Soil and Biota of Serpentine: A World View
2009 Northeastern Naturalist 16(Special Issue 5):39–55
Morphological Variation in Teucrium chamaedrys
in Serpentine and Non-Serpentine Populations
Dolja Pavlova*
Abstract - Teucrium chamaedrys is the most variable species in the genus Teucrium,
fitting Kruckeberg’s category of a bodenvag species. Six populations distributed on
serpentine and 3 populations off serpentine were investigated, and 23 morphological
features were studied by univariate and multivariate statistical analyses. The variation
was higher for the vegetative features and not clearly expressed for the generative
ones. In addition, metal concentration in the populations and soil were studied. The
species tolerant to the serpentine conditions demonstrated specific morphological
differences in stem length, stem length up to the first leave pair, and internode length
between second and third leave pairs. Morphological differences, geographical isolation,
and preliminary results on the karyology of T. chamaedrys in Bulgaria, suggest
that the populations studied were different ecotypes.
Introduction
Teucrium chamaedrys L. (Wall germander) is a widely distributed species
of Teucrium (Lamiaceae) found in Bulgaria and other countries in Central
Europe. This perennial plant occurs in all floristic regions of Bulgaria up to
1500 m above sea level (Markova 1992, Peev 1989) and shows a high degree
of morphological diversity. Reichinger (1941) considered it to be the most
variable taxon in the Teucrium genus and described 15 subspecies, most of
them locally distributed. These subspecies were not initially included in
Flora Europaea (Tutin et al. 1972) but were later added by Greuter et al.
(1986). Interest in T. chamaedrys is increased by the fact that it is one of
766 species of medicinal plants in the Bulgarian flora (Gussev 2005). The
distribution and the degree of presence of medicinal plants are directly correlated
to edaphic factors (Obratov-Petković et al. 2006). Also, the quantity
of active substances in plant tissues depends on many ecological factors that
affect the vegetative plant organs (Lombini et al. 1999).
The species demonstrates a wide ecological tolerance as it is found in
open grasslands, oak woodlands, pastures, calcareous and siliceous terrains,
and on serpentine outcrops. Serpentine outcrops are probably the most
extreme habitat conditions for this species. Serpentines and their soils are
characterized by toxic quantities of heavy metals (particularly Ni and Cr),
low Ca/Mg ratio, drought, and wide temperature fluctuations, and plant populations
growing on serpentine sites are likely adapted at some level to these
special edaphic conditions (Brooks 1987; Kruckeberg 1984, 1992). Many
*University of Sofia, Faculty of Biology, Department of Botany, Boulevard Dragan
Tzankov 8, 1164 Sofia, Bulgaria; pavlova@biofac.uni-sofia.bg.
40 Northeastern Naturalist Vol. 16, Special Issue 5
studies have documented variability of plant species growing on serpentine
habitats (Bratteler et al. 2006; Mayer and Soltis 1994; Štepankova 1996,
1997; Westerbergh and Rune 1996; Westerbergh and Saura 1992; Wright et
al. 2006).
The aims of this study were to investigate natural serpentine and nonserpentine
populations to: 1) document differences in morphological traits
between-populations, and 2) compare the chemical composition in soils and
plants from these populations.
Material and Methods
Sites and sampling
Nine populations of T. chamaedrys originating from localities distributed
in southern Bulgaria were investigated (Fig. 1, Table 1). Six sites were serpentine
and three were non-serpentine. The non-serpentine localities were
Figure 1. Map of Balkan Peninsula with distribution of the serpentines. Open circles
indicate serpentine populations. Filled circles indicate non-serpentine populations.
The numbers correspond to the localities described in Table 1.
2009 D. Pavlova 41
selected on both calcareous (Beledie Han) and siliceous (Rila) terrains. Random
plants within each locality were collected during 2006–2007. Voucher
specimens from all investigated populations were assigned a voucher number
(Table 1) and placed in the Herbarium of University of Sofia (SO). Soil
samples from five serpentine and two non-serpentine sites were collected to
determine their chemical composition.
Measurements
The investigation of morphological differences between serpentine and
non-serpentine plants was performed on 225 individuals (25 individuals per
site) using 23 morphological characters (Var. 1 to Var. 23; Table 2). For each
individual, a leaf from the second pair and a flower from the lower part of
the inflorescence were measured. Vegetative characters were studied on dry
plants, and flower characters were measured after boiling. One flower per
individual was boiled in distilled water for 1–2 min to facilitate measuring.
Table 1. List of the localities of the studied populations of Teucrium chamaedrys. # = number of
individuals sampled, Abbr. = abbreviations used for the populations (see text).
No Locality Voucher No # Abbr.
Serpentine populations
1 Central Rhodope Mts. – Parvenetz village, southeastward on SO 103375 25 P
the open stony slope, 277 m above sea level, N42°03.96',
E24°39.44', UTM Grid -LG-06; D. Pavlova, August 2007
2 Eastern Rhodope Mts. – Fotinovo village westward from the SO 104608 25 F
village, 421 m a.s.l., UTM Grid - LF-68; D. Pavlova,
October 2007
3 Eastern Rhodope Mts. – Dobromirtzi village, southwestward SO 104607 25 D1
from the village, on the basis of the hill, left side of the
road to Zlatodrad, 320 m a.s.l., N41°23.18', E25°12.24',
UTM Grid - LF-58; D. Pavlova, October 2007
4 Eastern Rhodope Mts. – Dobromirtzi village, southwestward SO 104604 25 D2
from the village, on the top of the hill, left side of the road
to Zlatodrad, 400 m a.s.l., UTM Grid - LF-58; D. Pavlova,
October 2007
5 Vlahina Mts. – Murdzova chuka peak, northward of Stara SO 104902 25 Z
Zeleznitza village, 720 m a.s.l., UTM Grid -FM-74;
D. Pavlova & A. Nedelcheva, July 2006
6 Ograzden Mts. – easterward from the Gega village, SO 104513 25 G
Black rocks locality, 600 m, a.s.l., UTM Grid - fl-69;
D. Pavlova & A. Nedelcheva, July 2007
Non-serpentine populations
7 Rila Mts. – meadows after Rila Monastery, left site of the SO 104606 25 R
road to Kirilova poljana, 1246 m a.s.l., N42°08.67',
E23°21.7'; UTM Grid - FM-96; D. Pavlova &
A. Nedelcheva, July 2007
8 Sofia region – Beledie han locality on calcareous terrain SO 104954 25 BH1
northern from Beledie Han village, 700 m a.s.l., UTM
Grid - FN-74; N. Tzoneva & A. Nedelcheva, April 2007
9 Sofia region – Beledie han locality on calcareous terrain SO 104955 25 BH2
northern from Beledie Han village, 720 m a.s.l., UTM
Grid - FN-75; N. Tzoneva & A. Nedelcheva, April 2007
42 Northeastern Naturalist Vol. 16, Special Issue 5
Statistical analysis
Univariate and multivariate statistical procedures were applied to study
morphological variation among the populations. Cluster analysis using
Euclidean distances and unweighted pair group average (UPGMA) as
computational criteria were used to examine the similarities between the
populations (Fig. 2). Canonical discriminant analysis (CDA) was applied
to discriminate the morphological variation and to differentiate serpentine
and non-serpentine populations (P < 0.001). Principal component analysis
(PCA) was used to show the loadings for each character and which character
contributed most for differences between groups. Eigen values were
extracted from the correlation matrix. Basic descriptive statistics, Tukey-test
for independence of groups, one-way ANOVA, and cluster analyses were
also used to determine the differences between the serpentine and non-serpentine
populations. All statistics were performed using StatSoft - Statistica
7 program.
Table 2. Characters investigated on the plant samples of Teucrium chamaedrys on the individuals
from serpentine (S) and non-serpentine (NS) soils, and their number (Var.). Values shown
are: mean and standard deviation (s.d.) for each soil type, P-level results of t-tests, and the
standardized coefficients (Root 1 and Root 2) of the variables which contribute most to the
group separation.
Variable S NS P
Character No mean s.d. mean s.d. levels Root 1 Root 2
Stem height [mm] Var. 1 76.93 37.24 119.69 47.72 0.00 -0.13 -0.39
Stem length from the bottom to Var. 2 23.45 16.45 37.59 21.54 0.00 0.15 -0.22
the first leaves pair [mm]
Leaf length [mm] Var. 3 17.51 9.05 18.56 3.15 0.33 -1.26 0.09
Leaf width [mm] Var. 4 7.79 2.40 9.68 1.90 0.00 0.26 0.06
Ratio Var. 3:Var 4 Var. 5 2.33 1.24 1.96 0.35 0.01 1.19 0.10
Leaf teeth number Var. 6 5.04 0.96 4.71 0.84 0.01 0.00 0.16
Middle leaf teeth length [mm] Var. 7 2.19 0.82 2.51 0.72 0.01 0.16 -0.04
Upper leaf teeth length [mm] Var. 8 1.28 0.45 1.32 0.47 0.54 0.10 -0.29
Petiole length [mm] Var. 9 3.40 1.24 4.89 1.34 0.00 -0.21 0.02
Internode length between 2nd Var. 10 9.96 3.82 16.00 8.67 0.00 0.21 -0.51
and 3rd leaf pair [mm]
Inflorescence length [mm] Var. 11 24.11 17.33 53.64 15.23 0.00 -0.09 -1.17
Inflorescence width [mm] Var. 12 13.31 9.00 14.48 2.33 0.52 -0.02 0.24
Ratio Var. 11:Var. 12 Var. 13 1.88 1.68 3.77 1.36 0.00 0.07 1.14
Number verticelasters in the Var. 14 4.11 1.71 7.60 1.26 0.00 0.37 0.14
inflorescence
Peduncle length [mm] Var. 15 2.01 1.80 2.06 0.46 0.90 0.07 0.00
Calyx length [mm] Var. 16 5.03 1.21 6.06 0.46 0.00 0.32 -0.08
Calyx tooth length [mm] Var. 17 1.79 0.61 2.02 0.23 0.06 0.12 0.07
Corolla tube length [mm] Var. 18 4.84 1.54 5.26 0.66 0.18 -0.12 -0.12
Corolla lower lip length [mm] Var. 19 11.78 3.79 12.04 2.27 0.74 0.04 0.06
Corolla lower lip width [mm] Var. 20 4.87 1.74 4.94 0.78 0.85 0.25 0.34
Tooth of the lower lip [mm] Var. 21 2.78 1.71 2.86 0.44 0.82 0.24 0.14
Bract length [mm] Var. 22 9.99 3.08 14.04 2.32 0.00 0.27 -0.08
Bract width [mm] Var. 23 3.75 1.54 6.00 1.29 0.00 -0.12 -0.05
2009 D. Pavlova 43
Soil and plant analyses
Seven composite soil samples were analyzed. Three soil cores per site at
a depth of 0–15 cm were obtained near the plants collected for analysis and
were composited for soil analyses. All plant samples were cleaned, dried,
and ground to a fine powder. Vegetative and floral plant tissues used in pharmacy
as Herba Teucrii chamaedri were analyzed for metal content. Element
concentrations were determined following the standard No. 11466/1995 of
extraction of trace elements soluble in aqua regia proposed by International
Organization for Standards (ISO). The total concentrations of Cd, Co, Cr,
Fe, Mn, and Ni in aqua regia extracts of soil were determined with flame
and atomic absorption spectrophotometers. All concentrations were within
the detection limits of the analyses used. Soil Ca/Mg ratio and soil pH (in
H2O) were also measured. The analyses were conducted at the Institute of
Soil Science “N. Poushkarov” in Sofia, Bulgaria.
Results
The statistical analyses found significant differences between plant populations
growing on serpentine and those on non-serpentine soils. The range
of variability of all morphological features in both groups of populations
overlapped considerably. Most notable is the substantial variability in the
vegetative set of characters compared to the generative parts of plants where
Figure 2. Cluster diagram showing the groups of similarity among the populations
investigated.
44 Northeastern Naturalist Vol. 16, Special Issue 5
variability was hardly detected. The groups of similarities, following the
cluster analysis, are synchronous with groups distinguished by the discriminant
and PCA analyses. The mean values and the standard deviation of the
investigated morphological characters for the serpentine and non-serpentine
population as well as P-values from t-tests of the differences between the
means are presented in Table 2. The results from Tukey-tests indicated only
9 of the analyzed characters (leaf length, upper leaf teeth length, inflorescence
width, peduncle length, calyx tooth length, corolla tube length, corolla
lower lip length, corolla lower lip width, and length of tooth of the lower
lip) were not significantly different (P < 0.05) between serpentine and nonserpentine
individuals. Basic descriptive statistics and one-way ANOVA
analyses demonstrated that the range of variability for most morphological
features in populations overlapped considerably. Most of the characters unsuitable
for discrimination of the populations were related to flower characteristics.
Conversely, the difference between serpentine and non-serpentine
populations was highly significant for the stem height, stem length up to
the first leaf pair, leaf width, internode length between the second and third
leaf pairs, length of flowering stem, number of flowers in verticelasters, and
length and width of bracts.
Cluster analysis
A cluster diagram of similarity among the nine populations based on
the 23 characters is presented in Figure 2. The nine populations formed
four clusters. The first group of similar serpentine populations included
Parvenetz (P), Dobromirtzi 2 (D2), and Zeleznitza (Z), and among them the
highest similarity observed was for P and D2. The second group included
the last three serpentine populations. The non-serpentine populations from
Beledie Han (BH1 and BH2) demonstrated the highest similarity to each
other and formed the third cluster. The cluster diagram shows that these
two non-serpentine populations are more closely related to some of the serpentine
populations than to other non-serpentine populations studied from
Rila (R). The population from Rila formed a separate, fourth cluster in the
diagram. The separation of this population was due to the highest stem
length, internode length between second and third leaf pair, inflorescence
length, and number of verticelasters in the inflorescence, which showed the
highest values from all studied populations. The vegetative characters contributed
the most to grouping the populations, while the generative traits
were more conservative.
Discriminant analysis
Canonical discriminant analysis (CDA) was applied to evaluate the
morphological variation between serpentine and non-serpentine populations
belonging to T. chamaedrys, where population was used as a classification
factor. The results are presented on a scatter diagram (Fig. 3). All characters
used in this analysis were significant (P < 0.00005) with the exception
of corolla tube length, for which P = 0.43. Three characters (inflorescence
2009 D. Pavlova 45
length, ratio of inflorescence length/width, and lower corolla lip length)
were not included due to their P-levels exceeding the limit. The results from
the analysis were obtained at Wilks’ Lambda = 0.0004, and P < 0.00005. The
analysis was based on two discriminant functions that account for the most
natural grouping of the population. The standardized coefficients of the variables
that contributed most to the group separation are given in Table 2.
The serpentine populations formed a relatively compact group that is
clearly distinguished from the non-serpentine populations. Though more
dispersed, the data from population Dobromirtzi (D1) was within the group
of the serpentines sites. The three non-serpentine populations are distributed
on the scatter diagram in two groups. The first group comprises the values
of the classification factors from the region of Sofia (BH1 and BH2), which
form a compact group, clearly distinguished and isolated from the group of
serpentine populations. The second group, although more dispersed, represents
the Rila (R) non-serpentine population. The position of this population
was closer to the compact group of the serpentine populations, but the discriminant
function 2 effectively separates it.
The application of the serpentine and non-serpentine ecotype as a classification factor suggests that stem height, stem length up to the first leaf pair,
leaf width, and internode length between the second and third leaf pairs are the
features which contributed most effectively to the discriminant function.
Figure 3. Scatter diagram of CDA of nine populations of Teucrium chamaedrys based
on 23 measured characters. The abbreviations used for the populations are given in
Table 1. S = serpentine populations, NS = non-serpentine populations.
46 Northeastern Naturalist Vol. 16, Special Issue 5
Principal component analysis
Percentage eigenvalues and factor loadings on the axes are reported in
Table 3. Ordination of the data set accounts for 51.9% with the first three
components. Plotting the first against the second axis (Fig. 4) produces a
two-dimensional scattergram where the loadings for each variable and their
contribution to each of the PCs are shown. In this case, the numbers of leaf
teeth and ratio between leaf length and leaf width with their positive coordinates
and correlations with factor 1 contribute to population divergence.
Most of the vegetative traits have positive coordinates and correlations with
factor 2. They had a clear negative correlation with the ratio between leaf
length and leaf width. The vegetative characters were well separated from
the generative ones. It is obvious that vegetative traits were more variable,
while some of the generative ones like corolla tube length and corolla lip
length and width were very closely correlated. An analysis using only floral
characters shows that the calyx traits contributed much to each of the PCs
and were more variable than the corolla traits. From the analysis of only the
vegetative characters, the numbers of leaf teeth and the ratio between leaf
length and leaf width were the most importance traits for separation of the
populations and were negatively correlated with the inflorescence traits.
Table 3. Percentage eigenvalues, variance explained by first three components, and factor loadings
of the variables.
Variable
code 1 2 3
Eigenvalue (%) 28.84 14.52 8.54
Cumulative (%) 28.84 43.36 51.90
Variables
Stem height StH -0.63 0.54 0.10
Stem length from the bottom to the 1st leaf pair StL -0.36 0.56 0.17
Leaf length Leafl-0.18 0.08 -0.91
Leaf width LeafS -0.46 0.49 -0.26
Ratio Var. 3:Var. 4 L/S 0.09 -0.23 -0.76
Leaf teeth number NTeeth 0.25 0.17 -0.11
Middle leaf teeth length MidLeafT -0.61 0.38 -0.23
Upper leaf teeth length UpLeafT -0.50 0.31 -0.30
Petiole length PetL -0.30 0.17 -0.23
Internode length between 2nd and 3rd leaf pair IntNode -0.71 0.43 0.04
Inflorescence length InflL -0.71 0.12 0.26
Inflorescence width InflS -0.19 -0.27 0.19
Ratio Var. 11:Var. 12 L1/S1 -0.58 0.12 0.24
Number verticelasters in the inflorescence fl-0.74 0.03 0.24
Peduncle length PedL -0.17 -0.28 0.03
Calyx length CaL -0.73 -0.32 0.01
Calyx tooth length CatL -0.38 -0.33 0.04
Corolla tube length Cot -0.62 -0.66 -0.03
Corolla lower lip length LipL -0.58 -0.67 -0.06
Corolla lower lip width LipS -0.54 -0.65 -0.07
Tooth of the lower lip TlipL -0.35 -0.48 -0.03
Bract length BrL -0.85 -0.03 -0.03
Bract width BrS -0.76 0.15 -0.05
2009 D. Pavlova 47
Soil and plant analyses
The results of the analysis of metal concentrations in soil and plant
samples of T. chamaedrys are given in Table 4.
The total Ca concentration in serpentine soil samples varied from 1840
mg/kg in site Dobromirtzi 2 (D2) to 8758 mg/kg in site Gega (G). In the nonserpentine
soil samples it ranged from 4569 mg/kg in site Rila (R) to 15,702
mg/kg in Beledie Han (BH1). Such high concentrations of Ca in Beledie Han
(BH1) are in conformity with the calcareous bedrock of the area. The content
of Mg was high in relation to Ca in all serpentine sites, and Ca/Mg ratios
were <1. The serpentine sample from Gega (G) had the highest Mg level,
with a value of 16,768 mg/kg. The soil samples from Rila and Beledie Han
had concentrations of Ca and Mg which are typical for non-serpentine substrates
and Ca/Mg ratio >1. While the amounts of Ca in the serpentine soils
were low, the concentrations in T. chamaedrys leaves were much higher. The
Ca/Mg ratio values in all plant samples were >1.
Figure 4. Principal component analysis plot variables (vectors). Length of the vectors
is proportional to the strength of the correlations between variables and one of the
PCs (factors). Variable codes as in Table 3.
48 Northeastern Naturalist Vol. 16, Special Issue 5
The serpentine soils studied are relatively rich in the toxic metals Ni, Cr,
and Co (Table 4). Nickel is known to be toxic in soils in quantities higher
than 500 mg/kg (Allen et al. 1974). The concentrations of Ni in the soil
samples were higher than 1000 mg/kg in all our sites except those in Gega,
Rila, and Beledie Han. The concentrations of Ni in the plant samples from
serpentines varied from 19.4 mg/kg to 28.4 mg/kg.
The amounts of Cr in all the serpentine sites, except Gega, were more
than 500 mg/kg and exceeded the upper limit for normal soils proposed by
Allen et al. (1974) and Brooks (1987) and were similar to soil Cr levels
reported by Karataglis et al. (1982) for northern Greece. Despite high total
soil Cr, the amounts of Cr taken up by plants were small. The plant sample
from Parvenetz (P) was the only sample where Cr (4.35 mg/kg) exceeded the
limits proposed by Kabata-Pendias and Pendias (1984).
The third element of this toxic group is Co. The amount of Co found in
soil and plant samples was lower than the limits of normal concentrations
proposed by Brooks (1987).
Table 4. Chemical composition (mg/kg on dry weight) of soil and plant samples. Population abbreviations:
F = Fotinovo, D1 = Dobromirtzi 1, D2 = Dobromirtzi 2, P = Parvenetz, G = Gega,
R = Rila, BH 1 = Beledie Han.
Populations
Serpentine Non-serpentine
F D1 D2 P G R BH 1
Ca
Soil 2120 1960 1840 2840 8758 4569 15,702
Plant 3600 3100 3500 3100 3368 8000 9420
Mg
Soil 12,633 5589 5832 2916 16,768 2187 5182
Plant 2700 1100 840 600 2065 1900 2123
Ca/Mg
Soil 0.17 0.35 0.32 0.97 0.52 2.08 3.03
Plant 1.33 2.81 4.16 5.16 1.63 4.21 4.43
Fe
Soil 47,200 72,800 71,000 42,800 25,774 20,900 36,291
Plant 168 363 474 538 503 380 489
Ni
Soil 1008 1428 1232 1312 101 24 39
Plant 19.4 23.9 28.4 21.7 24.8 0.8 1.1
Cr
Soil 672 542 548 591 36.5 21.9 52.2
Plant 1.30 1.38 2.92 4.35 1.40 0.14 0.21
Co
Soil 58 120 116 4 31 2 14
Plant 0.28 0.92 0.95 1.48 0.30 0.20 0.40
Cd
Soil 0.46 0.41 0.41 3.91 0.01 0.25 1.90
Plant 0.05 0.10 0.07 0.12 0.01 0.05 0.09
Mn
Soil 775 1895 1865 1505 1051 900 1994
Plant 18.0 26.3 30.0 30.0 18.8 52.0 64.0
pH 7.7 6.9 6.8 6.3 6.0 5.4 6.9
2009 D. Pavlova 49
The concentrations of Cd in the soils in all localities except Parvenetz (P)
and Beledie Han (BH1) were below the limits given by Allen et al. (1974).
The elevated Cd levels found in P and BH1 were probably caused by pollution
from nearby road traffic rather than from a property of the parent soil. Regardless
of soil Cd levels, Cd in T. chamaedrys plants were in the normal range.
The concentrations of Mn in soils varied between 775 and 1994 mg/kg,
and in plant tissues from 18 to 64 mg/kg. The high levels of Mn in the nonserpentine
(BH1) soil and also in the D1 and D2 soils is atypical and could
be caused by heavy road traffic in this area, the relief, the oak forest vegetation,
and/or the large percentage of organic material in the sample. The Mn
values in plants were within the range of the limits given by Kabata-Pendias
and Pendias (1984).
The concentration of Fe in all serpentine soil samples in this study were
found to be high, which is common in serpentine soil from the Balkan Peninsula
(A. Bani, Agricultural University of Tirana, Albania, pers. comm.;
Konstantinou and Babalonas 1996; Obratov-Petkovic et al. 2008; Pavlova
2001; Pavlova and Alexandrov 2003; Ritter-Studnicka and Dursun-Grom
1973; Vergano Gambi 1992). The concentrations of Fe in two of the plant
samples are slightly higher than the limit of 500 ppm proposed by Allen et al.
(1974). According to Ritter-Studnicka and Dursun-Grom (1973), the content
of Fe in plants should exceed 1000 ppm if they are considered to be as nonphysiological,
something shown by comparative measurements in serpentine
and non-serpentine soils.
The pH values for serpentine soils are often high and range from 6.1 to
8.8 (Brooks 1987, Kruckeberg 1984). The pH values in this study ranged
from 6.0 to 7.7 for the serpentine soils.
Discussion
The results of this study are similar to those provided by Štepankova
(1996, 1997), Westerbergh and Rune (1996), and Westerbergh and Saura
(1992) for other plant species. The variation in morphological traits in this
study are an additional confirmation of Berg’s (1960) hypothesis that the
size of the flowers in insect-pollinated plants should be selected to remain
constant regardless of the size of vegetative structures. Data from the PCA
clearly show that the correlations among floral traits and the correlations
among vegetative traits were significantly greater than the correlations across
these two groups of traits in T. chamaedrys populations. As Conner and
Sterling (1996) pointed out, such positive correlations within the floral
and vegetative trait groups do not indicate functional relationships among
traits. These correlations are due at least in part to overall size relationship
and probably reflect common developmental pathways.
Teucrium chamaedrys is widely distributed without preferences to any
type of rock and should be considered as a bodenvag species, which are those
widely distributed in serpentine and non-serpentine habitats (Kruckeberg
1992). The significant ecological differences between population groups
50 Northeastern Naturalist Vol. 16, Special Issue 5
were related to the differences in edaphic conditions of the serpentine sites
from the non-serpentine sites. In this study, T. chamaedrys populations were
dense and well developed in mesophilous habitats on calcareous and siliceous
terrains compared to serpentine populations.
The growth habit of T. chamaedrys differed between serpentine and
non-serpentine sites. The serpentine populations had lower stems, smaller
leaves, and shorter internodes compared to the non-serpentine populations.
Obratov–Petković et al. (2006) also noted that T. chamaedrys growing on
serpentines were less compact than those growing on limestone.
Denser indumentum and longer simple or glandular hairs covering the
stems, leaves, and bracts of the individuals growing on serpentines are also
important characters. Most serpentine populations of T. chamaedrys studied
in this work were densely covered by 3–5 celled glandular hairs. These hairs
were not mentioned by Bini-Maleci and Servettaz (1991), Grubesic et al.
(2007), or Navarro and El Qualidi (2000) for this species. Because hairs can
play an important role in various aspects of plant physiology and ecology in
Teucrium (Payne 1978), further investigations are needed.
The chemical composition of the soil collected from serpentine substrates
was similar to serpentine soils from other parts of the world (Brooks
1987), with concentrations of metals such as Ni and Cr uniformly high and
Ca/Mg quotients relatively low. The serpentine soils had abnormally high
contents of Ni, Cr, Cd, and Co. The ratio of Ca/Mg was <1 in the serpentine
soils and >1 in non-serpentine soils. The levels of Ca and Mg found in these
Bulgarian serpentine soils are typical for such soils from other areas (Brooks
1987; Kruckeberg 1984, 1992; Roberts and Proctor 1992). Similar to previous
findings (Brooks 1987, Karataglis et al. 1982, Proctor 1971, Roberts and
Proctor 1992, Walker 1954), while the amounts of Ca in the serpentine soils
were small, the amounts of Ca taken up by the plant were higher. According
to Proctor (1971), Ca is one of the elements contributing to the inhibition
of the heavy-metal toxicity, and it is possible that the plant takes up Ca to
compensate the toxic action of different toxic metals. Studying populations
of Buxus sempervirens L. (Common Box) in Greece, Karataglis et al. (1982)
suggested that the plant developed a mechanism to permit an excess soil Ca
to be taken by plant. Normally, the high Mg of ultramafic soils is reflected in
high Mg concentrations in plant tissues, but this result might also indicate an
unusual Mg and low Ca requirement observed in some experiments (Proctor
and Woodell 1975).
The total Ni content in the soil was comparable to Italian (Vergnan
Gambi et al. 1982), Greek (Babalonas et al. 1984), and Albanian (Shallari
et al. 1998) serpentine areas. The accumulation of Ni, Cr, and Co in the
above-ground plant parts for all serpentine populations was higher than in
non-serpentine ones. These data are in accordance with results presented
for T. montanum L. from Bulgaria (Pavlova and Alexandrov 2003), Serbia
(Obratov-Petković et al. 2008), and Albania (Shellari et al. 1998). The concentrations
of Ni found in plant samples from serpentines were high but not
2009 D. Pavlova 51
exceptional for T. chamaedrys, similar to findings of Shellari et al. (1998)
and Obratov-Petković et al. (2008) for different Teucrium species.
Ni amounts in T. chamaedrys were very low compared to the data for
other plants growing on serpentines found by Karataglis et al. (1982), Vergnano
Gambi et al. (1982), Konstantinou and Babalonas (1996), and Bani et
al. (2007), but higher than levels normally considered to be toxic to most
plants (Kabata-Pendias and Pendias 1984). Ni was taken up in higher quantities
than Cr, and the Ni/Cr ratio in plant tissues was always much higher than
in the soil. The low Cr concentrations in all studied plants corroborate the
data of Bani et al. (2007) and Brooks (1987) that serpentine plants contain
only trace quantities of Cr. At the same time, Cr concentrations were higher
than Co in all plant samples suggesting that plants adapted to serpentine soil
did not accumulate cobalt (Wallace et al. 1982). The ability of Buxus sempervirens
to accumulate large quantity of calcium from the soil (Karataglis
et al. 1982) may constitute one of the probable physiological mechanisms
developed in order to compensate for the toxic action of heavy metals like
Cr, Ni, Co, and Fe. Karataglis et al. (1982) consider toxic effects as almost
imperceptible in regards to the low levels of Co found in the soil and the
amounts taken up by the plants.
Brooks and Yang (1984) found the concentration of Mg in plant tissue to
be inversely proportional to the concentrations of other nutrients: Al, Fe, Co,
Mn, P, and Na. These data clearly suggest that the uptake of Mg comes at a
cost to the plant, as the uptake of other elemental nutrients is forfeited. According
to Brooks and Yang (1984), the heightened level of Mg in serpentine
soils and its antagonistic behavior toward other elements could be the most
important factor in the serpentine syndrome.
In contrast to other studies of serpentine plants (Bani et al., in press;
Konstantinou and Babalonas 1996; Pavlova 2001; Pavlova and Alexandrov
2003; Ritter-Studnicka and Dursun-Grom 1973; Vergano Gambi 1992), Fe
levels were not higher in plants. Babalonas et al. (1984) suggested that this
characteristic should be given more attention because it may be applicable
to all the serpentine flora of the Balkans.
The soil from Gega (G), considered to be a serpentine site (Zidarov
and Nenova 1995), had lower concentrations of Ni (101 mg/kg) and Cr
(36 mg/kg) than the other serpentine soils in this study. Although total soil
metal concentrations from G were intermediate between the serpentine and
non-serpentine study sites, the concentrations of the plant tissues from G
were similar to plant tissue concentrations at the other serpentine sites.
This result could be related to the specificity of the G site from a geological
point of view. The studied area is crossed by pegmatite-aplitic veins and as
a result, metasomatic rocks similar to gabbros appear that follow the stage
of syndeformation metamorphic recrystallisation and mark the beginning of
the ultrabasic rock assimilation (Kozhoukharova 1999).
Teucrium chamaedrys is a well-known herb with medicinal action and uses
as a stimulant, tonic, diaphoretic, and diuretic. Teucrium chamaedrys acts as a
52 Northeastern Naturalist Vol. 16, Special Issue 5
slight aperient, as well as a tonic. For pharmaceutical purposes, above-ground
plant parts (Herba Teucrii chamaedrys) are collected from natural and cultivated
populations (Nikolov 2006). According to ECCE (1994), the proposed
limits for average metal contents in plants are 0.4–4.0 mg/kg and 0.2–1.0
mg/kg for Ni and Cr, respectively. The data from the studied serpentine populations
were considerably higher than these limits. Although T. chamaedrys
is not a hyperaccumutator of heavy metals, its collection from serpentines for
medicinal purposes should be avoided as proposed also by Obratov-Petković
et al. (2008) and European Pharmacopoeia (2005).
The species T. chamaedrys is tolerant of serpentine soils, and the established
morphological variation of the vegetative parts of the plant can
be a response to the unusual conditions provided by the serpentine substrate.
Similar observations and ecotype differentiation for other species
were presented by Karataglis et al. (1982), Proctor (1971), Rajakaruna and
Bohm (1999), Štepankova (1996, 1997), etc., and in all cases, the plants
reacted in different ways to the serpentine substrates. As Kruckeberg
(1984) pointed out, the differences in morphology of serpentine races can
be taken as an indication of genotypic response to physical stress. The
serpentine population develops its own genetic pattern of adaptation to
the serpentine environment. According to Kruckeberg and Rabinowitz
(1985), various genes favorable for survival on the serpentine sites are accumulated
through selection over time, while other genes of the originally
non-serpentine population are eliminated by the selective action of the
serpentine habitats. Morphological differences, the preliminary results on
the karyology of T. chamaedrys in Bulgaria, a new chromosome number
reported for the population of the species from serpentines in Dobromirtzi
(D1) (Pavlova 2008), and the geographical isolation between studied populations
give us reason to continue experimental work to obtain additional
data to prove the existence of two ecotypes.
Acknowledgments
The author is thankful to Evgenia Stoimenova from the Institute of Mathematics,
Bulgarian Academy of Sciences in Sofia for her help in the discriminant analysis.
Bob Boyd from Auburn University, Auburn, AL, USA helped with useful comments
and suggestions on an earlier version of the manuscript. The anonymous reviewers
and the manuscript editor Marla McIntosh provided critical remarks to improve the
paper. The research was realized within Project VU-06/05 supported by the National
Research Council at the Ministry of Education and Science in Sofia, Bulgaria.
Literature Cited
Allen, S.E., H. Max Grimshow, J.A. Parkinson, and C. Quarmby. 1974. Chemical
Analysis of Ecological Materials, Blackwell Scientific Publications, Oxford,
UK. 555 pp.
Babalonas, D., S. Karataglis, and V. Kabassakalis. 1984. The ecology of plant populations
growing on serpentine soils. III. Some plant species from North Greece in
relation to the serpentine problem. Phyton (Austria) 24:225–238.
2009 D. Pavlova 53
Bani, A., G. Echevarria, S. Sulce, J. Morel and A. Mullai. 2007. In-situ phytoextraction
of Ni by a native population of Alyssum murale on an ultramafic site (Albania).
Plant Soil 293:79–89.
Bani, A., G. Echevarria, A. Mullaj, R. Reeves, J. Morel, and S. Sulce. In press. Ni hyperaccumulation
by Brassicaceae in serpentine soils of Albania and NW Greece.
Northeastern Naturalist.
Berg, R.L. 1960. The ecological significance of correlation pleiades. Evolution
14:171–180.
Bratteler, M., M. Baltisberger, and A. Widmer. 2006. QTL analysis of intraspecific differences
between two Silene vulgaris ecotypes, Annals of Botany 98(2):411–419.
Bini-Maleci, L., and O. Servettaz. 1991. Morphology and distribution of trichomes
in Italian species of Teucrium sect. Chamaedrys (Labiatae): A taxonomical evaluation.
Plant Systematics and Evolution 174:83–91.
Brooks, R.R. 1987. Serpentine and its Vegetation. A Multidisciplinary Approach.
Volume 1. Dioscorides Press, Portland, OR, USA. 407 pp.
Brooks, R.R., and X.H.Yang. 1984. Elemental levels and relationships in the endemic
serpentine flora of the Great Dyke, Zimbabwe and their significance as
controlling factors for this flora. Taxon 33:392–399.
Conner, J.K., and A. Sterling. 1996. Selection for independence of floral and vegetative
traits: Evidence from correlation patterns in five species. Canadian Journal
of Botany 74:642–644.
Element Concentration Cadasters in Ecosystems (ECCE). 1994. Progress Report.
Presented at the 25th General Assembly of International Union of Biological
Sciences (IUBS), Paris, France.
European Pharmacopoeia. 2005. Volume 2. Set with Supplements 5.1 and 5.2.
EDQM, Strasbourg, France.
Greuter, W., H.M. Burget, and G. Long. 1986. Med-Checklist. Volume 3., Conservatoire
et Jardin Botaniques ville de Genève, Genève, Switzerland. 395 pp.
Grubesic, R.J., S. Vladimir-Knezevic, D. Kremer, Z. Kalodera, and J. Vukovic. 2007.
Trichome micromorphology in Teucrium (Lamiaceae) species growing in Croatia.
Biologia (Bratislava) 62(2):148–156.
Gussev, C.H. 2005. Characteristic of wild medicinal plants resources in Bulgaria and
their sustainable management. Pp. 495–508, In A. Petrova, D. Dimitrova, and V.
Vladimirov (Eds.). Current State of Bulgarian Biodiversity: Problems and Perspectives.
Bulgarian Biodiversity Platform Ministry of Environment and Water,
Sofia, Bulgaria. 565 pp.
Kabata-Pendias, A., and H. Pendias. 1984. Trace elements in Soils and Plants. CRC
Press, Boca Raton, fl, USA. 315pp.
Karataglis, S., D. Babalonas, and B. Kabasakalis. 1982. The Ecology of plant populations
growing on serpentine soils. II. Ca/Mg Ratio and the Cr, Fe, Ni, Co concentrations
as development factors of Buxus sempervirens L. Phyton (Austria)
22:317–327.
Konstantinou, M., and D. Babalonas. 1996. Metal uptake by Caryophyllaceae species
from metalliferous soils in northern Greece. Plant Systematic and Evolution
203:1–10.
Kozhoukharova, E. 1999. Metasomatic gabboids: Markers in the tectono-metamorphic
evolution of the Eastern Rhodopes. Geologica Balcanica 29:89–109.
Kruckeberg, A.R. 1984. California Serpentines: Flora, Vegetation, Geology, Soils,
and Management Problems. University of California Press, Berkeley, CA,
USA. 180 pp.
54 Northeastern Naturalist Vol. 16, Special Issue 5
Kruckeberg, A.R. 1992. Plant life of western North American ultramafics. Pp. 31–73,
In B. Roberts and J. Proctor (Eds.). The Ecology of Areas with Serpentinized
Rocks: A World View. Kluwer Academic Publishers, Dordrecht, The Netherlands.
421 pp.
Kruckeberg, A.R., and D. Rabinowitz. 1985. Biological aspect of endemism in
higher plants. Annual Review of Ecology and Systematics 16:447–479.
Lombini, A., E. Danelli, C. Ferrari, and A. Simoni. 1999. Plant-soil relationships
in the serpentine screes of Mt. Prinzera (Northern Aennines, Italy). Journal of
Geochemical Exploration 64:19–33.
Markova, M. 1992. Teucrium L. Pp. 491–492, In S. Koziharov (Ed.) Opredelitel
na Vishite Rastenia v Balgaria. Nauka i Izkustvo, Sofia, Bulgaria. 788 pp. (in
Bulgarian).
Mayer, M.S., and P.S. Soltis. 1994. The evolution of endemics: A chloroplasts DNA
phylogeny of the Streptanthus glandulosus complex (Cruciferae). Systematic
Botany 19:537–574.
Navarro, T., and J. El Oualidi. 2000. Trichome morphology in Teucrium L. (Labiatae).
A Taxonomic review. Anales Jardin Botanico de Madrid 57(2):277–297.
Nikolov, S. (Ed.). 2006. Encyclopedia of Medicinal plants in Bulgaria. Publishing
House Trud, Sofia, Bulgaria. 566 pp. (in Bulgarian).
Obratov-Petković, D., I. Popović, S. Belanović, R. Kadović. 2006. Ecobiological
study of medicinal plants in some regions of Serbia. Plant Soil and Environment
52(10):459–467.
Obratov-Petković, D., I. Bjedov, and S. Belanović. 2008. The relationship between
heavy metal contents and bedrock in some species of genus Teucrium L., in
Serbia. Pp. 1–5, In G. Ruzichkova (Ed.). Proceedings of the 5th Conference on
Medicinal and Aromatic Plants of Southeast European Countries, Brno, Czech
Republic. (on CD-Rom). Mendel University of Agriculture and Forestry, Brno,
Czech Republic .
Pavlova, D. 2001. Concentration of heavy metals in plants growing on serpentine
soils in the Rhodopes Mts. (Bulgaria). Pp. 425–428, In N. Ozhatay (Ed.). Plants
of the Balkan Peninsula: Into the next Millennium. Proceedings of the Second
Balkan Botanical Congress. Volume 1. Publisher Department, Marmara University,
Istanbul, Turkey. 593 pp.
Pavlova, D. 2008. Reports (1664–1669). In G. Kamari, G., Blanchè, C. Siljak-
Yakovlev, and S. Siljak-Yakovlev (Eds.). Mediterranean chromosome number
reports-18. Flora Mediterranea 18:563–610.
Pavlova, D., and S. Alexandrov. 2003. Metal uptake in some plants growing on
serpentine areas in the Eastern Rhodopes mountains (Bulgaria). OT Sistematik
Botanik Dergisi 10(2):13–30.
Payne, W.W. 1978. A glossary of plant-hair terminology. Brittonia 30:239–255.
Peev, D. 1989. Teucrium L. Pp. 241–249, In V. Velchev and B. Kuzmanov (Eds.)
Flora Reipublicae Popularis Bulgaricae Volume 9. Publishing House Bulgarian
Academy of Sciences, Sofia, Bulgaria. 539 pp.
Proctor, J. 1971. The plant ecology of serpentine. II. Plant response to serpentine
soils. Journal of Ecology 59:397–410.
Proctor, J., and S.R.J. Woodell. 1975. The ecology of serpentine soils. Advances in
Ecology Research 9:256–366.
Rajakaruna, N., and B.A. Bohm. 1999. The edaphic factor and patterns of
variation in Lasthenia californica (Asteraceae). American Journal of Botany
86(11):1576–1596.
2009 D. Pavlova 55
Reichinger, H.K. 1941. Monographische Stiudie über Teucrium Sect. Chamaedrys.
Botanisches Archiv 42:335–420.
Ritter-Studnicka, H., and K. Dursun-Grom. 1973. Über den Eisen, Nickel und
Chromgehalt in einigen Serpentinpflanzen Bosniens. Osterach Botanische Zeitung
121:29–49.
Roberts B.A., and J. Proctor. 1992. The Ecology of Areas with Serpentinized Rocks: A
World View. Kluwer Academic Publishers, Dordrecht, The Netherlands. 421 pp.
Shallari, S., C. Schwartz, A. Hasko, and J.L. Morel. 1998. Heavy metal in soils and
plants of serpentine and industrial sites of Albania. Science of Total Environment
209:133–142.
Štepankova, J. 1996. Karyological variation in the group of Myosotis alpestris (Boraginaceae).
Folia Geobotany and Phytotaxonomy, Praha 31:251–262.
Štepankova, J. 1997. The effect of serpentine on morphological variation in the Galium
pumilum group (Rubiaceae). Thaiszia - Journal of Botany, Košice 7:29–40.
Tutin, T.G., V.H. Heywood, N.A Burges, D.M. Moore, D.H. Vaentine, and
S.M.Walters. 1972. Flora Europaea, Volume 3. Cambridge University Press,
London, UK.
Vergano Gambi, O. 1992. The distribution and ecology of the vegetation of ultramafic soils in Italy. Pp. 217–247, In B.A. Roberts, and J. Proctor (Eds.). The Ecology
of Areas with Serpentinized Rocks. A World View. Kluwer Academic Publishers,
Dordrecht, The Netherlands. 421 pp.
Vergano Gambi, O., R. Gabbrielli, and L. Pancaro. 1982. Nickel, chromium, and
cobalt in plants from Italian serpentine areas. Acta Oecologica 3(17):291–306.
Walker, R.B. 1954. The ecology of serpentine soils. II. Factors affecting plant growth
on serpentine soils. Ecology 35:259–266.
Wallace, A., M. Jones, and G.V. Alexander. 1982. Mineral composition of native
wood plants growing on a serpentine soil in California. Soil Science 134:42–44.
Westerbergh, A., and O. Rune. 1996. Genetic relationship among Silene dioica
(Caryophyllaceae) populations on and off serpentine: A review. Symbolae Botanicae
Upsalienses 46:277–284.
Westerbergh, A., and A. Saura. 1992. The effect of serpentine on the population
structure of Silene dioica (Caryophyllaceae). Evolution 46:1537–1548.
Wright, J., M. Stanton, and R. Scherson. 2006. Local adaptation to serpentine and
non-serpentine soils in Collinsia sparsiflora. Evolutionary Ecology Research
8:1–21.
Zidarov, N.G., and P. Nenova. 1995. Basic and ultrabasic rocks and related eclogites
from Serbo-Macedonian massif (SW Bulgaria). Proceeding of the XV Congress
of the CBGA, Athens, September 1995, Geological Society of Greece, Special
Publication No. 4:619–626.