do scales in comparison to otolith
age estimates, but pectoral fin ray sections may still
underestimate the age of fish older than age 5. The
precision and bias information in this study will be
useful to fisheries professionals in assessing age of
white suckers and other catostomids in the future.
Acknowledgments
We would like to thank the Gap Analysis Project
Office of the U.S. Geological Survey for funding. S.
Freeling, S. Wall, D. Hourigan, V. Wassink, and R.
Jensen provided assistance with fieldwork and sample
preparation. Additional thanks are extended to B.
Graeb, J. Duehr, C. Hoagstrom, and several anony-
mous reviewers for providing helpful comments on this
manuscript.
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