Flora (2003) 198, 377–388
http://www.urbanfischer.de/journals/flora
Evidence of the possibility of natural reciprocal crosses
between Pinus sylvestris and P. uliginosa based on the phenology
of reproductive organs
Adam Boratyński1*, Krystyna Boratyńska1, Andrzej Lewandowski1,
Zbigniew GoŁĄb2 & Piotr Kiciński3
1
2
3
Polish Academy of Sciences, Institute of Dendrology, Parkowa 5, 62-035 Kórnik, Poland
Stołowe Mts National Park, Słoneczna 31, 51-350 Kudowa, Poland
Forestry Faculty of Agricultural University, Department of Forest Botany, Wojska Polskiego 71d, 60-615 Poznań, Poland
Submitted: Feb 13, 2003 · Accepted, in revised form: Apr 30, 2003
Summary
Phenological observations of development of generative organs of Pinus sylvestris and P. uliginosa (= P. rotundata) were carried
out in spring of 1999, 2000 and 2001. The aim of the research was to verify the hypothesis that both taxa have a possibility of
reciprocal crossing. Two populations of P. uliginosa were tested, one on the Silesian Lowland (We
˛ gliniec) (altitude of 180m),
the other in the Stołowe mountains (Batorów) (at altitude of 750 m). The lowland population of P. uliginosa is not numerous
and surrounded by extensive P. sylvestris forests, the mountain one is 3 times more numerous, and the nearest population of
P. sylvestris is at a distance of 2km. Observations in the field were carried out twice a week during the period of development
of micro- and macro-strobili of both taxa. The results show that the P. sylvestris strobili developed every year earlier than those
of P. uliginosa. Nevertheless, this did not eliminate the possibility of cross pollination and gene flow from P. sylvestris toward
P. uliginosa on both localities of the last species. The possibility of pollination of P. sylvestris macrostrobili by P. uliginosa pollen was found also possible, but more restricted. Normally, on lowlands the same phenological phases take place about 10 days
earlier than in the mountains. This is documented for two years of observations of more or less typical whether conditions. An
earlier development of micro- and macrostrobili of both species in their mountain populations was observed in an observation
year characterized by an extremely early and warm spring.
Key words: “Pinus mugo complex”, microstrobili development, macrostrobili development
Introduction
Relationships among pine species of the subsection Sylvestres, including Pinus sylvestris L., P. mugo Turra,
P. uncinata Ramond and P. uliginosa Neumann (=
P. rotundata Link), have been the subjects of taxonomic
studies for the last several decades. Biometric, chemotaxonomic, biochemical genetic investigations, and
lately molecular methods have been used to determine
the relationships among the four taxa (e.g., Staszkiewicz & Tyszkiewicz 1969, 1972; Szweykowski &
Bobowicz 1983 ; Prus-GŁowacki & Szweykowski
1983 ; Bobowicz 1990 ; Neet-Sarqueda 1994 ; PrusGŁowacki & Stephan 1998 ; Prus-GŁowacki et al.
1998 ; Lewandowski et al. 2000 ; Wachowiak et al.
2000). The taxonomic position of P. uliginosa has been
discussed in the studies cited above. This taxon, originally described from the peat-bogs of the Stołowe and
Bystrzyckie Mountains in the Central Sudethians (Neumann 1837 ; Wimmer 1837), is morphologically intermediate between P. mugo Turra and P. sylvestris L.
(Staszkiewicz 1985, 1993), but also between P. mugo
* Corresponding author: Adam Boratyński, Polish Academy of Sciences, Institute of Dendrology, Parkowa 5,
62-035 Kórnik, Poland, e-mail : borata@man.poznan.pl
0367-2530/03/198/05-377 $ 15.00/0
FLORA (2003) 198
377
and P. uncinata (Christensen 1987). Consequently,
P. uliginosa is considered to be of hybrid origin, developed as a result of hybridization between those pairs of
species (Lewandowski et al. 2000). Participation of all
three species in the hybridization process cannot be
excluded (Lauranson-Broyer et al. 1997). Because of
its intermediate features, P. uliginosa is sometimes identified as the hybrid between P. mugo and P. sylvestris,
named P. ×rhaetica Brügger (Staszkiewicz 1985,
1993 ; Mirek et al. 1995 ; ZajĄc & ZajĄc 2001).
Hybrids between P. mugo and P. sylvestris occur
naturally in places where the species grow together
(Staszkiewicz & Tyszkiewicz 1969, 1972; BoratyŃski 1978 ; Szweykowski & Bobowicz 1983 ; Staszkiewicz 1985, 1993; Bobowicz 1990 ; Siedlewska
1994 ; Christensen & Dar 1997). Evidence for gene
flow between these species has been established on the
basis of biometric and genetic studies. Investigations
using isoenzymatic markers and DNA have shown that
gene flow between P. sylvestris and P. mugo is possible,
but restricted (Filppula et al. 1992; Lewandowski
et al. 2002).
The affinity of P. uliginosa to both P. sylvestris and
P. mugo has been recently confirmed on the basis of
isoenzyme systems (Lewandowski et al. 2000). This
also suggests the possibility of gene flow between P. sylvestris and P. mugo and, consequently, between P. sylvestris and P. uliginosa. However, to date it remains
unknown if the in situ phenology of strobili, pollen
release, and pollen reception enable their reciprocal
cross-pollination.
The main goal of the present study was to evaluate the
possibility of P. sylvestris and P. uliginosa cross-pollination on the basis of phenological observations of the
development of reproductive organs in locations where
they are growing together or close to each other. Another
aim was to compare the phenology and development of
reproductive organs of both taxa in spring both on a lowland and mountain sites.
Material and methods
Two populations of P. uliginosa were chosen for the study
(Table 1). The first is located at We
˛ gliniec, in the western part
of the Silesian Lowland, and consists of less than 100 individuals (Ambroży 1999), whereas the second is located at
Batorów, in the Stołowe Mountains (central Sudethians), and
includes about 300 individuals (GoŁĄb 1998). The population
of P. uliginosa at We
˛ gliniec is its northernmost location, isolated from other populations of the taxon and surrounded by
extensive forest stands of P. sylvestris. The population of
P. uliginosa at Batorów is isolated from other populations of
the taxon, and also from the nearest population of P. sylvestris.
P. sylvestris does not form extensive forest stands there and the
nearest population is about 2 km away from the P. uliginosa
stand.
Temperature and relative air humidity was measured on
both stands of Pinus uliginosa and on Szczeliniec Mt in spring
of the year 2000, using data loggers HOBO PRO RH/Temp.
H08-03208 (MicroDAQ, New Hampshire).
The phenological observations were carried out in 1999,
2000 and 2001, starting in early spring and ending with the end
of pollen release and reception on the last tested specimen.
Every year, 10 or more individuals of each of P. uliginosa and
P. sylvestris were observed at both locations (Table 1). The
trees ranged between 5–18m in height, but only the lowestgrowing micro- and megastrobili were sampled. About 10 conglomerations of microstrobili were observed to describe the
phenology of every individual male plant. Not in all cases sufficient megastrobili were formed to observe ten on every individual in a particular year, especially on P. uliginosa. In those
cases the smaller number of megastrobili was used to characterize the female phenology.
Observations of the development of P. sylvestris megastrobili and pollen release carried out mostly in seed-orchards by
many authors (Sarvas 1962, 1967, 1972; Jonsson et al. 1976;
Boydak 1977; ChaŁupka & Fober 1977; WesoŁy 1982;
Koski 1991; ChaŁupka 1993; Burczyk & ChaŁupka 1997;
Krizo 2001) were very helpful to form the basis of our investigations. The dates of the first observations were adjusted to
the development of P. sylvestris, which started earlier than
P. uliginosa. The frequency of observations depended on
weather conditions, chiefly temperature and precipitation
Table 1. Sampled populations of Pinus sylvestris and P. uliginosa
No.
Taxon
Location
Longitude
E
Latitude
N
Altitude
[m]
Number of
individuals analysed
1
Pinus sylvestris
15°14⬘
51°17⬘
180
12
2
Pinus uliginosa
15°14⬘
51°17⬘
180
14
3
Pinus sylvestris
16°19⬘
50°29⬘
900
10
4
Pinus uliginosa
Silesian Lowland, area
adjacent to nature reserve
at We
˛ gliniec
Silesian Lowland, nature
reserve at We
˛ gliniec
Stołowe Mts, Mt Szczeliniec
Wielki, on sandstone rocks
Stołowe Mts, Great Peat-bog
at Batorów
16°19⬘
50°29⬘
750
10
378
FLORA (2003) 198
(ChaŁupka 1993), but observations were usually made twice
a week with the use of binoculars. Four developmental stages
of megastrobili and six of microstrobili were distinguished
(Lännerholm 1976) during the field observations (Table 2).
The field research was preceded by examination of the development of megastrobili on specimens of P. sylvestris, P. uliginosa and P. mugo in the collections of the Kórnik Arboretum.
The duration of pollen release by microstrobili and pollen
reception by megastrobili were calculated separately for P. sylvestris and P. uliginosa in all four observed populations.
Results
Characteristics of phenology of micro- and
megastrobili of P. sylvestris and P. uliginosa
Springtime climate of 2000 was different on both
observed localities and characterized by a specific
course of temperature and relative air humidity (Figs 1
and 2). Both measured climatic factors were much more
stable in the mountains than in the lowland. Day and
night temperatures and relative air humidity in the
Stołowe Mts showed a much narrower range than on the
lowland site. There were also more dry days in the
mountains than in lowland (Fig. 2).
Timing of successive phenophases of micro- and
megastrobili of P. sylvestris and P. uliginosa at We˛gliniec and Batorów (Table 3) was different every year,
depending on weather conditions. The differences in
dates of phenophases between 1999 and 2001 (with a
late and cold spring) and 2000 (with an extremely early,
dry and warm spring) were as great as 30 days in the
case of P. sylvestris and even 35 days in P. uliginosa in
the Stołowe Mts. The differences between years, however, were reduced at We˛gliniec and were 15 –18 days
for P. sylvestris and 10 days for P. uliginosa (Table 3).
Fig. 1. Course of air temperature in April and first days of
May of 2000 at the Silesian Lowland (We
˛ gliniec) and Stołowe
Mts (Batorów) sites
In both species the megastrobili developed earlier
than the microstrobili (Figs 3 and 4). The first scales of
megastrobili were clearly visible and receptive a few
days before pollen release occured on the same individuals. The differences between starting dates of pollen
release and reception were greater in the Stołowe Mts
than on the Silesian Lowland (Tables 4 and 5). P. sylvestris and P. uliginosa exhibited similar differences between dates of development of micro- and megastrobili.
The differences depended on weather conditions in particular years. The differences were the smallest in 2000
and on average amounted to only about 0.5 days for
P. uliginosa and 1.4 days for P. sylvestris on the Silesian
Lowland, and 10 and 7 days, respectively, in the
Stołowe Mts.
In the years 1999 and 2001, characterized by cooler
and more humid springs, megastrobili developed and
were receptive up to 2 weeks before pollen release
occurred by the same individuals. In both localities pollen release by P. sylvestris and P. uliginosa started later
than pollen reception and ended at the same time or a
few days later or earlier, depending on year (Table 3).
Table 2. Developmental stages of micro- and megastrobili of Pinus sylvestris and P. uliginosa (after Johnsson et al. 1976)
Phase
Microstrobili
Megastrobili
0
1
Bud covered with scales, microstrobili invisible
Visible microstrobili
2
Microstrobili developed, without pollen release
3
Start of pollen release – at least one microstrobilus
dehiscent and releasing pollen grains when vibrating
the twig
Intensive pollen release; most microstrobili release
pollen when vibrating the twig
End of pollen release; most of microstrobili
completely opened, without pollen, only a
singular release pollen when vibrating the twig
Microstrobili without pollen
Bud covered with scales, megastrobilus invisible
Start of pollen reception; upper scales of megastrobilus
are visible as receptive
Intensive pollen reception; complete megastrobilus is visible
with most scales receptive
End of pollen reception – scales thickened, closed access
to the pollen chambers, but megastrobili not deflected
4
5
6
Megastrobili deflected
FLORA (2003) 198
379
generally shorter and varied between 5 and 18 days
(12.0 on average). Somewhat lower values were recorded at We˛gliniec (Table 6).
The periods of pollen reception of particular individuals of P. uliginosa in the Stołowe Mts ranged from
5 to 28 days (17.4 on average), and pollen release from
6 to 18 (12.6 on average), whereas at We˛gliniec pollen
reception lasted 7– 29 days (14.9 on average), and pollen release 5 –17 days (10.0 on average) (Table 6).
Fig. 2. Course of relative air humidity in April and first days
of May of 2000 at the Silesian Lowland (We
˛ gliniec) and
Stołowe Mts (Batorów) sites
The duration of pollen reception by particular individuals of P. sylvestris in the Stołowe Mts ranged from 7
to 28 days (15.0 on average) and was different in length
in particular years. The duration of pollen release was
Differences in development of strobili
between P. sylvestris and P. uliginosa
Pinus sylvestris released pollen and showed pollen
reception before P. uliginosa in the Stołowe Mts and at
We˛gliniec, but these differences show a considerable
year-to-year variability. At We˛gliniec the dates of successive phenological phases of P. sylvestris were earlier
than those of P. uliginosa (Table 7), but their duration
was usually similar in both species (Table 6). The
Table 3. Average dates of pheno-phases of development of micro- and macrostrobili of Pinus sylvestris and Pinus uliginosa in
We
˛ gliniec and Batorów
Location
We
˛ gliniec
Species
Pinus sylvestris
Year
1999
2000
2001
Pinus uliginosa
1999
2000
2001
Batorów
Pinus sylestris
1999
2000
2001
Pinus uliginosa
1999
2000
2001
380
FLORA (2003) 198
Micro- and macrostrobili
phases
Date of phenophases
[mm.dd]
start
intensive
end
Pollen release
Pollen reception
Pollen release
Pollen reception
Pollen release
Pollen reception
05.14
05.02
05.02
05.01
05.14
05.04
05.21–05.30
05.14–05.28
05.06–05.24
05.05–05.16
05.18 –05.28
05.06–05.26
06.04
06.02
05.28
05.19
05.30
06.06
Pollen release
Pollen reception
Pollen release
Pollen reception
Pollen release
Pollen reception
05.11
05.02
05.11
05.10
05.16
05.06
05.21–06.04
05.21–06.04
05.15–05.24
05.15–05.25
05.26–06.02
05.23–06.06
06.11
06.12
05.28
05.29
06.10
06.11
Pollen release
Pollen reception
Pollen release
Pollen reception
Pollen release
Pollen reception
05.24
05.13
04.26
04.20
05.28
05.14
05.28–06.05
05.27–06.03
04.30–05.08
04.26–04.30
06.01–06.09
05.21–06.01
06.13
06.15
05.11
05.07
06.14
06.14
Pollen release
Pollen reception
Pollen release
Pollen reception
Pollen release
Pollen reception
05.28
05.26
04.30
04.24
05.28
05.17
06.04–06.11
06.01–06.12
05.05–05.11
04.26–05.04
06.05–06.18
05.24–06.15
06.18
06.20
05.18
05.08
06.24
06.20
Fig. 3. Differences in development of
reproductive organs of Pinus sylvestris
at a Silesian Lowland (We
˛ gliniec) and
Stołowe Mts (Szczeliniec) site
release of pollen by P. sylvestris took place every year at
the time of intensive reception of pollen by megastrobili
of P. uliginosa (Fig. 5). Pollen release in P. uliginosa
occurred at the end of pollen reception of megastrobili
of P. sylvestris (Fig. 6).
In the Stołowe Mts the first phases of the development of micro- and megastrobili of P. sylvestris took
place on average 6 days earlier than those of P. uliginosa (Table 7). Intensive pollen release by P. sylvestris
from Mt. Szczeliniec near Batorów lasted 9 days. The
megastrobili of this species were receptive for about 30
days. P. uliginosa released pollen intensively for 8 days
and its megastrobili were receptive for about 25 days
(Table 3). The differences between the starting dates of
phenological phases of pollen release and development
of megastrobili of P. sylvestris and P. uliginosa were
much smaller in 2000, which was characterized by an
extremely early, warm and dry spring.
Intensive release of pollen by P. sylvestris from
Szczeliniec Wielki Mt took place when P. uliginosa
megastrobili were receptive (Fig. 7), whereas pollen
release by P. uliginosa occurred at the end of pollen
reception by megastrobili of P. sylvestris (Fig. 8) in all
three years of observation, just as occurred at We˛gliniec.
Discussion
Phenological phases typically occur earlier on the lowlands than in the mountains. According to this rule, the
spring development of vegetation on the Silesian Lowland, the region of Węgliniec, should take place about
10 days earlier than in the Stołowe Mts (Molga 1974).
The phenological observations on pollen release and
FLORA (2003) 198
381
Fig. 4. Differences in development of
reproductive organs of Pinus uliginosa
at a Silesian Lowland (We
˛ gliniec) and
Stołowe Mts (Batorów) site
reception of P. sylvestris and P. uliginosa confirmed this
pattern only in 1999 and 2001. By contrast, in 2000,
when spring was early and warm, earlier pollen release
and reception was observed in both, P. sylvestris and
P. uliginosa in the Stołowe Mts. This can probably be
explained by the influence of deep inversions of temperatures on the Silesian Lowland at the northern foothills
of Sudethians (Schmuck 1969). The specific response
of the populations of P. sylvestris and P. uliginosa from
the Stołowe Mts to the atypical springtime temperature
regime in this year possibly results from this inversion.
The smaller differences between cold and warm years
in dates of phenophases at We˛gliniec than at Batorów
are difficult to explain without the analysis of previous
weather conditions in the years of observations (Sarvas
1967 ; Boydak 1977; ChaŁupka 1993). We have not
sufficient climatic data, but a comparison of the air tem382
FLORA (2003) 198
peratures and relative humidity of April and May of
2000 from We˛gliniec and Batorów (Figs. 1 and 2) shows
that the delay of development of micro- and megastrobili of both species observed at We˛gliniec in 2000 can
be interpreted as a result of the influence of greater oscillations between day and night temperatures and higher
average relative air humidity of this site.
Observations of the phenological phases of P. sylvestris pollen release and pollen reception in seed-orchards
showed that differences in the dates of them typically
amount to one to three days on average (Jonsson et al.
1976 ; Boydak 1977; Koski 1991; ChapŁuka 1993 ;
Dengler, after ChaŁupka 1993). In our data these differences were greater, especially in the years with cold
and humid springs, but comparable and even shorter in
the year with an extremely dry and warm spring (Table 4
and 5).
Table 4. Delay of starting dates of pollen release as compared with pollen reception in Pinus sylvestris
Tree no.
Delay of pollen release [days]
Silesian Lowland
1
2
3
4
5
6
7
8
9
10
11
12
Stołowe Mts
1999
2000
2001
Average
1999
2000
2001
Average
–3
7
4
15
3
4
10
10
15
3
10
14
0
3
0
0
3
0
3
3
0
0
5
0
5
5
5
5
5
5
11
6
9
11
11
9
1
5
3
6.7
3.7
3
8
6.3
8
4.7
8.7
7.7
9
7
9
12
7
7
10
8
8
8
10
3
3
6
0
10
6
11
10
11
15
13
22
13
15
15
13
17
14
15
11.3
7.7
11.3
10.3
7.3
10.7
9.7
12
10.7
11.3
15.2
10.2
Average
7.7
1.4
7.3
5.4
8.5
7.0
Standard
deviation
5.58
1.76
2.67
2.50
1.50
3.77
2.56
1.450
Table 5. Delay of starting dates of pollen release as compared with pollen reception in Pinus uliginosa
Tree no.
Delay of pollen release [days]
Silesian Lowland
1
2
3
4
5
6
7
8
9
10
11
12
13
14
Stołowe Mts
1999
2000
2001
Average
1999
2000
2001
Average
7
0
0
7
4
4
7
7
7
–
–7
14
0
15
4
–
0
0
0
0
0
0
0
–
0
0
2
0
–
–
3
–
11
9
0
7
0
–
–2
9
9
12
–5.5
–0
–1.0
–3.5
–5.0
–4.3
–2.3
–4.7
–2.3
–
–3.0
–7.7
–3.7
–9.0
–
0
6
–
6
6
–
6
0
3
–
7
11
–
7
14
7
–
11
13
–
15
15
–
13
10
13
13
10
13
–
7.33
10.67
–
8.67
10.0
10.0
9.50
7.0
9.67
10.0
12.8
9.1
Average
5.0
0.5
9.9
–3.4
3.9
Standard
deviation
5.70
1.19
4.83
–3.00
2.64
Intensive pollen release by both species lasted about
6 –12 days, which is comparable with literature data
(Chalupa 1964 ; Jonsson et al. 1976; WesoŁy 1982 ;
Burczyk & ChaŁupka 1997). The megastrobili were
receptive for a longer time (Table 3).
2.78
1.79
1.24
Pollen perception by Pinus uliginosa took place at the
moment of full pollen release by P. sylvestris every year.
Thus, the probability of pollination of P. uliginosa
megastrobili with P. sylvestris pollen seems to be high.
It is also strongly greater at We˛gliniec, in particular if we
FLORA (2003) 198
383
Fig. 5. Development of megastrobili of
Pinus uliginosa (- - - - ) and microstrobili of P. sylvestris (
) at the Silesian
Lowland site
take into consideration the rather small number of individuals of P. uliginosa there and large number of individuals of P. sylvestris in the immediate vicinity. The possibility of pollination of individuals of P. sylvestris by P.
uliginosa pollen appears much lower.
The difference between possibilities of pollination
P. uliginosa by P. sylvestris pollen can be even greater if
we accept the rule “first come – first served” (Sarvas
1972). According to that rule, the first pollen grain that
enters the pollen chamber takes part in fertilization.
There is also some possibility of pollination of P. uliginosa megastrobili in the Stołowe Mts. by pollen of
P. sylvestris transported from lowlands. The time differences between pollen release by P. sylvestris on the
Table 6. Average duration of pollen release and pollen reception in Pinus uliginosa and P. sylvestris
Year
Site
Average duration [days]
Pinus uliginosa
1999
2000
2001
384
Silesian Lowland
Stołowe Mts
Silesian Lowland
Stołowe Mts
Silesian Lowland
Stołowe Mts
FLORA (2003) 198
Pinus sylvestris
Reception
Pollen release
Reception
Pollen release
15.2
14.3
8.8
11.3
20.6
24.8
9.1
10.4
8.3
10.9
11.3
12.9
16.2
20.1
10.7
9.9
14.3
15.0
8.3
14.0
8.0
9.4
10.8
12.3
Fig. 6. Development of megastrobili of
Pinus sylvestris (- - - - ) and microstrobili of P. uliginosa (
) at the Silesian
Lowland site
lowland and pollen reception by P. uliginosa in the
mountains would permit this process. Additionally,
P. sylvestris produces great amounts of pollen grains per
hectare of the adult forests (Sarvas 1962 ; ChaŁupka
& Fober 1977; Koski 1991; ChaŁupka 1993). The
species predominates in the forests on the lowland of
Central Europe and the pollen grains are normally trans-
ported for a hundreds and sometimes thousands of kilometers by convecting air flows (Tikhomirov 1950). By
contrast, the pollination of P. sylvestris by pollen of
P. uliginosa, and also of P. mugo, seems to be rather
unlikely, because pollen release in the mountains is considerably delayed in relation to the period of pollen
reception in the lowland locations.
Table 7. Delay of pollen release by microstrobili and pollen reception by megastrobili in Pinus uliginosa as compared to Pinus sylvestris
Year
Site
Average delay [days]
Pollen release
1999
2000
2001
Silesian Lowland
Stołowe Mts
Silesian Lowland
Stołowe Mts
Silesian Lowland
Stołowe Mts
Pollen reception
start
intensive
end
start
intensive
end
6
5
8
3
5
2
6
8
8
5
4
5
5
6
8
6
9
10
2
13
9
4
1
3
8
9
8
5
13
7
7
5
7
4
7
9
FLORA (2003) 198
385
Fig. 7. Development of megastrobili of
Pinus uliginosa (- - - - ) and microstrobili of P. sylvestris (
) at the
Stołowe Mts site
Conclusions
Our three-year record of phenological observations
shows that periods of development of megastrobili of
P. uliginosa and microstrobili of P. sylvestris overlap,
enabling cross-pollination (Figs. 5 and 7) at both, a
mountain and a lowland site. Development of P. uliginosa microstrobili is delayed as compared to P. sylvestris megastrobili, but does not strictly rule out crosspollination, but such an event will have a much lower
probability (Figs. 6 and 8).
The differences in the dates of development of microand megastrobili of both species varied significantly
during three years of observation, but in each year crosspollination was principally possible. The possibility of
pollination of P. uliginosa by P. sylvestris may be strongly increased if this follows the rule “first come – first
served”.
A substantially greater possibility of pollination of
P. uliginosa megastrobili by P. sylvestris pollen creates
the potential danger of genetic erosion in the first spe386
FLORA (2003) 198
cies, especially in the small population of the species
which is surrounded by P. sylvestris at We˛gliniec.
In 2000, characterized by an early, warm and dry
spring, the populations of P. sylvestris and P. uliginosa in
the mountain site of the Stołowe Mts developed reproductive organs earlier than those at We˛gliniec (Silesian
Lowland). This was probably due to the effects of a temperature inversion, but a specific response of the mountain populations to the anomalous temperature climate
cannot be excluded. The megastrobili of P. uliginosa developed earlier than microstrobili in any case, as it is the
rule and even more pronounced in P. sylvestris too.
Acknowledgements
The study was sponsored by the Polish Committee for Scientific Research Grant 6P04G 060 16 with support of Institute of
Dendrology. We express our warm thanks to Dr. WŁadysŁaw
ChaŁupka for critical revision of manuscript and Dr. Mark
G. Tjoelker for English editing.
Fig. 8. Development of megastrobili of
Pinus sylvestris (- - - - ) and microstrobili of P. uliginosa (
) at the Stołowe Mts site
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