Abstract
The most important center of speciation in the genus Gagea is thought to be in Central Asia. Here, we focus on species diversity in southeastern Kazakhstan (around Almaty, Ili-Alatau range of the Western Tian-Shan mountains). We studied an elevational transect, reaching from lowland steppes to the alpine zone (500–2750 m a. s. l.), and carried out detailed morphological and molecular investigations for populations of Gagea spp. Nine species were identified in different altitudinal zones; one of these (Gagea almaatensis) is described as new to science. We could detect two altitudinal contact zones between closely related species: G. filiformis and G. granulosa (sect. Minimae), and G. almaatensis and G. kuraminica (sect. Gagea). Morphological and molecular investigations (ITS data and cpDNA networks) indicate ongoing hybridization of co-occurring G. filiformis into G. granulosa and putative bidirectional hybridization events between G. almaatensis and G. kuraminica.
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Introduction
The species-rich, complex genus Gagea Salisb. (Liliaceae; more than 320 species, see Levichev 2013) comprises small bulbiferous geophytes, which are mainly vegetatively propagated. Diversification in the genus is generally influenced by polyploidization and reticulated intra-sectional hybridization (e.g., Peruzzi 2008; Peterson et al. 2009, 2011; Peruzzi et al. 2011; Zarrei et al. 2012; Tison et al. 2013).
Within the last two decades, morphological characters of the genus Gagea were intensively studied based on wild and cultivated plants and available herbarium vouchers. As a result, several new species were described especially in the species-rich sections Didymobulbos s.l. (Tison et al. 2013; Kayıkçı et al. 2014; Tekşen and Erkul 2014) and Gagea (e.g., Levichev 1988, 1998, 2001; Henker 2005; Peruzzi et al. 2007; Peterson et al. 2011; Henker et al. 2012). The plants express species-specific growth patterns during ontogenesis (e.g., Levichev and Jezniakowsky 2008), which are already documented for a number of species (e.g., Levichev 2011, 2013). Vegetative reproduction (via bulbils) is combined with generative reproduction (via seeds), but the proportion of both reproductive modes varies widely among species. One extreme is the virtually clonal Gagea spathacea (Hayne) Salisb., reproducing by bulbils only (Levichev et al. 2010; Pfeiffer et al. 2012). In contrast, some species such as G. incrustata Vved., G. taurica Steven or G. alexeenkoana Miscz. never form vegetative bulbils (Levichev 2005). If bulbils are present, their quantity, location, form and structure represent important features for species differentiation (e.g., Levichev 1999a; Peterson et al. 2011; Tison et al. 2013). In addition, patterns of bulbil formation are highly species-specific and much diversified within the genus and its sections (Schnittler et al. 2009, 2013; Beisenova et al. 2015). Based on the comparison of several Gagea species (Schnittler et al. 2013), two main patterns of bulbil formation were found: “type I bulbils” (a single or several bulbils are produced as soon as the replacement bulb has reached a certain diameter and then formed throughout the life of the plant as long as the bulb stays above this threshold) and “type II bulbils” (only temporarily produced in immature, sufficiently large non-flowering plants). In addition, both strategies may occur simultaneously for bulbils with different locations (for instance, type I basal bulbils accompanied by type II suprabasal bulbils).
According to current knowledge, southwestern Central Asia harbors about 70 % of all described Gagea species (Levichev 2013). The Western Tian-Shan and the Pamir Alai mountains are considered as two centers of speciation (Levichev 1999b; Levichev and Jezniakowsky 2008; discussed in Peterson et al. 2009). The Flora of Uzbekistan lists 68 species (Tojibaev et al. 2014; 82 species according to I.G. Levichev, unpubl. data), and the flora of China includes 17 species (Xinqi and Turland 2000). Numerous species have been described recently for the Chinese region of Inner Mongolia (three species: Zhao and Zhao 2003, 2004; Zhao and Yang 2006), Xinjiang, China (three species: Peterson et al. 2011) and Pakistan (17 species: Ali 2006; Levichev 2006; Levichev and Ali 2006; Ali and Levichev 2007). In the Flora of Kazakhstan (Baitenov 2001), 39 Gagea species are recorded. Of these, 12 taxa (31 %) are endemic to the country.
In southeastern Kazakhstan, we studied an elevational transect (500–2750 m a. s. l.) reaching from lowland steppes around Almaty until the alpine zone of the Ili-Alatau range (Zailiysky Alatau) in the Northern Tian-Shan mountain range. For speciation, altitudinal gradients are interesting due to gradients in numerous abiotic (e.g., temperature, hours of sunshine, ultraviolet radiation, moisture) and biotic factors (discussed, e.g., in Abbott and Brennan 2014). In the contact zones between different altitudinal vegetation zones, previously isolated lineages can come in contact and interspecific crossing can take place. However, only a few hybrid zones have been studied until now (discussed in Levichev 2013; Abbott and Brennan 2014). In general, interspecific crossings in the hybrid zones will result in complex patterns of genetic variation and the formation of new genotypes (see Levichev 2013; e.g., Harrison and Larson 2014; Marques et al. 2014). In some cases, these new genotypes, resulting from introgression, are able to colonize new habitats.
Depending on the weight given to morphological and/or molecular characters, different infrageneric classifications exist (Levichev in Peterson et al. 2008 vs. Zarrei et al. 2011: discussed in Peterson et al. 2011; Peruzzi 2012a). This study generally adopts (except for sect. Didymobulbos s.l.; including sect. Fistulosae according to Peruzzi et al. 2008a) the infra-generic classification of Levichev (see Peterson et al. 2008). However, the taxonomic status of Gagea serotina (L.) Ker-Gawl. is controversial (also between the authors of this study). This species is either included into the genus Gagea (Peruzzi et al. 2008b, 2011; Peruzzi 2012a; Zarrei et al. 2009, 2011), or excluded [Lloydia serotina (L.) Rchb.: e.g., Levichev 2002: 236, 2013; Levichev et al. 2010: 478; Peterson et al. 2008].
The aim of this study was (1) to investigate the species composition of Gagea within different altitudinal ranges in the Ili-Alatau range, (2) to identify altitudinal contact zones of closely related species, and (3) to find evidence for putative hybridization between closely related co-occurring species by using a combination of morphological and molecular methods. In addition to the analysis of the ITS region (ITS1 + 5.8S rRNA + ITS2) obtained by direct sequencing, we employed a network approach successfully used in taxonomically difficult species complexes (e.g., Gagea: Peterson et al. 2010, 2011; Tison et al. 2013; Erythronium: Bartha et al. 2015; Allium: Gurushidze et al. 2008, 2010; Bellevalia: Borzatti von Loewenstern et al. 2013; Crocus: Harpke et al. 2014, 2015; Doronicum: Peruzzi et al. 2012; Pachschwöll et al. 2015) to analyze the genealogical relationships between chloroplast haplotypes. ITS types and cpDNA haplotypes (psbA-trnH IGS + trnL-trnF IGS) were investigated and considered regarding the altitudinal distribution of the respective species. The applied markers already proved to be suitable to solve phylogenetic and taxonomic problems within the genus (Peruzzi et al. 2008a; Peterson et al. 2008, 2011; Zarrei et al. 2009; Tison et al. 2013; see also discussion for psbA-trnH haplotypes in Pang et al. 2012; Naciri and Linder 2015), but as well for the detection of parental species of hybridogenic taxa (Peterson et al. 2004, 2009, 2011; Tison et al. 2013). In addition, we describe a new species of sect. Gagea.
Materials and methods
Studied altitudinal vegetation zones
Within the study region, five major vegetation zones can be distinguished. Zone I is formed by lowland steppes around Almaty (500–800 m a. s. l.). Zone II is formed by the foothills (800–1100 m a. s. l.) of the Ili-Alatau range where species-rich deciduous forests alternate with tall grass steppes. This zone includes as well the city of Almaty. Zone III extends to species-rich deciduous forests on lower slopes (1100–2000 m a. s. l.) of the Ili-Alatau range, which intergrade with shrubby mountain steppes on south-exposed, steep and rocky slopes. Zone IV is constituted by the belt of spruce forests (Picea schrenkiana Fisch. & C.A.Mey, 2000–2400 m a. s. l.). Since recruitment of spruce is slow to absent on steep south-exposed slopes, especially with rock outcrops, the conifers may as well be replaced by shrubby mountain steppes in such places. Zone V includes alpine meadows above the timberline (ca. 2400 m a. s. l.). All these vegetation zones, but especially valley plains and shallow slopes, are moderately grazed by livestock. Zones III–V can be disturbed by avalanches occurring on steep slopes. Further information about the studied region, climate data, and maps are provided by Gurikov (1981), Bolch (2007), and Bolch et al. (2011).
Sampling of plant material
The field study was carried out in the second half of April 2013. All taxa of Gagea were preliminary determined in the field. Wherever possible, several populations for a species were sampled from different sites and from different altitudes and vegetation zones. Numbers of collected individuals depended on (1) the size of population, (2) the extent of observed morphological variability, (3) the altitudinal distribution of populations, and (4) taxonomic criteria. Morphological variable populations and such in areas with co-occurring species were intensely sampled. For molecular studies and reference material (see “Appendix”), several individuals per site were preserved as herbarium specimens. All individuals of a given site received the same number (Arabic numerals ending with-AP2013). At least ten individuals for each species were deposited in the herbaria HAL and LE. Vouchers for the new species were prepared in duplicate and deposited in HAL (holotype) and LE, HAL (isotypes). For morphological analyses, we sampled patches of plants of all stages (juvenile non-flowering individuals and flowering individuals) exhaustively, analyzing as well all young and non-flowering plants around the older ones, to obtain a sample representing all growth stages.
Morphological investigations
Morphological investigations were carried out on fresh plant material (for detailed voucher information, see “Appendix”). For Gagea kuraminica Levichev, a total of 263 plants were analyzed (AP16-2013: n = 48; AP24-2013: n = 73; AP27-2013: n = 54; AP49-2013: n = 88); for G. filiformis (Ledeb.) Kar. & Kir. measurements were taken from 300 plants (AP20-2013: n = 182; AP26-2013: n = 118); for G. granulosa Turcz. 247 plants (AP1-2013: n = 218; AP4-2013: n = 29) were studied. For G. almaatensis sp. nov. (AP43-2013: n = 13), sampling was limited by small population sizes. Quantitative morphological studies were carried out as described in Schnittler et al. (2009). For plants the following traits were analyzed: the diameter of replacement bulb (if deviating strongly from a spherical form, two perpendicular measurements were taken), the number of flowers, the number and size of bulbils, the length and width of the first (basal) leaf, and the width of the first inflorescence bract. On a separate set of plants being ahead in flowering due to lower elevation or more suitable exposure, seeds were counted separately for each capsule of a plant. These counts included 105 capsules of G. filiformis (AP52-2013), 109 of G. granulosa (AP1-2013) and 104 of G. kuraminica (AP49-2013).
Genomic DNA extraction, PCR amplification and sequencing
Molecular analyses included 83 individuals of Gagea (for detailed voucher information, see “Appendix”) sampled within the five investigated altitudinal vegetation zones, representing nine taxa and 60 populations: Gagea almaatensis sp. nov.: n = 4 (three populations), G. bulbifera (Pall.) Salisb.: n = 7 (6 populations), G. divaricata Regel: n = 2 (one population), G. filiformis: n = 28 (18 populations), G. granulosa: n = 13 (9 populations), G. liotardii (Sternberg) Schult. & Schult.f. (=G. fragifera (Vill.) Ehr.Bayer & G.López; see also Levichev 2006: 942): n = 5 (5 populations), G. kuraminica: n = 11 (9 populations), G. tenera Pascher: n = 1 (one population), and G. cf. turkestanica Pascher: n = 10 (8 populations). In addition, two individuals (AP24b-2013; AP40-2013) morphologically intermediate between G. almaatensis and G. kuraminica were investigated. A small segment of air-dried leaf material (about 10 mg per voucher) was used for DNA isolation with the DNeasy Plant Mini Kit (Qiagen, Hilden, Germany), following the manufacturer’s protocol. PCR was performed with 50 ng genomic DNA in 20 μl reactions (Ready To Go™ PCR Beads, Amersham Bioscience) in a GeneAmp PCR System 9700 (Perkin Elmer). Primers for amplification of trnL-trnF intergenic spacer (IGS) and psbA-trnH IGS were taken from Sang et al. (1997); primers (ITS 5 and ITS 4) for the ITS region (ITS1 + 5.8S rRNA + ITS2) were used according to White et al. (1990). Gel-purified PCR products (50–200 ng) were prepared as “u-mixes” via the StarSEQ® Sequencing Service (StarSeq, Mainz, Germany).
Sequence and phylogenetic analyses
All newly obtained sequences (234) were submitted to the EMBL nucleotide database (for details and accession numbers, see “Appendix”). In addition, we included in the analysis sequences obtained during previous studies (Peterson et al. 2008, 2009, 2011). Sequence alignment was performed utilizing the Clustal-W multiple alignment procedure (Thompson et al. 1994) in Bioedit (version 7.0.9.0; Hall 1999), followed by manual adjustment. For each locus, the best-fitting model of DNA evolution was assessed with MRMODELTEST 2.3 (Nylander 2004). Nuclear data were subjected to phylogenetic analyses using Bayesian phylogenetic inference (BI) with MRBAYES 3.2 (Ronquist et al. 2012). Tulipa cretica Boiss. & Heldr. was used as outgroup (see Peterson et al. 2008, 2011). Generally, all ITS regions are putatively functional, checked according to Harpke and Peterson (2008a, b). For BI 2 times 4 chains were run for two million generations under the appropriate models of sequence evolution (nuclear data set: GTR + Gamma + I), sampling a tree every 1000 generations. Converging log-likelihoods, potential scale reduction factors for each parameter and inspection of tabulated model parameters in MRBAYES suggested that stationarity had been reached in all analyses. The first 25 % of trees of each run were discarded as burn-in. Two independent runs of BI analysis were performed to confirm that separate analyses converged on the same result. Each of these two analyses resulted in the same topology and similar posterior probabilities (pp) for nodal support.
By comparing the positions in which the ITS (ITS1 + 5.8S rRNA + ITS2) sequences of Gagea filiformis and G. granulosa differed, the putative hybrid ITS sequence was generated. For the detection of molecular intermediates of Gagea granulosa and G. filiformis, direct sequencing data of the ITS region were compared to this putative hybrid sequence.
To utilize the advantage of networks (e.g., Gurushidze et al. 2010) over tree-building methods for analyzing cpDNA sequence data in closely related species, we calculated haplotype networks for the species of sect. Minimae and sect. Gagea using TCS (Clement et al. 2000). The sequences of both chloroplast loci (psbA-trnH IGS + trnL-trnF IGS) were concatenated. To obtain a chloroplast haplotype genealogy, insertions/deletions (indels) in the alignment that likely originated from single mutational events were reduced to single alignment positions. Length variation at one mono-nucleotide repeat (T) in the trnL-trnF IGS was generally excluded from the analyses due of the uncertain homology of the respective sequence positions. This shortened alignment was subjected to statistical parsimony analysis in TCS where gaps are treated as a fifth character state.
The number of parsimony-informative sites (ITS region; psbA-trnH IGS + trnL-trnF IGS) was determined using DnaSP v5.10.01 software; excluding gap sites (Librado and Rozas 2009).
Results
Species diversity within altitudinal ranges
The lowland steppes (Fig. 1, zone I) around Almaty were inhabited by Gagea bulbifera (Pall.) Salisb. and G. divaricata Regel (520 m a. s. l.). Here, G. bulbifera was the only very abundant species on moderately grazed steppes with light, sandy soils and on remnants of rich steppe of mixed soil (520–864 m a. s. l.). Together with G. bulbifera, G. cf. turkestanica Pascher (Table 1) was found on isolated patches of remaining steppe around Almaty (790–1119 m a. s. l.; zone II); with uniform, relatively large populations on rich steppes on mixed soil (AP54-2013) and small, scattered populations on cultivated regions such as parks and gardens (e.g., AP46-2013: within the city center of Almaty; AP50-2013: Kok-Tobe Park). In addition, at a single location within the city limits (zone II) G. tenera Pascher (831 m a. s. l.) was found. Four species were regularly found in the Ili-Alatau range, occupying different altitudinal zones. These are G. liotardii (Sternberg) Schult. & Schult.f. [synonyms: G. emarginata Kar. & Kir., G. fragifera (Vill.) Ehr.Bayer & G.López; see Levichev 2006: 942; 1498–2733 m a. s. l.; zones III–V], G. granulosa Turcz. (839–1994 m a. s. l.; zones II–III), G. filiformis (Ledeb.) Kar. & Kir. (1089–2733 m a. s. l.; zones III–V), and G. kuraminica Levichev (1192–2380 m a. s. l.; zones III–IV). The alpine meadows (zone V) are characterized by G. filiformis as the by far most common species. In addition, G. almaatensis sp. nov. (see Taxonomic treatment), a new taxon of sect. Gagea, occurred in small populations. This species inhabits open alpine meadows and was occasionally observed in lower altitudes in avalanche gullies (1994–2557 m a. s. l.; zones IV–V). In addition, a single small population of G. bulbifera was recorded on rock outcrops in open, shrubby mountain steppe (2003 m a. s. l.; zone III) of the upper Medeu valley. Two of the nine investigated species (G. bulbifera of sect. Bulbiferae and G. divaricata of sect. Platyspermum) were the only representatives of their sections. Sect. Didymobulbos s.l. was represented by two species (G. tenera and G. liotardii), which occurred in different altitudinal zones without any contact. The other five species belong to section Minimae and Gagea, respectively, and occurred in different, yet overlapping, altitudinal zones (for contact zones, see Table 1; Fig. 1; for comparison of habitat preferences, see Table 1).
In Gagea filiformis and G. granulosa (sect. Minimae), neither juvenile nor flowering plants could be told apart without a close examination of the bulbils (for morphological characters, see Table 2). Both species possess persistently formed type I bulbils. However, plants of G. filiformis possess a cream to pale yellow tunica of the parent bulb and older individuals form a single lateral bulbil. In contrast, plants of G. granulosa show typically a purple-tinted outer tunica; older plants develop on average 4.3 (up to 13) bulbils arranged in a belt around the parent bulb. Gagea granulosa also has lower threshold for bulbil formation than G. filiformis (>50 % of young G. granulosa form bulbils if the bulb has reached 1 mm in diameter; in G. filiformis, the 50 % threshold is around 2 mm bulb diameter). Nevertheless, very young plants of both species lacking bulbils cannot be distinguished. Especially plants of G. filiformis (spanning a larger elevational belt than G. granulosa; Fig. 1; Table 1) were variable in size. Also G. granulosa populations were found to be variable except for two isolated populations within the city of Almaty (AP1-2013, 839 m a. s. l.; AP4-2013, 862 m a. s. l.), which were morphologically uniform. On several other sites, G. filiformis and G. granulosa were growing together (e.g., AP7-2013, AP20-2013, AP23-2013, AP45-2013, AP58-2013; found between 1192 m and 1994 m a. s. l.; see “Appendix”).
The two species of sect. Gagea, Gagea kuraminica and G. almaatensis, are morphologically well differentiated (e.g., by features of bulbil, width of the basal leaf, and form of the inflorescence). Individuals of G. kuraminica with a candelabrum-like inflorescence are 8–16 cm tall; basal leaves are 3–4.5 mm wide. Flowering plants have obliquely drop-shaped bulbs with a thin and papery, light brownish gray tunic. Bulbils of type II (absent in flowering plants) develop on the tip of a very short stolon which does not exceed 0.5 mm in length. Dormant bulbils possess a smooth gray tunic with brown tints. Individuals of G. almaatensis (see also Taxonomic treatment) lack the candelabrum-like inflorescence and are 7.5–15 cm tall, basal leaves are 2–4 mm wide. Flowering plants have obliquely drop-shaped bulbs with a thin and coriaceous, pale brown tunic. Dormant vegetative bulbils of G. almaatensis are characterized by a dark brown tunic with a heavily pitted structure that resembles honey combs. The two species also prefer different elevations (G. almaatensis: 1994–2557 m a. s. l.; G. kuraminica: 1192–2380 m a. s. l.; Fig. 1; Table 1).
Some individuals of G. kuraminica were found to be morphologically intermediate between G. kuraminica and G. almaatensis (AP24b-2013: alpine meadow below an avalanche gully, vegetation zone III, 1994 m a. s. l.; AP40-2013: open alpine meadows, vegetation zone V, 2733 m a. s. l.). Within the investigated populations of G. kuraminica, we observed as well individuals with deviating morphology (AP29-2013: plants smaller than usual for all ontogenetic stages; bulbils olivaceous gray, tunic with an inconspicuous pitted structure, region zone II, 2437 m a. s. l., moist alpine meadow with many tall forbs).
ITS phylogeny
In the ITS (ITS1 + 5.8S rRNA +ITS2) tree (Fig. 2 based on 55 ingroup taxa and Tulipa cretica as outgroup taxon; including 166 sequences; 290 variable and 217 parsimony-informative sites out of 580 total sites; alignment: Online Resource 1; for voucher information, see “Appendix”) samples of Gagea tenera, G. liotardii and G. bulbifera were found to be monophyletic grouping together with accessions from other origins. All included taxa of Gagea sect. Minimae (Fig. 2: clade A; pp 1.00) form a strongly supported monophyletic clade splitting into two subclades: first, a polytomic subclade comprising all samples of G. filiformis, G. granulosa, G. davlianidzeae Levichev (Fig. 2: subclade A-1; pp 0.90) and G. minima and G. nigra L.Z.Shue, emend. Schnittler, the latter two forming a highly supported clade; second, a subclade comprising all samples of G. confusa A.Terracc.: (Fig. 2: subclade A-2; pp 1.00). In the strongly supported monophyletic clade of sect. Gagea (Fig. 2: clade B; pp 1.00) G. terraccianoana Pascher is separated from all other species. The latter form a polytomic subclade with G. xiphoidea, G. huochengensis, G. angelae, G. almaatensis and G. kuraminica × G. almaatensis clustering together (Fig. 2: subclade B-1; pp 1.00). A second subclade includes all samples of G. kuraminica from Kazakhstan, G. almaatensis × G. kuraminica and nine accessions of G. cf. turkestanica (Fig. 2: subclade B-2; pp 1.00). Finally, G. kuraminica 11 (holotype from Uzbekistan) and one accession of G. cf. turkestanica grouped together with all European species in subclade B-3 (Fig. 2; pp 1.00).
ITS data of Gagea filiformis and G. granulosa
Results from direct sequencing of the ITS region (ITS1 + 5.8S rRNA + ITS2) of Gagea filiformis (23 individuals of 13 populations) and Gagea granulosa (12 individuals of 8 populations) are given in Table 3 together with the altitudinal occurrence of the investigated plants in the Ili-Alatau range (for voucher information, see “Appendix”).
The ITS sequence of the investigated individual of Gagea granulosa (gra) from a morphologically uniform population (gra5: AP4-2013, 862 m a. s. l.; below the contact zone: 1089–1994 m a. s. l.) showed no ambiguous sites and corresponded to a published sequence of G. granulosa from Kazakhstan (EMBL/NCBI Accession Number AM287278; Peterson et al. 2008). Sixteen out of 17 G. filiformis individuals (fil) sampled in the contact zone and all six individuals of G. filiformis (fil10 and fil11: AP30-2013, fil12 and fil13: AP33-2013, fil14: AP34-2013, fil17: AP42-2013; Table 3) in altitudes above the contact zone (2380–2733 m a. s. l.) shared the identical ITS sequence lacking any ambiguous site. For both species, the ITS region differs in the Ili-Alatau range at 16 positions (ITS1: seven point mutations; ITS2: eight point mutations plus one indel of 1 bp length; Table 3). Based on these differences between G. filiformis and G. granulosa, we generated the putative ITS hybrid sequence resembling the parental sequence variation (see Table 3). The ITS sequence of three G. granulosa individuals (gra12 and gra14: AP45-2013, gra15: AP58-2013; Table 3) collected in the contact zone corresponded to the putative hybrid sequence. The ITS sequence of six further investigated individuals of G. granulosa from the contact zone also corresponded to this sequence in most of their position and corresponded to G. filiformis and G. granulosa, respectively, at the other positions (see Table 3). In addition, at same locations (AP45-2013, AP58-2013; Table 3) G. granulosa individuals with slightly different ITS sequences were found. Finally, two individuals of a morphologically uniform population of G. granulosa growing below the contact zone (gra6 and gra7: AP1-2013, 839 m a. s. l.) corresponded to the putative hybrid sequence at most but not all positions.
cpDNA haplotype network of sect. Minimae
For all accessions of sect. Minimae, including six species (including 64 sequences; 16 variable and parsimony-informative sites out of 418 total sites; alignment: Online Resource 2; for voucher information, see “Appendix”), TCS inferred a network with a connection limit of 19 steps and 49 haplotypes, 32 of these are recognized as missing intermediates (Fig. 3). Closest to the putative root of the network was the haplotype of Gagea nigra (separated by one step; Fig. 3). All samples of G. davlianidzeae, G. nigra and G. minima were found each with a single haplotype. The different haplotypes of G. filiformis (n = 9) and G. granulosa (n = 4) were found at distinct positions within the network separated by up to 30 (G. filiformis) and up to 9 steps (G. granulosa), respectively (Fig. 3). Also in the Ili-Alatau range, different haplotypes were observed for the two species of sect. Minimae (G. filiformis: n = 5, haplotypes c1, c3–c6; G. granulosa: n = 2, haplotypes c1 and c2; see Fig. 3). Eleven out of 12 G. granulosa individuals sampled in the elevational transect in the Ili-Alatau range (839–1994 m a. s. l.) had the haplotype c1 (Fig. 3; Table 3). Only for one G. granulosa individual (gra13: AP45-2013, 1941 m a. s. l.; Fig. 3) haplotype c2 was found. In contrast, in G. filiformis from the Ili-Alatau range transect, five cpDNA haplotypes were found with different altitudinal distributions (c1: 1994 m a. s. l.; c3: 1089–1941 m a. s. l., c4: 1099–2733 m a. s. l., c5 and c6: 1301 m a. s. l.; Fig. 3; Table 3).
cpDNA haplotype network of sect. Gagea
For the accessions of sect. Gagea including 27 species (including 69 sequences; 40 variable and 35 parsimony-informative sites out of 410 total sites; alignment: Online Resource 3; for voucher information, see “Appendix”), TCS inferred a network with a connection limit of 20 steps and 111 haplotypes, with 83 of these as missing intermediates (Fig. 4). Closest to the putative root of the network (Gagea cf. fedtschenkoana Pascher: fed2, fed3) was the haplotype of G. aipetriensis Levichev (separated by four steps only). Gagea almaatensis had a single haplotype (Fig. 4), which was observed as well for an individual morphologically intermediate between G. almaatensis and G. kuraminica (alm × kur: AP24b-2013), G. ancestralis, G. xiphoidea, and one accession from G. huochengensis. Also the haplotype of all investigated G. kuraminica samples from the Ili-Alatau range (Fig. 4) was identical (separated by 18 steps from the holotype from Usbekistan) but found as well for seven accessions of G. cf. turkestanica and a morphological intermediate between G. kuraminica and G. almaatensis (kur × alm: AP40-2013). For G. cf. turkestanica from Kazakhstan, we found five haplotypes separated by 3−36 steps (Fig. 4).
Discussion
Gagea species in the Ili-Alatau
Six of nine species found by us have already been recorded for Kazakhstan (Pavlov 1958; Baitenov 1969, 1985, 2001; for synonyms, see Levichev and Jezniakowsky 2008; and WCSP 2015): Gagea bulbifera (sect. Bulbiferae), G. divaricata (sect. Platyspermum), G. granulosa and G. filiformis (sect. Minimae), G. liotardii and G. tenera (sect. Didymobulbos s.l. according to Peruzzi et al. 2008a; see also Peruzzi et al. 2011; and Tison et al. 2013). Gagea liotardii (sect. Fistulosae, according to Levichev in Peterson et al. 2008), whose name is controversial (G. liotardii vs. G. fragifera; see Levichev 2006 and discussion and references in Peterson et al. 2011), was found in the Ili-Alatau not only in the alpine zone but also at lower altitudes (AP39-2013: disturbed alluvial forest, 1498 m a. s. l.), whereas the species occurred only between 2150 and 2350 m a. s. l. in the Chinese Tian-Shan (Peterson et al. 2011). According to our knowledge (see also Pavlov 1958; Baitenov 1958, 1969) G. granulosa constitutes a new record for the Ili-Alatau (Zailiysky Alatau).
Furthermore, we found three morphologically distinguishable species belonging to sect. Gagea. One of these species has morphological characters which allow to differentiate it from closely related species and is therefore described as G. almaatensis sp. nov. Based on morphological characters (see also Beisenova et al. 2014), individuals of several populations could be circumscribed as G. kuraminica although they were genetically clearly differentiated by both ITS and cpDNA data from the holotype (from Uzbekistan; Levichev 1988). In addition, we found plants resembling G. turkestanica Pascher. This taxon is considered as conspecific with G. capusii A.Terracc. in WCSP (2015) and in the Flora of Kazakhstan (Pavlov 1958), but Levichev recognizes it as an independent species (Levichev and Jezniakowsky 2008). Our material, here named G. cf. turkestanica, differs from G. capusii and G. turkestanica by candelabrum-like pedicels and a lower number of flowers. In contrast to G. almaatensis and G. kuraminica, the populations of G. cf. turkestanica have mostly individuals with a single flower (populations AP50-2013, AP54-2013, AP56-2013); some individuals possess a yellow tunic of the parent bulbs and darker, finely granulated bulbils (AP54-2013). According to the molecular results G. cf. turkestanica was found to be polymorphic in cpDNA sequences. Most investigated individuals were related to but clearly different from G. capusii (cpDNA and ITS data). Almost all investigated vouchers from Kazakhstan differ from material from Kyrgyzstan determined as G. turkestanica (cpDNA; ITS data not available). Several samples of G. cf. turkestanica are identical with G. kuraminica from Kazakhstan, in both ITS and cpDNA sequences. Therefore, the taxonomic status of our plants determined as G. cf. turkestanica remains unclear. The material may belong to a species complex including some closely related lowland species, or could represent a hybrid swarm between G. turkestanica and related species. The phylogenetic tree obtained in this study confirms earlier results: first, the monophyly of the sections Bulbiferae and Minimae [according to the classification of Levichev presented in Peterson et al. (2008), Peruzzi (2012a)], and second, the molecular differentiation of G. nigra from G. filiformis and all other representatives of sect. Minimae (Peterson et al. 2011).
However, the phylogenetic tree based on ITS sequences was characterized by polytomies within sect. Gagea which includes the apparently new taxon. Highly similar ITS and/or cpDNA regions between morphologically distinguishable taxa are frequently observed within sect. Gagea (China, Xinjiang province: Gagea angelae Levichev & Schnittler, G. huochengensis Levichev, Peterson et al. 2011; Europe: G. pomeranica Ruthe, G. megapolitana Henker, G. marchica Henker, Kiesew., U.Raabe & Rätzel; Henker et al. 2012; Peterson et al. 2004, 2009; this study) but as well in other sections of the genus (sect. Platyspermum: Zarrei et al. 2012; sect. Didymobulbos s.l.: Tison et al. 2013). In general, low variability in molecular markers indicates recent speciation (e.g., Eryngium: Calviño et al. 2008; Pimpinella: Wang et al. 2014) which is often connected with rapid radiations that coincided with the colonization of new territories. Also, Fernández-Mazuecos and Vargas (2015) found only low taxonomic signals in plastid DNA sequences of Linaria sect. Versicolores but a pronounced geographic structure and assumed rapid diversification of plastid DNA lineages. Our cpDNA network of the taxa from sect. Gagea seems to be geographically structured, too. For instance, European and eastern Asian species occur usually at the tips (see also Peterson et al. 2009). However, additional sampling is needed, including further taxa and geographical areas to allow for meaningful analyses. Furthermore, the resolution of phylogenetic relationships in Gagea could be improved by the application of additional molecular markers, e.g., additional cpDNA regions or low-copy genes. Increasing the number of cpDNA markers has been successfully used to obtain a higher resolution (Harpke et al. 2014) and better branch support although this is not guaranteed (discussed, e.g., in Calviño et al. 2010; Naciri and Linder 2015). Chloroplast capture/hybridization and incomplete sorting of ancestral lineages could confound phylogenetic inference (Gurushidze et al. 2010), and often, it is difficult to distinguish between incomplete lineage sorting and hybridization. However, nuclear single-copy markers can contribute to the detection of hybridization events. In Gagea, data from partial sequences of the nuclear single-copy conserved ortholog set (COS) gene pCOSAt103 (Peterson et al. 2011) revealed intra-sectional gene flow between closely related species in the sections Minimae and Gagea. This was in agreement with ITS and cpDNA data demonstrating these incongruences to be caused by hybridization. However, while such nuclear single-copy markers are suitable to detect recent or ancient hybridization (e.g., Erol et al. 2015), their suitability to define species borders of morphologically well differentiated species is limited. For instance, in allopolyploids frequently multiple copies can be found (Peterson et al. 2011; Harpke et al. 2015). Zarrei et al. (2012) found that haplotype lineages of the low-copy nuclear gene malate synthase from 12 taxa and 609 sequences in the Gagea reticulata species complex were not fully congruent with current species circumscription and morphology. The latter authors expect that additional data will not reveal a simple phylogenetic pattern in the actively evolving genus Gagea. This is in agreement with our experience from many years of morphological and molecular studies. AFLP (amplified fragment length polymorphism) or microsatellites may help to disentangle relationships among closely related taxa in the genus. This approach was successfully used in hybridizing and polyploid complexes (Doronicum, Asteraceae: Pachschwöll et al. 2015) as well as in young and or relatively rapidly evolving groups (Leptinella, Asteraceae: Himmelreich et al. 2014). Oberprieler et al. (2014) argue that the joint investigation of sequence and fingerprint data with biogeographical and ecological data is an effective way to disentangle reticulate relationships in polyploid species complexes. Although AFLPs are capable to resolve relationships among closely related species or within species, the marker is dominant and fragments are anonymous. This disadvantage can be avoided, when restriction-site-associated DNA sequencing (RADseq; e.g., Miller et al. 2007) or genotyping by sequencing (GBS; Elshire et al. 2011) is applied, as these methods generate mostly biallelic single nucleotide polymorphism (SNP) information in addition to dominant characters (0/1; if fragments are absent within certain individuals). These methods were already successfully applied in detecting hybridization events (e.g., Eaton and Ree 2013).
Hybridization among Gagea species in altitudinal contact zones
Hybridization has been shown to be an important evolutionary mechanism in plants (e.g., Abbott et al. 2013; Gómez et al. 2015) and an important driver of speciation processes in the species-rich genus Gagea (e.g., Peruzzi 2008; Peterson et al. 2009; Tison et al. 2013). Hybrid zones have the potential to generate evolutionary novelties through introgression (discussed, e.g., in Abbott and Brennan 2014; Gómez et al. 2015). For Gagea, hybridization can be expected in areas where closely related species come into contact. In the Ili-Alatau, in habitats with co-occurring, closely related species, morphologically and/or genetically intermediate individuals were observed. This study reveals intra-sectional hybridization in two species complexes, G. filiformis/Gagea granulosa (sect. Minimae) and G. almaatensis/G. kuraminica (sect. Gagea) in the Ili-Alatau range.
Morphological and molecular data indicate an ongoing introgression (for “introgressive hybridization,” see discussion in Harrison and Larson 2014) of Gagea filiformis into G. granulosa. In the broad contact zone (observed from 1089 to 1994 m a. s. l.) of these species, all investigated G. granulosa individuals had the same cpDNA haplotype (maternal part: G. granulosa) but intermediate ITS sequences resembling the parental sequence variation in G. filiformis and G. granulosa in different ways. The assumption of ongoing hybridization is supported by the observed co-occurrence of both species in almost all investigated sites in the altitudinal contact zone in the Ili-Alatau. In contrast, almost all investigated individuals of G. filiformis within and above the contact zone were found to have identical ITS sequences lacking any intermediate or ambiguous sites. Explanations could be that (i) hybridization is mostly unidirectional with G. granulosa as the maternal parent or (ii) it is presumably easier to differentiate G. filiformis (developing always one bulbil) from putative hybrids than G. granulosa, since hybridogenous plants are likely to develop more than one bulbil.
In the absence of reproductive isolation, species boundaries might easily be disrupted (discussed for Orchidaceae in Marques et al. 2014). This was also found in the Gagea lutea/G. pratensis species complex (sect. Gagea) where both parental species normally occurring in different habitats (in the same elevation) came in contact (Peterson et al. 2004, 2009; Zonneveld et al. 2015). Pfeiffer et al. (2013) showed that the taxa of the latter hybrid complex are not reproductively isolated and can interbreed, forming a hybrid swarm (see also discussion in Wörz et al. 2012). Several species of the taxonomically difficult sect. Minimae (eight species, Levichev in Peterson et al. 2008) frequently co-occurred (e.g.; G. filiformis, G. davlianidzeae, and G. lowariensis Pascher: Ali and Levichev 2007; I.G. Levichev personal observation; G. nigra and G. davlianidzeae in the Chinese Tian-Shan: Peterson et al. 2011; G. filiformis and G. granulosa in the Ili-Alatau: this study). In contrast to the situation found in the Chinese Tian-Shan (Peterson et al. 2011) where gene flow between G. nigra (990–2250 m a. s. l.) and G. davlianidzeae (1928–2250 m a. s. l.) was only rarely indicated in the small altitudinal contact zone (1928–2250 m a. s. l.) by molecular data (incongruent ITS and cpDNA data; data of pCOSAt103), in this study abundant gene flow between G. filiformis and G. granulosa was found. This is underlined by the observation that both G. filiformis and G. granulosa showed a comparably high seed set (Table 2). In contrast, seed set was observed in the Chinese Tian-Shan for G. nigra only but not for the morphologically uniform G. davlianidzeae. ITS and cpDNA data indicate a differentiation of G. nigra from all other representatives of its section which can be explained by stronger reproduction barriers leading to the endemic species G. nigra, which is closely related to G. filiformis but differs in both morphology and molecular traits. Several species of the sect. Minimae were found with different ploidy levels (discussed in Peterson et al. 2011; Peruzzi 2012b: 37 % of the investigated vouchers were polyploids) indicating intra-sectional hybridization. Although cpDNA lineages can display a clear geographic structure and are not necessarily in agreement with patterns of nuclear DNA data and/or taxonomic concepts (e.g., Fernández-Mazuecos and Vargas 2015), we expect haplotype pattern within sect. Minimae to be created mainly by hybridization. The network positions of the cpDNA haplotypes of G. filiformis from Kazakhstan separated by many steps are not in agreement with the geographical distribution of the respective accessions.
In contrast to the situation in the Chinese Tian-Shan, where gene flow between Gagea angelae (1980−2250 m a. s. l.) and G. huochengensis (1550−2250 m a. s. l.) was only evident in data of pCOSAt103 (Peterson et al. 2011), in this study hybridization between morphologically and molecularly well-differentiated G. kuraminica and G. almaatensis was indicated by incongruent ITS and cpDNA data found in morphologically intermediate individuals. In the latter, we did not found any intermediate or ambiguous position in ITS sequences. This indicates ancient hybridization events followed by concerted ITS evolution (discussed, e.g., in Koch et al. 2003). Gagea kuraminica showed regular seed set in the Ili-Alatau (34.7 ± 2.0 seeds per plant; n = 100). Unfortunately, for G. almaatensis no data on seed set are available (due to later flowering time and small population sizes). In the small contact zone between 2000 and 2400 m a. s. l. both species seem to prefer different habitats: G. almaatensis grows in avalanche gullies, while G. kuraminica grows in pastures. In addition, we expect hybridization events between G. kuraminica, inhabiting elevations from 1200 to 2400 m a. s. l., and the lowland populations of G. cf. turkestanica (800–1100 m a. s. l.), which may involve further, yet undiscovered lowland species. In the present study dealing with 27 of 56 species known for sect. Gagea (Peterson et al. 2008), 111 haplotypes were recognized with a high proportion (74.5 %) of missing intermediates. Even if the number of missing intermediates should decrease if further species are included, the distances in the cpDNA haplotype network are rather large. This indicates that the chloroplast genomes within the section had enough time to differentiate, probably benefiting from geographical isolation (e.g., between Europe and Asia). However, the presence of distinct haplotypes within one species or even population is better explained by assuming recent hybridization between previously differentiated species rather than incomplete lineage sorting.
Recent hybridization events are often expected to be caused by human activities, which facilitate contact between potentially hybridizing but geographically isolated species. About 25 % of the species endemic for the Spanish Sierra Nevada currently form hybrids, mostly with widespread lowland congeners (Gómez et al. 2015). A similar scenario was also discussed for the Gagea liotardii/Gagea villosa species complex of sect. Didymobulbos s.l. (Peruzzi et al. 2011). Both putative hybrids of the two species (Gagea microfistulosa Levichev and G. polidorii J.-M.Tison) grow at elevations lower than found for G. liotardii (alpine) but higher than G. villosa (lowlands and foothills). In the vicinity of the city of Almaty, still the largest urban center of Kazakhstan, we can as well expect hybridization caused by human impacts. The region has a long history of transhumance: livestock grazing on lowland steppes in winter and moves up to alpine meadows in summer. The pastures replacing forest vegetation were invaded by species from open grasslands of lowland steppes and alpine meadows, like Gagea species, where they came in contact and hybridized. In mountain ranges, dispersal of seeds, vegetative bulbils, and bulbs of Gagea is probably influenced by flooding, wind, avalanches, or animals (Levichev 2013). In a park within the city, we found a morphological uniform hybrid population of G. filiformis and G. granulosa below the altitudinal range of G. filiformis, and possibly this population was introduced from higher elevations by soil transport or plant stock. G. filiformis and G. granulosa abundantly grow together and hybridized over the whole broad contact zone (observed from 1089 to 1994 m a. s. l.). In contrast, we recorded putative hybrids of G. kuraminica and G. almaatensis also above the altitudinal distribution of both parental species (2733 m a. s. l.). Dispersal of seeds or bulbils by birds may provide an explanation (Levichev et al. 2010).
Conclusions
In different ranges of the Tian-Shan (for the eastern Chinese Tian-Shan, see Peterson et al. 2011) characterized by different assemblages of closely related Gagea species, hybridization in altitudinal contact zones seems to be evident. Our observations on species and their altitudinal distribution indicate that speciation in Gagea sect. Minimae could be driven mainly by hybridization, but in sect. Gagea by both hybridization and geographical isolation (see also Peterson et al. 2009, 2011). For the mesophilic species of sect. Gagea, we expect a high rate of diversification, speciation, and endemism especially in the mountains of the Tian-Shan range surrounded by steppes or irrigated farmland. The sharp differences in meso-climate between N- and S-exposed slopes, but as well the strong altitudinal precipitation gradient should favor ongoing local speciation processes. As a consequence of our geographically restricted studies and according to our cpDNA network, we expect that more, yet undiscovered species of sect. Gagea exist in the Tian-Shan mountains, representing a center of species diversity for Gagea.
Taxonomic treatment
Gagea almaatensis Levichev, A.Peterson & J.Peterson, sp. nov.—TYPE: Kazakhstan, Ili-Alatau range, Almaty, ca. 22 km S Almaty, Lake Bol. Almatinskoje, 2557 m a. s. l., 43°03′09″N, 76°59′23″E, 23 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP43-2013 (holotype: HAL119703, isotypes: HAL119702, LE01010036) (Figs. 5, 6).
Description: Plants occurring solitary or in small groups, 7.5–15 cm tall; glabrous except for pedicels and margins of inflorescence bracts. Bulbs obliquely drop-shaped, 7–10 mm in diameter in flowering plants, tunic pale brown, thin, and coriaceous. Juvenile plants develop a single vegetative bulbil per year. Dormant vegetative bulbils are characterized by a dark brown tunic with a heavy pitted structure resembling honey combs. Generative plants do not develop bulbils. Peduncles are 5.5–10.5 cm tall (3–5.5 cm above soil), in cross-sectional quadrangular, and 0.3–0.8 mm in diameter. Basal leaf single, linear, exceeding the inflorescence one-fourth to one-fifth, 2–4(5) mm wide, cross-sectional angular, its lower side with three indistinct keels. Inflorescence bracts 2–4, nearly opposite to each other, the lowermost floral leaf (the second basal leaf) concaulescent with the peduncle, slightly exceeding the inflorescence, (12)38–52 mm long and 1.5–3 mm wide, narrowly lanceolate, erect, sometimes the upper end slightly reclining. All inflorescence leaves possess white ciliate hairs on their margins. Inflorescence fasciculate, with (1)3–7 flowers, short branched, pedicels of different length, in length equal to the perigon of the flower or slightly exceeding it, erect, not candelabrum-like. Perigon leaves narrowly lanceolate, ends rounded, those of the external whorl hooded, 0.7–1.5 cm long and 1.5–2.5 mm wide, inside yellow, outside greenish; leaves of the outer whorl slightly larger than those of the inner whorl, the latter with yellow margins at the outer side. Ovary oblong, sessile. Anthers yellow.
Diagnosis: Gagea almaatensis differs from G. brevistolonifera Levichev, G. ancestralis Levichev, and G. xiphoidea Levichev by a single sessile bulbil; from G. praemixta Vved. and G. angelae Levichev & Schnittler by the absence of stolons; from G. longiscapa Grossh. by the bulbil focused downwards (not pressed up); from G. huochengensis Levichev by the heavily pitted tunic of the dormant bulbil, a basal leaf slightly exceeding the inflorescence and straight pedicels; therefore, the inflorescence lacks the candelabrum-like appearance.
Habitats: Alpine meadows and avalanche gullies between 2000 and 2500 m a. s. l.
Distribution area: Kazakhstan, Ili-Alatau range.
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Acknowledgments
For supporting field work and a research stay of S. Beisenova in Germany in the frame of its CabNet program, we wish to thank the German Academic Exchange Service (DAAD). Saltanat Beisenova wants to thank as well the authorities of N. I. Gumilyev Natl. Univ., Astana, for travel support and mentoring, in particular Prof. I. Bersimbayev. For providing further plant material, we would like to thank Jānis Rukšāns. We would like to thank the anonymous reviewers for helpful comments.
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Appendices
Appendix
Voucher information and GenBank accession numbers of the sequences used in this study. Taxon: place, date, collector, collection number: voucher number: EMBL/NCBI accession numbers: trnL–trnF IGS, psbA–trnH IGS, ITS1 + 5.8S rRNA + ITS2 (#sequences taken from EMBL/NCBI;—denotes lacking sequences). Information of collection dates, collectors, and collection numbers are only given for the material sampled in the Ili-Alatau range during the field excursion in 2013.
Gagea afghanica A.Terracc.: Iran, Province Khorasan: 52/04DNALevichevLE: HAL101785: –, –, AM087953. G. aipetriensis Levichev: Ukraine, Crimea: 15/04DNALevichevLE, HAL01801: AJ970178, AM049259, AM087955. G. almaatensis Levichev, A.Peterson & J.Peterson sp. nov.: (1) Kazakhstan, Ili-Alatau range, Almaty, 22 km S Almaty, Lake Bol. Almatinskoje, 2557 m a. s. l., 43°03′09″N, 76°59′23″E, 23 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP43a-2013: HAL119703, LE01010036: LN874781, LN874710, LN874873. (2) Kazakhstan, Ili-Alatau range, Almaty, 22 km S Almaty, Lake Bol. Almatinskoje, 2557 m a. s. l., 43°03′09″N, 76°59′23″E, 23 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP43b-2013: HAL119702: LN874782, LN874711, LN874874. (3) Kazakhstan, Ili-Alatau range, Almaty, 1.2 km NNW Shymbulak ski ressort, 1994 m a. s. l., 43°08′24″N, 77°04′25″E, 21 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP44a-2013: HAL119714: LN874783, LN874712, LN874875. (4) Kazakhstan, Ili-Alatau range, Almaty, 1.9 km S Shymbulak ski ressort, 2437 m a. s. l., 43°06′44″N, 77°04′26″E, 23 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP32-2013: HAL119695: LN874784, LN874713, LN874876. G. almaatensis × kuraminica: Kazakhstan: Ili-Alatau range: Almaty, 1.2 km NNW Shymbulak ski ressort, 1994 m a. s. l., 43°08′24″N, 77°04′25″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP24b-2013: HAL119688: LN874785, LN874714, LN874877. G. altaica Schischk. & Sumnev.: Kazakhstan, 51/04DNALevichevLE, HAL101786: –, –, AM162670. G. ancestralis Levichev: Russia, Republic Altai: 144/10DNALevichevLE: FR690249, FR690844, FR691052. G. angelae Levichev & Schnittler: (1) China, Xinjiang, Tian-Shan: LE00002135: FR690259, FR691028, FR690104. (2) China, Xinjiang, Tian-Shan: HAL108473: FR690266, FR691035, FR690111. (3) China, Xinjiang, Tian-Shan: HAL108477: FR690262, FR691031, –. G. artemczukii Krasnova: Ukraine, Crimea: 19/04DNALevichevLE, HAL101481: AM180470, AM409339, AM409331. G. bulbifera (Pall.) Salisb.: (1) China, Xinjiang, Urumqi: HAL107953: –, –, FR689753. (2) Russia, District Astrakhan: 2/04DNALevichevLE, HAL101840: –, –, AM162669. (3) Kazakhstan, Almaty, 14 km S Kapchagay, 521 m a. s. l., 43°44′24″N, 77°01′16″E, 19 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP11-2013: HAL118024: –, –, LN874788. (4) Kazakhstan, Almaty, 14 km S Kapchagay, 521 m a. s. l., 43°44′18″N, 77°00′43″E, 19 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP12-2013: HAL118026: –, –, LN874789. (5) Kazakhstan, Ili-Alatau range, Almaty, 2.1 km NE Medeu statium, 2003 m a. s. l., 43°10′12″N, 77°04′42″E, 20 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP18-2013: HAL118081: –, –, LN874790. (6) Kazakhstan, Ili-Alatau range, Almaty, 2.1 km NE Medeu statium, 2003 m a. s. l., 43°10′12″N, 77°04′42″E, 20 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler AP19a-2013: HAL119676, LE01010034: –, –, LN874791. (7) Kazakhstan, Ili-Alatau range, Almaty, 2.1 km NE Medeu statium, 2003 m a. s. l., 43°10′12″N, 77°04′42″E, 20 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP19b-2013: HAL119675: –, –, LN874792. (8) Kazakhstan, Ili-Alatau range, Almaty, 28 km W Almaty, small hills S Turar, 790 m a. s. l., 43°14′58″N, 76°32′13″E, 26 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP55-2013: HAL118028, LE01010035: –, –, LN874793. (9) Kazakhstan, Ili-Alatau range, Almaty, 29 km W Almaty, near settlement Uschkonyr, 864 m a. s. l., 43°13′15″N, 76°33′10″E, 26 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP57-2013: HAL118030: –, –, LN874794. G. capusii A.Terracc.: Uzbekistan: 24/04DNALevichevLE, HAL101839: AJ969123, AM085143, AM422455. G. circumplexa Vved.: Uzbekistan: 30/04DNALevichevLE, HAL101795: –, –, AM265529. G. confusa A.Terracc.: (1) Iran, Teheran: 13/04DNALevichevLE, HAL101803: AJ890369, AJ973173, AM087949. (2) #Iran: Zarrei&Zarrei35266(TUH)(Kew 23137): EU912267, EU939238, EU912040. (3) #Iran: TUH-EBOT.EXP.35712(TUH)(Kew 23169): EU912268, EU939239, EU912041. G. davlianidzeae Levichev: (1) China, Xinjiang, Tian-Shan: HAL107948: FR690236, FR690831, FR689755. (2) China, Xinjiang, Tian-Shan: HAL107943: FR690240, FR690835, FR689759. (3) China, Xinjiang, Tian-Shan: HAL107941: FR690241, FR690836, FR689760. (4) China, Xinjiang, Tian-Shan: HAL107946: FR690237, FR690832, –. (5) China, Xinjiang, Tian-Shan: HAL107939: FR690242, FR690837, –. G. divaricata Regel: (1) Kazakhstan, Almaty, 14 km S Kapchagay, 520 m a. s. l., 43°44′28″N, 76°01′20″E, 19 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP9a-2013: HAL118078, LE01010032: –, –, LN874795. (2) Kazakhstan: Almaty, 14 km S Kapchagay, 520 m a. s. l., 43°44′28″N, 76°01′20″E, 19 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP9b-2013: HAL118079: –, –, LN874796. (3) Kazakhstan, Kapchagay: 146/10DNALevichevLE: –, –, LN874797. G. dschungarica Regel: Kyrgyzstan: 14/04DNALevichevLE, HAL101802: –, –, AM087952. G. erubescens (Besser) Besser: Ukraine: 25/04DNALevichevLE, G-103LE, HAL103861: AM180469, AM238516, AM493953. G. fedtschenkoana Pascher: (1) Kazakhstan, Astana, mown lawns with steppe remnants near the administration building of the Gumilev University, Republican Ave, 360 m a. s. l., 51°10′52″N, 71°25′23″E: HAL117627: LN874767, LN874696, LN874849. G. cf. fedtschenkoana: (2) Kazakhstan, Tenis-Korgalshinskii nature reserve ca. 115 km WSW Astana, environs of the station 50°28′38″N, 250 m a. s. l., 69°32′44″E: HAL117626, LE01010043: LN874768, LN874697, LN874850. (3) Kazakhstan, Tenis-Korgalshinskii nature reserve ca. 115 km WSW Astana, steppe 2 km N of the station, 260 m a. s. l., 50°29′45″N, 69°32′48″E: HAL117628, LE01010044: LN874769, LN874698, LN874851. G. filiformis (Ledeb.) Kar. & Kir.: (1) Western Tian-Shan: 72/09DNALevichevLE: FR690250, FR690845, FR689768. (2) Kazakhstan: 12/04DNALevichevLE, HAL101804: AM084904, AM161459, AM180457. (3) Kazakhstan, Ili-Alatau foothills, Almaty, 5 km SE Almaty, Medeu valley, 1192 m a. s. l., 43°11′15″N, 77°00′07″E, 18 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP7b-2013: HAL118049: LN874716, LN874645, LN874809. (4) Kazakhstan: Ili-Alatau range: Almaty, 1.1 km NE Medeu statium, 1821 m a. s. l., 43°09′60″N, 77°04′28″, 20 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP14a-2013: HAL118050: LN874717, LN874646, LN874810. (5) Kazakhstan, Ili-Alatau range, Almaty, 1.1 km NE Medeu statium, 1821 m a. s. l., 43°09′60″N, 77°04′28″, 20 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP14b-2013: HAL118051: LN874718, LN874647, LN874811. (6) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP20a-2013: HAL118057, LE01010046: LN874719, LN874648, LN874812. (7) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler AP20b-2013: HAL118055: LN874720, LN874649, LN874813. (8) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP20c-2013: HAL118054: LN874721, LN874650, LN874814. (9) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP20d-2013: HAL118053: LN874722, LN874651, LN874815. (10) Kazakhstan, Ili-Alatau range, Almaty, 1.9 km S Shymbulak ski ressort, 2437 m a. s. l., 43°06′44″N, 77°04′06″, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler AP30a-2013: HAL119715: LN874723, LN874652, LN874816. (11) Kazakhstan, Ili-Alatau range, Almaty, 1.9 km S Shymbulak ski ressort, 2437 m a. s. l., 43°06′44″N, 77°04′06″, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP30b-2013: HAL118062: LN874724, LN874653, LN874817. (12) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km SSW Shymbulak ski ressort, 2380 m a. s. l., 43°06′59″N, 77°04′26″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP33a-2013: HAL118065: LN874725, LN874654, LN874818. (13) Kazakhstan, Ili-Alatau range: Almaty, 1.5 km SSW Shymbulak ski ressort, 2380 m a. s. l., 43°06′59″N, 77°04′26″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP33b-2013: HAL118064: LN874726, LN874655, LN874819. (14) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km SSW Shymbulak ski ressort, 2380 m a. s. l., 43°06′59″N, 77°04′26″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP34-2013: HAL118063: LN874727, LN874656, LN874820. (15) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km NW Medeu stadium, 1498 m a. s. l., 43°10′09″N, 77°02′25E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP38a-2013: HAL118067: LN874728, LN874657, LN874821. (16) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km NW Medeu stadium, 1498 m a. s. l., 43°10′09″N, 77°02′25″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP38b-2013: HAL118068: LN874729, LN874658, LN874822. (17) Kazakhstan, Ili-Alatau range, Almaty, 22 km S Almaty, Lake Bol. Almatinskoje, 2733 m a. s. l., 43°03′22″N, 76°58′05″E, 23 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP42-2013: HAL118069: LN874730, LN874659, LN874823. (18) Kazakhstan, Ili-Alatau foothills, Almaty, 4 km SE Almaty, around TV tower, 1099 m a. s. l., 43°13′36″N, 76°58′26″E, 25 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP51-2013: HAL118070: LN874731, LN874660, LN874824. (19) Kazakhstan, Ili-Alatau foothills, Almaty, 4 km SE Almaty, around TV tower, 1089 m a. s. l., 43°13′50″N, 76°58′29″E, 25 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP52-2013: HAL118073: LN874732, LN874661, LN874825. (20) Kazakhstan: Ili-Alatau foothills: Almaty, 3 km NW Medeu stadium, 1301 m a. s. l., 43°10′48″N, 77°00′43″E, 27 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP59a-2013: HAL118074: LN874733, LN874662, LN874826. (21) Kazakhstan: Ili-Alatau foothills, Almaty, 3 km NW Medeu stadium, 1301 m a. s. l., 43°10′48″N, 77°00′43″E, 27 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP59b-2013: HAL118075: LN874734, LN874663, LN874827. (22) Kazakhstan: Ili-Alatau foothills: Almaty, 3 km NW Medeu stadium, 1301 m a. s. l., 43°10′48″N, 77°00′43″E, 27 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP59c-2013: HAL118076: LN874735, LN874664, LN874828. (23) Kazakhstan: Ili-Alatau range: Almaty, 1 km SSE Medeu stadium, 1875 m a. s. l., 43°09′06″N, 77°04′01″, 29 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP60-2013: HAL118077: LN874736 LN874665, LN874829. (24) Kazakhstan, Ili-Alatau range, Almaty, 1.2 km NNW Shymbulak ski ressort, 1994 m a. s. l., 43°08′24″N, 77°04′25″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP25-2013: HAL118059: LN874737, LN874666, LN874830. (25) Kazakhstan, Mountains over Almaty, at Observatory: DNAIPK12KZ-123: –, –, LN874831. (26) Kazakhstan: Sharyn Canyon: HAL115984: LN874738, LN874667, LN874832. (27) Kazakhstan, Mramornij (Marble) pass, W end of Altai: DNA IPK12KZ-102: –, –, LN874833. (28) Kazakhstan, near Kegen Pass, HAL116095: LN874739, LN874668, LN874834. (29) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°8′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP23-2013: HAL118058: LN874740, LN874669, –. (30) Kazakhstan, Ili-Alatau foothills: Almaty, 5 km SE Almaty, Medeu valley, 1192 m a. s. l. 43°11′15″N, 77°00′07″, 18 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP7c-2013: HAL118039: LN874753, LN874682, LN874847. G. graeca (L.) Irmisch.: Greece, Crete: HAL105185: –, –, AM939649. G. graminifolia Vved.: Kyrgyzstan, 114/09DNALevichevLE: –, –, FR689769. G. granulosa Turcz.: (1) –: 11a/04DNALevichevLE, HAL101805: –, –, AM265533. (2) Russia, Sibiria: 141/09DNALevichevLE: FR690253, FR690848, –. (3) Ukraine, Poltava: 100/09DNALevichevLE: FR690252, FR690847, –. (4) Kazakhstan, Tian-Shan: 11b/04DNALevichevLE, HAL101836: AM180463, AM238517, AM287278. (5) Kazakhstan, Ili-Alatau foothills, Almaty, 862 m a. s. l., 43°13′34″N, 76°54′49″E, 18 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP4-2013: HAL118037: LN874741, LN874670, LN874835. (6) Kazakhstan, Ili-Alatau foothills, Almaty, 839 m a. s. l., 43°14′57″N, 76°56′42″E, 17 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP1a-2013: HAL118035, LE01010049: LN874742, LN874671, LN874836. (7) Kazakhstan, Ili-Alatau foothills, Almaty, 839 m a. s. l., 43°14′57″N, 76°56′42″E, 17 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP1b-2013: HAL118033: LN874743, LN874672, LN874837. (8) Kazakhstan, Ili-Alatau foothills, Almaty, 5 km SE Almaty, Medeu valley, 1192 m a. s. l., 43°11′15″N, 77°00′07″E, 18 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP7a-2013: HAL118038: LN874744, LN874673, LN874838. (9) Kazakhstan, Ili-Alatau range, Almaty, 300 m NW Medeu statium, 1721 m a. s. l., 43°09′37″N, 77°03′33″E, 20 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP13-2013: HAL118040: LN874745, LN874674, LN874839. (10) Kazakhstan, Ili-Alatau range, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP21-2013: HAL118042: LN874746, LN874675, LN874840. (11) Kazakhstan, Ili-Alatau range, Almaty, 1.2 km NNW Shymbulak ski ressort, 1994 m a. s. l., 43°08′24″N, 77°04′25″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP28-2013: HAL118043: LN874747, LN874676, LN874841. (12) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP45a-2013: HAL118046: LN874748, LN874677, LN874842. (13) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP45b-2013: HAL118045: LN874749, LN874678, LN874843. (14) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP45c-2013: HAL118044: LN874750, LN874679, LN874844. (15) Kazakhstan, Ili-Alatau foothills, Almaty, 3 km NW Medeu stadium, 1301 m a. s. l., 43°10′48″N, 77°00′43″E, 27 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP58a-2013: HAL118048: LN874751, LN874680, LN874845. (16) Kazakhstan, Ili-Alatau foothills, Almaty, 3 km NW Medeu stadium, 1301 m a. s. l., 43°10′48″N, 77°00′43″E, 27 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP58b-2013: HAL118047: LN874752, LN874681, LN874846. (17) Kazakhstan, near Panteleimonovka vil.,: DNA12KZ-117: –, –, LN874848. G. helenae Grossh: Russia, Dagestan: 22/04DNALevichevLE, HAL101798: AJ969120, AM161461, AM265531. G. huochengensis Levichev: (1) China, Xinjiang, Tian-Shan: HAL108466: FR690269, FR691038, FR690114. (2) Kazakhstan: 132/09DNALevichevLE, HAL107949: FR690274, FR691042, FR690118. (3) China, Xinjiang, Tian-Shan: HAL108468: FR690272, FR691041, –. (4) China, Xinjiang, Tian-Shan: HAL108467: FR690271, FR691040, –. G. jensii Levichev & Schnittler: China, Xinjiang: HAL108482: FR690256, FR691025, FR690101. G. kuraminica Levichev (1) Kazakhstan, Ili-Alatau foothills, Almaty, 5 km SE Almaty, Medeu valley, 1192 m a. s. l., 43°11′15″N, 77°00′07″E, 18 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP6-2013: HAL119683, LE01010038: LN874770, LN874699, LN874852. (2) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km NE Medeu statium, 1920 m a. s. l., 43°10′02″N, 77°04′36″E, 20 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP16-2013: HAL119685, LE01010050: LN874771, LN874700, LN874853. (3) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km NW Medeu stadium, 1498 m a. s. l., 43°10′09″N, 77°02′25″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP49-2013: HAL119704, LE01010042: LN874772, LN874701, LN874854. (4) Kazakhstan, Ili-Alatau range, Almaty, 1.2 km NNW Shymbulak ski ressort, 1994 m a. s. l., 43°08′24″N, 77°04′25″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP24a-2013: HAL119687: LN874773, LN874702, LN874855. (5) Kazakhstan, Ili-Alatau range, Almaty, 1.2 km NNW Shymbulak ski ressort, 1994 m a. s. l., 43°08′24″N, 77°04′25″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP24c-2013: HAL119689: LN874774, LN874703, LN874856. (6) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km SSW Shymbulak ski ressort, 2380 m a. s. l., 43°06′59″N, 77°04′26″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP36c-2013: HAL119697: LN874775, LN874704, LN874857. (7) Kazakhstan, Ili-Alatau range, Almaty, 1.2 km NNW Shymbulak ski ressort, 1994 m a. s. l., 43°08′24″N, 77°04′25″E, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP44b-2013: HAL119713: LN874776, LN874705, LN874858. (8) Kazakhstan, Ili-Alatau range, Almaty, 1.5 km SSW Shymbulak ski ressort, 2380 m a. s. l., 43°06′59″N, 77°04′26″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP37-2013: HAL119700, LE01010038: LN874777, LN874706, LN874859. (9) Kazakhstan, Ili-Alatau range, Almaty, 1.9 km S Shymbulak ski ressort, 2437 m a. s. l., 43°06′44″N, 77°04′26″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP29a-2013: HAL119693, LE01010040: LN874778, LN874707, LN874860. (10) Kazakhstan, Ili-Alatau range, Almaty, 1.9 km S Shymbulak ski ressort, 2437 m a. s. l., 43°06′44″N, 77°04′26″, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP29b-2013: HAL119692: LN874779 LN874708, LN874861. (11) Uzbekistan, Tian-Shan, Kurama range, 2500 m a. s. l.,: 151/14DNALevichevLE (holotype): LN874780, LN874709, LN874862. G. kuraminica × almaatensis Kazakhstan, Ili-Alatau range, Almaty, 22 km S Almaty, Lake Bol. Almatinskoje, 2733 m a. s. l., 43°03′22″N, 76°58′05″E, 23 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP40-2013: HAL119701: LN874786, LN874715, LN874878. G. liotardii (Sternberg) Schult. et Schult.f. (= G. fragifera (Vill.) Ehr.Bayer & G.López): (1) China, Xinjiang, Tian-Shan: HAL107898: –, –, FN868162. (2) Ukraine, Crimea: 29a/04DNALevichevLE, HAL101797: –, –, AM265532. (3) Italy: CLU12693: –, –, AM422468. (4) Kazakhstan: 29b/04DNALevichev LE, HAL101796: –, –, AM180455. (5) Kazakhstan, Tenis-Korgalshinsky Nature Reserve, Astana: HAL117634: –, –, LN874799. (6) Kazakhstan, Ili-Alatau range, Almaty, 1.7 km NW Shymbulak ski ressort, 1941 m a. s. l., 43°08′30″N, 77°03′51″, 21 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP22-2013: HAL118013, LE01010041: –, –, LN874800. (7) Kazakhstan, Ili-Alatau range, Almaty, 1.9 km S Shymbulak ski ressort, 2437 m a. s. l., 43°06′44″N, 77°04′26″, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP31-2013: HAL118015: –, –, LN874801. (8) Kazakhstan, Ili-Alatau range, 1.5 km NW Medeu stadium, road to Medeu, 1498 m a. s. l., 43°10′09″N, 77°02′25″E, 22 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP39-2013: HAL118018: –, –, LN874802. (9) Kazakhstan, Ili-Alatau range, Lake Bol. Almatinskoje, 2733 m a. s. l., 43°03′22″N, 76°58′05″E, 23 Apr 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP41-2013: HAL118032: –, –, LN874803. (10) Kazakhstan, Mountains over Almaty: DNA IPKKZ124: –, –, LN874804. (11) Morocco: Marrakech: HAL116006: –, –, LN874805. G. lutea Ker Gawl.: (1) Germany, Saxony-Anhalt: –: AJ419165, AJ416368, AJ427544. (2) Russia, Caucasus: 16/04DNALevichevLE, HAL101800: AM110255, AM161456, AM265530. (3) Italy, Calabria CLU12696: AM265606, AM409354, AM287282. (4) #Iran: Zarrei35285(TUH)(Kew 23148): EU912281, EU939250, EU912052. G. marchica Henker, Kiesew., U.Raabe & Rätzel: Germany, Alt-Zeschdorf: HAL118006: LN874754, LN874683, LN874808. G. megapolitana Henker: Germany: HAL101644: AM084902, AM161455, AM931553. G. minima (L.) Ker Gawl.: (1) Italy, Calabria, Pollino Massif: CLU12698: AM283109, AM282996, AM287273. (2) Ukraine, Carpathians: 9/04DNALevichevLE, HAL101808: AM238539, AM238524, AM087948. (3) Russia, Republic Tatarstan, Nizhnyaya Kama: 10/04DNALevichevLE, HAL101806: AM180471, AM238519, AM180459. (4) Germany, Saxony-Anhalt: –: AJ419164, AJ416374, AJ427546. G. nakaiana Kitag.: Russia, Khabarovsk Territory: 17/04DNALevichev, 55LE, HAL101799: AM110256, AM161457, AM180454. G. neopopovii Golosk.: Eastern Kazakhstan, Za-Iliskii Altai: 120/09DNALevichevLE: –, –, FR689770. G. nigra L.Z.Shue, emend. Schnittler: (1) China, Xinjiang, Urumqi: HAL108464: FR690123, FR691010, FR690081. (2) China, Xinjiang, Urumqi: HAL108452: FR690135, FR691022, FR690095. (3) China, Xinjiang, Urumqi (N9714, Sichuan Univ., Chengdu): 134/10DNALevichevLE: FR690137, FR691024, –. (4) China, Xinjiang, Tian-Shan, Bogda-Shan, Tianchi Lake: HAL108459: FR690125, FR691012, FR690083. (5) China, Xinjiang, Tian-Shan, Bogda-Shan, Tianchi Lake: HAL108460: FR690128, FR691015, –. (6) China, Xinjiang, Tian-Shan, Bogda-Shan, Tianchi Lake: HAL108456: FR690129, FR691016, –. (7) China, Xinjiang, Tian-Shan, Bogda-Shan, Tianchi Lake: HAL108183: FR690131, FR691018, –. (8) China, Xinjiang, Tian-Shan, Bogda-Shan, Tianchi Lake: HAL108457: FR690132, FR691019, –. (9) China, Xinjiang, Tian-Shan, Bogda-Shan: HAL108184: FR690134, FR691021, –. G. ova Stapf: China, Xinjiang, Urumqi: HAL107951: –, –, FR689762. G. paczoskii (Zapal.) Grossh.: Italy: HAL104323: AM903072, AM903061, AM903051. G. pauciflora Turcz. ex Ledeb.: Mongolia, Ulan Bator: HAL070423: –, –, AM409330. G. podolica Schult. & Schult.f.: Ukraine: 21/04DNALevichevLE, HAL101832: AM084903, AM238525, AM409334. G. pomeranica Ruthe: (1) Germany, Saxony-Anhalt HAL095842: AJ419167, AJ416375, AJ427543. (2) Germany, Mecklenburg-Western Pomeranica: HAL095846: LN874787, AJ429194, –. G. pratensis (Pers.) Dumort.: (1) Germany, Saxony-Anhalt: HAL095847: AJ419162, AJ416372, AJ427542. (2) Italy: CLU12703, AM265607, AM903059, AM903047. G. pusilla (F.W.Schmidt) Sweet: cultivated: 18/04DNALevichevLE, HAL101831: AM180464, AM161458, AM422453. G. reticulata (Pall.) Schult. et Schult.f.: Israel, Central Negev: Z34650: –, –, AM087954. G. rubicunda Meinsh. emend. Levichev: Estonia: 26/04DNALevichevLE, HAL103855: AM238541, AM409338, AM493954. G. rufidula Levichev: (1) China, Xinjiang, Tian-Shan: HAL107929: –, –, FR689764. (2) Kyrgyzstan: 149/09DNALevichevLE: –, –, FR689767. G. serotina (L.) Ker Gawl. (=Lloydia serotina (L.) Reichenb.): (1) Kazakhstan: 45a/04DNALevichevLE, HAL101789: –, –, AM087956. (2) Russia, Karachaevo-Cherkessian Rep.: HAL117624: –, –, LN874806. (3) USA, Alaska, Alaska range: HAL117490: –, –, LN874807. G. shmakoviana Levichev: Russia, Altai: 23/04DNALevichevLE, HAL101830: AM265520, AM287265, AM422454. G. spathacea (Hayne) Salisb.: Germany, Saxony-Anhalt: HAL095844: –, –, AJ427541. G. stipitata Merckl. ex Bunge: Iran, Province Khorasan: 49/04DNALevichevLE, HAL101828: –, –, AM409336. G. tenera Pascher: (1) Kyrgyzstan: HAL101843: –, –, AM422460. (2) Iran: Zarrei & Golzarian 35256(TUH)(Kew 23152): –, –, EU912074. (3) Kazakhstan, Ili-Alatau foothills, Almaty, 831 m a. s. l., 43°15′0″N, 76°56′41″E, 18 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP3-2013: HAL118080, LE01010033: –, –, LN874798. G. terraccianoana Pascher: (1) Russia: 55/04DNALevichevLE, HAL103853: AM287280, AM287268, AM493955. (2) Mongolia: Bogd-Ul Mountains: HAL070426: AJ890367, AJ973169, –. G. tisoniana Peruzzi, Bartolucci, Frignani & Minutillo: Italy: CLU14920: AM409358, AM409349, AM422466. G. transversalis Steven: Ukraine, Crimea: 56/04DNALevichevLE, 365LE, HAL101783: AJ890370, AJ973167, AM162671. G. turkestanica Pascher: (1) Kyrgyzstan: 20/04DNALevichevLE, HAL103850: AM238534, AM287267, –. G. cf. turkestanica (2) Kazakhstan, Ili-Alatau range, Almaty, 28 km W Almaty, small hills S Turar, 790 m a. s. l., 43°14′58″N, 76°32′13″E, 26 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP54a-2013: HAL119707, LE01010039: LN874755, LN874684, LN874863. (3) Kazakhstan: Ili-Alatau range: Almaty, 28 km W Almaty, small hills S Turar, 43°14′58″N, 76°32′13″E, 790 m a. s. l., 26 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP54b-2013: HAL119710: LN874756, LN874685, LN874864. (4) Kazakhstan, Ili-Alatau foothills, Almaty, Panfilov park, 831 m a. s. l., 43°15′00″N, 76°56′41″E, 24 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP46-2013: HAL118082: LN874757, LN874686, LN874865. (5) Kazakhstan, Almaty: 130/09DNALevichevLE: LN874758, LN874687, LN874866. (6) Kazakhstan, Jezkazgan: 131/09DNALevichevLE: LN874759, LN874688, –. (7) Kazakhstan, Almaty, 950 m a. s. l.: 119/09DNALevichevLE: LN874760, LN874689, –. (8) Kazakhstan, Ili-Alatau foothills: Almaty, 831 m a. s. l., 43°15′00″N, 76°56′41″E, 18 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP2a-2013: HAL119678: LN874761, LN874690, LN874867. (9) Kazakhstan, Ili-Alatau foothills, Almaty, 831 m a. s. l., 43°15′00″N, 76°56′41″E, 18 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP2a-2013: HAL119679: LN874762, LN874691, LN874868. (10) Kazakhstan, Ili-Alatau foothills, Almaty, 862 m a. s. l., 43°13′34″N, 76°54′49″E, 18 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP2a-2013: HAL119680: LN874763, LN874692, LN874869. (11) Kazakhstan, Ili-Alatau foothills, Almaty, 4 km SE Almaty, park around the TV tower, 1119 m a. s. l., 43°13′49″N, 76°58′38″E, 25 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP53-2013: HAL119708: LN874764, LN874693, LN874870. (12) Kazakhstan, Ili-Alatau foothills, Almaty, 4 km SE Almaty, around TV tower, 1099 m a. s. l., 43°13′36″N, 76°58′26″E, 25 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP50-2013: HAL119705: LN874765, LN874694, LN874871. (13) Kazakhstan, Ili-Alatau range, Almaty, 29 km W Almaty, near settlement Uschkonyr, 864 m a. s. l., 43°13′15″N, 76°33′10″E, 26 April 2013, A. and J.Peterson, S.Beisenova, M.Schnittler, AP56-2013: HAL119711: LN874766, LN874695, LN874872. G. uliginosa Siehe & Pascher: #Iran: Zarrei et al. TUH-EBOT.EXP.35304,(TUH)(Kew 23153): –, –, EU912089. G. vegeta Vved.: Uzbekistan: 32/04DNALevichev, 339aLE, HAL103691: –, –, AM287275. G. villosa (Bieb.) Sweet: Germany, Saxony-Anhalt: –: –, AJ427545. G. xiphoidea Levichev: (1) Russia, Republic Altai: 71/09DNALevichevLE: FR690138, FR691044, FR690097. (2) Russia, Republic Altai, district Kosch-Agaczensis: 102/09DNALevichevLE: FR690139, FR691045, FR690098. G. cf. xiphoidea (3) China, Xinjiang, Tian-Shan: HAL108479: FR690140, FR691046, FR690099. Tulipa cretica Boiss. & Heldr.: Greece, Crete: HAL099934: –, –, AM180461.
Information on Electronic Supplementary Material
Online Resource 1 ITS alignment used for BI and resulting tree.
Online Resource 2 cpDNA alignment used for TCS of sect. Minimae.
Online Resource 3 cpDNA alignment used for TCS of sect. Gagea.
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Peterson, A., Harpke, D., Levichev, I.G. et al. Morphological and molecular investigations of Gagea (Liliaceae) in southeastern Kazakhstan with special reference to putative altitudinal hybrid zones. Plant Syst Evol 302, 985–1007 (2016). https://doi.org/10.1007/s00606-016-1313-7
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DOI: https://doi.org/10.1007/s00606-016-1313-7