42 (1): (2018) 71-90
Original Scientific Paper
Distribution and variability of the Balkan endemic
Geum bulgaricum (Rosaceae) - a species of European
concern
Dmitar Lakušić1✳, Gordana Tomović1, Chavdar Gussev2, Zoltán Barina3, Sonja
Siljak-Yakovlev 4, Nevena Kuzmanović1, Ivana Janković1 and Snežana Vukojičić1
1 University of Belgrade, Faculty of Biology, Institute of Botany and Botanical Garden, Takovska 43, 11000 Belgrade,
Serbia
2 Institute of Biodiversity and Ecosystem Research, Bulgarian Academy of Sciences, Acad. Georgi Bonchev St., bl.
23, 1113 Sofia, Bulgaria
3 Department of Botany, Hungarian Natural History Museum, H-1431 Budapest, Pf. 137, Hungary.
4 Ecologie Systématique Evolution, Univ. Paris-Sud, CNRS, AgroParisTech, Université Paris-Saclay, 91400, Orsay,
France
ABSTRACT: As a European endemic restricted to a few European countries, Geum bulgaricum is here
treated as a “target species” or “species of European concern”. Although of great international
significance, its distribution is insufficiently known. Based on several years of field studies and
analyses of herbarium and literature data, we have determined that G. bulgaricum is a Balkan
endemic plant distributed in Albania, Bosnia and Herzegovina, Bulgaria, Montenegro, and
Serbia. Although the range of its distribution is divided into two main parts - “eastern” (the
Rila Mountains in the Rhodope-Rila mountain system) and “western” (several mountains in
the Dinaric system and one isolated population in the northeastern part of the Scardo-Pindic
system) - in fact all populations are grouped into four disjunctions. Based on our studies of
extensive chorological data and estimation of the number of individuals and condition of the
populations, we have now defined G. bulgaricum as IUCN NT in Albania and Montenegro, and
VU D2 E in Serbia. Also, we have confirmed its status as NT in Bulgaria, and changed its status
from LR to VU D2 E in Bosnia and Herzegovina. The species is most often found in alpine
and subalpine acidophilous (Juncetea trifidi) and calcicolous (Elyno-Seslerietea) grasslands and
swards, as well as in the vegetation of scree habitats (Thlaspietea rotundifolii), rocky crevices
(Asplenietea trichomanis), subalpine belts of krummholz pine (Roso pendulinae-Pinetea
mugo), and very localised serpentine outcrops. Its ecological optimum is in the subalpine and
alpine vegetation belt. Furthermore, we here provide the first insight into the differentiation
of its populations. We found that the Rhodope-Rila and Dinaric populations are slightly
differentiated on the morphological level and well differentiated with respect to genome size.
The name Geum bulgaricum is lectotypified.
Keywords: Balkan Peninsula, endangered species, genome size, Geum, lectotype, morphology
Received: 04 May 2017
Revision accepted: 17 August 2017
UDC: 497:58.1:574.9
DOI: 10.5281/zenodo.1173554
correspondence: dlakusic@bio.bg.ac.rs
✳
© 2018 Institute of Botany and Botanical Garden Jevremovac, Belgrade
vol. 42 (1)
72
INTRODUCTION
MATERIALS AND METHODS
The species Geum bulgaricum was described by Josif
Pančić (1814–1888) on the basis of material collected
in August of 1882 in the Rila Mountains of Bulgaria
(Pančić 1883). This is a European endemic (Gajewski 1968; Ozinga & Schaminée 2005; Kurtto 2009)
distributed in the central part of the Balkan Peninsula (Gajewski 1957; Kurtto et al. 2004). Although the
species was declared to be a “target species” or “species
of European concern” (Ozinga & Schaminée 2005),
its distribution is insufficiently known. To be specific,
Ozinga & Schaminée (2005) stated that the species has
been registered in three countries, Kurtto (2009) in
four countries, but in fact it is distributed in five Balkan
countries with two disjoint parts of its range. One group of populations inhabits subalpine and alpine habitats
on the siliceous bedrock of the Rila Mountains in the
Rhodope-Rila mountain system, while the other group
inhabits high mountain carbonate habitats of the Dinaric mountain system (mountain systems according to
Stevanović et al. 2009).
After the last consolidation of the list of strictly
protected plant species, G. bulgaricum was included
in Annex I of the Bern Convention (Heywood 2009).
According to national legislations, G. bulgaricum is a
protected species in Bulgaria (BDA 2007), Montenegro
(Sl RCG 76/2006), and Serbia (Sl RS 5/2010), and it is
included in the red lists of the floras of Bosnia and Herzegovina (as LR in Đug et al. 2013) and Bulgaria (as
NT in Peev & Tsoneva 2009).
Although it is of great international importance,
data on the distribution of this species are scattered in
numerous papers and herbarium collections, and precise or georeferenced records are lacking. Also, there
are no data regarding its inclusion in any known recovery program (Heywood 2009).
Recent findings of Geum bulgaricum at several localities in Montenegro and Albania, as well as the availability of a number of herbarium specimens collected on different sites in Bulgaria, Serbia, Montenegro,
Albania, and Bosnia and Herzegovina, have provided
new insights into the distribution and the need to protect this internationally significant species. Hence, the
main aim of this contribution was to gather all known
data about distribution of the species and its ecological
affinities in order to provide detailed information for
efficient conservation planning. Given that up to now
G. bulgaricum was not the object of any detailed studies, our second aim was to provide preliminary insight
into morphological variability, variability of genome
size, and the presumed differentiation between the
Rhodope-Rila and the Dinaric populations.
Distribution and estimation of threatened status. Our
investigations are based on recent field studies, analysis of herbarium material deposited at BEO, BEOU, BP,
BREM, P, SARA, SO, and SOM (acronyms according to
Thiers 2017), and literature data. Data on occurrence of
the species in the field were recorded using a GPS device (Garmin eTrex Legend HCx and Garmin eTrex Vista
C). All other data on the distribution were georeferenced
in the OziExplorer 3.95 4s program. The chorological
data are presented using a grid map with squares of c. 10
km × 10 km based on the universal transverse Mercator
(UTM) projection (Lampinen 2001), grid zone 34T. Latitudes and longitudes are given in terms of the World
Geodetic System 84 (WGS84).
Estimation of the threatened status of G. bulgaricum
on the territories of Europe, Bulgaria, Serbia, Montenegro, Albania, and Bosnia and Herzegovina was based on
IUCN (2001) criteria and categories.
Morphometric analyses. Morphological study and
morphometric analyses were carried out on herbarium
specimens from the Rila Mountains in Bulgaria, Mt.
Čvrsnica in Bosnia and Hercegovina, and the Prokletije
Mountains in Montenegro deposited in BEOU and SOM.
The 16 morphological character states measured in this
study are listed in Table 1. Descriptive statistics were
calculated for each character state. A principal component analysis (PCA) was performed on the complete
dataset to show the overall morphological variation and
the relationships between individuals. The hypothesis of
morphological separation of the three analysed populations was tested by a canonical discriminant analysis
(CDA). Tukey’s HSD post-hoc test of homogenous groups for unequal N was used to check the significance of
morphological differences. All measurements were performed using Digimizer Image Analysis software, Version 4.6.1 (MedCalc Software 2005–2016). Statistical
analyses were performed using the Statistica 7.0 package
(StatSoft 1996).
Flow cytometry for genome size assessment. For genome size measurements, 15 individuals were analysed
from three populations of G. bulgaricum (five individuals
from each of the three populations, viz., those of the Mt.
Rila, Mt. Čvrsnica, and the Prokletije Mountains). DNA
amounts were determined by flow cytometry following
Marie & Brown (1993). Cell nuclei were isolated from
young leaves of at least five individuals per population.
Tomato [Solanum lycopersicum Montfavet ‘63-5’ (2C =
1.99 pg, Lepers-Andrzejewski et al. 2011)] was used
as an internal standard. The standard and investigated
species leaf tissues were simultaneously chopped with a
razor blade in a Petri dish in 600 μl of cold buffer (Gif
D. Lakušić et al.: Distribution and variability of Geum bulgaricum
Nuclear Buffer) of the following composition: 45 mM
MgCl 2, 30 mM sodium citrate, 60 mM 4-morpholinepropane sulphonate (pH 7), 0.1 % (w/v) Triton X-100, 1%
polyvinylpyrrolidone (~10,000Mr, Sigma P6755), 5 mM
sodium metabisulphite, and 10 µg/ml RNase (Sigma Aldrich, Saint Quentin, France). The suspension of nuclei
was filtered through nylon mesh (pore size 30 µm) and
kept at 4°C. Nuclei were stained with 50 μg/ml propidium iodide (Sigma), a specific DNA fluorochrome-intercalating dye. For each sample, at least 5 000 to 10 000
nuclei were measured. The 2C DNA value was calculated using the linear relationship between the fluorescent
signals from stained nuclei of unknown Geum species
and the known Solanum lycopersicum internal standard. Tukey’s HSD post-hoc test of homogenous groups
was used to analyse the differences in genome size of the
three populations.
RESULTS
Distribution and ecology. Geum bulgaricum is a Balkan
endemic plant distributed in Albania, Bosnia and Herzegovina, Bulgaria, Montenegro, and Serbia. Although
the range of its distribution is divided into two main
parts - “Eastern” (the Rila Mountains in the Rhodope
-Rila mountain system) and “Western” (several mountains in the Dinaric mountain system and one isolated
population in the northeast part of the Scardo-Pindic
system) - in fact all populations are grouped into four
disjunctions: “Bulgarian”, “Herzegovinian”, “Montenegrin-Albanian”, and “E Albanian”. The average distance
is c. 450 km between the“Bulgarian” and “Herzegovinian” disjunctions, c. 300 km between the“Bulgarian”
and “Montenegrin-Albanian” disjunctions, c. 260 km
between the“Bulgarian” and “E Albanian” disjunctions,
c. 200 km between the “Herzegovinian” and “Montenegrin-Albanian” disjunctions, and c. 50 km between the
“Montenegrin-Albanian” and “E Albanian” disjunctions
(Fig. 1). The existence of G. bulgaricum in mountains of
the Scardo-Pindic system (Kunora e Lurës) in E Albania
is confirmed here for the first time.
In Albania the presence of G. bulgaricum was confirmed for Mt. Škelsen (above Tropoja), Mt. Maja Hekuravë
(near the village of Bunjaj), the Prokletije Mountains,
the Mt. Bješka maze, Mt. Maja e Bërdashës, Mt. Maja
e Boshit, Mt. Maja Strebishit, Qafa e Valbonës, Qafa e
Pejës, Tarabosh, the vicinity of Thethi, and Shtegu i Dhenve (Hayek 1917, 1924, 1927; Jávorka 1926; Rohlena
1942; Pénzes 1954; Tutin et al. 1968; Demiri 1983; Qosja et al. 1992; Vangjeli 2003, 2015; Kurtto et al. 2004;
Shuka et al. 2008; Ball 2011; Meyer 2011; Schütt
s.d.). Also, a field observation for Mt. Kunora e Lurës in
the most northwestern part of the Scardo-Pindic mountain system (Kunora e Lurës, 1850 m, 10.05.1975, Vangjeli Tartari - Shuka pers. com.) was confirmed during
our own field investigations (herbarium specimen
BP758300!). At the same time, the literature record for
Mt. Korab (Shuka & Malo 2010), which is based on a
field observation (Korabi Mt, 29.07.2009. M. Mersinllari
- Shuka pers. com.), has to be treated as questionable,
since it was not confirmed either during field investigations or in the herbarium material from the studied
herbarium collections. In Bosnia and Herzegovina, G.
bulgaricum was recorded on Mt. Prenj (Ortiš and Tisovica peaks), Mt. Čvrsnica (Plasa and Muharnicа), and Mt.
Čabulja (Protić 1908; Malý 1923; Beck 1927; Lubarda
2013). In Montenegro, it can be found in the following
places: Mt. Sinjavina (Babji Zub peak), the Kučke Planine Mountains (Žijovo, the lake Rikavačko Jezero), the
Prokletije Mountains (above Gusinje, Fuša Rudnices, the
Karanfili-Kotlovi peaks, Mt. Maja Potkajs, Mt. Zeletin,
Mt. Čakor, Mt. Hajla, Mt. Suha Planina, Sjenova) (Baldacci 1892; Rohlena 1904, 1942; Rechinger 1935; Lakušić 1964, 1968, 1991; Šmarda 1968; Markišić 1984;
Vuksanović 2003, 2016; Stešević & Petrović 2004).
In Serbia, it grows in the Prokletije Mountains (Mt. Koprivnik: Krš Čvrlje, Mt. Ljubenička Planina-Jelivi Sluzi;
Mt. Lumbardska Planina: Žuti Kamen peak; above the
lake Nedžinatsko Jezero; Mt. Prilepska Planina; Mt. Hajla; Mt. Žljeb: Maja Rusolija, Savine Vode) (Rechinger
1935; Rudski 1936, 1949; Grebenščikov 1943; Diklić
& Nikolić 1961; Janković & Bogojević 1962-1964
(1967); Lakušić 1968, 1984; Šmarda 1968; Gajić 1972;
Janković 1972, 1998; Markišić 1986; Rexhepi 1986,
1989-1990 (1991), 2013; Amidžić & Belij 1995; Amidžić
1997, 2003; Amidžić & Krivošej 1998; Jovović et al.
1998; Matović & Tatić 2002; Amidžić & Panjković
2003; Janković & Amidžić 2003; Tomović 2007). The
literature record for Mt. Radočelo (Krivača) (Sigunov
1979; Nikolić et al. 1986) has not been confirmed in
the field and remains questionable. The presence of the
species in the Šar Planina Mountains (Mihajlov et al.
1998) has to be treated as erroneous. In Bulgaria, it can
be found only in the Rila Mountains (locus classicus)
(Assenov 1973; Markova 2006; Petrova & Vladimirov 2010). Subpopulations (mosaic with low to medium
abundance) are recorded among alpine and subalpine
rocks and on screes in the four parts of the mountain
- East Rila or the Musala Ridge, Central Rila or the Skakavets Ridge, Northwest Rila, and Southwest Rila or the
Kapatnik Ridge (Bondev 1959; Ganchev 1963; Tashev
& Pavlov 1995; Dimitrov et al. 1996; Peev et al. 2000;
Roussakova 2000, 2003; Roussakova & Georgieva
2003; Vladimirov et al. 2015). The species is represented
in the National Ecological Network (BDA 2007) in four
strict reserves (the Parangalitsa, Ibar, Central Rila, and
Rila Monastery Forest Reserves) and the Rila Monastery
Nature Park and Rila National Park (Peev et al. 2000;
Roussakova & Valchev 2000; Roussakova & Georgieva 2003; Tsoneva & Peev 2003; Vladimirov et al.
73
74
vol. 42 (1)
Fig. 1. Distribution of Geum bulgaricum (UTM grid zones 33T and 34T; dots correspond to basic MGRS squares of 10 × 10 km).
2015); in the BGIPA 096 Rila Important Plant Area (Spiridonov et al. 2012); and at the Natura BG 0000495 Rila
site (Roussakova 2013, 2015; Roussakova & Gussev
2015). Detailed data on occurrence of the given species
are given in the Specimina Visa and Field Observations
sections below.
Geum bulgaricum is most often found in alpine and
subalpine acidophilous (Juncetea trifidi Hadač in Klika
et Hadač 1944) and calcicolous (Elyno-Seslerietea Br.-Bl.
1948) grasslands and swards, as well as in the vegetation
of scree habitats (Thlaspietea rotundifolii Br.-Bl. 1948),
rocky crevices [Asplenietea trichomanis (Br.-Bl. in Meier
et Br.-Bl.1934) Oberd. 1977], subalpine belts of krummholz pine (Roso pendulinae-Pinetea mugo Theurillat in
Theurillat et al. 1995), and very localised serpentine out-
crops (Pavlova 2012). Although its total altitudinal range
extends between 1200 m a.s.l in the Prokletije Mountains and 2700 m a.s.l in the Rila Mountains, the ecological optimum of this species is in the subalpine and alpine
vegetation belt (1800–2600 m a.s.l.).
Morphology. Our preliminary morphometric investigations showed that G. bulgaricum is characterised by pronounced morphological variability, relating in particular to stem and pedicel height and thickness, the number
of flowers, achene dimensions, and indumentum characteristics (Fig. 2, Table 1).
According to the position of individuals along the
first two PCA axes, G. bulgaricum represents a morphologically relatively homogeneous group (Fig. 3A). On
the first two axes, populations from the Dinarides and
D. Lakušić et al.: Distribution and variability of Geum bulgaricum
Fig. 2. A–C. Geum bulgaricum from the Rila Mountains [A—habit (photo Y. Bosseva), B—capitulum (26 June 2015, photo S. Tsoneva),
C—indumentum (date and photographer, same as for B)]; D–F. Geum bulgaricum from Ljubokuč in the Prokletije Mountains [D—
habit (13 July 2016, photo D. Lakušić), E—capitulum (date and photographer, same as for D), F—indumentum(date and photographer,
same as for D)].
the Rila Mountains broadly overlap in the central part
of the PCA1–PCA2 space and are just partially separated on the ends of the positive and negative parts of
the first axis (Fig. 3A). Canonical discriminant analysis (CDA) conducted on three a priori defined groups
showed that all three groups just barely overlap (Fig.
3B). Plotted along the first and the second discriminant
axes, all three groups were positioned in distinct parts
of the DA1–DA2 space. Scores of the population from
the Prokletije Mountains are grouped on the positive
part of the first axis, scores of the population from Mt.
Čvrsnica are grouped on the negative part of the first
75
76
Table 1. Basic statistics for morphological characters of Geum bulgaricum (all measured values are in millimetres).
RHODOPES
Valid N Mean
Min
St_h
18
stem - width at the base
St_w
18
3,39
1,91
flower pedicel - length
Pd_l
26
flower pedicel - width
Pd_w
indumentum of flower
peidcel - thick
Max St.Dev. St.Error Valid N Mean
Max St.Dev. St.Error Valid N Mean
16,89
17
0,77
0,18
17
92,18
36,79 188,02 33,51
6,57
28
8
1,36
1,08
2,06
0,33
0,12
28
0,90
0,48
1,27
Pd_ind
8
1,20
0,87
1,80
0,30
0,11
28
0,71
0,34
number of flowers in
inflorescences
Fl_no
16
5,38
2,00
9,00
2,06
0,52
14
3,79
leaf petiole - width of
the base
Lb_pt_w
18
12,90
9,44
18,39
2,64
0,62
14
12,20
leaf petiole - length
Lb_pt_l
18
182,82 107,74 236,53 34,34
8,09
terminal leaflet - length
Lb_tl_l
18
84,04
59,13 117,91 18,40
terminal leaflet - width
Lb_tl_w
18
calyx toth - length
Ca_In_l
calyx toth - width
Max St.Dev. St.Error
35
0,55
0,13
35
110,22 71,87 193,65 31,30
5,91
54
0,20
0,04
36
1,00
0,48
2,06
0,30
0,05
1,04
0,18
0,03
36
0,82
0,34
1,80
0,29
0,05
2,00
6,00
1,12
0,30
30
4,63
2,00
9,00
1,85
0,34
7,55
17,42
3,23
0,86
32
12,59
7,55
18,39
2,88
0,51
14
188,10 99,41 250,58 43,93
11,74
32
185,13 99,41 250,58 38,25
6,76
4,34
15
78,23
14,79
3,82
33
81,40
55,06 117,91 16,86
2,93
128,74 98,50 175,32 24,82
5,85
15
120,52 75,87 153,35 25,96
6,70
33
125,00 75,87 175,32 25,29
4,40
23
10,06
6,64
13,26
1,69
0,35
27
10,70
8,87
13,62
1,15
0,22
50
10,40
6,64
13,62
1,44
0,20
Ca_In_w
23
6,19
3,96
9,47
1,15
0,24
27
6,14
4,67
8,19
0,90
0,17
50
6,16
3,96
9,47
1,02
0,14
epicalyx toth - length
Ca_Ou_l
21
6,02
3,99
8,45
1,12
0,24
26
7,29
4,94
9,47
1,28
0,25
47
6,72
3,99
9,47
1,36
0,20
epicalyx toth - width
Ca_Ou_w
21
2,66
1,76
3,74
0,57
0,12
26
2,13
1,36
3,37
0,47
0,09
47
2,37
1,36
3,74
0,58
0,08
achenes - height
Ah_l
8
3,35
2,86
3,53
0,21
0,07
21
3,87
2,95
4,88
0,53
0,11
29
3,73
2,86
4,88
0,52
0,10
achenes - width
Ah_w
8
1,03
0,77
1,27
0,15
0,05
21
1,24
0,90
1,50
0,14
0,03
29
1,18
0,77
1,50
0,17
0,03
St_l
8
16,49
12,01
18,51
1,95
0,69
21
16,47
12,11
19,91
2,13
0,46
29
16,48
12,01
19,91
2,05
0,38
St_H_L
8
2,78
2,27
3,68
0,49
0,17
21
3,03
1,98
3,90
0,43
0,09
29
2,96
1,98
3,90
0,45
0,08
hair on style - length
4,67
495,54 383,77 604,29 75,08
Min
18,21
style - length
422,20 296,96 554,29 71,67
Min
TOTAL
3,11
2,00
55,06
4,05
99,10
457,82 296,96 604,29 81,27
3,26
1,91
4,67
13,74
0,68
0,11
101,53 36,79 193,65 33,34
4,54
vol. 42 (1)
stem - height
DINARIDES
D. Lakušić et al.: Distribution and variability of Geum bulgaricum
Fig. 3. A — Principal component
analysis (PCA) of individuals of
Geum bulgaricum from the Rila
Mountains and the Dinarides; B —
Canonical discriminant analysis
(CDA) of individuals of Geum
bulgaricum from the Rila Mountains,
the Prokletije Mountains, and Mt.
Čvrsnica based on all morphological
characters.
axis, while scores of the population from the Rila Mountains are grouped on the positive part of the second axis.
Unexpectedly, scores of the population from the Rila
Mountains on the first axis are positioned between the
two Dinaric populations. Despite that, in CDA we recognised three separate groups, but Tukey’s HSD posthoc
test for all characters showed that these differences are
not statistically significant (Table 2).
Although no general differentiation in regard to all
morphological character states was established, significant differences between the Rhodope-Rila and the Dinaric populations were observed when we analysed separate groups of individual characters. Thus, statistically
significant differences were established with respect to
characters of the indumentum, seeds, and epicalyx (Table 2). In all three groups of characters, G. bulgaricum
77
vol. 42 (1)
78
from the Rila Mountains represents a homogenous group significantly different from the Dinaric populations.
As in canonical discriminant analysis (CDA), Tukey’s
HSD posthoc test showed that regarding some morphometric characters, the population from the Rila Mountains, quite unexpectedly, has an intermediate position
between the two Dinaric populations. In fact, regarding
seed (Ah_l + Ah_w + St_l + St_H_L) and stem (St_h
+ St_w) features, populations from the Rila Mountains
and Mt. Čvrsnica form a homogenous group (Table 3).
Genome size. Our studies showed that the nuclear DNA
amount (2C value) ranged from 4.79 in the population
from the Prokletije Mountains to 6.58 in that from the
Rila Mountains. The mean value of all investigated populations was 5.72 pg. Furthermore, the populations from
the Rhodope-Rila system (the Rila Mountains) and the
Dinaric system (Mt. Čvrsnica and the Prokletije Mountains) have statistically significant different genome sizes
(Fig. 4). The 2C value in the population from the Rila
Mountains ranged from 6.24 to 6.58 with a mean value
of 6.39 pg, while this index in the Dinaric population
ranged from 4.79 to 5.83 with a mean value of 5.39 pg. It
is noteworthy that in the population from the Prokletije Mountains, two individuals are recorded with significantly smaller 2C values (4.80 and 4.90 pg) than the
average value (5.39 pg) for the Dinaric population.
Tukey’s HSD posthoc test for 2C values showed that the
differences in genome sizes between Rhodope-Rila and Dinaric individuals are statistically significant (Tables 2, 3).
Threatened status. On the basis of the obtained new
chorological data and estimation of the number of individuals and condition of the populations, we can define
G. bulgaricum as IUCN NT in Bulgaria, Albania, and
Montenegro; and as VU D2 E in Serbia and Bosnia and
Herzegovina.
DISCUSSION
Although data on the presence of G. bulgaricum outside the territory of Bulgaria were published soon after
Pančić’s discovery of this species in 1882 in the Rila
Mountains (Baldacci 1892 - Montenegro; Protić 1908
- Bosnia and Herzegovina; Hayek 1917 - Albania; Rechinger 1935 - Serbia), the distribution of this “species
of European concern” remained insufficiently known
and in some aspects controversial. In most of the relevant botanical literature, there are different data about the distribution of G. bulgaricum, both in regard to
the number of states (Gajewski 1968; Ozinga & Schaminée 2005; Kurtto 2009) and in regard to the position
of the populations within geographical regions (Gajewski 1957; Kurtto et al. 2004).
While Gajewski (1968) correctly stated that G. bulgaricum is distributed on “mountains of S Yugoslavia,
Albania, and SW Bulgaria (Ju Al Bu)”, on his map of
the distribution there are no data about the occurrence of G. bulgaricum in Albania and Montenegro. At the
same time, one large part of the species’ range is located in the Šar Planina Mountains and the mountains
Skopska Crna Gora and Rujan on the border between
Macedonia and Serbia (Gajewski 1957). This error on
the map was probably taken by later authors to indicate
that the species G. bulgaricum is also present in the Republic of Macedonia and the Šar Planina Mountains in
the south of Serbia. Additionally, although Kurtto et
al. (2004) provided a completely correct map with clear
indication that the species is present in Montenegro, in
the last relevant source (Kurtto 2009) it was stated that
the species is distributed only in Albania, Bosnia and
Herzegovina, Bulgaria, and Serbia (Al BH Bu Sr). Finally, Ozinga & Schaminée (2005) stated that the species
is registered only in three European countries, without
indicating which countries.
As a result of our research, the occurrence of G. bulgaricum was confirmed in five Balkan countries: Albania, Bosnia and Herzegovina, Bulgaria, Montenegro,
and Serbia. Its range of distribution is divided into two
main parts. The first part is in the Rila Mountains, the
second in the central and southeastern Dinarides and
northwest corner of the Scardo-Pindic mountain system. Furthermore, all populations are grouped into four
clearly separated disjunctions: “Bulgarian”, “Herzegovinian”, “Montenegrin-Albanian” and “East Albanian”. At
the same time, all literature records for the presence of
the species in the Šar Planina Mountains and at other localities in the Republic of Macedonia have to be treated
as erroneous, which is in accordance with the opinion of
Мicevski (1998). Several localities were newly discovered in Albania and Montenegro, and it appears to be a
relatively common species in the vegetation of subalpine
-alpine silicious and calcareous grasslands, screes, and
stands of krummholz pine.
As an endemic with a very restricted range of distribution in Europe, G. bulgaricum is defined as a species of
great international (Ozinga & Schaminée 2005; Heywood 2009) and national (Sl RCG 76/2006; BDA 2007;
Peev & Tsoneva 2009; Sl RS 5/2010; Đug et al. 2013)
significance. However, except for Bulgaria and Bosnia
and Herzegovina, previous assessments of the status and
vulnerability of this species at national or regional levels
is completely missing. We therefore here define G. bulgaricum as IUCN NT in Albania and Montenegro, and as
VU D2 E in Serbia and Bosnia and Herzegovina, based
on our extensive chorological data and estimation of the
number of individuals and condition of the populations.
It is well documented that the Balkan Peninsula represents one of the European centres of diversity (Turrill 1929; Hewitt 2011; Nieto Feliner 2014) and endemism (Turrill 1929; Stevanović et al. 2003, 2007;
Stevanović 2005; Tan et al. 2007; Tomović et al. 2014).
D. Lakušić et al.: Distribution and variability of Geum bulgaricum
Table 2. Tukey’s HSD post-hoc test for morphometric and genome size characters of Geum bulgaricum of two groups, viz. the population
of the Rila Mountains vs. that of the Dinarides. The full names of morphometric characters and the corresponding acronyms are given
in Table 1. Values given in bold are statistically significant.
Homogenous Groups
all characters
1
Dinarides
****
Rila Mts.
****
indumentum (Pd_w + Pd_ind)
1
Dinarides
epicalyx (Ca_In_l + Ca_In_w)
genome size (2C)
0.000
Dinarides
2
0.032
Dinarides
It is estimated that its vascular flora comprises ca 8000
native taxa, including 2600–2700 endemics. The highly
structured topography, extremely different recent climatic conditions, refugial character, and very involved
geological history of the Balkan Peninsula have resulted
in its becoming a very complex territory in the phytogeographical sense. With respect to its phytogeography, the
Balkan Peninsula is differentiated into many phytochoria of subregion and province rank (Horvat et al. 1974;
Jäger & Welk 2003). The Dinaric and Rhodope-Rila
mountain systems have very different geographical, geological, and historical features, and these two mountain systems belong to different phytochoria of subregion
rank (the Illyrian vs. the Balkan subregion). Accordingly,
many well-known endemic plants (Illyrian vs. Balkan
endemics) are geographically restricted to one of these
two areas (Horvat et al. 1974; Tomović et al. 2014). At
the same time, the recent discovery of several new or neglected cryptic species, as in Campanula (Lakušić et al.
2013a; Janković et al. 2016), Edraianthus (Surina et al.
2009; Lakušić et al. 2013b, 2016), and Sesleria (Kuzmanović et al. 2013), indicates that crypto speciation is very
common in this area. It is important to note that this
Rila Mts.
0.002
2
0.002
Dinarides
Rila Mts.
0.006
2
0.006
Dinarides
Rila Mts.
0.000768
****
Rila Mts.
Rila Mts.
0.032
****
1
Dinarides
2
****
Rila Mts.
Rila Mts.
0.000
****
1
Dinarides
Dinarides
****
Rila Mts.
stem (St_h + St_w)
2
****
1
Dinarides
0.084
****
Rila Mts.
Rila Mts.
0.084
****
1
Dinarides
Dinarides
****
Rila Mts.
seed (Ah_l + Ah_w + St_l + St_H_L)
2
Populations
****
0.000768
kind of speciation, which is noticeable in genetic structure but not readily apparent in morphological characters, exhibits a strong phytogeographical pattern in the
spatial sense. To be specific, all these recently discovered
cryptic taxa are defined as local or stenoendemics, which
are characteristic of phytochoria at the level of a single
floristic province or district. With this in mind, as well as
the fact that G. bulgaricum is not only geographically but
also ecologically strongly differentiated into the siliciphilous Balkan (Rhodope-Rila) and calciphilous Illyrian
(Dinaric) populations, it was expected that differentiation would be found on both the morphological and the
cytogenetic levels, which could have implications for the
taxonomic treatment of this species.
Given that up to now, G. bulgaricum has not been the
object of any detailed studies, we are here providing the
first insight into the differentiation of its populations.
We found that the Rhodope-Rila and Dinaric populations are slightly differentiated on the morphological
level and well differentiated with respect to genome size.
With respect to qualitative features, the Rhodope-Rila and Dinaric populations showed clear morphological
differences (Fig. 2). The plants from the Rila Mountains
79
vol. 42 (1)
80
Table 3. Tukey’s HSD post-hoc test for morphometric and genome size characters of Geum bulgaricum of three groups, viz., the
population of the Rila Mountains vs. that of the Prokletije Mountains vs. that of Mt. Čvrsnica. The full names of morphometric
characters and the corresponding acronyms are given in Table 1. Values given in bold are statistically significant.
Homogenous Groups
all characters
1
Čvrsnica
****
Prokletije
****
Rila
****
indumentum (Pd_w + Pd_ind)
1
Čvrsnica
****
Prokletije
****
Rila
seed (Ah_l + Ah_w + St_l + St_H_L)
Rila
****
Rila
****
****
2
****
****
****
Rila
****
Čvrsnica
****
Prokletije
****
genome size (2C)
2
1
Prokletije
1
Rila
are more robust, with a thicker stem, a thicker and denser
indumentum with many glandular hairs, a larger number of flowers, and more or less erect flowering branches. By way of contrast, the Dinaric plants are elongated,
with a thinner and scattered indumentum on the stem
(without or sometimes with just a few glandular hairs),
and with a very characteristic downward bent of terminal parts of the flower stalk. However, these differences,
which are noticeable at first glance, were not confirmed
by our morphometric analysis, which showed that the
level of variation of the analysed characters is very high
and that overlapping occurs between the populations.
Hence, it must be stated that we do not at the moment
have enough arguments to conclude that the Dinaric
and Rhodope-Rila populations are clearly differentiated
at the morphological level.
Unlike the situation with morphology, we found
strong statistical evidence indicating that the Rhodope
Rila
0.730
0.112
0.361
0.112
0.361
Čvrsnica
Prokletije
Rila
0.646
0.003
0.000
0.003
0.000
Čvrsnica
Prokletije
Rila
0.001
0.525
0.001
2
0.000
0.525
0.000
Čvrsnica
Prokletije
Rila
0.726
0.008
****
Prokletije
Čvrsnica
2
****
Čvrsnica
Prokletije
0.646
****
1
stem (St_h + St_w)
2
****
Prokletije
epicalyx (Ca_In_l + Ca_In_w)
Čvrsnica
0.730
****
1
Čvrsnica
2
Populations
0.726
0.091
0.008
0.091
Čvrsnica
Prokletije
Rila
0.704
0.275
0.044
0.704
0.275
0.044
Čvrsnica
Prokletije
Rila
0.999
0.003
0.003
0.999
****
0.003
0.003
-Rila and Dinaric populations are well differentiated with
respect to genome size, most likely on the level of ploidy.
From the results of a previous study of genome size in the
hexaploid species G. urbanum (2C = 3,01 pg) (Pustahija et al. 2013), we can assume that G. bulgaricum from
the Rila Mountains is dodecaploid (12x - 2C~6pg), while
populations from the Dinarides are predominantly decaploids (10x - 2C~5pg), with a few octoploid individuals
(8x - 2C~4pg) from the Prokletije Mountains.
As in the case of chorologic data, data on the chromosome number of this species are also very scarce and insufficiently clear. To be specific, we found only three published sources containing information about its chromosome number. In fact, all three chromosome numbers
assumed by us on the basis of genome sizes have already
been reported: 2n = 10x = 70 was reported in Gajewski
(1957, 1958), 2n = 8x = 56 in Gajewski (1968), and finally
2n = 12x = 84 in Baltisberger (2006). Unfortunately,
D. Lakušić et al.: Distribution and variability of Geum bulgaricum
Fig. 4. Box plots of genome sizes for different populations of
Geum bulgaricum.
only Baltisberger (2006) provided precise information
on the origin of his material (Rila Mountains, northeast
of Musala), so it remains unclear whether Gajewski counted chromosomes on plants from the Dinarides or on
ones from the Rila Mountains.
CONCLUSIONS AND OUTLOOK
Given that our morphometric study was carried out on
herbarium specimens that were not collected for formal morphometric analysis, and in view of the fact that
the measured specimens were in different phenological
phases, the morphometric results presented here should
be considered as preliminary. For these reasons, additional morphological studies based on specimens collected specifically for morphometric analyses (an equal
number of individuals for each population and individuals collected in the same phenological stage) are needed. Furthermore, molecular phylogeographical studies
would be helpful in solving the taxonomic status of the
Dinaric and Rhodope-Rila populations. We therefore
decided for the time being to solve only the basic nomenclatural question related to the name Geum bulgaricum. We leave a more thorough taxonomic treatment
to planned future detailed studies on the morphological,
cytogenetic, and molecular levels.
Geum bulgaricum Pančić, Elem. Fl. Bulg. 26 (1883)
Lectotype (designated here): Bulg. bor. occid [Bulgaria
borealis occidentalis], sub m. [monte] Rilo, ad rivulum
montanum, Aug 882 [Augusto 1882], J. Pančić s.n.
(BEOU 4541!) (Fig. 5).
Protologue citation: in elatioribus m. Rilo in ripa saxosa
rivuli ad viam qua itur a coenobio Rila ad Samokov.
Other original material examined: Bulgaria bor. oc-
Fig. 5. Lectotype of Geum bulgaricum Pančić (BEOU 4541).
cid. [borealis occidentalis], m. [monte] Rilo, in saxosis
rivularibus, Aug 882 [Augusto 1882], J. Pančić s.n. (BP
459167!)
Note: We found two herbarium specimens belonging
to the original material collected by Pančić in August
of 1882 in the Rila Mountains. The details on the labels
match the information provided in the protologue. However, the specimen from BEOU is more representative
than the one from the BP herbarium, having flowers and
fruits which bear important diagnostic characters. We
therefore here designate it as the lectotype.
Specimina Visa
ALBANIA (UTM Grid zone 34T). — Nordhange der
“Prokletije”, in der alpinen Region, c. 1700 m, 17.07.1914,
I. Dörfler No. 485 (WU!); “Prokletija”-Gebiet, in du alpinen Region am Nordhange der “Prokletija”, c. 1700 m,
14.07.1914, I. Dörfler 485 (BP168053!); distr. Scutari, Alpes alb. sept., m. Parun, [CM88], in rupestribus alpinis,
A. Baldacci 171 (P02567975!); P02567979!); Parun, Maja
Strebiscit, [CM88], Kalk, 1700 m, 19.07.1933, B. Schütt
(BREM03042!); Parun-Gebirge, [42.299191 N, 19.631539
81
82
vol. 42 (1)
E / CM88], 27.07.1928, B. Schütt (BREM03041!); distr.
Scutari, Alpes alb. sept., m. Šala supra Abata, [CM98],
in rupestribus alpinis, 23.07.1897, A. Baldacci 171
(P02542171!); P02567984!); Q. e Pejs über Okol in Thethi, [42.44398353 N, 19.77268381 E / CM99], 07.1939, B.
Schütt (BREM03046!); Q. e Pejës - Nikç, [42.44398353
N, 19.77268381 E / CM99], Kalk, 1800 m, 02.08.1933, B.
Schütt (BREM03040!); Albania sep. Alpet, mt. Radohin,
prope pagum Thethi, [CM99], in rupestribus declivibus, 1800 m.s.m., 23.07.1960, P. Jakucs A22 (BP589851!);
Сеси, изнад језера на седлу Пејаси код катуна
[CM99], кречне стрме стене, 23.08.1938, P. Černjavski,
det. P. Černjavski (BEO11413!); Bridashe b. Boga,
[CM99], 30.07.1929, B. Schütt (BREM03039!); District of
Shkodër (Rrethi i/Shkodrës), Prokletije Mountains: between Bogë and Okol, southern slope of Mount Shtegu
(2081 m), 42.391110 N, 19.727710 E, [CM99], on limestone rocks, 1805 m.s.m., 29.05.2005, Z. Barina, D. Pifkó
(BP183242!); distr. Klementi, Prokletije pl., supra Nikći
(Scirta), [42.484761 N, 19.698662 E / CN90], in rupestribus, 04.08.1901, A. Baldacci 26 (P02542169!); Distr.
Klementi, Alpine Felsen du Fuša Rudnices, [CN90], c.
1800 m, 15.07.1914, I. Dörfler No. 498 (WU!); District of
Shkodër (Rrethi i Shkodrës), Prokletije Mountains: pass
Pejes (qafa Pejes), 2,5 km north of Okol, near “Buni i
Gropazt”, 42.441920 N, 19.772620 E, [CN90], in rocky
grassland on limestone, 1710 m.s.m., 31.05.2005, Z. Barina, D. Pifkó (BP182863!); from the camp to the tap in
the cirque of Mount Ezertse [от лагера до чешмата в
циркуса на връх езерце] [DM09], 29.07.1958, B. Kitanov, S. Petrov [Б. Китанов, С. Петров], det. D. Stoyanov [Д. Стоянов] (SO97884!); the cirque of Mount
Ezertse [циркусът на връх езерце] [DM09], 29.07.1958,
B. Kitanov, S. Petrov [Б. Китанов, С. Петров], det. B.
Kitanov, S. Petrov [Б. Китанов, С. Петров] (SO101877!);
Bertiscus, in jugo Qafa Valbons inter vallem Valbona
et Theti, [DM09], in solo calcareo, 2000 m, 04.07.1955,
S. Jávorka & Ujhelyi (BP273325!); District of Shkodër
(Rrethi i Shkodrës), Prokletije Mountains: southeastern
part of Mount Alis (2471 m), between pass Valbona
(qafa Valbones) and Ragam, 42.409210 N 19.811760 E,
[DM09], on limestone rocks, 1770 m.s.m., 02.06.2005, Z.
Barina, D. Pifkó (BP182897!); Bertiscus, sub rupe Maja
Drosks versus cacumen Maja Hekuravet, [DM19], in
solo calcareo, 2600 m, 01.07.1955, Ujhelyi (BP273326!);
Montes Albaniae borealis versus opp. Djakova extensi,
Montes Hekurave, supra “Fune Hekurave” ad pagum.
Bunjaj, [DM19], in saxosis in valle alpestri, c. 18002000 m, 24.08.1918, S. Jávorka (BP168847!); Hekuravë,
[42.38428418, 19.97057579 / DM19], 07.1935, B. Schütt
(BREM03045!); Curraj i Epërm, [DM19], 13.07.1929,
B. Schütt (BREM03044!); District of Tropojë (Rrethi i
Tropojës), Albanian Alps Mountains (Alpet Shqiptare,
Bjeshkët e Nemuna, Prokletije), west of town Bajram
Curri, west of the village of Dopsidol, on the northern slope of Mt. Marbicit (1855.0 m), 42.366760 N,
20.019000 E, [DM19], on limestone rocks, 1622 m.a.s.l.,
30.05.2009, Z. Barina, G. Lunk, D. Pifkó, D. Schmidt,
det. Z. Barina (BP748103!); county of Dibër (Rrethi i Dibrës), Mt. Ruja e Lura above the village of Fushë Lurë,
41.78203 N, 20.24341 E, [DM32], on limestone rocks,
1781 m.a.s.l., 21.06.2013, Z. Barina, D. Pifkó, det. Z.
Barina (BP758300!); Montes Albaniae borealis ad occidentem opp. Djakova extensi, montes Škelsen supra
pagum Tropoja, [DN20], in saxosis calcareis, c. 2100 m,
07.09.1918, S. Jávorka (BP168848!);
BOSNIA AND HERZEGOVINA (UTM Grid zone
33T). — Čabulja planina, 1480 m, 09.08.1906, K. Malỳ
s.n. (BEOU!); Felswände der Čabulja, Nordabhang des
Sedlo, [YJ11, YJ12], ca. 1500 m, 09.07.1906, K. Malỳ
(SARA17811!; SARA 17812!; SARA 17813!); Čvrsnica planina, montis Muharnica, [YJ13], in saxosis alpinis, solo calcareo, 10.08.1922, K. Malỳ s.n. (BEOU!);
Čvrsnica, Muharnica, 43.63166 N, 17.63436 E, [YJ13],
1761 m, 09.07.2016, D. Lakušić, N. Kuzmanović, I. Janković 46017 (BEOU!); Čvrsnica, Pešti-brda, iznad Bukove
glave, [YJ12], u pukotinama krečnjačkih stijena, N exp.,
c. 1900 m, 17.09.1966, Č. Šilić, Đ. Đaran, det. Č. Šilić
(SARA17809!); Čvrsnica planina, Drinača, [YJ13], c.
1950 m, 25.07.1933, V. Loschingg (SARA17808!); Čvrsnica planina, stijene ispod Ostrovače, [YJ13], 22.07.1933, V.
Loschingg (SARA17807!).
BULGARIA (UTM Grid zone 34T). — Bulg. bor. occid,
sub m. Rilo, ad rivulum montanum, 08.1882, J. Pančić
4541 (BEOU!, Herbarium Pancicianum; Bulgaria bor.
occid., m. Rilo, in saxosis rivularibus, 08.1882, J. Pančić
(BP459167!); M. Rila, in alpinis, 1903, O. Bierbach
(P02567983!); Rila, mezi kamenim, 08.1904, J. Mrkvička
(SOM39840!, SOM39843); Rila [Рила], 08.1935, K. Popov [К. Попов,] det. К. Popov(SO37760!); alpine zone of
Rila Mountains. [алписката зона на Рила], 0507.09.1919, B. Stefanoff (SOM39834!); Rila Mts, prope l.
d. Eli dere, [Chepinska reka], in saxosis, c. 2250 m,
21.07.1909, B. Davidov, det. B. Davidov (U185598!); mt.
Topla Rila, “Polič” supra rivum Dupnička Bistritza,
[FM87], in saxosis umbrosis, 2100 m, 27.07.1912, B. Davidoff (SOM39831!); Mt. Topla Rila, supra fontes rivi
Otovitza, [FM87], in saxosis humidis, 2450 m, 28.07.1912,
B. Davidoff (SOM39846!); Rila, kod jezera Kalin i brane,
42.17104 N, 23.251367 E, [FM87], silikat, 2327 m,
30.07.2014, M. Niketić, G. Tomović, S. Đurović, U.
Buzurović 41136 (BEOU!); Mt. Bela. Rila, inter locus Sedem ezera, [FM97], in rupestribus, 2300 m, 21.07.1909,
B. Davidoff (SOM39850!); mt. Rila, Sedemte rilski ezera
[Edi gjol /FM97], 22.07.1919, B. Achtaroff (SOM39823!);
Rila Mts., Sedemte rilski ezera, [Edi gjol /FM97], in saxosis supra Mugheto, 2250 m, 21.07.1909, B. Davidoff
(SOM39848!, 39849!, 39853); Rila Mts., ad Elenin Vrh,
[FM97], in rivularibus, 1910, Jv. K. Urumov (SOM39824!);
Rila Mts., Černi Iskar, [FM97], in saxosis graminosis,
D. Lakušić et al.: Distribution and variability of Geum bulgaricum
2300 m, 05.08.1920, B. Davidoff (SOM39826!); Rila Mts.,
around the Malyovitsa lakes [Рила, край Мальовишките
езера] [FM97], wet rocky places [влажни скалисти
места], 2400 m [м.н.в.], 27.08.1969, B. Kuzmanov [Б.
Кузманов] БК-69890 (SOM119946!); Rila Mts., in Malyovitsa cirques [Рила, из Мальовишките циркуси]
[FM97], on rocky meadows in abundance [по скалните
поляни в изобилие], 23.07.1940, A. Radoslavov (SOM!,
SOM39863!); Rila Mts., Malyovitsa [Рила, Мальовица]
[FM97], 24.07. 1919, B. Achtaroff [Б. Ахтаров]
(SOM39857!); in the region of Malyovitsa [в района на
Мальовица] [FM97], around the Pinus mugo localities
and rocky places at ca. [край клековите огнища и
скални места на около] 2500 m [м надм. в.], 04.07.1978,
Docheva, Todorova, Peev [Дочева, Тодорова, Пеев], det.
D. Peev [Д. Пеев] (SOM136337!); to peak Malyovitsa
[към вр. Мальовица] [FM97], rocky slopes between the
lower and second terraces [скалисти склонове между
долната и втората тераса], 16.06.1985, S. Tsoneva [С.
Цонева], det. S. Tsoneva [С. Цонева] (SOM144761!);
Rila mountain massif, Malyovitsa peak [Горн. масив
“Рила”, верш. “Мальовица”] [FM97], among wet rocks
and on wet stony meadows [в влажных разелинах скал
и на влажн. Каменист. лугах], 2300-2600 m [м над ур
моря], 11.07.1948, A. Yurkovski [А. Юрковский]
(SOM39861!); Rila, Malyovitsa, 42.169529 N, 23.36783 E,
[FM97], alpine grasslands, Juncetea trifidi, granite, 2615
m, 11.07.2015, D. Lakušić, N. Kuzmanović, I. Janković
42757 (BEOU!); Rila Mts., Urdina river [Рила, Урдина
река] [FM97], 1500 m, 24.07.1919, B. Achtaroff
(SOM39833!, SOM39855!, SOM39860!); Rila Mts., around the Makedonya hut, Blagoevgradska Bistritsa river
[Рила пл. под х. “Македония” р. Благоевгр. Бистрица]
[GM05], on steep slopes between Pinus mugo [по стръмните склонове между клека], 2225 m [м н.в.],
06.07.1955, I. Penev [Ив. Пенев], det. I. Penev [Ив. Пенев] (SO37766!); Rila Mts. Smradlivoto Lake [Рила
Смрадливото езеро] [GM06], 2000’, B. Achtaroff
(SOM39835!); Central Rila Mts., along the road between
the Ribni Lakes and the Partisanska Polyana [Централна Рила планина по пътя между Рибни езера и Партизанска поляна] [GM06], 07.1986, S. Gheorghieff [С.
Георгиев], det. S. Gheorghieff [С. Георгиев] (SO94096!);
Rila Mts., Kanarata, [GM06], in saxosis alpinis, 2600 m,
26.07.1909, B. Davidoff (SOM39862!); Montes Rila, infra
opp. Samokov, in valle alpestri Levi Isker prope Mala
Cerkva, [GM07], 20-21.06.1929, S. Jávorka (BP454135!);
Mt. Bela Rila, supra rivum Dolna Leva Reka, [GM07], in
saxosis, 2250 m, 17.07.1911, B. Davidoff (SOM39830!,
SOM39854!); Rila Mts., decl. orient. “Sakan Dupka”,
[GM07], in saxosis umbrosis, 2400 m, 06.07.1909, B. Davidoff (SOM39864!, SOM39865!, SOM39867!, SO83837!);
SE Rila Mts., NE of the mountain Suha vapa, S of the
Grnčar chalet, [GM16], slopes with Pinus mugo, wet areas in scree, 1900 m, 24.07.1980, P. Frost-Olsen 3467
(P00897993!); Sud-est du Massif Rila, au nord-est du Mt.
Suha vapa, au sud de Grančar chalet, [GM16], pente couverte de Pinus mugo sur sol graveoleux humide, 1900
m, 24.07.1980, P. Frost-Olsen 3467, det. P. Frost-Olsen
(P04198971!, L987251 660!); Rila Mts., [Рила], peak
Mussala [Сталин], [GM17], eastern slope [източният
склoн], 2880-2900 m. 04.07.1957, I. Bondev [Ив. Бондев]
(SOM109121!); around the Sara-Gyol, Chadur Tepe and
Mussala [покрай Саръ Гьол Чадър Тепе и Мусала],
[GM17], among rocks and on rocky meadows, in abundance [по скалите и скалните поляни, доста
разпрстр.], 06.09.1919, B. Achtarov (SOM39836!); Rila
pl., Musalensky masiv, [GM17], 07.1927, J. Zolikoffer
(SOM39829!); Rila, Musala, [GM17], 2300 m, 25.07.1993,
Jovanović, S. 155/93 (BEOU!); Rila, pored staze od hiže
Musala ka vrhu Musala, [GM17], silikat, 05.08.2013, N.
Kuzmanović, S. Đurović 39634 (BEOU!); Musalla,
[GM17], 26.07.1892, J. Wagner 51 (BP192810!); Musala,
[GM17], 1906, unknowun coll. (SOM39839!); m. Musala,
[GM17], in rivularibus, 17.07.1907, Jv. K. Urumov
(BP168853!); m. Musala, [GM17], J. K. Urumov 618
(BP168850!); m. Musala, [GM17], 04.08.1899, V. Střibrný
(P02542172!); Mt. Musala, [GM17], in excelsis humidis
summae regionis alpinae, 02.08.1920, Jv. K. Urumov
(SOM39841!); Mt. Musala, [GM17], in rivularibus, 1906,
Jv. K. Urumov (SOM39842!); Mt. Musala, [GM17], in
rivularibus, 1908, I. K. Urumoff (SOM39837!); ad cuc.
Musala, [GM17], in saxosis alpinis, 2600 m, 18.08.1913,
B. Achtaroff (SOM39825!); Мусала, [GM17], 02.08.1912,13.07.1903, (SOM39844!); Mussala [Мусала], [GM17],
2700 м, 26.06.1932, B. Achtarov [Б. Ахтаров],
(SOM39828!); Mussala [Муссала], [GM17], Mussala
[Муссала], [GM17], 08.1905, V. Střibrný (SOM39838!,
39845!, 39847!); South Rila, Suhoto Lake [Южна Рила,
Сухото езеро], [GM17], 07.1980, S. Tonkov [Сп. Тонков],
det. S. Tonkov [Сп. Тонков] (SO90328!); Rila Mts., the
peak Deno [Рила, на в. Дено], [GM17], very humid grassy places, western slope, ca. [силно влажни тревисти
места по западна склон, към] 2400 m [м.н.в.],
22.06.1968, N. Vihodcevski [Н. Виходцевски], det. N. Vihodcevski [Н. Виходцевски] (SO37767!); Rila Mts.,
cacumine Deno, [GM17], in saxosis declivibus, solo
granitico, 2300 m, 23.07.1952, B. Kitanov, det: B. Kitanov
(SO37768!, BP168070!); Rila Mts., Bistrtsa Lakes, near
Mussala [Рила пл., Бистрични езера под Мусала],
[GM17], 08.1897, V. Střbrný [В. Стрибърни], det. V.
Střbrný [ В. Стрибърни] (SO37762!); Rhodope centralis,
montis Musala supra locus alpinos, i.c. supra fontes
Maritzae fluvium, non procul ad urbe Samokov, [GM17],
in rupestribus alpinis, 26.07.1892, J. Wagner s.n.
(BEOU!); Montes Rhodope occidentales, in monte Musalla prope Čamkoria (Borovets), [GM17], in rupestribus,
substr. silic., c. 2200-2600 m.s.m., 24.-26.07.1930. K. H.
Rechinger fil. (BP168051!); Rhodope centralis, montis
Musala supra locus alpinos, i.c. supra fontes Maritzae
fluvium, non procul ad urbe Samokov, [GM17], in rupestribus alpinis, 26.07.1892, J. Wagner (BP192821!,
83
84
vol. 42 (1)
BP168851!); (P02567976!, P02542170!, P04202637!);
Rhodopes centralis, montis Mušala, supra fontes fl.
Maritzae non procul oppido Samokov, [GM17], in rupestribus alpinis, 26.07.1892, J. Wagner 7703/2935
(BP688978!); 2935 (P02567974!, P04166218!, P02542168!);
Rila Mts., Marichini springs near Mussala [Рила пл.,
Маричини извори под Мусала], [GM17], 11.08.1899, V.
Střbrný [В. Стрибърни], det. V. Střbrný [В. Стрибърни]
(SO37761!); Rila Mts., on the shores of the upper Marichino Lake [Рила планина, край бреговете на горно
Маричино езеро], [GM17], 14.07.1988, D. Peev [Д.
Пеев], det. D. Peev [Д. Пеев] (SOM149660!); mt. Zelena
Rila, ad rivum Desni Ibar, [GM27], in saxosis, 2200 m,
16.08.1911, B. Davidof, (SOM39832!); Rila Mts, the peak
Ibar [Рила, на в. Ибър], [GM27], on steep rocks and
rocky soils, northeastern slopes, [по стръмни скали и
скални почви с. изт. склонове, на в.] 2600 m [м],
06.09.1919, B. Achtaroff, (SOM39827!); mt. Zelena Rila,
Kotlinite, [GM37], in saxosis mughetosis, 2200 m,
13.08.1912, B. Davidoff (SOM39866!); Eastern Rila Mts.,
above the hut Belmeken, rocks on the path to the sprort
base of Belmeken [Изт. Рила, над х. Белмекен, на скали до пътеката за спортната база Белмeкен], [GM37],
eastern exposure [източно изложение], 2350 m [м.
надм. в.], 28.07.2007, A. Tashev [Ал. Ташев], det. A. Tashev [Ал. Ташев] (SOM165610!); Rila Mts, Belmeken
[Рила пл., на Белмекен], [GM37], on rocky wet slopes
[по скалисти влажни склонове], 12.08.1947, A, Yanev
[Ас. Янев], det. A. Yanev [Ас. Янев] (SO37769!); Rila
Mts., around the upper Belmeken Lake [Рила пл., около
г. Белмекенско езеро], [GM37], on wet slopes [по влажните места на склоновете], 12.07.1889, St. Gheorghieff
(SO37765!); mt. Zelena Rila, Sinžirli Čal, [GM37], in
rupestribus, 12.07.1893, B. Davidoff (SOM39851!); mt.
Zelena Rila, Sinžirli Čal, [GM37], in rupibus inter
Mugheto, 12.07.1893, B. Davidoff (SOM39852!); Rila Mts.
Sungurli Chal [Рила планина, Сунгурли чал], [GM37],
on rocky places [по скалисти места], 12.07.1889, St.
Gheorghieff (SO37763!); Rila Mts., Kostenetski Balkan,
Kotlinite, [Рила пл., Костенецки балкан, Котлините]
[GM37], 13.07.1889, St. Gheorghieff (SO37764!).
MONTENEGRO (UTM Grid zone 34T). — Gusinje, Brada Vezirik b. Gusinje, [DN00], 09.07.1939, B.
Schütt (BREM03047!); Bertiscus, m. Bijelić supra Gusinje, [DN00], 07.1933, V. Lindtner, det. V. Lindtner
(BEO11415!); m. Белић [Bjelič / DN00], кречњаци алписког појаса [krečnjaci alpiskog pojasa], 22.07.1933,
П. Черњавски, И. Рудски, В. Линдтнер, det. V. Nikolić
(BEO11410!); Prokletije, Bjelič, Borit katun, [DN00],
krečnjak, 1900 m, 06.06.1988, D. Lakušić 31/88 (BEOU!);
Prokletije, Maja Kolata, [DN00], Asplenietea rupestris,
krečnjak, 2400 m, 05.07.1995, V. Stevanović, D. Lakušić,
M. Niketić, Z. Bulić, S. Hadžiablahović 368/95 (BEOU!);
Prokletije, Maja Karanfilit, Krošnja, [DN00], stene,
1300-2200 m, 26.07.2003, M. Niketić, G. Tomović, S.
Hadžiablahović 17682 (BEOU!); Prokletije, Ćafa Borit,
[DN00], krečnjak, 07.07.2005, M. Niketić, G. Tomović
19876 (BEOU!); Prokletije, Ropojana, 42.497000
N, 19.816660 E, [DN00], sipari, Drypetea spinosae,
krečnjak, 1260 m, 28.07.2011, D. Lakušić, S. Vukojičić,
G. Tomović, N. Kuzmanović, B. Surina, R. Di Pietro, A.
Radalj 33657 (BEOU!); Prokletije, Karanfili, Kotlovi, 42
29.980 N, 19 47.853 E, [DN00], snežanici, Salicetea herbaceae, krečnjak, c. 1500 m, 17.07.2010, D. Lakušić 31210
(BEOU!); Prokletije, Maja Karanfili, Ljubokuč, 42.51224
N, 19.79424 E, [DN00], 1635 m, 13.07.2016, D. Lakušić,
N. Kuzmanović, I. Janković, 46018 (BEOU!); Prokletia,
Gebirge bei Gussinje, [42.56309696, 19.83769266 /
DN01], 12.07.1927, B. Schütt (BREM03043!); Bertisci,
Zeletin, Rogovi, [DN02], versus septentr., solo calcareo, 2000 m, 14.07.1924, M. Šoškić s.n. (BEOU!); Montenegro, ad fines arnautorum, in mte Zeletin, [DN02],
c. 1700 m, rarissime, 06.1903, J. Rohlena (BP168854!);
Prokletije, Čakor-Vaganica, [DN12], pašnjaci, 18502110 m, 24.07.1971, V. Nikolić, N. Diklić, det. N. Diklić
(BEO46825!); distr. Kuči, Žijovo, m. Hat, [42.547185 N,
19.498693 E / CN71], in rupestribus, 02.09.1902, A. Baldacci 42 (P02542167!, P02567977!, P02567978!); distr.
Kuči, Čafa Velja supra Rikavac, [CN81], in rupestribus, 01.08.1900, A. Baldacci 265 (BEOU!); (P02542173!,
P02567980!, P02567982!); Prokletije, Kučke Prokletije, Velji vrh, [CN81], krečnjak, 19.07.2003, D. Lakušić,
F. Conti, Z. Bulić, M. Niketić, G. Chiasetti, G. Tomović
18511 (BEOU!); Prokletije, Kučke Prokletije, cirkovi ispod Pasjaka, 42.57964 N, 19.56673 E [CN81], 1749
mnv , sipari, krečnjak, 15.07.2017, D. Lakušić, B. Surina, N. Kuzmanović, I. Janković, P. Glasnović, Balant,
M. (BEOU!); distr. Kuči, ad Mirčev do supra Rikavac,
[42.572895 N, 19.599391 E / CN81], in rupestribus alpinis, 14.07.1898, A. Baldacci 194 (P02542174!, P02567981!,
P02567985!).
SERBIA (UTM Grid zone 34T). — Prokletije, Prilepske planine, [DN21], 21.06.1957, M. Janković s.n., det. G.
Tomović (BEOU!); Prokletije, Nedžinat, [DN22], osuline i kamenjari, 2200-2450 m, 15.07.1973, V. Nikolić, N.
Diklić, M. Bogdanović, det. N. Diklić (BEO46828!); Prokletije, Nedžinat, [DN22], predeo oko jezera, mešovita
četinarska šuma, krečnjak, N exp., c. 2000 m, 27.07.1971,
V. Nikolić, N. Diklić, det. N. Diklić (BEO46826!); Mt.
Неџинат, при врху изнад језера [Nedžinat, pri vrhu
iznad jezera / DN22], кречњачке стене код Mughetuma, 28.08.1933, P. Černjavski, I. Rudski, V. Lindtner, det.
P. Černjavski (BEO11412!); Bertisci, m. Hajla, [DN23],
2200 m, 08.1922, Gošović, St. s.n. (BEOU!); m. Hajla ad
Peć, [DN23], in pratis humidis, solo calcareo, c. 2200 m,
09.1957, D. Mirić, det. V. Lindtner (BEO46827!); Prokletije, Koprivnik, Belopoljski stanovi-Maja Ljubenić-Jelivi
sluzi, [DN31], 09.07.1958, M. Janković s.n. (BEOU!);
Prokletije, Koprivnik, [DN32], Mugus sa Wulfeniom,
10.07.1963, M. Janković s.n. (BEOU!); Проклетије, Крш
D. Lakušić et al.: Distribution and variability of Geum bulgaricum
Чврље, [Prokletije, Krš Čvrlje] [DN32], 06.07.1963, M.
Janković s.n. (BEOU!); Bertisci, m. Koprivnik, [DN32],
in saxosis humidis regionis subalpine, 15.06.1923, N.
Košanin s.n. (BEOU!); Bertisci, m. Koprivnik, [DN32],
in saxosis humidis regionis subalpine, 15.06.1923, Th.
Soška s.n. (BEOU!); Mt. Koprivnik, ca. urb. Peć, [DN32],
in glareosis, in Pinus mughi, c. 2300 m, 07.07.1935, O.
Grebenščikov, det. O. Grebenščikov (BEO11411!); Žljeb,
Maja Rosulija, [DN33], 2000-2100 m, 25.06.1932, I. Rudski, det. V. Nikolić (BEO11414!);
Field observations
ALBANIA (UTM Grid zone 34T). — District of Malësi e
Madhe (Rrethi i Malësisë së Madhe), Bjeshkët e Nemuna
Mts. (Prokletije Mts.), above the village of Bogë, north
of the peak Mt. Maja e Dragomirit (1901.6 m) and northeast of the peak Mt. Maja e Borës (1780 m), 42.40866 N,
19.61152 E, [CM89], in Bosnian pine forest, on limestone,
1618 m, 07.12.2010, Barina, Z. et al.; District of Malësi e
Madhe (Rrethi i Malësisë së Madhe), Bjeshkët e Nemuna
Mts. (Prokletije Mts.), above the village of Bogë, W of the
bjeshkë (pasture) „Jaraku“, towards Mt. Maja e Bridashes
(2125.2 m), 42.41958 N, 19.65321 E, [CM89], on limestone rocks, 1866 m, 13.07.2010, Barina, Z. et al.; District of
Malësi e Madhe (Rrethi i Malësisë së Madhe), Bjeshkët e
Nemuna Mts. (Prokletije Mts), above the village of Bogë,
Qafa e Mushkut Pass, 42.42995 N, 19.69161 E, [CM99],
on limestone rocks, 2234 m, 13.07.2010, Barina, Z. et al.;
District of Malësi e Madhe (Rrethi i Malësisë së Madhe), Bjeshkët e Nemuna Mts. (Prokletije Mts.), between
the villages of Bogë and Nikç, north of the pasture Surta e Bogës, at Tarn Liqeni i Bogës, 42.45114 N, 19.71193
E, [CN90], in rocky grassland, on limestone, 1729 m,
14.07.2010, Barina, Z. et al.; District of Malësi e Madhe
(Rrethi i Malësisë së Madhe), Bjeshkët e Nemuna Mts.
(Prokletije Mts), above the village of Nikç, on the S slope
of Mt maja e Shnikut (2552.2 m), 42.4674 N, 19.74484 E,
[CN90], in limestone scree, 2259 m, 15.07.2010, Barina,
Z. et al.; District of Malësi e Madhe (Rrethi i Malësisë së
Madhe), Bjeshkët e Nemuna Mts. (Prokletije Mts.), above
the village of Nikç, on the southern slope of Mt. Maja e
Shnikut (2552.2 m), 42.46105 N, 19.74306 E, [CN90], in
rocky grassland, on limestone, 1870 m, 15.07.2010, Barina, Z. et al.; District of Tropojë (Rrethi i Tropojës), on
the northern slope of Mt. Maja e Ershelit, above village
Peraj, 42.3013 N, 19.8557 E, [DM08], in limestone scree,
1441 m, 15.07.2014, Barina, Z. et al.; District of Tropojë
(Rrethi i Tropojës), Mt. Maja e Shtrazës, above village Peraj, 42.30975 N, 19.84522 E, [DM08], on limestone rocks,
1907 m, 16.07.2014, Barina, Z. et al.; District of Tropojë
(Rrethi i Tropojës), Gropat e Shtarzes, above village Peraj,
42.31171 N, 19.85205 E, [DM08], in northrern exposed,
closed grassland, on limestone, 1823 m, 17.07.2014, Barina, Z. et al.; District of Tropojë (Rrethi i Tropojës), Gropat e Shtarzes, above village Peraj, 42.31284 N, 19.85601
E, [DM08], in northrern exposed, closed grassland, on
limestone, 1620 m, 17.07.2014, Barina, Z. et al.; District
of Tropojë (Rrethi i Tropojës), Gropa e Grades, above
village Peraj, 42.33474 N, 19.85024 E, [DM08], in rocky
grassland, on limestone, 1630 m, 18.07.2014, Barina, Z. et
al.; District of Tropojë (Rrethi i Tropojës), Mts. Albanian
Alps (Alpet Shqiptare, Bjeshkët e Nemuna, Prokletije),
west of town Bajram Curri (Kolgecaj), on the northern
slope of the 2026 m high mount south of mt maja e Dhive (2333 m), 42.34041 N, 19.98508 E, [DM18], in rocky
grassland, on limestone, 2022 m, 02.06.2009, Barina, Z.
et al.; District of Tropojë (Rrethi i Tropojës), on the northern slope of Mt maja e Gavnit (2509 m) above homestead stanet e Droçës, above village Dragobi (Hajdaraj),
42.39832 N, 19.93963 E, [DM19], in rocky grassland, on
limestone, 1654 m, 21.07.2012, Barina, Z. et al.; District
of Tropojë (Rrethi i Tropojës), on the slope of Mt Alshines (2211 m), above village Curraj i Epërm, 42.38067
N, 19.96711 E, [DM19], in rocky grassland, on limestone,
2331 m, 22.07.2012, Barina, Z. et al.; District of Tropojë
(Rrethi i Tropojës), on the southern slope of Mt maja e
Gavnit (2509 m) above village Curraj i Epërm, 42.38557
N, 19.92471 E, [DM19], in rocky grassland, on limestone,
1985 m, 23.07.2012, Barina, Z. et al.; Kukës county, Shkëlzen Mts, Mt Maja e Radeshës above village Kërnajë,
42.433615 N, 20.086204 E, [DM29], on limestone rocks,
2050 m, 23.05.2016, Barina, Z. et al.; District of Dibër
(Rrethi i Dibrës), Mt Ruja e Lura above village Fushë
Lurë, 41.78441 N, 20.24803 E, [DM32], in rocky grassland, on limestone, 1846 m, 21.06.2013, Barina, Z. et al.;
District of Dibër (Rrethi i Dibrës), Mt Ruja e Lura above
village Fushë Lurë, 41.77728 N, 20.25961 E, [DM32], on
limestone rocks in dolina, 1713 m, 21.06.2013, Barina, Z.
et al.; District of Tropojë (Rrethi i Tropojës), on Mt Maja
a Gjytetit (2044 m), above village Çerem, 42.47773 N,
19.9852 E, [DN10], in limestone scree, 2128 m, 10.07.2011,
Barina, Z. et al.; District of Tropojë (Rrethi i Tropojës),
between homesteads Gjarpnit e Siperme and Gjarpnit a
Poshtme, above village Dragobi, 42.46473 N, 19.99193 E,
[DN10], in limestone karst, 2043 m, 10.07.2011, Barina,
Z. et al.; District of Tropojë (Rrethi i Tropojës), Mts. Albanian Alps (Alpet Shqiptare, Bjeshkët e Nemuna, Prokletije), above town Tropojë, on the northern slope of mt.
Shkëlzen (2404.4 m), 42.46181 N, 20.11676 E, [DN20], on
limestone rocks, 2009 m, 06.06.2009, Barina, Z. et al.;
District of Tropojë (Rrethi i Tropojës), Mts. Albanian
Alps (Alpet Shqiptare, Bjeshkët e Nemuna, Prokletije),
above town Tropojë, at the northern foot of cliffs of mt.
Shkëlzen (2404.4 m), 42.46461 N, 20.12662 E, [DN20],
in closed mountaine grassland, on limestone, 2041 m,
06.06.2009, Barina, Z. et al.
MONTENEGRO (UTM Grid zone 34T). — Prokletije,
Plavsko-Gusinjske Prokletije, Planinica, [42.681458 N,
20.014671 E / DN12], 2000 m, sipari, krečnjak, 15.07.2015,
B. Surina, N. Kuzmanović; Prokletije, Kučke Prokletije,
cirkovi ispod Surdupa, [42.585924 N, 19.545372 E / CN81],
85
vol. 42 (1)
86
1750 m, sipari, krečnjak, 15.07.2017, D. Lakušić, B. Surina,
N. Kuzmanović, I. Janković, P. Glasnović, Balant, M.; Prokletije, Kučke Prokletije, cirkovi ispod Štitana, [42.575852
N, 19.558760 E / CN81], 1850 m, sipari, krečnjak, 14.07.2017,
D. Lakušić, N. Kuzmanović, I. Janković.
Acknowledgements — This work was supported by Ministry of Education and Science of the Republic of Serbia
(Grant No. 173030 to D. Lakušić). Many thanks to the
curators of BEO, BEOU, BP, BREM, P, SARA, SO, and
SOM for help while searching for the type material and
permission to reproduce images of the herbarium specimens. Thanks to Lulezim Shuka (Tirana), Sonya Tsoneva (Sofia), and Yulia Boseva (Sofia) for data and images
of plants from Albania and Bulgaria. The authors also
thank Dr. Spencer C. Brown from the Institut des Sciences du Végétal (CNRS, Gif-sur-Yvette) for his expert assistance in flow cytometry on the IMAGIF platform of
cytometry. Finally, many thanks to an anonymous reviewer for very valuable comments and suggestions.
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REZIME
Rasprostranjenje i varijabilnost Geum bulgaricum
(Rosaceae), vrste od evropskog interesa
Dmitar Lakušić, Gordana Tomović, Chavdar Gussev, Zoltán Barina, Sonja
Siljak-Yakovlev, Nevena Kuzmanović, Ivana Janković i Snežana Vukojičić
K
ao evropski endemit, sa arealom ograničenim na nekoliko evropskih država, Geum bulgaricum Pančić je
definisan kao “ciljna vrsta” ili “vrsta od evropskog interesa”. Iako se radi o vrsti od velikog međunarodnog
značaja, njeno rasprotranjenje je nedovoljno poznato. Na osnovu viešegodišnjih terenskih istraživanja,
analize herbarskih i literaturnih podataka, potvrđeno je da je G. bulgaricum balkanska endemična vrsta
rasprostanjena u Albaniji, Bosni i Hercegovini, Bugarskoj, Crnoj Gori i Srbiji. Njen areal je podeljen na dva
glavna dela “istočni” (Rila u Rodopskom planinskom sistemu), i “zapadni” (nekoliko planina u Dinarskom
i jedno izolovano nalazište u severoistočnom delu Skardo-Pindskog planinskog sistema), u okviru koga su
sve populacije grupisane u četiri disjunkcije. Vrsta se najčešće nalazi u alpijskim i subalpisjkim acifofilnim
(Juncetea trifidi) i kalcifilnim (Elino-Seslerietea) rudinama, a ređe i u vegetaciji sipara (Thlaspietea rotundifolii),
pukotina stena (Asplenietea trichomanis), žbunjacima bora krivulja (Roso pendulinae-Pinetea mugo) i veoma
lokalizovano na serpentinskim kamenjarima. Ukupan dijapazon nadmorskih visina se kreće između 1200 i
2700 m. Horološki podaci su su prikazani na UTM karti 10 × 10 km, a veliki broj nalaza je georeferenciran
sa koordinatama u WGS84 sistemu. Na osnovu horoloških podataka i procene stanja poplacija G. bulgaricum
je definisan kao IUCN NT u Bugarskoj, Albaniji i Crnoj Gori, i VU D2 E u Srbiji i Bosni i Hercegovini. S
obzirom da do sada G. bulgaricum nije bio predmet bilo kakvih detaljnih studija, u radu je prikazan prvi
uvid u diferencijacije populacije. Pokazano je da se Rodopske i Dinarske populacije neznatno razlikuju na
morfološkom nivou, ali i das u veoma dobro izdiferencirane u pogledu veličine genoma. Na kraju je izvršena i
lektotipifikacija imena Geum bulgaricum.
Ključne reči: Balkansko poluostrvo, ugrožene vrste, veličina genoma, Geum, lektotip, morfologija