- freely available
Land 2013, 2(3), 328-350; doi:10.3390/land2030328
Published: 16 July 2013
Abstract: Agricultural expansion has eliminated a high proportion of native land cover and severely degraded remaining native vegetation. Managers must determine where degradation is severe enough to merit restoration action, and what action, if any, is necessary. We report on grassland degraded by multiple factors, including grazing, soil disturbance, and exotic plant species introduced in response to agriculture management. We use a multivariate method to categorize plant communities by degradation state based on floristic and biophysical degradation associated with historical land use. The variables we associate with degradation include abundance of the invasive cool-season grass, tall fescue (Schedonorus phoenix (Scop.) Holub); soil organic carbon (SOC); and heavy livestock grazing. Using a series of multivariate analyses (ordination, hierarchical clustering, and multiple regression), we identify patterns in plant community composition and describe floristic degradation states. We found vegetation states to be described largely by vegetation composition associated primarily with tall fescue and secondarily by severe grazing, but not soil organic carbon. Categorizing grasslands by vegetation states helps managers efficiently apply restoration inputs that optimize ecosystem response, so we discuss potential restoration pathways in a state-and-transition model. Reducing stocking rate on grassland where grazing is actively practiced is an important first step that might be sufficient for restoring grassland with high native species richness and minimal degradation from invasive plants. More severe degradation likely requires multiple approaches to reverse degradation. Of these, we recommend restoration of ecological processes and disturbance regimes such as fire and grazing. We suggest old-field grasslands in North America, which are similar to European semi-natural grassland in composition and function, deserve more attention by conservation biologists.
Anthropogenic impacts have been documented across more than three-quarters of the Earth’s ice-free terrestrial surface [1,2], and the global intensification of land use threatens biodiversity in human-impacted areas [3,4]. Multifunctional landscapes comprised of natural and semi-natural ecosystems set in the context of intensive land use can address multiple goals of production and conservation [5,6,7], but severe degradation can overcome ecosystem resilience and reduce ecosystem stability and function through catastrophic state shifts .
In degraded environments, conservation of native biodiversity and restoration of ecosystem function often requires some degree of ecosystem restoration to a less-degraded state. As such, managers must often determine the causes of ecological degradation before proceeding with restoration. When degradation factors are clear and controllable, restoration can be managed agronomically and proceeds linearly towards a restoration objective, such as pre-settlement conditions . For example, restoring native grassland from cropland agriculture typically involves managing for maximal native species diversity and minimal non-native species by planting a diverse mix of native species and removing exotic species [10,11].
Restoration of intensively cultivated areas is fairly straightforward, but the best course of restoration action for sites degraded by multiple factors can be elusive. Specific sources of degradation might not be readily identifiable because they result from multiple causative factors that vary spatially and temporally, and the response to restoration might be non-linear and unpredictable [12,13,14]. Land-use history, recent disturbance, and invasive species create legacies with long-term impacts on plant community composition that strongly resist change toward the desired restoration outcome [12,15,16]. Restoration and conservation under such conditions require an ecological approach using the initial extent of floristic degradation to identify appropriate restoration action and outcomes [9,17].
We construct vegetation states to describe floristic degradation in nine old-field grassland tracts in south-central Iowa and north-central Missouri, USA. This study was prompted by a clear need to identify patterns of floristic degradation that influence other taxa in these grasslands [18,19,20]. We use multivariate analyses to categorize floristic degradation into vegetation states with plant species data, a common approach in rangelands worldwide [21,22,23]. We also use soil organic carbon (SOC) as an indicator of biophysical degradation because both cultivation and severe grazing have been shown to reduce SOC content .
We report the relationship between native and exotic plant species abundance, grazing history, and a regionally-ubiquitous invasive plant species, the Eurasian, cool-season grass, tall fescue (Schedonorus phoenix (Scop.) Holub). Tall fescue is one of the most economically-important grasses in eastern North America since its introduction in the 1940’s , but tall fescue has since been shown to reduce native plant species richness, fire spread, and habitat quality in grassland [26,27,28,29,30].
We predicted that patterns of plant community composition (i.e., vegetation states) correspond to patterns in three factors of degradation: tall fescue abundance, grazing history and soil organic carbon. To inform restoration action, we use a state-and-transition framework [31,32] to discuss potential degradation and restoration pathways with respect to conservation in working grassland landscapes.
2. Experimental Section
2.1. Study Area
2.1.1. Environment and Soils
Our study was located in a 30,000 ha tallgrass prairie ecosystem spanning Ringgold County, Iowa, and Harrison County, Missouri, USA known as the Grand River Grasslands. Long-term mean annual rainfall is 91 cm; mean January and July temperatures are −6 °C and 24 °C, respectively . Soils of the study area belong to the Gara-Armstrong-Pershing association, which the Soil Survey of Ringgold County, IA (; p. 10) describes as “gently sloping to steep, well drained to somewhat poorly drained, loamy and silty soils formed in glacial till, a paleosol derived from glacial till, and loess; on uplands and stream benches.” Tracts were dominated by two soil types, Gara loam (Fine-loamy, mixed, superactive, mesic Mollic Hapludalfs) and Armstrong loam (fine, smectitic, mesic Aquertic Hapludalfs), with slopes ranging from 9 to 25 percent and 5 to 14 percent, respectively .
2.1.2. Current and Historical Land Use
The Grand River Grasslands have been identified as the best known opportunity to restore a functional tallgrass prairie system in the Central Tallgrass Prairie ecoregion of North America, but only 11% of the GRG is in some form of conservation reserve (The Nature Conservancy, unpublished data). The Grand River Grasslands are a working landscape in which researchers work to reconcile multiple functions including agricultural production, ecosystem function, and biodiversity conservation .
We selected nine grassland tracts (15–31 ha) identified by The Nature Conservancy as moderate to high in conservation value, based on the presence of clusters of native prairie species (The Nature Conservancy, unpublished data). Although the conservation value was assigned at the tract level, evidence suggested that land-use history—and thus floristic and biophysical condition—might vary within each tract as well as between tracts. For example, each tract was clearly in a perennial grassland state, but composition appeared to vary in the relative dominance of native and exotic species . Furthermore, the sources of exotic plants are unknown, e.g., whether species were intentionally sown, either at the tract or landscape scales, and if not, at what spatial and temporal scales encroachment occurred. As such, we expected to observe a range of degradation within tracts and among tracts.
Grazing history was determined by interviewing current and previous landowners and managers who reported that four tracts were grazed by cattle during the growing season (May through October) at stocking rates up to 15 animal unit months/ha within five years prior to our study. We applied the category “historically severely grazed” to these four sites, and the category “historically ungrazed” to the remaining five sites . We also queried previous landowners and managers about cultivation history and reviewed available aerial imagery of the tracts beginning in the 1930s and extending through the study period. Although no evidence of cultivation was reported or observed, we cannot rule out that some areas of some tracts were farmed for brief periods following European settlement.
We established six permanent modified Whittaker plots  per tract to sample presence and abundance of vascular plant species. Plot locations were selected at random within each of the two most dominant soil types (three plots on each soil type) via GIS to control for catena and distance from edges to ensure similar landscape position and minimal edge effects among plots across all tracts. All tracts were relatively high on the landscape.
Within modified Whittaker plots, sampling occurred at four different scales: 0.5 m2, 2.5 m2, 250 m2, and 500 m2. Abundance (canopy cover of individual species) was sampled within 10 0.5-m2 quadrats, indexed by the Daubenmire  canopy cover index. Sedges (Cyperaceae) were identified to family. In plots larger than 0.5 m2, only species presence was recorded. For purposes of analyses, species found outside of the 10 quadrats but within the 500 m2 plot were assigned a cover value of 0.01. Sampling occurred twice during the growing season—once in late May-early June and again in August 2006—to account for plant growth and senescence and therefore community change through the growing season. The maximum canopy cover value of each species across both sampling periods was used in analyses.
To measure soil degradation within the modified Whittaker plots, we use soil organic carbon (SOC) depletion because SOC declines with cultivation and similarly-intense disturbances (e.g., severe grazing) that substantially disturb the vegetation matrix and soil [24,41,42,43]. Each modified Whittaker plot was represented by a composite soil sample created by combining four 15-cm cores taken from each corner of the 500-m2 plot. Samples were analyzed for pH (soil slurry method) and total carbon by volume (loss on ignition method). Correction for inorganic carbon content was unnecessary because pH of all samples was ≤7.0. To contextualize our soil organic carbon data, we compared our SOC values to regional data taken from cultivated fields of the same soil types available online from the National Cooperative Soil Survey .
2.3. Data Analysis
2.3.1. Patterns of Degradation
We associated plant community composition with potential sources of degradation—SOC, grazing history, and invasive species—using the ordination technique Non-metric Multidimensional Scaling (NMDS) . We chose the Canberra distance measure for our NMDS distance matrix, which ranges from zero (identical community composition) to one (complete dissimilarity) for its sensitivity to rare species . We also used the Canberra distance matrix to calculate community dissimilarity among individual plots, tracts, and tracts grouped by historical grazing severity. These analyses were performed with the metaMDS and vegdist functions, respectively, in the VEGAN package for program R [47,48,49]. To minimize stress, the NMDS was projected in k = 4 dimensions.
Because it is a degradation factor in this study, tall fescue was excluded from the plant community data used in the NMDS. We plotted a smooth surface over the first two dimensions of the NMDS projection  to evaluate the association between tall fescue canopy cover and variation in plant community composition. We also calculated the correlation between the ordination and measures of plant community composition (total species richness, exotic and native species abundance, and proportion of native species richness) and compared these richness and abundance data across the historically severely grazed and ungrazed subgroups via Student’s t-tests assuming unequal variance.
2.3.2. Sources of Degradation
We tested the effect of degradation factors on plant community composition with a full-interaction, Multivariate Analysis of Variance (MANOVA) model with the manova function in R, after determining no collinearity existed among the predictor variables. Tall fescue canopy cover, SOC, and grazing history were predictor variables, and scores for all four NMDS axes were used as co-dependent response variables (e.g., ). The model ranked independent variables in terms of their relative importance to the model with F statistics approximated by Wilks’ lambda.
2.3.3. Vegetation States
To group plant composition data from modified Whittaker plots, we used hierarchical clustering of the full plant community dataset, including tall fescue. Hierarchical clustering (R function hclust) calculated dissimilarity in plant community composition based on the Canberra distance matrix, from which four groups were discernibly distinct using the R function cutree. Post-hoc analysis indicated that plant communities of two of the four groups identified by the cutree function were similar in abundance of tall fescue, native species richness, total species richness, or proportion native species cover in pair-wise student’s t-tests (p > 0.10). Therefore, we consolidated these two groups into a single vegetation state for subsequent analyses (Appendix Figure A1).
To determine distinctiveness of the three vegetation states in terms of plant community composition, we tested for dissimilarity in plant community composition among vegetation states with the adonis function in the VEGAN package . We also identified the degradation factors and plant community variables that were associated with differences among vegetation states. We began by fitting a linear mixed-effect regression model (LME) in which vegetation state was tested as a response variable against the following predictor variables: tall fescue abundance, grazing history, proportion native species abundance, and Simpson’s diversity (1/D). We accomplished this with the lme function in the nlme package for program R . We then used the stepwise model selection function stepAIC in R to identify variables associated with vegetation state. The stepAIC function removes and re-combines predictor variables from the initial LME model and returns the model with the lowest Akaike’s An Information Criterion (AIC); the minimal AIC value indicates the most parsimonious model likely to best explain variation in the response variable . Finally, to confirm the unique identity of the three plant communities from each other (i.e., the states), we compared the three states for tall fescue abundance, native species richness, total species richness, proportion native species cover and Simpson’s diversity index (1/D) with pair-wise student’s t-tests.
3.1. Pattern of Vegetation Degradation
The nine study tracts contained diverse assemblages of both native and exotic species, but tall fescue was the most frequently-occurring and most abundant plant on most tracts. Only Kentucky bluegrass (Poa pratensis L.) was observed more frequently (49 vs. 43 out of 54 Whittaker plots, respectively), but mean canopy cover of Kentucky bluegrass was less than that of tall fescue (12% ± 2% s.e. vs. 38% ± 3% s.e., respectively). All Whittaker plots contained exotic species, although several were dominated by native species (Table 1). We observed 196 species across 51 dicot families and 3 grass subfamilies, in addition to sedges. We observed 129 flowering herbaceous (forb) species, 14 legumes, 18 warm-season grasses, 18 woody species, and 14 cool-season grasses. Seventy-one percent of the species were native.
|Table 1. Ten most abundant species (percent of total canopy cover) within each of three vegetation degradation states identified by hierarchical clustering of 196 plant species abundance sampled from nine tracts in the Grand River Grasslands of south-central Iowa and north-central Missouri, USA.|
|Vegetation Degradation State||Scientific Name||Common Name||Status||Mean Relative Abundance (%) ±95% CI|
|High||Schedonorus phoenix||Tall fescue||Exotic||41 ± 5|
|Poa pratensis||Kentucky bluegrass||Exotic||20 ± 5|
|Bromus inermis||Smooth brome||Exotic||11 ± 6|
|Veronia baldwinii||Baldwin’s ironweed||Native||6 ± 4|
|Setaria pumila||Yellow foxtail||Exotic||3 ± 4|
|Solanum carolinense||Horse nettle||Native||2 ± 2|
|Daucus carota||Wild carrot||Exotic||2± 1|
|Dactylis glomerata||Orchardgrass||Exotic||2± 1|
|Medicago lupulina||Black medic||Exotic||1± 1|
|Solidago canadensis||Tall goldenrod||Native||1± 1|
|N = 3, E = 7||Sum = 89|
|Moderate||Schedonorus phoenix||Tall fescue||Exotic||30 ± 4|
|Medicago lupulina||Black medic||Exotic||14 ± 4|
|Sporobolus clandestinus||Rough dropseed||Native||12 ± 3|
|Kummerowia striata||Japanese clover||Exotic||7 ± 4|
|Poa pratensis||Kentucky bluegrass||Exotic||6 ± 2|
|Aristida oligantha||Prairie threeawn||Native||5 ± 3|
|Lotus corniculatus||Birdsfoot trefoil||Exotic||4 ± 4|
|Daucus carota||Wild carrot||Exotic||3 ± 1|
|Dichanthelium oligosanthes||Scribner’s rosette grass||Native||2 ± 1|
|Phleum pratense||Timothy||Exotic||2 ± 1|
|N = 3, E = 7||Sum = 83|
|Low||Sorghastrum nutans||Indiangrass||Native||11 ± 6|
|Schedonorus phoenix||Tall fescue||Exotic||9 ± 5|
|Cyperaceae||Sedges||Native||9 ± 2|
|Andropogon gerardii||Big bluestem||Native||9 ± 5|
|Sporobolus clandestinus||Rough dropseed||Native||7 ± 2|
|Lotus corniculatus||Birdsfoot trefoil||Exotic||6 ± 4|
|Poa pratensis||Kentucky bluegrass||Exotic||6 ± 2|
|Solidago canadensis||Tall goldenrod||Native||6 ± 4|
|Symphoricarpos orbiculatus||Coralberry||Native||4 ± 3|
|Schizachyrium scoparium||Little bluestem||Native||4 ± 3|
|N = 7, E = 3||Sum = 71|
Floristic composition oriented along a gradient of tall fescue abundance, and severely grazed tracts separated from ungrazed tracts in the ordination (Figure 1). Mean plot-level Canberra distance of 0.83 (±0.01) in the NMDS indicates that species composition varied greatly among Whittaker plots, but Whittaker plots generally clustered by tract (F = 7.07, p < 0.01, R2 = 0.56) and grazing history (F = 11.35, p < 0.01, R2 = 0.18) (Figure 1). Tracts and Whittaker plots scoring to the right of the ordination plot (Figure 1) had both greater native species richness (R2 = 0.52, p < 0.001) and a larger proportion of native species canopy cover (R2 = 0.78, p < 0.001) relative to plots scoring to the left. The pattern of plant community composition in the ordination had no association with differences in soil type or slope classification (data not shown).
|Table 2. Results of a Multivariate Analysis of Variance (MANOVA) model comparing tall fescue canopy cover, soil organic carbon, and grazing history effects on the position of modified Whittaker plot communities in ordination space (NMDS Axis 1 and Axis 2 site scores; see Figure 1) for nine grassland tracts in the Grand River Grasslands of southern Iowa and northern Missouri, USA. F statistics, approximated from Wilks’ lamba, rank the importance of model terms in explaining site scores. Boldface indicates significant terms in the MANOVA model.|
|MANOVA Model Terms||Wilks’ Approx. F||P|
|Tall fescue canopy cover (TF)||50.16||<0.001|
|Severe grazing history (Gr)||31.56||<0.001|
|Soil Organic carbon (SOC)||12.90||<0.001|
|TF × SOC||2.24||0.08|
|SOC × Gr||2.08||0.25|
|TF × SOC × Gr||1.43||0.24|
|TF × Gr||1.41||0.25|
3.2. Sources of Degradation
Tall fescue canopy cover was the most important variable in the MANOVA model of plant community degradation, followed by severe grazing history and SOC (Table 2). The composite variables generated by NMDS describe variation in plant community composition (Figure 1) along a gradient of tall fescue abundance (Figure 2A), grazing history and, to a lesser extent, a gradient of SOC (Figure 2B).
Portions of some tracts might have been cultivated at some time in the past based on SOC (i.e., SOC of about 2.5% or less) (Figure 2B), but SOC in these tracts was generally greater than SOC in cultivated fields of the same soil types (Figure 3). SOC ranged from a low of 1.8%, equivalent to the mean SOC of cultivated soil in similar soils in this region , in a Whittaker plot at Ringgold North to a high of 3.9%, indicating no cultivation, in a Whittaker plot at Gilleland (Figure 3). Mean SOC at the tract level ranged from 2.2% (±0.1) in Ringgold North to 3.3% (±0.2) in Pawnee.
3.3. Degradation States
Three states of vegetation degradation differed in plant community composition in the analysis of dissimilarity (p = 0.03), and showed no overlap when superimposed over the original NMDS ordination (Figure 4). Because of the strong relationships between native species richness and tall fescue abundance in the pattern of degradation, we categorize the three states (hereafter, degradation states) as low, moderate, and high degradation (Table 1). Although each biotic factor varied significantly across the degradation states, soil organic carbon did not vary with degradation (Figure 5). There were also several instances of outliers (Figure 5).
The linear mixed-effect model returned by stepwise AIC model selection included the following variables: tall fescue abundance (t = 2.01, p = 0.05), native species richness (t = 2.06, p < 0.05), and Simpson’s diversity (t = 2.87, p < 0.01). Neither proportion native species abundance, total species richness, nor soil organic carbon was included in the most parsimonious model. However, each varied significantly across the three vegetation states, along with native species richness (Figure 5). Tall fescue abundance did not differ between the high and moderate states, but tall fescue abundance in the low degradation state was significantly lower than the other two states (Figure 5). Conversely, diversity (1/Simpson’s D) was similar between the moderate and low states of degradation, but was significantly lower in the high degradation state (Figure 5).
As predicted, patterns of plant species richness and abundance clearly segment into three degradation states (Figure 4), which correspond with patterns of two primary degradation factors in these grasslands—tall fescue abundance and a history of severe grazing (Figure 1). While SOC varied substantially across sampled plots (Figure 2B) (Table 2), there was no association between SOC and floristic degradation states (Figure 5). Tall fescue abundance, total and native species richness, proportion native species abundance, and plant species diversity all varied across degradation states (Figure 5).
We use a state-and-transition model (Figure 6) to describe hypothetical degradation and restoration pathways among three states of vegetation degradation in the Grand River Grasslands. Potential pathways, when validated by research or practice, target restoration action and inform restoration goals for management of degraded grassland based on the baseline floristic conditions our results describe.
4.1. Degradation Pattern and Pathways
Our multivariate approach effectively described patterns of vegetation degradation and categorized abundance data from 196 plant species into three distinct vegetation states. As with other applications in which multivariate analyses were used to assess rangeland condition (e.g., ), we identified a single species—tall fescue—that described a gradient of vegetation degradation. However, tall fescue abundance alone was not the sole factor that distinguishes degradation states: vegetation degradation was characterized by inverse relationships between richness and abundance of native and exotic species along the gradient of tall fescue invasion (Figure 6). The importance of multiple variables in describing degradation state likely explains variation around the mean values of degradation factors when plotted individually (see whiskers and outliers in Figure 5). These plant communities might also be in transition between states, and further research will determine whether they are following degradation or restoration pathways (Figure 6).
These results support a pattern in which native species richness has a stronger negative association with tall fescue abundance than with grazing history, and other exotic species increase with tall fescue abundance . In fact, species abundance data emphasize the pattern shown by species richness: Tall fescue abundance had a stronger negative correlation with proportional abundance of native plants than with native species richness (Figure 1).
A history of severe grazing was associated with the pattern of plant community composition (Figure 1). Generally, light to moderate herbivory maintains native plant species richness in grassland [53,54]. While severe grazing can degrade plant communities , native species richness in the Grand River Grasslands did not decline under severe grazing . It appears that grazing history has a greater effect on species abundance than species presence, and grazing might be associated with variation in community composition within vegetation states (Figure 4).
It is clear that grazing affects the pattern of plant community composition but might not have the long-lasting legacy as tall fescue invasion. Severe grazing might be a potential contributor to degradation between the low and moderate degradation states (D.1), but likely has less of a direct influence on other degradation pathways (D.2 and D.3) (Figure 6). Of unknown relevance is the fact that grazing history is documented here at the tract level, and plant community composition at the modified Whittaker plot level (within tracts).
4.2. Managing Pathways between States for Restoration
The literature lacks clear insight into restoration pathways for grassland impacted by both severe grazing and tall fescue invasion, so we offer several hypotheses for restoration to states less degraded by tall fescue. Where heavy grazing is the primary degradation factor, restoration might consist initially of allowing severely grazed tracts to recover from the biotic legacy of overgrazing , although highly-degraded vegetation might not respond to grazing cessation alone . Response time of native vegetation to reduced grazing can vary between several years to several decades depending on level of degradation and ecosystem productivity [57,58,59]. In the Grand River Grasslands, native species abundance might increase following grazing cessation , but we hypothesize that relative response to grazing cessation decreases as the severity of degradation increases (pathways R.1, R.2, and R.3, respectively) (Figure 6). Invasive plant species—tall fescue, specifically—are the primary factor of degradation in the Grand River Grasslands. Prescribed fire is often used to control invasive plant species , but fire alone might be limited to R.1 and maintaining the low degradation state (Figure 6) if native plant abundance is too low to outcompete exotics following fire. For example, prescribed fire alone is ineffective against tall fescue when it occurs in high abundance .
Combining ecological disturbances might be more effective than singular management practices. Patch burn-grazing (heterogeneity-based management), in which grazing activity is concentrated within spatially-discrete burned patches, is an effective combination of disturbances with other difficult-to-control invasive plants , and with time, might contribute to restoration pathways R.2 and R.3. However, directly restoring highly-degraded grassland to prairie (R.3) within a narrow time frame likely depends upon herbicide treatment  and/or reseeding native plants and then managing with fire and grazing .
Ultimately, grazing management probably mediates the success of restoring ecosystem processes to restore plant communities (e.g., restoration pathways R.1 and R.2). Heterogeneity-based rangeland management can be stymied by low fuel load and patchy fuel distributions that often occur in overgrazed grassland [64,65]. Tall fescue, specifically, can further complicate patch burn-grazing management by disrupting fire spread, an effect that is exacerbated by fuelbed conditions that follow severe grazing [29,30].
A final consideration is the pattern of soil degradation, and the effect of soil on vegetation restoration response. Many state-and-transition models also consider the soil base  because plant-soil interactions can be important in describing degradation . For example, tillage of prairie reduces soil organic carbon and recovery can take several years or decades ; thus historical cultivation of these grasslands likely affects degradation and restoration. However, cultivation history remains unknown (Figure 3), and our soil organic carbon data is inconclusive with respect to the pattern of floristic degradation. We suggest further research into soil condition and plant-soil interactions in these and similar grasslands, both to infer cultivation history and inform management.
4.3. Biodiversity Conservation in Working Grassland Landscapes
In North America, the conservation value of human-impacted ecosystems might be under-rated by the assumption that long-term conservation value is contingent on the reversal of temporary degradation factors , such as the extirpation of exotic species from grassland. However, undisturbed vegetation states within high quality natural grasslands are not the only plant communities that contribute to grassland conservation. In Europe, scientists and managers distinguish semi-natural grassland as a unique land-use and highlight its role in biodiversity conservation, particularly in agricultural areas [69,70,71]. Semi-natural grasslands reflect the adaptation of wild flora and fauna to centuries of relatively low-intensity land use that created ecosystems distinct from natural communities [69,72,73]. Even when semi-natural areas provide only sub-optimal habitat, they connect otherwise isolated patches of high-quality habitat across the landscape matrix .
The old-field plant communities described here resemble European semi-natural grassland in composition, function, and possibly conservation value. For example, the suite of exotic plants in the Grand River Grasslands includes several species and many functionally-similar congenerics found in European semi-natural grasslands [75,76,77]. In the Grand River Grasslands, avian and invertebrate communities within and among tracts overlap considerably [18,20,78] and some species respond to ecological management despite degradation by invasive plants and severe grazing . These patterns suggest that each grassland state contributes to biodiversity conservation at the landscape level, which is consistent with countryside biogeography theory . We encourage further research to develop the concept of semi-natural grassland as a functional term in the mosaic of North American working landscapes.
Whether in Europe or North America, semi-natural grasslands merit attention to their potential conservation value before—and perhaps even without—costly restoration inputs. Plant communities comprised of exotic and native species might constitute novel ecosystems without natural analogy that none-the-less can contribute to the conservation of biodiversity and the restoration of ecosystem services . In degraded North American rangeland, managers should focus on restoration of pattern and process, such as a mosaic of spatially-variable and temporally-variable disturbance regimes and essential habitat structure [80,81].
Restoring degraded rangeland is not always straightforward. Multivariate analysis is effective in reducing multi-dimensional data—such as species-level plant community datasets—into categorical groups useful to determine the extent of floristic degradation and inform management decisions when degradation results from multiple causative factors. We show how free-to-download, open-source software can help managers make sense of multi-species data to identify patterns of floristic degradation and predict restoration action. Step-by-step guides to these methods, written by plant ecologists, are available [47,82].
Managers of human-impacted rangeland should recognize its potential conservation value before—and perhaps even without—costly restoration inputs. Plant communities comprised of exotic and native species might constitute novel ecosystems without natural analogy that none-the-less contribute to biodiversity conservation and provision of ecosystem services . In degraded North American rangeland, managers should focus on the restoration of pattern and process, such as a mosaic of spatially-variable and temporally-variable disturbance regimes and essential habitat structure [80,81].
This work was supported by the Iowa Agriculture and Home Economics Experiment Station, the Oklahoma Agricultural Experiment Station, the Iowa State Wildlife Grants program with the U.S. Fish and Wildlife Service Wildlife and Sport Fish Restoration Program (#T-1-R-15); USDA Cooperative State Research, Education and Extension Service’s National Research Initiative (#2006-35320-17476); and the Leopold Center for Sustainable Agriculture. We thank R. Harr, S. Rusk, and D. Farnsworth for data collection and other help; and P. Dixon, D. Cook and D. Adams for statistical advice. The manuscript was improved by the comments of three anonymous reviewers.
Conflict of Interest
The authors declare no conflict of interest.
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|Table A1. Attributes for 54 modified Whittaker plot plant communities used in hierarchical clustering (Figure A1) based on 196 plant species abundance sampled from nine tracts in the Grand River Grasslands of south-central Iowa and north-central Missouri, USA. Plot code represents nomenclature used in Figure A1: “Pasture.Patch.Plot” uses an abbreviation of the pasture name and the first letter of cardinal directions to locate each plot nested within patches . Pasture names correspond with NMDS ordination in Figure 1A of the main text. Native species richness, total species richness, Proportion native abundance, and Simpson’s diversity (1/D) are summarized in Figure 5 in the main text.|
|Plot Code||Tract||Grazing History||Floristic Degradation State||Native Species Richness||Total Species Richness||Proportion Native Abundance||Simpson’s Diversity (1/D)|
|LT. C.S||Lee Trail||Ungrazed||Medium||28||34||0.80||6.02|
|PyN.N.N||Pyland North||Severely grazed||High||12||29||0.02||3.44|
|PyN.N.S||Pyland North||Severely grazed||High||26||43||0.31||4.8|
|PyN.S.N||Pyland North||Severely grazed||Low||21||39||0.22||9.69|
|PyN.S.S||Pyland North||Severely grazed||Low||36||54||0.28||4.52|
|PyN.W.N||Pyland North||Severely grazed||Low||28||47||0.12||7.18|
|PyN.W.S||Pyland North||Severely grazed||Low||26||46||0.37||6.35|
|PyS.N.N||Pyland South||Severely grazed||Low||35||49||0.41||4.98|
|PyS.N.S||Pyland South||Severely grazed||Low||33||53||0.45||7.99|
|PyS.S.N||Pyland South||Severely grazed||Low||33||50||0.31||5.88|
|PyS.S.S||Pyland South||Severely grazed||Low||29||48||0.13||4.62|
|PyS.W.N||Pyland South||Severely grazed||Low||32||48||0.52||7.06|
|PyS.W.S||Pyland South||Severely grazed||Low||25||42||0.22||3.71|
|PyW.C.N||Pyland West||Severely grazed||Low||23||37||0.14||4.48|
|PyW.C.S||Pyland West||Severely grazed||Medium||30||47||0.29||3.42|
|PyW.N.N||Pyland West||Severely grazed||Medium||27||47||0.2||5.61|
|PyW.N.S||Pyland West||Severely grazed||Medium||31||48||0.16||3.92|
|PyW.S.N||Pyland West||Severely grazed||Medium||24||39||0.33||6.8|
|PyW.S.S||Pyland West||Severely grazed||Medium||30||47||0.52||4.96|
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