Introduction

The Carex flava complex belongs to one of the most taxonomically difficult groups because of a lack of clear morphological discontinuities (e.g. Havlíčková 1982; Crins and Ball 1989a,b; Pykälä and Toivonen 1994; Jiménez-Mejías et al. 2012) and the presence of numerous hybrids (Schmid 1982; Więcław and Koopman 2013; Więcław and Wilhelm 2014). The Carex flava complex in Europe is considered consisting of six species (Więcław 2017). These taxa are usually small in size and have short rhizomes; they usually have a solitary subcylindrical male spike on top of the inflorescence, above globose to oblong female spikes with more or less inflated, ovoid-ellipsoid utricles with a distinct bifid beak (Chater 1980). In Poland, the C. flava group contains four taxa: C. flava, C. lepidocarpa subsp. lepidocarpa, C. demissa subsp. demissa and C. viridula var. viridula (Więcław 2014a). Carex viridula var. pulchella, identified earlier in Poland by Zając (1968), is most likely part of the continuum of variation within var. viridula resulting from effects of local habitat conditions (Więcław 2017). The most important for the identification of taxa of the C. flava group are generative characters, particularly dimensions of the utricle and beak, from the longest in C. flava via C. lepidocarpa and C. demissa to the shortest in C. viridula, as well as the beak length/utricle length ratio, the diminishing order of which starts with C. flava to proceed via C. demissa, C. lepidocarpa to C. viridula (e.g. Pykälä and Toivonen 1994; Więcław 2014a). In addition, two or more taxa of the C. flava aggregate may share a site; such mixed populations frequently contain hybrids (e.g. Więcław and Wilhelm 2014; Schmidt et al. 2018).

Carex flava and C. viridula are frequent in Poland, whereas C. lepidocarpa is relatively rare. Carex demissa is found scattered across the country, mostly in the south (Więcław 2014b). The relatively most common hybrids are C. ×alsatica [C. demissa × C. flava] and C. ×subviridula [C. flava × C. viridula]. In Poland, the taxa from the C. flava group usually grow in fens, wet meadows, along lake, sea and pond shores, along ditches, roadsides, in pastures, along streams and rivers, and less frequently in forests (Więcław 2014b). They colonize diverse substrates, from organic to sandy and from acidic to alkaline, usually humid and moist (e.g. Davies 1956; Schmid 1984; Crins and Ball 1989b). Sedges of the C. flava complex can grow in different plant assemblages, usually representing the classes Scheuchzerio palustris-Caricetea fuscae, Isoëto-Nanojuncetea, Littorelletea uniflorae, Molinio-Arrhenatheretea, Phragmito-Magnocaricetea and Alnetea glutinosae (e.g. Hájková et al. 2010; Hájek and Hájková 2011; Šumberová 2011; Šumberová and Hrivnak 2013; Vončina 2017). For example, C. flava and C. lepidocarpa are regarded as species typical of communities included in the Caricion davallianae, for example Caricetum paniceo-lepidocarpae (Kwiatkowski 1999), Carici flavae-Blysmetum compressi, Carici flavae-Eriophoretum latifolii (Zamfirescu and Zamfirescu 2006), Valeriano simplicifoliae-Caricetum flavae (Pawłowski et al. 1960; Hájek 1999; Hájek and Hájková 2002; Hájek et al. 2005) and Carici flavae-Cratoneuretum (Hájek et al. 2005). On the other hand, because of the morphological similarity of the sedges and difficulties in their identification, some phytosociological publications treat them as a broadly-defined aggregate; for example, Jarolímek and Šibík (2008) mentioned Carex flava agg. as diagnostic for the class Scheuchzerio palustris-Caricetea fuscae and the alliance Caricion davallianae (see also Hájek 2002; Peterka et al. 2017). Moreover, most phytosociological and ecological studies were focused on C. flava and C. lepidocarpa, and less so on C. demissa and C. viridula (e.g. Hájek 1999, 2002; Hájek and Hájková 2002). In addition, closely related species which are poorly morphologically differentiated can be easily overlooked or the differences observed may be regarded as a manifestation of habitat-dependent variation. Therefore, this study was aimed at identifying types of plant assemblages capable of supporting species of the C. flava complex and at determining relationships between soil properties and species composition and diversity of vegetation with C. flava agg.

The results presented are part of a comprehensive study on the taxa of the C. flava complex in Poland, with a particular reference to inter- and intra-specific differentiation, taxonomy and hybridisation within the group (Więcław and Podlasiński 2013; Więcław and Koopman 2013; Więcław and Wilhelm 2014; Więcław 2014a,b, Więcław 2017).

Material and methods

Field sampling

Field data were collected in 2012–2014 in Poland from various habitats, for example from upland and lowland, coastal and inland, from calcareous, extremely and moderate-rich fens and wet grasslands to poor habitats such as dunes and sandy lake shores (Fig. 1; Online Resource 1). A total of 129 plots were sampled in patches with the presence of species from C. flava agg., specifically 16 with C. demissa subsp. demissa, 57 with C. flava s.str., 19 with C. lepidocarpa subsp. lepidocarpa and 37 with C. viridula var. viridula. The sedges were identified using the keys of Pykälä and Toivonen (1994) and Więcław (2014a).

Fig. 1
figure 1

Locations of Carex flava agg. sampling sites. 1, 2, 3, 4 . . . – number of relevé; relevés 1, 3, 5–15, 21, 26, 28–36, 38–47, 55–58 – samples with C. flava from fens and wet grasslands without Valeriana dioica subsp. simplicifolia (cluster VII); relevés 2, 4, 16, 27, 37 – samples with C. flava from Alnus forest (cluster VIII); relevés 17–20, 22–25, 48–51, 53, 54 – samples with C. flava from fens and wet grasslands with Valeriana dioica subsp. simplicifolia from the Bieszczady Mts (cluster VI); relevés 52, 66, 68–72 – samples with C. demissa from poor acidic fens (cluster Va); relevés 59, 60–65, 67, 73 – samples with C. demissa from moderate-rich fens and fen grasslands (cluster Vb); relevés 74–92 – samples with C. lepidocarpa (cluster I); relevés 106–109 and 119–129 – samples with C. viridula from fens and wet grasslands (cluster II); relevés 93–105 – samples with C. viridula from sandy lake shores (cluster IIIa), relevés 110, 112–114 – samples with C. viridula from sites near a chalk mine (cluster IIIb), relevés 111, 115–118 – samples with C. viridula from dunes (cluster IV).

The area of vegetation plots was in the range of 10–30 m2. The species cover in each plot was estimated using a nine-grade scale (van der Maarel 1979). All the vascular plant and bryophyte species were recorded and their respective cover-abundances were coded as follows: 1 (one or a few individuals); 2 (rare and less than 1% cover); 3 (less than 5% cover; several specimens); 4 (less than 5% cover; abundant); 5 (5–12.5% cover); 6 (12.5–25% cover); 7 (25–50% cover); 8 (50–75% cover); 9 (75–100% cover). At each plot, three soil samples were collected with an Egner's soil sampler from the plant root zone (0–25 cm). The three samples were combined to form a single soil sample, representing a given plot and used for chemical analyses.

Soil analysis

Soil samples were dried at room temperature, and then rubbed through a sieve to remove fractions larger than 1 mm. The following properties were determined in the thus-prepared material: organic matter content (as loss on ignition at 550°C), pH (potentiometrically in 1 M KCl), contents of assimilable nutrients (phosphorus P, potassium K, magnesium Mg and calcium Ca, using the American Society of Agronomy method; Sparks et al. 1996), carbonates (Scheibler’s method; Tatzber et al. 2007) and total carbon C and nitrogen N (CHNS analyser, Costech Analytical Technologies Inc.; Sparks et al. 1996). The latter assay provides data for calculating the C/N ratio. The ratio between organic carbon and nitrogen (C/N) is one of the indicators of soil fertility. The lower the ratio, the more fertile the soil.

Data processing

Two multivariate statistical techniques were used to analyse the vegetation data: the two-way indicator species analysis (TWINSPAN package, v. 2.3; Hill and Šmilauer 2005) and the cluster analysis (MVSP package, v. 3.1; Kovach 1985–1999). Each of these approaches provides a somewhat different view on the structure of the data, and when employed together they can be used to better understand the diversification of the vegetation. Clusters resulting from divisions (TWINSPAN) with eigenvalues greater than 0.3 are treated as the final clusters which, however, do not necessarily constitute communities. The cluster classification (MVSP) was performed using the minimum variance, based on the squared Euclidean distance.

The statistical significance of differences between empirical distributions of the data analysed and the theoretical normal distribution was examined using the Shapiro–Wilk test. Since distributions of most data sets deviated from normality, the non-parametric U Mann-Whitney test, Kruskal–Wallis test and Dunn's multiple comparisons test were used to examine whether differences between sites of C. flava agg. species and between relevés (Shannon diversity index, the evenness and number of species) were significant. Calculations were performed using the software package Statistica v. 13.1 for Windows (StatSoft, Inc. 2013). The Shannon diversity index and the evenness were calculated for each relevé using the MVSP package (Kovach 1985–1999).

Relationships between vegetation plots and environmental factors were determined using the software package CANOCO v. 4.51 (ter Braak and Šmilauer 2002). Vegetation distribution patterns in relation to environmental variables were explored using canonical correspondence analysis (CCA), after detrended correspondence analysis (DCA) detected a unimodal structure of the species data (the gradient length represented by the first ordination axis was greater than 3 SD). The Monte Carlo permutation test was further applied to test for statistical significance of environmental variables.

Nomenclature

The nomenclature of vascular plants, Carex taxa and mosses follows World Flora Online (WFO 2020), Koopman (2015) and Ochyra et al. (2003), respectively. The phytosociological units are in compliance with the syntaxonomic nomenclature of the vegetation of Europe (Mucina et al. 2016). Assignment to phytosociological units below the class level follows Matuszkiewicz (2018) and Dierßen (2001). The fen terminology is in accordance with Hajek et al. (2006). Specimens collected in the field have been deposited in the Herbarium Stetinensis (SZUB).

Results

Floristic composition and diversity of plant communities with taxa representing Carex flava agg

The TWINSPAN resulted in eight final clusters (I–VIII; see Online Resource 2 and 3). The first division of the dataset separated plots with C. lepidocarpa and C. viridula from C. flava and C. demissa. The division was based on indicators: C. viridula with a coverage of 3 or more, and C. lepidocarpa with a coverage of 2 or more. All the relevés with C. lepidocarpa coverage of more than 2 were assigned to a single vegetation unit (cluster I) whereas the relevés with C. viridula coverage of 3 and more were divided into three groups (Online Resource 2). The division of the three groups was based on indicators: Bryum pseudotriquetrum with a coverage of 2 and more (cluster III) and Pohlia nutans with a coverage of 1 and more (cluster IV). Cluster II contained relevés dominated by species of the classes Scheuchzerio palustris-Caricetea fuscae (e.g. Carex nigra, C. panicea, Campylium stellatum) and Molinio-Arrhenatheretea (e.g. Molinia caerulea, Lythrum salicaria, Deschampsia cespitosa). All the relevés with C. demissa were assigned to a single vegetation unit (cluster V), with a C. demissa coverage of 3 and more (Online Resource 3), as an indicator. The relevés with C. flava were divided into three clusters. Clusters VI and VIII were identified by the presence of Valeriana dioica subsp. simplicifolia and Alnus glutinosa, respectively. Cluster VI covers relevés taken exclusively in the mountainous area in south-eastern Poland whereas cluster VII groups relevés from both lowlands throughout the country and mountains and uplands, mainly in the South-West of Poland. These relevés are distinct by the absence of Valeriana dioica subsp. simplicifolia, while V. dioica s.str. is frequent (Online Resource 3).

The MVSP resulted in the division of the entire dataset into two main groups; the first one contained relevés with C. lepidocarpa and C. viridula, while relevés in the other group contained relevés with C. flava and C. demissa (Fig.2a). Further analyses of the main groups showed that some relevés with C. viridula were included in the group with C. lepidocarpa, while some of the relevés with C. flava were assigned to the group with C. demissa (Fig. 2b, c). The MVSP demonstrated a separate nature of relevés with C. viridula from dunes (cluster IV versus clusters III and II), shores of water bodies and the vicinity of a chalk mine (cluster IIIa versus cluster IIIb), as well as relevés with C. demissa (cluster Va versus Vb) and those with C. flava (cluster VI versus cluster VII), see Fig. 2b,c; Online Resource 2 and 3).

Fig. 2
figure 2

Results of hierarchical cumulative classification using Euclidean distance-based minimum variance techniques. a – Results for the entire dataset; b – Analysis for plots of C. lepidocarpa (cluster I) and C. viridula (II – samples from fens and wet grasslands, IIIa – sandy lakeshores, IIIb – sites near a chalk mine, and IV – dunes); c – Analysis for C. demissa (Va – samples from poor acidic fen and Vb – moderate-rich fens and fen grasslands) and C. flava (VI – samples with C. flava from fens and wet grasslands with Valeriana dioica subsp. simplicifolia from Bieszczady Mts, VII – fens and wet grasslands without Valeriana dioica subsp. simplicifolia, and VIII – from Alnus forest).

Relevés with C. lepidocarpa (cluster I) were similar in terms of their floristic composition and proportions of species (Online Resource 2). Such a species composition is characteristic of the association Caricetum paniceo-lepidocarpae. It is dominated by diagnostic species such as C. lepidocarpa and C. panicea; there are also calciphilous vascular plants (e.g. Carex flacca, Epipactis palustris and Parnassia palustris) and mosses (e.g. Campylium stellatum and Fissidens adianthoides, see Online Resource 2). The number of species per relevé averaged 22; Shannon’s diversity index and evenness averaged 4.22 and 0.96, respectively (Table 1).

Table 1 Diversity of species occurrence in phytocoenoses with Carex flava agg.; results of Kruskal–Wallis test and post hoc Dunn's multiple comparisons test, showing significance of differences in Shannon's index, evenness and number of species. F – C. flava s.str.; D – C. demissa; L – C. lepidocarpa; V – C. viridula; × – mean; P – statistical significance. The Significance level of P ≤ 0.05 is denoted in bold.

Relevés featuring C. viridula, taken along lake shores (cluster IIIa), were distinct by the presence of species representing the classes Montio-Cardaminetea, Potamogetonetea, Littorelletea uniflorae and Isoëto-Nanojuncetea. Samples from the vicinity of the chalk mine (cluster IIIb) showed a low contribution of species representing the classes listed above (only Cardamine amara, Bryum pseudotriquetrum and Drepanocladus polycarpos were present) whereas species belonging to the Phragmito-Magnocaricetea (e.g. Cladium mariscus, Carex disticha, Schoenoplectus tabernaemontani) and Molinio-Arrhenatheretea (e.g. Juncus subnodulosus, Linum catharticum) occurred. Some relevés contained the calciphilous Samolus valerandi and Campylium stellatum (Online Resource 2). Plots dominated by C. viridula, occurring on exposed sandy shores (cluster IIIa), were classified as the assemblage Ranunculo-Juncetum bulbosi, variant with C. viridula. The assemblage was made up of several Juncus species (J. articulatus, J. bufonius, J. bulbosus) and a number of fen species such as Agrostis canina and Hydrocotyle vulgaris (Online Resource 2).

Patches featuring C. viridula observed in depressions between dunes (cluster IV) were characterized by the presence of species representing the classes Oxycocco-Sphagnetea (e.g. Drosera rotundifolia, Vaccinium oxycoccus, Aulacomnium palustre) and Nardetea strictae (Calluna vulgaris, Pohlia nutans, Empetrum nigrum), and the order Scheuchzerietalia palustris (Drosera anglica, Lycopodiella inundata, Sphagnum teres). Relevés with C. viridula from wet grasslands and fens (cluster II) showed a presence of species from the class Molinio-Arrhenatheretea (e.g. Lysimachia vulgaris, Ranunculus acris, Lotus pedunculatus) and the order Caricetalia fuscae (e.g. Hydrocotyle vulgaris, Carex nigra, Veronica scutellata, see Online Resource 2). The fen and wet grassland relevés differed significantly from those of dunes in terms of the Shannon diversity index and the species richness (P = 0.0193 and P = 0.0091, respectively) as well as from those from lake shores (P = 0.0048 and P = 0.0040, respectively). The species richness in fen and wet grassland averaged 21 per relevé (Shannon index of 4.12) and 11 (Shannon index of 3.29) and 14 species (Shannon index of 3.56) in dune and lakeshore relevés, respectively.

The relevés with C. demissa were divided into two groups (Va and Vb; see Fig. 2c and Online Resource 3). Those included into cluster Va were distinct by the presence of species representing the classes Nardetea strictae (e.g. Nardus stricta, Potentilla erecta) and Oxycocco-Sphagnetea (Sphagnum fallax, Polytrichum strictum), as well as by a lower contribution of wet grassland species, compared to relevés in cluster Vb (Online Resource 3). The two groups identified by the MVSP were significantly different in their numbers of species (23 and 31 in clusters Va and Vb, respectively; Z = −2.2229; P = 0.0262), the Shannon diversity index (4.35 and 4.80 for clusters Va and Vb, respectively; Z = −2.1170; P = 0.0343) and evenness (0.97 and 0.98 for clusters Va and Vb, respectively; Z = −2.4346; P = 0.0149).

The C. flava relevés proved most species-rich, the Shannon index and the evenness being at their highest as well (Table 1). Relevés acquired in the Bieszczady Mountains (cluster VI) were significantly different from the remaining relevés (clusters VII and VIII) in terms of their Shannon index, evenness, and the number of species (5.07 vs 4.77 and 4.75, P = 0.0042; 0.98 vs 0.97 and 0.97, P = 0.0208; 38 vs 30 and 30, P = 0.0042, respectively). The Bieszczady Mts support a floristically rich variant of the Valeriano simplicifoliae-Caricetum flavae which featured, fairly frequently, Valeriana dioica subsp. simplicifolia and Eriophorum latifolium, while in other regions the assemblages with C. flava featured fairly abundant Valeriana dioica s.str. All the relevés with C. flava showed an abundance of Juncus articulatus and small sedges such as C. panicea and C. nigra (Online Resource 3). Moreover, species primarily characteristic of wet grassland associations (e.g. Anthoxanthum odoratum, Briza media, Cirsium palustre, Climacium dendroides, Festuca rubra, Geum rivale, Myosotis scorpioides and Ranunculus acris) were also frequent. Some relevés from cluster VII were dominated by wetland species, for example Blysmus compressus (relevés 15 and 21), Carex hartmanii (40 and 41) and Equisetum palustre (12, 14 and 43, see Online Resource 3.

Distribution of plots and species along environmental gradients

The CCA results indicate that all the variables analysed accounted for 14.36% of the total variance in the species data (Table 2). The first axis and all the canonical axes were significant as tested by the unrestricted Monte Carlo permutation test (first axis: P = 0.026; all axes: P = 0.006). The results of forward selection in the CCA revealed seven variables (pH, N, K, C, CaCO3, P and Ca) to be statistically significant and to account for 11.55% of the total variance in species composition (Table 3).

Table 2 Summary of CCA of vegetation samples collected at sites with the presence of species from the C. flava complex.
Table 3 Forward selection results with the test of variable significance for vegetation samples collected at sites with the presence of species from the C. flava complex. C – carbon concentration; N – nitrogen concentration; C/N – ratio between organic carbon and nitrogen concentration; org. mat. – organic matter content; pH – soil pH; Ca – calcium concentration; CaCO3 – carbonates concentration; Mg – magnesium concentration; P – phosphorus concentration; K – potassium concentration; * significance level P ≤ 0.05.

In the ordination space (CCA), all the C. lepidocarpa relevés occupy the right-hand part of the diagram and are associated with relatively high pH values and soil Ca, Mg, CaCO3, C and N, as well as with a relatively high C/N ratio (Fig. 3; Table 4). The C. lepidocarpa habitat differed significantly from habitats of C. demissa, C. flava and C. viridula by being relatively rich in carbonates, calcium and magnesium in the soil, as well as showing a high soil pH (Table 5).

Fig. 3
figure 3

Ordination diagram of vegetation samples and environmental variables along the first two CCA axes; cluster I – samples with C. lepidocarpa; cluster II – samples with C. viridula from fens and wet grasslands; cluster IIIa – samples with C. viridula from sandy lake shores; cluster IIIb – samples with C. viridula from sites near a chalk mine; cluster IV – samples with C. viridula from dunes; cluster Va – samples with C. demissa from poor acidic fens; cluster Vb – samples with C. demissa from moderate-rich fens and fen grasslands; cluster VI – samples with C. flava from fens and wet grasslands with Valeriana dioica subsp. simplicifolia from the Bieszczady Mts; cluster VII – samples with C. flava from fens and wet grasslands without Valeriana dioica subsp. simplicifolia; cluster VIII – samples with C. flava from Alnus forest; * – statistically significant variables, significance level P ≤ 0.05. For abbreviations of soil properties, see Table 3.

Table 4 Soil properties at Carex flava agg. sites sampled. F – C. flava s.str.; D – C. demissa; L – C. lepidocarpa; V – C. viridula; C – carbon, N – nitrogen; × – mean; SD – standard deviation; range – minimum and maximum values; ** – for the pH measured on a log scale, only the range and extreme values (in brackets) are given. For abbreviations of soil properties, see Table 3.
Table 5 Results of Kruskal–Wallis test and post hoc Dunn's multiple comparisons test, showing significance of differences in soil properties at Carex flava agg. Sites sampled. F – C. flava s.str.; D – C. demissa; L – C. lepidocarpa; V – C. viridula; the significance level of P ≤ 0.05 is marked with bold. For abbreviations of soil properties, see Table 3.

Relevés of C. viridula are scattered in the ordination space; however, most samples collected from dunes (cluster IV) and lake shores (cluster IIIa) are positioned in the left-hand side of the diagram and are associated with relatively low values of most soil parameters studied (Fig. 3; see also Table 5). The relevés taken from fens and wet grasslands (cluster II) are concentrated mainly in the central part of the diagram whereas samples collected from sites near the chalk mine (cluster IIIb) are placed in the right-hand part of the diagram together with samples of C. lepidocarpa. Statistically significant differences, primarily concerning pH and soil contents of organic matter, C, N, Mg, Ca and CaCO3 were detected between relevés from dunes (IV) and fens and wet grasslands (II), as well as between dunes (IV) and sites near the chalk mine (IIIb), see Fig. 4a–h.

Fig. 4
figure 4

Ranges of soil properties at C. flava agg. sites in Poland. Large boxes indicate 25–75% of the interquartile ranges; small boxes are medians; circles denote outliers; asterisks mark extreme values. Carex lepidocarpa – cluster I; C. viridula – II, IIIa, IIIb, IV; C. demissa – Va, Vb, C. flava – VI, VII, VIII (the cluster numbers are compatible with Online Resource 2 and 3). The diagrams show statistically significant differences only within C. viridula (between four clusters), C. demissa (between two clusters) and C. flava (between three clusters) sites. The significance of differences between species sites is shown in Table 5. a – Carbon, P = 0.0019, P1 = 0.0416, P2 = 0.0013, P3 = 0.0023, P4 = 0.0058; b – Nitrogen, P = 0.0016, P1 = 0.0028, P2 = 0.0005, P3 = 0.0038; c – Organic matter content, P = 0.0262, P1 = 0.0416, P2 = 0.0009, P3 = 0.0029, P4 = 0.0083; d – pH value, P = 0.0021, P1 = 0.0008, P2 = 0.0050; e – Potassium, P = 0.0275, P1 = 0.0000, P2 = 0.0232; f – Magnesium, P = 0.0426, P1 = 0.0293, P2 = 0.0014, P3 = 0.0009, P4 = 0.0189; g – Calcium, P = 0.0107, P1 = 0.0027, P2 = 0.0003, P3 = 0.0081; h – Carbonates, P = 0.0493, P1 = 0.0055, P2 = 0.0285.

All the relevés with C. demissa occupy the left-hand part of the CCA diagram and are associated with relatively low values of most soil parameters studied (Fig. 3). The upper part of the diagram contains the relevés from poor acidic fens (cluster Va), while the relevés from moderate-rich fens (cluster Vb) are grouped in the central part. Significant differences between them concerned pH and the soil Ca content (Fig. 4d,g).

Plots of C. flava are scattered on the CCA diagram; however, relevés from the Bieszczady Mts (cluster VI) are situated in the upper part whereas the remaining relevés from fens and wet grasslands (cluster VII), as well as all the forest relevés (cluster VIII), are grouped in the lower part (Fig. 3). Statistically significant differences between the Bieszczady relevés and the other relevés were revealed for soil organic matter content, as well as for concentrations of carbon, nitrogen, magnesium and potassium (Fig. 4a-c,f,e).

Discussion

Vegetation types with taxa representing Carex flava agg

We delimited nine vegetation types with taxa included in the Carex flava group that differed in their species composition and response to soil properties.

Carex lepidocarpa is a characteristic species of the assemblage Caricetum paniceo-lepidocarpae from the alliance Caricion davallianae (Kwiatkowski 1999). In Poland C. lepidocarpa grows only in calcareous sites (calcareous, extremely rich and rich fens). Those habitats are severely threatened due mainly to general and wide-scale disturbances in hydrological conditions (Wołejko et al. 2005; Šefferová Stanová et al. 2008; Grootjans et al. 2015). Moreover, C. lepidocarpa is sensitive to changes in hydrology and becomes increasingly rare. It is regarded as threatened in some Central European countries (Pykälä 1994).

Carex flava s.str. is found in calcareous, rich and moderate-rich fens and wet grasslands as well as in alder thickets and woods. In Poland, it grows on soils with a wide pH range, from (4.3–)5.0 to 7.6. Carex flava is one of the diagnostic species of the Valeriano simplicifoliae-Caricetum flavae, found in mountainous regions, throughout the flysch zone of the Slovak, Polish and Ukrainian Carpathians, and occasionally in Czechia (Pawłowski et al. 1960; Hájek 1999; Hájek and Hájková 2002, 2011; Hájek et al. 2002). In Poland, Koczur and Nicia (2013) reported a substantial variability in the assemblage, mainly produced by the wide range of the habitat parameters, notably the soil pH, varying from (5.8–)6 to (7.6–)8 (see also Mazurek and Nicia 2006); our study, however, showed the Valeriano simplicifoliae-Caricetum flavae to be a rather homogenous fen community (see also Hájek 1999), despite the habitat varying from acidic to slightly alkaline (from 5.0 to 7.6). The assemblage showed a fairly constant floristic composition, but a high number of species from the class Molinio-Arrhenatheretea points to its potential to become transformed into a grasslands community. In Czechia, the Valeriano simplicifoliae-Caricetum flavae is vicariant to the Valeriano dioicae-Caricetum davallianae in the mountainous regions of the Western Carpathians (Hájek and Hájková 2011). In Poland we found patches featuring Carex flava and Valeriana dioica s.str. as well as other species diagnostic for the Valeriano dioicae-Caricetum davallianae, for example Carex panicea, Potentilla erecta, Succisa pratensis, Calliergonella cuspidata (Hájek and Hájková 2011); however, C. davalliana was not found at any of our sites and the proportion of wet grasslands species was considerable. In Poland, V. dioica subsp. simplicifolia and V. dioica s.str. are vicariants; the former occurs mainly in the East and South-East whereas the latter is known from the central and western part of the country (Zając and Zając 2001). According to Zarzycki et al. (2002), the taxa are similar in their habitat requirements, but are different in terms of their continentalism and, to a lesser extent, in acidity preference: V. dioica subsp. simplicifolia is sub-continental and usually grows on alkaline soils (more seldom on soil with neutral pH), whereas V. dioica s.str. is a sub-Atlantic species and grows on neutral pH soils. Our study confirmed the presence of the Valeriano simplicifoliae-Caricetum flavae in the Bieszczady Mountains, while the remaining patches with C. flava (outside of the Bieszczady) are heterogenous and represent various associations, usually the wet grasslands ones from the class Molinio-Arrhenatheretea.

Carex demissa usually occurs in poor and moderate-rich fens as well as along forest roads and paths. In Poland, it was usually reported from acidic sites (pH 3.4–5.5) with usually a very low calcium concentration and with a carbonate-poor soil. It was only at a single site, the northernmost one, about 700 m away from the Baltic Sea shore, that C. demissa was found growing on soil with a pH exceeding 7. In Central and Southern Europe, C. demissa is usually found on acidic and slightly acidic soils, for example in Switzerland (Schmid 1984), Bulgaria, Czechia, and Slovakia (Stoeva and Štepánková 1990). In Northern Europe (e.g. in Finland), C. demissa is weakly calciphilous and occurs on nutrient-rich soils. According to Pykälä and Toivonen (1994), this lends support to the known observation of a species strengthening its requirements at the boundary of its range. In Poland, the structure and floristic composition of communities with C. demissa as well as the soil parameters, mainly pH, correspond with those typical of the Carici echinatae-Sphagnetum (cluster Va) and Carici canescentis-Agrostietum caninae (cluster Vb), see Hájek and Hájková (2002, 2011), Hájek et al. (2008), and Koczur and Nicia (2013). The habitat of the latter represents one of the most common types of fen grasslands on non-calcareous bedrock in Central Europe (e.g. Dítě et al. 2007; Hájek and Hájková 2011; Matuszkiewicz 2018).

Carex viridula usually grows in open habitats (e.g. wet grasslands, fens, dunes, lake and pond shores) and is capable of colonising variable and unstable sites (Davies 1956; Schmid1984; Stoeva and Štepánková 1990; Więcław 2014a,b, 2017). The sedge has been reported from various plant assemblages, mainly the classes Isoëto-Nanojuncetea, Littorelletea uniflorae and Scheuchzerio palustris-Caricetea fuscae (e.g. Šumberová 2011; Šumberová et al. 2011).

In Poland, C. viridula is regarded as one of the species characteristic of the Cyperetum flavescentis from the class Isoëto-Nanojuncetea, which appears spontaneously on emergent bottom and shores of water reservoirs (Popiela 1997; Matuszkiewicz 2018). However, our study found C. viridula to grow, along lake shores, in Ranunculo-Juncetum bulbosi communities from the class Littorelletea uniflorae (see also Szańkowski and Kłosowski 2006; Hrivnák et al. 2011; Šumberová et al. 2011). All the sites with C. viridula located along lake shores were supported by the bryophyte Bryum pseudotriquetrum, which is common in wet and moderately infertile sites (Ellenberg et al. 1991). According to Dierßen (2001) this species can also occur on slightly acidic habitats such as fens and lake shores.

Communities featuring C. viridula and occurring in humid dune depressions along the Polish Baltic Sea coast are similar to marsh assemblages of the class Scheuchzerio palustris-Caricetea fuscae. Theurillat et al. (2015) distinguished, within the class Scheuchzerio palustris-Caricetea fuscae, the alliance Caricion viridulo-trinervis, which covers low-sedge vegetation of wet, phosphorus-limited dune slacks of Atlantic coasts of Western Europe (see also Peterka et al. 2017). On the other hand, Sival and Grootjans (1996) frequently recorded C. viridula on dune slacks of the island of Schiermonnikoog in the northern part of the Netherlands in a pioneer assemblage with Littorella uniflora, Samolus valerandi, Radiola linoides and Juncus bulbosus. In Poland, the relevés made in between-dune depressions were distinct in showing the presence of the bryophyte Pohlia nutans, common and often abundant on wet or dry, acidic, peaty, sandy or gravelly soil on heaths and moors, in sand dunes, acidic grassland, bogs, and woods. It avoids base-rich or calcareous sites (Ellenberg et al. 1991).

Carex viridula is fairly frequently found also in fens and wet grasslands across a wide spectrum of soil conditions (e.g. Więcław and Podlasiński 2013), in communities representing both the class Scheuchzerio palustris-Caricetea fuscae and the Molinio-Arrhenatheretea. According to Hájek et al. (2008), C. viridula reached a high cover in disturbed moderately rich fens in Bulgaria and occurred with some calciphilous species, for example Eriophorum latifolium and Parnassia palustris. In Poland, C. viridula can also grow at sites with a high soil calcium carbonate level (see also Więcław and Podlasiński 2013) and is capable of colonizing heavily disturbed sites (Więcław 2017). Thus, the ecological niche of C. viridula is very wide, compared to that of C. flava, C. lepidocarpa and C. demissa. Carex viridula grows in various plant communities without any tight syntaxonomic affinity.

Ecological differentiation within closely related species

In Poland, the Carex flava complex includes four closely related sedge species (Więcław 2014a), which, as shown in this study, occupy diverse habitats and have diverse ecological requirements. In general, many closely related taxa may be distinctly different in their ecological preferences (e.g. Dakskobler et al. 1999; Hölzel 2003; Koutecká et al. 2011; Budzhak et al. 2016). A clear differentiation, both in the community composition, soil properties, and habitat types was revealed within the Bolboschoenus maritimus group (Hroudová et al. 1999). According to Hroudová et al. (1999), the closely related taxa of the Bolboschoenus maritimus group show a much stronger ecological than morphological differentiation (no distinct diagnostic characters). Our investigation has shown that C. lepidocarpa and C. demissa are the most ecologically isolated species of the C. flava complex. The former was found on calcareous and extremely rich fens (Caricion davallianae) whereas the latter was reported from poor and moderately rich fens (Sphagno-Caricion canescentis and Caricion canescenti-nigrae). However, earlier morphological studies on the C. flava group in Poland showed C. lepidocarpa and C. demissa to be fairly distinctly separated morphologically, mainly in the dimensions of the generative characters (Więcław 2014a). Similarly, taxa within the Festuca varia group were well separated both morphologically and ecologically, syntaxonomic studies on the group showing the presence of five vicariating regional associations and one edaphically determined association, growing on ecologically different sites (Wallossek 1999). Other studies, addressing species of the Molinia caerulea complex in Central Europe (Molinia caerulea s.str. and M. arundinacea), showed differences in their morphology and chromosome number (Dančák et al. 2012) as well as in habitat preferences (Budzhak et al. 2016). Comparative studies on three related species of the genus Viola, combined with their phytosociology and environmental parameters showed the species to differ in terms of their association with the soil moisture gradient and chemistry (Hölzel 2003). Koutecká et al. (2011) reported results of phytosociological research which clearly separated three Myosotis species from the Myosotis palustris group into different types of habitats and plant communities. They found only two locations with the simultaneous presence of two Myosotis species (M. caespitosa and M. nemorosa). These examples show closely related species to differ fairly distinctly in terms of micro-species morphology and to be clearly separated by ecological preferences. This pattern is, however, not so pronounced within the C. flava complex.

Our study showed the C. flava taxa to be capable of sharing a habitat, except for C. lepidocarpa and C. demissa, distinctly separated ecologically in Poland. Carex lepidocarpa and C. flava s.str. Can co-occur on calcareous and rich fens (Caricion davallianae). They are clearly different morphologically (e.g. Schmid 1984; Crins and Ball 1989a,b; Pykälä and Toivonen 1994; Więcław 2014a), but mixed populations frequently support hybrids, whereby an unequivocal species identification is challenging (Więcław and Wilhelm 2014). The ecological amplitude of Carex flava s.str. is wider than that of C. lepidocarapa; the former species can also grow on wet grasslands and moderate-rich fens, where frequently co-occurs with C. demissa and their hybrid (C. ×alsatica). Carex flava s.str. and C. demissa are rather well separated morphologically, but the problem of intermediate hybrids present in their mixed populations appears here as well (Więcław and Wilhelm 2014).

Carex viridula is encountered both in calcareous, extremely and moderately rich fens, wet grasslands, and in very poor habitats such as dunes and sandy lake shores. Carex viridula frequently co-occurs with both C. lepidocarpa and C. flava, and much more seldom with C. demissa (Więcław 2014a,b) and hybridizes with all three mentioned species (Więcław and Wilhelm 2014; Schmidt et al. 2018). Carex viridula is morphologically different from both C. flava and C. lepidocarpa, mainly in its much smaller utricles and shorter beaks, but is morphologically very close to C. demissa (e.g. Pykälä and Toivonen 1994; Hedrén 2003; Więcław 2014a). Noteworthy is the fact that Carex viridula is the only species of the C. flava complex which grows on sandy lake shores and in dune depressions.

To sum up, detailed knowledge on closely related species, combining results of taxonomic and environmental studies, allows us to fairly precisely determine the ecological amplitude of narrowly-defined species. The combination of an ecological and taxonomic approach may lead to a better understanding of the evolutionary ecology of plants.