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Predictors of Occurrence of the Aquatic Macrophyte Podostemum ceratophyllum in a Southern Appalachian River
Jane E. Argentina, Mary C. Freeman, and Byron J. Freeman

Southeastern Naturalist, Volume 9, Issue 3 (2010): 465–476

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2010 SOUTHEASTERN NATURALIST 9(3):465–476 Predictors of Occurrence of the Aquatic Macrophyte Podostemum ceratophyllum in a Southern Appalachian River Jane E. Argentina1,*, Mary C. Freeman2, and Byron J. Freeman3 Abstract - The aquatic macrophyte Podostemum ceratophyllum (Hornleaf Riverweed) commonly provides habitat for invertebrates and fishes in flowing-water portions of Piedmont and Appalachian streams in the eastern US. We quantified variation in percent cover by P. ceratophyllum in a 39-km reach of the Conasauga River, TN and GA, to test the hypothesis that cover decreased with increasing non-forest land use. We estimated percent P. ceratophyllum cover in quadrats (0.09 m2) placed at random coordinates within 20 randomly selected shoals. We then used hierarchical logistic regression, in an information-theoretic framework, to evaluate relative support for models incorporating alternative combinations of microhabitat and shoal-level variables to predict the occurrence of high (≥50%) P. ceratophyllum cover. As expected, bed sediment size and measures of light availability (location in the center of the channel, canopy cover) were included in best-supported models and had similar estimated-effect sizes across models. Podostemum ceratophyllum cover declined with increasing watershed size (included in 8 of 13 models in the confidence set of models); however, this decrease in cover was not well predicted by variation in land use. Focused monitoring of temporal and spatial trends in status of P. ceratophyllum are important due to its biotic importance in fastflowing waters and its potential sensitivity to landscape-level changes, such as declines in forested land cover and homogenization of benthic habitats. Introduction Aquatic plants often influence lotic communities by modifying habitats and increasing structural complexity for stream biota (Fritz et al. 2004). One species of aquatic plant, Podostemum ceratophyllum Michaux (Hornleaf Riverweed), often dominates the in-stream vegetative communities of streams and rivers in eastern North America (Everitt and Burkholder 1991, Grubaugh and Wallace 1995). Where abundant, the plant can increase local macroinvertebrate abundance and biomass (Grubaugh and Wallace 1995, Hutchins et al. 2004, Nelson and Scott 1962) and influence fish habitat use (Argentina et al., in press; Connelly et al. 1999; Etnier and Starnes 1993). Podostemum ceratophyllum primarily occurs in relatively shallow areas of moderate to swift flow over coarse bed sediments (termed “shoals” in larger rivers) in rivers and streams along the east coast of the United States and Canada and portions of Central America (Philbrick and Crow 1983, Philbrick and Novelo 2004). Factors influencing occurrence of the plant within and among patches of suitable habitat have not been reported, and widespread population declines have been noted (Munch 1993, Philbrick and Novelo 2004). 1Institute of Ecology, University of Georgia, Athens, GA 30602. 2US Geological Survey, Patuxent Wildlife Research Center, Athens, GA 30602. 3Georgia Museum of Natural History, University of Georgia, Athens, GA 30602. *Corresponding author - 466 Southeastern Naturalist Vol. 9, No. 3 Podostemum ceratophyllum is of particular interest because it is one of the few macrophytes in North America adapted to fast-flowing waters (Mulholland and Lenat 1992, Wallace et al. 1992), and for its potential for modifying benthic habitat for aquatic fauna, including stream fishes. Water velocities within P. ceratophyllum beds can be more than 50% slower compared to flow above the plant beds (Grubaugh and Wallace 1995), which can cause deposition of suspended sediment and organic matter (Nelson and Scott 1962, Sand-Jensen 1998), in turn decreasing turbidity downstream (Madsen et al. 2001). In addition, the plant’s root structures may stabilize bed sediments, thereby decreasing the rate of downstream bed migration during periods of high flow. Finally, the plant’s stems and leaves increase the surface area available for aquatic invertebrates and epiphytic periphyton (Grubaugh and Wallace 1995, Hutchens et al. 2004, Nelson and Scott 1962). Podostemum ceratophyllum has been shown to increase invertebrate productivity of Piedmont streams (Grubaugh and Wallace 1995) and invertebrate biomass and species richness in Blue Ridge streams (Hutchens et al. 2004). Thus, P. ceratophyllum cover may indirectly benefit insectivorous fishes by increasing prey availability, which may explain positive correlations observed between P. ceratophyllum occurrence and several stream fishes (Etnier and Starnes 1993, Hagler 2006, Marcinek 2003). We conducted this study to investigate evidence for specific, alternative factors as causes of P. ceratophyllum variation among shoals in a southern Appalachian river that harbors populations of multiple imperiled aquatic species. We hypothesized that P. ceratophyllum decreased in relation to increasing agricultural land use (and decreasing forest cover), but recognized that local variables such as canopy cover also likely influenced plant occurrence. Therefore, we assessed the relationships between P. ceratophyllum and three categories of habitat variables expected to influence occurrence of the macrophyte: microhabitat (i.e., sediment size and location at the point of observation within a shoal), channel-unit (i.e., shoal characteristics such as channel slope and canopy cover), and landscape (considering drainage area and land use upstream and in the riparian buffer). This assessment enabled us to further examine the effects landscape factors may have on P. ceratophyllum cover after accounting for local influences. Methods Study location We conducted this research in the biologically diverse Conasauga River, which drains 1873 km2 in the southern Appalachian Blue Ridge and the Valley and Ridge physiographic provinces, in the headwaters of the Coosa River basin, GA and TN. Our study reach is a 38.8-km portion of the Conasauga River mainstem, between river kilometers 36.6 and 75.4 (measured upstream from the mouth), which encompasses the known extant ranges of the three federally protected fishes within the Conasauga River. The study reach also spans a natural gradient of stream size, with drainage area increasing from 226 to 794 km2, and with elevation decreasing from 293 m to 189 m. 2010 J.E. Argentina, M.C. Freeman, and B.J. Freeman 467 We selected study sites for investigating P. ceratophyllum from all shoal habitat within the Conasauga River study reach. To estimate shoal habitat availability, we canoed the study reach during May and June 2005 and used a handheld GPS to record the location of each shoal encountered. We then divided the mainstem study reach into four equidistant segments, and randomly chose five shoals within each of the four sections (for a total of 20 study shoals) for further study. Vegetation measurements and habitat variables We measured percent cover of P. ceratophyllum and habitat variables at each of the 20 randomly selected shoals. We used a 0.093-m2 PVC-frame quadrat subdivided into sixteen 7.6-cm x 7.6-cm squares to estimate percent P. ceratophyllum cover at 50 randomly selected locations within each shoal. At each random location, we counted the number of frame squares containing P. ceratophyllum attached to the bed sediments. We also measured the medial axis of two sediment particles chosen haphazardly from the PVC frame at each of the 50 locations, for a total of 100 samples, to give an estimate of bed sediment size at each shoal where we assessed P. ceratophyllum cover. At three of the twenty shoals, we collected the P. ceratophyllum within 16 quadrats (4 samples in each category:1–4 squares, 4–8 squares, 9–12 squares, and 13–16 squares occupied) to estimate the relationship between plant cover and biomass. We removed all P. ceratophyllum within these quadrats to plastic bags and returned the samples to a laboratory where plant material was separated from remaining sediment and detritus, and then dried, ashed, and weighed to estimate ash-free dry mass (AFDM). We log-transformed P. ceratophyllum biomass and regressed biomass against the number of quadrat units occupied. We evaluated variation in the physical characteristics of channel slope, shoal length, and percent canopy cover. At each shoal, channel slope was estimated using a Topcon autolevel and a stadia rod. We measured shoal length in meters, and determined percent canopy cover by averaging measurements taken with a spherical densiometer at nine evenly spaced locations. Finally, we measured turbidity (NTU; with a Hach Turbidmeter 2100) at the time each shoal was visited. All field surveys took place between July and September 2005, during low-flow periods. Land cover upstream of each shoal was estimated using ArcView® 3.3 geographic information systems (GIS) software. We used digital US Geological Survey (USGS) topographic maps to delineate watershed boundaries of each shoal. Within each delineated watershed, we used a 1:24,000 hydrography network to further delineate 100-m buffers that extended from each shoal along the mainstem to the headwaters from each shoal, and 100-m buffers that extended 1 km upstream of each shoal along the mainstem. We used the 2001 USGS National Land Cover Database zone 60 land cover to estimate percent row-crop agriculture in the watershed and in the100-m buffers extending upstream from each shoal. Agricultural land cover in the watershed was strongly correlated with agricultural land cover within the stream buffer for the entire upstream drainage (r = 0.96), but not within the 1-km length buffer (r = 0.10). 468 Southeastern Naturalist Vol. 9, No. 3 Predictive models for P. ceratophyllum We used an information-theoretic approach (Burnham and Anderson 2002) to determine the best-supported model from a suite of alternative models relating cover by P. ceratophyllum at a given point to local, channel unit, and landscape factors. The point-counts of P. ceratophyllum cover were strongly non-normally distributed, with 57% of observations having 0 cover, and the remaining counts approximately evenly distributed between 2 (12.5%) and 16 (100%) squares occupied. Therefore, rather than use point-counts of P. ceratophyllum cover as the response variable, we used logistic regression to model the probability of at least 50% cover (≥8 squares in the sample frame) as a binomial variable. We thus assumed that 50% or greater P. ceratophyllum cover represented a high level of P. ceratophyllum cover and may be high enough to be of potential biological significance to invertebrates and insectivorous fishes, though there are no published data suggesting a significant level of P. ceratophyllum for either fish or invertebrates. We modeled P. ceratophyllum cover using a hierarchical regression design. Specifically, we used all point observations (n = 1000) of P. ceratophyllum cover (recorded as <50% or ≥50%) in a regression model with predictor variables measured for the individual shoal and/or at the observation point (Table 1). All models included a random effect for shoal identity to account for autocorrelation among repeated observations within shoals (Singer 1998). Parameters for logistic regression models, including the null model (i.e., no predictor variables) and models with all combinations of the shoal-level and observation-point variables (excluding models that included both buffer land use and watershed land use) were estimated using Proc NLMIXED in SAS (SAS version 9.1, 2002). We used Akaike’s information criterion (AIC) to assess relative support among our candidate models; AIC is an entropy-based measure of relative fit among alternative models fit to a given data set, with the best-supported model having the lowest AIC value (Burnham and Anderson 2002). We counted model parameters for estimating AIC as the fixed effects (i.e., predictor variables) plus the random effect and the model intercept. Akaike weights, which range from zero to one and represent the relative degree of support for a given model in the candidate set, were calculated from the AIC values (Burnham and Anderson 2002). We retained for evaluation all models that had weights within 1/8th of the AIC weight of the best-supported model (Royall 1997), except where Table 1. Variables used in logistic regression analysis of occurrence of high (≥50%) P. ceratophyllum cover. Category Variable Observation-point Median sediment size (mm) Position within the channel (center 50% or outer 25% of channel width) Channel unit Percent canopy cover Shoal slope (cm/m, log transformed) Landscape Drainage area (km2) Percent agriculture in a 100-m buffer extending 1 km upstream of each site Percent row-crop agriculture in the watershed 2010 J.E. Argentina, M.C. Freeman, and B.J. Freeman 469 the addition of variables to the best-supported model did not improve the model log-likelihood (Burnham and Anderson 2002). Results Longitudinal variation in shoal habitat and land use We mapped 131 shoals in the 38.8-km study reach of the Conasauga River (Fig. 1). Total shoal habitat in that stretch of the river was 13.6 km out of the total 38.8 km, or 33% of the study reach. The 20 shoals randomly selected Figure 1. Location of the Conasauga River, TN and GA (inset), and mapped and surveyed shoals within the study reach. 470 Southeastern Naturalist Vol. 9, No. 3 for sampling encompassed 1.5 km and 11% of all available shoal habitat. The shoals were steeper and longer upstream (Argentina et al. 2010) and became less steep and shorter downstream. Average sediment size was 560–690 mm in the upstream-most portion of the reach and decreased to 14–44 mm in the downstream half of the reach. On average, shoals were separated upstream and downstream by 375 m from other shoals, and the distance between shoals increased downstream. Land use in the basin shifts from primarily forest in the headwaters, to increasing agricultural use in the middle of the reach and urban influence in the downstream sections. Estimated percent total forest cover in the basin decreases from about 99% to 68% from the upstream to downstream boundaries of the study reach. This pattern corresponds to an increase from 0.6% to 6% in developed land cover (including low- and high-density developed), and from 0.04% to 21.9% in agricultural land covers (grassland, pasture, and row crop), from upstream to downstream (Argentina et al. 2010). Longitudinal trends in P. ceratophyllum occurrence Percent P. ceratophyllum cover (quantified as the percent of squares within the sampling frame occupied) averaged from less than 1% to 55% across the 20 randomly selected shoals (Fig. 2), with an average cover of 17%. At most sampled shoals, P. ceratophyllum biomass and surface area appeared sparse, even when measured cover (i.e., number of squares occupied) was high. Ash-free biomass (ln-transformed) measured at 3 shoals increased with increasing cover of P. ceratophyllum (P <0.05), although the relation was not strongly linear (r2 = 0.35; Fig. 3). Hierarchical modeling to relate physical variables to the probability of ≥50% P. ceratophyllum cover resulted in nine models in the confidence set Figure 2. Number of sampling quadrats with greater than 50% coverage out of 50 samples at each of the 20 shoals. Shoals are plotted (not to scale) from upstream to downstream and labeled as distance from the mouth. 2010 J.E. Argentina, M.C. Freeman, and B.J. Freeman 471 of models (i.e., with model weights within 1/8th of the top model; Table 2). The two observation-point variables, bed sediment size and location within the channel (within 25% of the edge or in the middle 50%), were present in all models in the confidence set, indicating microhabitat characteristics were direct drivers of P. ceratophyllum cover. Each of the shoal-specific variables was present in at least one of the models in the confidence set. The best-supported model contained location within the channel, median sediment size, percent canopy cover, and drainage area. The next best-supported model was 58% as likely to be the best model and included location within the channel, median sediment size, and percent canopy cover as in the top model, but instead of drainage area it included percent row-crop land-cover in the watershed (Table 2). All the other models within the confidence set were less than 50% as likely as the bestsupported model to be the best model among those evaluated. Model parameter estimates were strongly consistent among models for the two observation-points variables (location within the channel and sediment size), relatively consistent for effects of canopy cover and drainage area, and variable for effects of slope and the two land-cover variables. Overall, the strongest drivers of high P. ceratophyllum cover in our data set were location in the center 50% of the channel, sediment size, drainage area, and canopy cover. Across all models, P. ceratophyllum was 2.9 to 3.0 times more likely to have high cover in the center half of the channel rather than near the edges (Table 3; odds ratios were estimated as e(parameter estimate) [Agresti 2002], and range from 2.9 to 3.0 for the variable location in channel). Also across all models, high P. ceratophyllum cover was about 3% more likely with each 10-mm increase in sediment size (Table 3; odds ratios were estimated as e(parameter estimate, 1 mm increase )(10), and ranged from 1.028 to 1.029). Figure 3. Podostemum ceratophyllum biomass (ash-free dry mass, ln (g) AFDM) collected from sampling quadrats plotted in relation to number (0 to 16) of quadrat units occupied. A simple linear regression fit is imposed on the data, as ln mass = -2.3699 + 0.2021(units occupied); r2 = 0.35. 472 Southeastern Naturalist Vol. 9, No. 3 The probability of high P. ceratophyllum cover decreased by an estimated 2 to 3% with each 1% increase in average site canopy cover (Table 3, odds ratios ranged from 0.97 to 0.98). The probability of high P. ceratophyllum cover also decreased about 3% for every 10-km2 increase in drainage area (Table 3; odds ratios were estimated as e(parameter estimate, 1 km increase )(10), and ranged from 0.96 to 0.97). Effects of the remaining variables on P. ceratophyllum cover were imprecisely estimated (shown by large standard errors on parameter estimates) and inconsistent among the models that included these variables (Table 3). The second-most strongly supported model included an estimated decline of 31% (odds ratio = 0.69) in the occurrence of high P. ceratophyllum cover with each 1% increase in row-crop land use, but 95% confidence intervals for the estimated effect of row-crop land use include 0 (no effect). Discussion Podostemum ceratophyllum generally occurs in high-velocity, wide, shallow shoal habitat, typically characterized by coarse bed sediments and relatively steep stream slope (Hutchens et al. 2004, Nelson and Scott 1962). Our models indicate local features (sediment size, location in the channel) are better predictors of occurrence of P. ceratophyllum than shoal slope or watershed land use. From our predictive models, P. ceratophyllum is more likely to occur in the center of the channel and in areas with larger sediment sizes, indicating strong physical control on its presence. Because P. ceratophyllum persists in shoals by attaching to rock substrates, bedrock and coarse bed sediments that are only displaced by high velocities provide better habitat than shifting sand and gravel. The large effect of location in the channel on high P. ceratophyllum cover in our models suggests light availability also strongly influenced P. ceratophyllum growth. We also found a negative effect of canopy cover at a shoal on occurrence of high P. ceratophyllum cover. Everitt and Burkholder (1991) similarly found that riparian shading influenced macrophyte community composition in a stream flowing over a granite outcrop in North Carolina, with P. ceratophyllum dominating only in the more open sites. We also observed a five-fold increase in base-flow turbidity coincident with the longitudinal decrease in P. ceratophyllum cover (Argentina et al. 2010), and it is conceivable that elevated water turbidity could also limit light for benthic macrophytes. We did not include turbidity in our models because we did not expect, a priori, that a single point-in-time turbidity measurement would be predictive of P. ceratophyllum cover. Additionally, observations of abundant P. ceratophyllum in other large Piedmont rivers, including the Etowah (Hagler 2006), Flint (Marcinek 2003), and Middle Oconee (Grubaugh and Wallace 1995) rivers in Georgia, where water turbidity commonly exceeds levels in the downstream portion of the Conasauga study reach (about 12 NTUs) suggested that turbidity was unlikely to limit the plant in the Conasauga. What did cause downstream declines in P. ceratophyllum cover in the Conasauga mainstem shoals? We found no strong support for an effect 2010 J.E. Argentina, M.C. Freeman, and B.J. Freeman 473 Table 2. Logistic regression models for predicting high (≥50%) P. ceratophyllum cover, for the 9 best-supported models. Models are listed in order of support, showing number of model parameters (K), AIC values, AIC values relative to the best-supported model (Δ AIC), and confidence-set adjusted model AIC weights (wi). Location Sediment Canopy Drainage Agriculture Row-crop Model in channel size cover (%) Slope area in buffer (%) land use (%) K AIC Δ AIC W(i) 1 X X X X 6 625.3 0 0.292 2 X X X X 6 626.4 1.1 0.169 3 X X X 5 626.7 1.4 0.145 4 X X X 5 627.1 1.8 0.119 5 X X X X 6 628.4 3.1 0.062 6 X X X X 6 628.4 3.1 0.062 7 X X X X 6 628.6 3.3 0.056 8 X X X 5 628.9 3.6 0.048 9 X X X X 6 629.0 3.7 0.046 Table 3. Parameter estimates (and standard errors) for predictor variables included in logistic regression models for predicting high (≥50%) P. ceratophyllum cover, for the 9 best-supported models. Models are listed in order of support as in Table 2. The random effect estimate is also shown for each model. Variables included in model Location in Canopy Agriculture Row-crop Model channel Sediment size cover (%) Slope Drainage area in buffer (%) land use (%) Random effect 1 1.085 (0.230) 0.0028 (0.0004) -0.027 (0.014) -0.0033 (0.0016) 0.800 (0.437) 2 1.084 (0.231) 0.0028 (0.0004) -0.025 (0.0003) -0.376 (0.228) 0.949 (0.493) 3 1.073 (0.230) 0.0029 (0.0004) -0.0041 (0.0018) 1.034 (0.532) 4 1.072 (0.230) 0.0029 (0.0004) -0.034 (0.016) 1.087 (0.561) 5 1.077 (0.230) 0.0028 (0.0004) 0.165 (0.318) -0.0035 (0.0021) 1.041 (0.532) 6 1.079 (0.231) 0.0028 (0.0004) -0.028 (0.017) 0.248 (0.296) 1.070 (0.545) 7 1.074 (0.230) 0.0029 (0.0004) -0.0035 (0.0041) 0.087 (0.531) 1.051 (0.548) 8 1.075 (0.231) 0.0028 (0.0004) 0.483 (0.290) 1.293 (0.631) 9 1.067 (0.230) 0.0028 (0.0004) -0.0041 (0.0018) -0.0044 (0.012) 1.032 (0.526) 474 Southeastern Naturalist Vol. 9, No. 3 of agricultural land use on occurrence of high P. ceratophyllum cover, as we hypothesized, after accounting for effects of local factors. In the bestsupported model with row-crop agriculture (model 2), the model coefficient is negative, indicating the possibility of a negative effect of buffer loss and agriculture in the buffer, but this is not consistent with model 7, and both have large confidence intervals around these estimates. Agricultural land cover in the riparian buffer upstream from each shoal showed a negative effect on the occurrence of high P. ceratophyllum cover in only one model in the confidence set, again with wide confidence intervals around this estimate. Thus, these data did not show clear, direct effects of replacing forest with agriculture on P. ceratophyllum. We also did not expect a natural decline in P. ceratophyllum with increase in drainage area over the size range of the Conasauga drainage (i.e., 200–800 km2), again because we know the plant occurs abundantly in shoal habitats in other, larger Piedmont rivers with higher drainage areas (e.g., >2000 km2, Flint River; >400 to1500 km2, Etowah River; 1000 km2, Middle Oconee River). We suspect that other, unmeasured changes associated with the downstream decline of forested land cover are imposing stress on river biota in the lower portion of the study reach. Increased baseflow turbidity along the mainstem of the Conasauga River could be correlated with other changes in water quality, as well as increased sedimentation (Walters et al. 2003). Stormflow transport of sediment and contaminant loading from agricultural lands and local urbanization may also increase in the lower portion of the study reach. For example, we have observed dense benthic algal growths that covered extensive areas of the channel, including patches of P. ceratophyllum, during recent droughts in lower portions of the study reach (B.J. Freeman, unpubl. data), possibly reflecting nutrient loading. Additionally, shoals are less numerous and farther apart in the lower Conasauga, which could limit recolonization following disturbance. Local population stability of P. ceratophyllum may depend on clonal growth, as seed production is low compared to other plants within Podostemaceae (mean of 12 per seed capsule, with only 39 capsules per plant) and dispersal ability is unknown but assumed to be low (Philbrick and Novelo 1997). Therefore, P. ceratophyllum may be slow to recover following disturbances such as sediment scour or pulses of herbicides, especially if plants have to recolonize habitat across long distances. Focused monitoring efforts could help resolve trends in P. ceratophyllum status and the relative influence of changing water quality, sedimentation, or channel adjustments on P. ceratophyllum persistence. We have assessed P. ceratophyllum by quantifying cover, which is relatively easily measured and can provide a useful measure of macrophyte dominance (Everitt and Burkholder 1991). We have also observed, however, that cover may not be strongly correlated with plant biomass, and biomass might provide a better measure of P. ceratophyllum contribution to benthic habitat for other biota. We measured a wide range of plant biomass at varying levels of cover. Scour and grazing (e.g., by birds, turtles, Castor canadensis Kuhl (Beaver); Parker et al. 2007) can shorten P. ceratophyllum stems, reducing biomass but leaving stems and root structure in place that may subsequently regrow. Adding 2010 J.E. Argentina, M.C. Freeman, and B.J. Freeman 475 a measure of average stem length to assessments of percent cover could provide an effective field measure of P. ceratophyllum status that is more closely correlated with biomass, without requiring the additional resources needed to collect and process plant samples. Understanding factors driving P. ceratophyllum is of interest particularly because of the plant’s importance as habitat for macroinvertebrates (Grubaugh and Wallace 1995, Hutchens et al. 2004, Nelson and Scott 1962) and fishes (Argentina et al. 2010). Podostemum ceratophyllum is perhaps the most common macrophyte in fast-flowing waters of Piedmont and Appalachian streams (Mulholland and Lenat 1992, Wallace et al. 1992). Declining occurrence of the plant may signal changes in occurrences and productivity of other stream biota. Our research in the Conasauga River has illustrated that local bed sediment size and average shoal canopy cover are important predictors of P. ceratophyllum cover, and that influences of other factors can be evaluated effectively in models that include local along with larger-scale factors. Acknowledgments We would like to thank members of the Freeman lab, especially Judith Barkstedt, Paula Marcinek, James Norman, and Rebecca Bourquin, for help in the field and in the lab. Comments by Jim Peterson, Tom Kwak, Stuart Welsh, and two anonymous reviewers greatly improved this manuscript. Funding was provided by grants to B.J. Freeman from the Georgia Department of Natural Resources and the Tennessee Wildlife Resources Agency. Literature Cited Agresti, A. 2002. Categorical Data Analysis, Second Edition. John Wiley and Sons, Inc., Hoboken, NJ. 710 pp. Argentina, J.E., M.C. Freeman, and B.J. Freeman. 2010. 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