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(American Journal of Botany. 2004;91:1930-1935.)
© 2004 Botanical Society of America, Inc.


Systematics and Phytogeography

Morphological variation in Sarracenia purpurea (Sarraceniaceae): geographic, environmental, and taxonomic correlates1

Aaron M. Ellison2,5, Hannah L. Buckley3,6, Thomas E. Miller3 and Nicholas J. Gotelli4

2Harvard University, Harvard Forest, P.O. Box 68, Petersham, Massachusetts 01366 USA; 3Department of Biological Science, Florida State University, Tallahassee, Florida 32306 USA; 4Department of Biology, University of Vermont, Burlington, Vermont 05405 USA

Received for publication February 9, 2004. Accepted for publication August 3, 2004.


    ABSTRACT
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS
 DISCUSSION
 LITERATURE CITED
 
Geographic variation in morphology reflects phenotypic responses to environmental gradients and evolutionary history of populations and species and may indicate local or regional changes in environmental conditions. The pitcher plant (Sarracenia purpurea) illustrates these principles. At local scales, its morphology reflects nutrient availability. At points along its broad geographic range (from Florida to northern Canada) morphology has been used to distinguish subspecies and varieties, but there has been no detailed study of the continuum of morphological variation across this entire range. Patterns of morphological variation in S. purpurea were characterized as a function of climatic and environmental conditions at 39 sites spanning its range. Differences in pitcher size and shape were strongly correlated with temperature, annual precipitation, and availability of ammonium and calcium in peat pore water. Pitcher shape (lip width, mouth diameter, and pitcher width) in Florida panhandle populations differed significantly from pitcher shape of all other populations, even after accounting for environmental correlations. In contrast, the northern and southern subspecies of S. purpurea (the latter exclusive of the Florida panhandle populations) cannot be distinguished based on these morphological measurements alone. These results support a recent proposal that identifies the Florida populations as a distinct species, Sarracenia rosea.

Key Words: carnivorous plants • geography • morphology • phylogeography • Sarracenia purpureaSarracenia rosea


    INTRODUCTION
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS
 DISCUSSION
 LITERATURE CITED
 
Geographic variation in plant morphology is a function of phenotypic changes in response to local environmental conditions, genetic variation and evolution among populations, and the biogeographic history of an individual species. Characteristics such as leaf shape are constrained genetically, yet they also can be affected greatly by the local environment in which they develop (Thompson, 1991 ; Schlichting and Pigliucci, 1998 ). Morphological variation and geographical separation among populations are also prerequisite to the formation of subspecies and species (Losos and Glor, 2003 ). Phylogeographic analysis can be used to illuminate the interplay of climate, geographical history, and evolutionary dynamics in generating new taxa (Avise et al., 1987 ; Templeton et al., 1995 ; Arbogast and Kenagy, 2001 ).

The North American pitcher plants in the genus Sarracenia exemplify the joint roles of these processes. All of the species are sympatric in the southeastern United States, a hot spot for biological diversity in North America (Peet and Allard, 1993 ; Donovan et al., 2000 ; Maskas and Cruzan, 2000 ). Since the end of the Pleistocene glaciation ca. 10 000 yrs ago, one species, Sarracenia purpurea L., has rapidly extended its range much further north, and its range now spans more than 30° of latitude and 70° of longitude. Pitcher morphology varies greatly, both within and among species, reflecting differences among sites in growing conditions (Ellison and Gotelli, 2002 ; Schnell, 2002 ) as well as genetic differentiation (Godt and Hamrick, 1999 ).

Sarracenia purpurea sensu lato (sensu Gleason and Cronquist, 1991 ) is a long-lived, rosette-forming, perennial carnivorous plant that grows in sphagnum bogs, poor fens, seepage swamps, and pine savannas of the eastern United States and Canada (Schnell, 2002 ). Its broad geographic range includes the entire coastal plain of the eastern United States (the Florida panhandle to Cape Cod), New England and the northern United States westward through the Great Lakes region, and all of Canada east of the Continental Divide (Schnell, 2002 ; Buckley et al., 2003 ). Not surprisingly, there is pronounced morphological variability in S. purpurea across its range, and botanists have named two subspecies based on quantitative and qualitative differences in pitcher morphology (Schnell, 1979 , 2002 ).

The two subspecies of S. purpurea, S. purpurea subsp. purpurea and S. purpurea subsp. venosa, are distinguished by the shape of the pitcher hood, the ratio of pitcher length to the diameter of the pitcher opening, the presence or absence of hairs on the outside of the pitcher, and flower color (Schnell, 2002 ). The size and shape of pitchers, however, can change dramatically in response to local environmental conditions (Mandossian, 1966 ; Ellison and Gotelli, 2002 ), and flower color is variable. Hence, Gleason and Cronquist (1991) did not accept the subspecies distinction and considered these two subspecies to be only geographic varieties.

The geographic boundary separating S. purpurea subsp. purpurea and S. purpurea subsp. venosa occurs in southern Delaware and northern Maryland and is defined by the southernmost extent of the Pleistocene glaciation: S. purpurea subsp. purpurea grows in formerly glaciated areas, whereas S. purpurea subsp. venosa grows only in unglaciated areas. Historical biogeography suggests that S. purpurea subsp. purpurea is derived from S. purpurea subsp. venosa, the former having colonized northern latitudes after glaciation. Furthermore, allozyme analysis suggests that S. purpurea subsp. venosa and its varieties are more genetically similar to each other than any of them are to S. purpurea subsp. purpurea (Godt and Hamrick, 1999 ).

A disjunct group of populations of S. purpurea subsp. venosa occurs on the Florida panhandle. This population has been described as a separate variety, S. purpurea subsp. venosa var. burkii Schnell (Schnell, 1993 ), but based on pitcher morphology, flower color, and height of the flower scape, Naczi et al. (1999) proposed that it be considered an entirely separate species, S. rosea Naczi, Case & Case. Further, allozyme analysis illustrates that S. purpurea subsp. venosa var. burkii is genetically distinct from both S. purpurea subsp. purpurea and S. purpurea subsp. venosa. Covariance of environmental conditions and morphology has not been assessed for either S. purpurea subsp. venosa or S. purpurea subsp. venosa var. burkii, in contrast to the detailed work on the covariance between environmental conditions and morphology of S. purpurea subsp. purpurea (Mandossian, 1966 ; Ellison and Gotelli, 2002 ). Taxonomic distinctions that are made based on morphology and do not account for the entire range of variability in a taxon may lead to its being split unnecessarily into multiple taxa.

We characterized patterns of variation in vegetative morphology of S. purpurea subsp. purpurea, S. purpurea subsp. venosa, and S. purpurea subsp. venosa var. burkii throughout their range in North America. We used these data, along with detailed environmental measurements, to partition morphological variation among geographic/climatic and environmental factors. We asked three questions:

  1. Is the observed morphological variation of northern and southern populations of S. purpurea associated with environmental and climatic gradients?
  2. Do S. purpurea subsp. venosa and S. purpurea subsp. venosa var. burkii, like S. purpurea subsp. purpurea, respond morphologically to local environmental conditions?
  3. Are observed patterns of morphological variation concordant with identification of infraspecific taxa based on previous morphological and allozyme analyses, and if taken together, do these data support the recent proposal (Naczi et al., 1999 ) that S. purpurea subsp. venosa var. burkii be considered a separate species, S. rosea?


    MATERIALS AND METHODS
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS
 DISCUSSION
 LITERATURE CITED
 
Between 1 May and 14 September 2001, we sampled 39 populations distributed throughout the range of S. purpurea (Fig. 1). These populations appeared not to have suffered from significant anthropogenic disturbance. Sampling was timed to occur approximately three weeks after flowering, by which time all plants had begun to produce new pitchers. Thus, within the growing season, southern sites were sampled earlier than northern sites. Site-selection criteria included population size (>50 plants), the likely ability of the population to withstand the damage of destructive sampling, and accessibility; state or local agencies and landowners permitted all collections. Because carnivorous plant collectors and hobbyists have planted S. purpurea widely, we sampled only native, rather than introduced (adventive) populations (as determined by local Natural Heritage programs and other authorities). We were unable to sample the other described variety of S. purpurea, S. purpurea subsp. venosa var. montana Schnell & Determann, which is a threatened endemic limited in distribution to the Blue Ridge Mountains and adjacent piedmont of southwestern North Carolina, northwestern South Carolina, and northeastern Georgia (Schnell and Determann, 1997 ). Because we sampled after plants had flowered, we did not collect data on flower color or shape.



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Fig. 1. Map of North America showing the 39 sample locations. Symbols indicate described subspecies of Sarracenia purpurea (open circles: 27 populations of S. purpurea subsp. purpurea; solid circles: 7 populations of S. purpurea subsp. venosa) or 5 populations of S. purpurea subsp. venosa var. burkii (solid triangles)

 
The latitude, longitude, and elevation of each site were determined using a hand-held GPS (global positioning system) unit accurate to ±50 m. Climatic variables were obtained for each site from the nearest (<100 km) weather stations and included 10-year means of the number of frost days per year; annual precipitation and snowfall; monthly, December minimum, July maximum, annual minimum and annual maximum temperatures; and variance in monthly temperature.

At each site, we laid a 1-m-wide belt transect across the longest axis of the Sarracenia population. If this axis was longer than 100 m, we used a 100-m transect centered on this axis. This transect was then divided into 20 equally spaced marks (maximum of 5 m apart), and the nearest pitcher plant to each mark was identified. For each of these 20 plants, we measured the maximum diameter of the rosette. For the first (largest) pitcher of the current year, we measured (±1 mm) the pitcher length, diameter of the pitcher mouth, the thickness of the pitcher lip, the maximum width of the pitcher, and the width of the wing (keel); see Ellison and Gotelli (2002) for an illustration of these measurements. The thickness of the lip of the pitcher and the ratio of pitcher length to mouth diameter have been used as key characters to distinguish among S. purpurea subsp. purpurea, S. purpurea subsp. venosa, and S. purpurea subsp. venosa var. burkii (Naczi et al., 1999 ; Schnell, 2002 ).

Because size and shape of S. purpurea subsp. purpurea pitchers are known to vary with light and vegetation cover (Mandossian, 1966 ), we visually estimated percentage cover of vegetation in a 1-m2 quadrat centered on each plant. Because there was no consistent set of co-occurring species across the range of S. purpurea, we distinguished percentage cover of functional groups: trees, shrubs, terrestrial or aquatic forbs, graminoids, ferns, lycopods, Sphagnum, other bryophytes, fungi, and lichens.

Relative wing width of pitchers (wing width/total pitcher width) previously has been correlated with pore-water nitrogen concentrations (Ellison and Gotelli, 2002 ). Therefore, we examined covariance between pitcher morphology and nutrient concentrations in pore water. We took five pore-water samples, evenly spaced across the sample transect. Fifty-mL water samples were extracted using clean Tygon tubing from 50 cm long x 2.5 cm diameter capped and perforated PVC tubes that were sunken into the peat. For each sample, we measured pH and calcium (mg/L) with Orion ion-sensitive electrodes (Thermo Electron Corp, Woburn, Massachusetts, USA), and phosphate (PO4-P), nitrate (NO3-N), and ammonium (NH4-N) (all in mg/L) spectrophotometrically using US-EPA standard methods (Bledzki and Ellison, 1998 ; Clesceri et al., 1998 ). Pore-water samples were not taken in eight southern sites, due to insufficient water availability in the drier sandy soils.

Some data reduction was performed prior to analysis. First, because the unit of interest was the site (N = 39 sites), the relationships between morphology and geographic, environmental, and climatic variables were based on means at each site (of N = 20 plants or vegetation samples per site; N = 5 pore-water samples per site). Because of correlations among climatic variables, among vegetation variables, and among pore-water chemical variables, we performed principal component analysis (PCA) to generate two principal axes that accounted for the majority of variance of each of these sets of predictor variables. All variables were standardized (transformed into standard-deviation units, or Z scores) prior to performing the PCA (Gotelli and Ellison, 2004 ). We also extracted two principal axes describing pitcher size and shape using PCA on the (similarly standardized) morphological variables measured for each pitcher. We separately analyzed two morphological variables used to separate the subspecies of S. purpurea (the width of the pitcher lip and the pitcher length:mouth diameter ratio) and the morphological ratio known to co-vary with pore-water nitrogen concentration (relative wing width).

All morphological variables (principal axis scores or the three distinct variables) were regressed on the environmental predictor variables. Stepwise multiple regression and Akaike's information criterion (AIC: Burnham and Anderson, 2002 ) were used to identify the best-fitting model and the variables that best predicted pitcher morphology.

Our first two questions addressed geographic and environmental correlates of morphological variability without regard to taxonomic distinctions. Therefore, we initially analyzed the data without classifying the observations according to infraspecific designations. These analyses illustrate patterns of covariance between morphological traits and climate, vegetation, and pore-water chemistry across the entire geographic range of S. purpurea.

Our third question asked if observed patterns of morphological variation were concordant with identification of infraspecific taxa by other authors based on morphology. To address this question, we used one-way analysis of variance (ANOVA) to test whether plant morphology (both the principal axis scores and the three distinct morphological variables) differed consistently among S. purpurea subsp. purpurea, S. purpurea subsp. venosa, and S. purpurea subsp. venosa var. burkii. In these ANOVAs, taxonomic designation was considered a fixed factor. A priori contrasts were used to test (a) whether S. purpurea subsp. venosa var. burkii differed from the two S. purpurea subspecies and (b) whether the two subspecies of S. purpurea differed from each other. Last, an analysis of covariance (ANCOVA) was used to determine if morphological differences among infraspecific taxa remained after accounting for covariance between morphological and environmental variables. All data analyses were done using S-Plus version 6.1 (Insightful Corporation, Seattle, Washington, USA).


    RESULTS
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS
 DISCUSSION
 LITERATURE CITED
 
Data reduction through principal component analysis
Climatic data were well summarized by the first two principal axes (Table 1), which together accounted for 96% of the variation among sites. The first principal axis was strongly correlated with latitude (r2 = 0.94) and reflected temperature differences among the sites (cool, northern sites had high values for this axis). The second principal axis reflected differences in precipitation among the sites (sites receiving more rain and snow had high values for this axis). Southern sites were intermediate in precipitation, whereas differences in precipitation among northern sites were associated with longitude: western sites were drier than eastern sites.


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Table 1. Results of the principal component analysis on the nine climatic variables. The first two principal axes accounted for 96% of the variance in the data. Values shown are the loadings of each variable on each of the first two axes

 
Two principal axes accounted for 60% of the variation in vegetation composition. The first principal axis separated Sphagnum-shrub bogs (high values on the axis) from poor fens and seepage swamps with higher densities of graminoids and forbs (low values on the axis). The second axis reflected light available to pitcher plants. Shady sites with many trees or shrubs had high values on this axis, and sunny sites with few trees or shrubs had low values on this axis. Neither of these vegetation axes was correlated with latitude, longitude, or climate.

Data for pore-water chemistry were available for 31 of the 39 sites, and the first two principal axes accounted for 61% of the variation in water chemistry among those sites (Table 2). The first principal axis reflected ammonium and calcium availability (sites with high concentrations of these two ions had large values on this axis), whereas the second principal axis reflected pH and phosphate concentrations (sites with high pH and high PO4 concentrations had large values on this axis). The first principal axis also was correlated with the latitude (r = 0.60), illustrating the well-known increase in nitrogen deposition rates at higher latitudes (Ollinger et al., 1993 ).


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Table 2. Results of the principal component analysis on the five soil chemistry variables. The first two principal axes accounted for 61% of the variance in the data. Values shown are the loadings of each variable on each of the first two axes

 
The first two principal axes of plant morphology accounted for 81% of the variation among sites (Table 3). The first principal axis reflected pitcher size differences (plants with tall and wide pitchers have high values for this axis). The second principal axis reflected differences in pitcher shape (plants with thin lips, narrow mouths, and large wings had large values on this axis).


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Table 3. Results of the principal component analysis on the site means of the six morphological variables measured for each plant. The first two principal axes accounted for 81% of the variance in the data. Values shown are the loadings of each variable on each of the first two axes

 
Predictors of site-specific morphology
The first set of analyses was conducted without regard to taxonomic identity. All composite and individual morphological variables were best predicted by climate variables. The second principal axis of climate (dominated by precipitation) was the best predictor of the two morphological principal axes and pitcher lip width (Fig. 2). In general, pitchers from wetter sites were larger (Fig. 2A) and had thicker lips (Fig. 2B, 2C). The length:mouth ratio was inversely related to temperature variables (the first principal axis of climate) (Fig. 3A). Tall pitchers with relatively narrow tubes were more common in warmer, southern sites while shorter, relatively stout pitchers predominated in cooler, northern sites. Relative wing width was marginally correlated only with the first principal axis of pore-water chemistry. Pitchers with relatively large wings occurred in sites with high concentrations of ammonium and calcium in the pore water (Fig. 3B). Neither bog type (vegetation PC-1) nor vegetation stature and composition (PC-2), a proxy for light availability, were correlated with any morphological character.



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Fig. 2. Relationship between climate and three measures of pitcher-plant morphology. In all cases, the predictor variable (x-axis) is the second principal axis of climate, which is dominated by precipitation (see Table 1 for all loadings). Symbols are as in Fig. 1 . The line is the best-fit linear regression. A. Pitcher size (the first morphological principal axis: see Table 3 for all loadings) as a function of climate. Slope = 0.22, r2 = 0.21, P = 0.049. B. Pitcher shape (the second morphological principal axis: see Table 3 for all loadings) as a function of climate. Slope = –0.40, r2 = 0.15, P = 0.019. C. Lip width alone of pitchers as a function of climate. Slope = 0.21, r2 = 0.20, P = 0.005

 


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Fig. 3. Relationship between derived measures of pitcher-plant morphology and environmental variables. A. The ratio of pitcher length to mouth diameter as a function of the first principal axis of climate (dominated by temperature: see Table 1 for all loadings). Slope = –0.29, r2 = 0.18, P = 0.02. B. The ratio of wing width to total pitcher width as a function of the first principal axis of pore-water chemistry (dominated by NH4 and calcium availability: see Table 2 for all loadings). Slope = 0.12, r2 = 0.09, P = 0.09. Symbols for both A and B as in Fig. 1

 
Differences among infraspecific taxa
The primary character that separated S. purpurea subsp. venosa var. burkii from both S. purpurea subsp. purpurea and S. purpurea subsp. venosa was the thickness of the pitcher lip (Fig. 2B, 2C; F2,36 = 5.39, P = 0.009, one-way ANOVA). Based on results of a priori contrasts, Sarracenia purpurea subsp. venosa var. burkii had significantly (P = 0.003) thicker lips ( = 3.0 ± 0.56 [SD] mm, range 2.3–3.8 mm) than did the two S. purpurea subspecies combined (2.2 ± 0.59, range 0.7–3.2 mm), but lip thickness did not differ (P = 0.19) between the two subspecies of S. purpurea (S. purpurea subsp. purpurea: 2.3 ± 0.56, range 1.2–2.8 mm; S. purpurea subsp. venosa excluding S. purpurea spp. venosa var. burkii: 1.9 ± 0.68, range 0.7–2.8 mm). The second principal axis of morphology, for which the loadings (Table 3) were dominated by lip thickness, pitcher mouth diameter, and wing width, also separated these taxa (Fig. 2B; F2,36 = 4.37, P = 0.02, one-way ANOVA). The results of the a priori contrasts on the second principal axis of morphology were identical to the contrasts on lip thickness alone. Sarracenia purpurea subsp. venosa var. burkii had significantly lower scores (P = 0.01) than the two other infraspecific taxa of S. purpurea for the second principal axis of morphology, and these morphological features did not differ between the two subspecies of S. purpurea (P = 0.08). None of the other morphological characters that we measured— pitcher length:mouth diameter ratio (Fig. 3A), relative wing width (Fig. 3B), or the first principal axis of morphology (Fig. 2A)—differed at all among the three taxa (F2,36 = 2.12, P = 0.13; F2,36 = 0.99, P = 0.38; F2,36 = 1.20, P = 0.31, one-way ANOVAs on the three variables, respectively), so we did not examine the contrasts between S. purpurea subsp. venosa var. burkii and S. purpurea or between the two subspecies of S. purpurea.

The inclusion of either or both of the principal axes of climate as covariates in the analysis of variance (i.e., an ANCOVA) on plant morphology does not alter our conclusions. Sarracenia purpurea subsp. venosa var. burkii still separates out from the two subspecies of S. purpurea (P = 0.004 for the a priori contrast), and the two subspecies of S. purpurea are not distinguishable (P = 0.86 for the a priori contrast).


    DISCUSSION
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS
 DISCUSSION
 LITERATURE CITED
 
Our results illustrate that morphological variation in S. purpurea is associated with environmental conditions, geography, and taxonomic identity. Morphology of the two subspecies of S. purpurea is correlated with environmental conditions. Both size and shape of pitchers of S. purpurea subsp. purpurea and S. purpurea subsp. venosa are primarily a function of precipitation (the dominant variable loading on the second principal axis of climate), which itself varies consistently with longitude. The primary morphometric ratio used to distinguish between the two subspecies (pitcher length:mouth diameter) co-varies with temperature (the dominant variable loading on the first principal axis of climate), which itself is strongly correlated with latitude.

There is some indication that available nutrients may also alter the amount of tissue in the pitcher wing relative to the width of the pitcher itself. Sites with high levels of ammonium and calcium tend to have plants with larger wings and narrower pitchers than do sites with lower levels of these nutrients, although most of the variation among sites remains unexplained. This pattern is consistent with the hypothesis of Givnish et al. (1984) that relative allocation of resources to carnivorous structures results from the "costliness" of producing carnivorous structures. Pitchers with relatively large wings are photosynthetically more efficient than those with relatively small wings (Ellison and Gotelli, 2002 ) and predominate when more nutrients are available.

Our data illustrate that there is no obvious way to distinguish these subspecies on morphological grounds alone, supporting Gleason and Cronquist's (1991) treatment of these subspecies as simple geographic varieties of S. purpurea. The two principal morphological characters used to distinguish S. purpurea subsp. purpurea from S. purpurea subsp. venosa, the ratio of pitcher length to mouth diameter and the thickness of the pitcher lip (Schnell, 2002 ), do not differ between northern and southern populations of S. purpurea. Because the two varieties co-occur in the mid-Atlantic states where their ranges overlap, introgression and hybridization are possible (Godt and Hamrick, 1999 ). Additional genetic analysis (e.g., DNA sequencing) and field investigations of hybridization between S. p. purpurea and S. p. venosa are needed to resolve their taxonomic status definitively.

Our data do clearly support the differentiation of S. purpurea subsp. venosa var. burkii from S. purpurea, however. Sarracenia purpurea subsp. venosa var. burkii differs not only in the morphological characters measured here, but also in pitcher and flower color (Naczi et al., 1999 ), height of the flower scape (Naczi et al., 1999 ), and seed size and germination characteristics (Ellison, 2001 ).

Overall, these conclusions are consistent with earlier results of allozyme analysis (Godt and Hamrick, 1999 ). Sarracenia purpurea subsp. venosa var. burkii is genetically quite distinct from the recognized infraspecific taxa of S. purpurea. Sarracenia purpurea subsp. venosa and S. p. purpurea are genetically similar, and the allozyme data, which suggest that S. purpurea subsp. venosa is derived relative to S. purpurea subsp. purpurea, are at odds with the geographic distribution, which suggests that S. purpurea subsp. purpurea is a postglacial derivative of S. purpurea subsp. venosa. Godt and Hamrick (1999) , also point out that the genetic grouping of S. purpurea subsp. venosa (and S. purpurea subsp. venosa var. montana) with S. purpurea subsp. purpurea is not consistent with a taxonomic system that places S. purpurea subsp. venosa var. burkii into S. purpurea subsp. venosa.

It could be argued that the observed differences between S. purpurea subsp. venosa var. burkii and S. purpurea simply reflect correlated habitat factors because the southern populations are in the warmest sites (Fig. 3A) and are intermediate in precipitation (Fig. 2A). However, including either or both of the principal axes of climate as covariates into an ANCOVA does not alter our conclusions. Sarracenia purpurea subsp. venosa var. burkii remains distinctive from S. purpurea, and the subspecies of S. purpurea are not separable morphologically. Overall, these results support the recognition of Sarracenia purpurea subsp. venosa var. burkii as the distinct species S. rosea (Naczi et al., 1999 ). Recognition of its status as a distinct species also would facilitate protection of the rare S. rosea (Godt and Hamrick, 1999 ). The comprehensive geographic analysis described herein is a useful tool for understanding morphometric variation and its information value for taxonomic studies.


    FOOTNOTES
 
1 The authors thank all the local and state officials who permitted our collecting; Jim Cuthbertson, Chris Oakley, and Sarah Yinger for assistance in the field; Shawn Havery for digitizing images; and Elizabeth Farnsworth and two anonymous reviewers for constructive critiques of the manuscript. This research was supported by grants DEB-0083617 to TEM, AME, and NJG, and DEB-0091776 to TEM from the U.S. National Science Foundation. Back

5 E-mail: aellison{at}fas.harvard.edu Back

6 Present address: Bioprotection and Ecology Division, P. O. Box 84, Lincoln University, Canterbury, New Zealand Back


    LITERATURE CITED
 TOP
 ABSTRACT
 INTRODUCTION
 MATERIALS AND METHODS
 RESULTS
 DISCUSSION
 LITERATURE CITED
 
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Bledzki L. A. A. M. Ellison 1998 Population growth and production of Habrotrocha rosa Donner (Rotifera: Bdelloidea) and its contribution to the nutrient supply of its host, the northern pitcher plant, Sarracenia purpurea L. (Sarraceniaceae). Hydrobiologia 385: 193-200[CrossRef][ISI]

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G. Ne'eman, R. Ne'eman, and A. M. Ellison
Limits to reproductive success of Sarracenia purpurea (Sarraceniaceae)
Am. J. Botany, November 1, 2006; 93(11): 1660 - 1666.
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