The small genus
Two
The species
The aim of the study was to show the new records of
The study area was located mainly within the Bieszczady National Park – only the lower section of the Wołosaty stream flows through the territory of the San Valley Landscape Park. The bedrock of this area is built of sedimentary rocks such as sandstones and siltstones, rarely marl and conglomerates referred to as Carpathian flysch (Winnicki, Zemanek 2009).
The Wołosaty stream, known as “Wołosatka” in its upper section, is a left tributary of the San River. The source of the stream is located at an altitude of 1200 m a.s.l. At first, the Wołosatka flows from the east to the west in the depression between the ridges of the mountains. Near Ustrzyki Górne, the stream changes its course to the north and from here it is referred to as the “Wołosaty” stream. It flows into the River San behind the village of Stuposiany at an altitude of 550 m a.s.l. (Kukuła 2002; the Bieszczady and Sanocko-Turczańskie Mountains – tourist map).
The Terebowiec stream is 8.01 km long. The mouth of the creek is located at an altitude of 650 m a.s.l., while the source – at an altitude of 1225 m a.s.l. The Terebowiec stream flows into the Wołosatka stream in Ustrzyki Górne and the two streams together form the Wołosaty stream. The slopes of the valley are covered with old trees with a dominance of
The Rzeczyca stream is a left tributary of the Wołosaty stream, with a length of 13.17 km. The sources of the stream are located at the foot of Połonina Caryńska at an elevation of 1030 m a.s.l., while the mouth of the stream is located at an altitude of 660 m a.s.l. (Czarnecka 2005).
Studies were conducted at nine sampling sites in the Wołosatka, Wołosaty, Rzeczyca and Terebowiec streams between 2013 and 2015 (Fig. 1).
Samples were collected in September 2013, May and October 2014, and October 2015 from available habitats, such as stones (at all sampling sites) and aquatic macrophytes (mainly from mosses and green algae). The temperature, pH, dissolved oxygen and electrolytic conductivity were measured in situ. Water samples for chemical analysis were collected at the same time. Algae samples were preserved in 4% solution of formaldehyde.
Chemical analysis of the water was carried out in the Departmental Laboratory of Analysis of Environmental Health and Materials of Agricultural Origin of the University of Rzeszów by means of DIONEX ICS–5000+DC liquid chromatography equipment.
Diatom samples were prepared according to methods used by Kawecka (1980) for river algae. A portion of each sample was cleaned with a mixture of sulfuric acid and potassium dichromate at a 3:1 ratio, and then washed in a centrifuge (at 2500 rpm). Diatoms were mounted in synthetic resin (Pleurax; refractive index 1.75).
Diatoms were identified and counted under a Carl Zeiss Axio Imager A2 microscope equipped with a 100× Plan Apochromatic objective with differential interference contrast (DIC) for oil immersion (NA 1.4).
Diatom identification was supported by the following references: Krammer & Lange-Bertalot (1986), Sala et al. (1993), Levkov and Ector (2010), Hofmann et al. (2011) and Bąk et al. (2012).
Species composition was determined in the collected samples by counting 400 specimens in randomly selected fields under a light microscope. Species with a content above 5% in a given diatom assemblage were defined as the most abundant ones.
For SEM observations, samples were coated using a Quorum Q 150OT ES Turbo-Pumped Sputter Coater with 20 nm of gold, and observed under a Hitachi SU 8010 scanning electron microscope (SEM) at the Subcarpathian Center for Environmental Research and Innovation at the University of Rzeszów.
Water in the studied streams was mostly alkaline; pH values were lower (near to neutral) only in September 2013. Electrolytic conductivity ranged from 78 to 284 µS cm-1. The oxygen saturation level was high in each sampling season. Furthermore, the water was characterized by a low nutrient content and average calcium content (30.3-41.6 mg l-1) (Table 1).
Values of water physicochemical parameters in the Wołosaty stream and tributaries in 2013-2015, and description of sampling sites together with the most frequent accompanying diatom taxa (* below the limit of detection)
Streams
Wołosatka
Wołosaty
Rzeczyca
Terebowiec
Total number of sampling sites
2
4
1
2
Width
m
3-6
4-20
1.5-3
5-7
Depth
0.1-0.3
0.2-0.4
0.1-0.3
0.2-0.4
Type of the bottom
stones, at the first site stones covered with mosses in 30-40%
stones, at sites 5-6 stones covered with mosses and other algae from the genus Chlorophyta in 20-30%
stones
stones, at site 8, larger stones covered with mosses
Insolation
site 1 – low site 2 – high
high at all sites
low
site 8 – low site 9 – average
physicochemical parameters
Temperature
°C
8.0-12.2
5.6-10.8
7.4-10.0
6.1-9.3
pH
6.4-8.8
6.5-8.6
6.4-8.4
6.4-8.4
Conductivity
µS cm-1
78-254
146-278
97-246
86-284
O2
mg l-1
10.16-10.67
10.65-11.44
10.6-10.24
10.67-11.06
Cl-
0.43-5.33
0.65-5.35
0.60-5.31
0.41-5.59
11.05-20.69
12.79-26.77
16.31-33.34
12.53-27.19
1.67-2.46
1.94-3.15
1.78-3.20
2.01-2.86
*
*-0.64
*
*
0.06-0.71
0.14-0.88
0.04-0.06
0.06-0.13
Mg2+
5.00-7.82
5.26-10.12
5.33-9.32
5.62-10.10
Ca2+
30.31-34.25
33.72-41.55
38.75-39.72
32.42-35.31
The most frequent taxa
(Hust.) Levkov & Ector (Fig. 2 m-u, Fig. 3)
The precise morphological description of the
Under a light microscope, valves of
Comparison of the valve morphology and occurrence of
Taxa
Length (µm)
12.4-31.0
8.9-14.2
16.5-26.5
Width (µm)
4.6-6.3
3.8-4.3
4.2-6.4
Number of striae in 10 µm
9-13 most commonly 10-11
12-15
7-9
Occurrence
Always as single cells, found on stones and most frequent on mosses.
Very rare, found on stones and mosses.
Very rare, found mostly on stones. The rarest of the three taxa found in the analyzed samples.
There is no detailed information on the occurrence of this species, because it was only recently distinguished from
According to Levkov and Ector (2010),
The species was identified in each of the streams surveyed in this study, at all the selected sites: the Wołosatka, Wołosaty, Rzeczyca and Terebowiec streams. The species was always present as individual cells. The species was observed more frequently only in the Terebowiec stream, but with the maximum abundance of only 0.5% in the total species composition of diatom assemblages. At each study site, it was associated with
The studies carried out in the Wołosaty stream and its tributaries suggest that