PART 7
Biological Monitoring
The biological monitoring of agreed groups of aquatic and
terrestrial fauna is carried out on six complex monitoring areas on the Slovak
side. On these areas the phytocoenological observations were realised as well,
which record the spring and the summer aspect of plant communities. The aquatic
macrophytes observation was restarted again in 1999. The monitoring continued by
the method of phytocoenological relevés of Braun-Blanquet till 2002, as it was
introduced at start of the monitoring. In 2003, due to unification of
observation methods, the Slovak side started to use the Kohler index method in
the frame of aquatic macrophytes monitoring. The same groups of fauna and flora,
agreed in the frame of joint monitoring, are monitored at 31 monitoring sites on
the Hungarian side (Fig. 7-1). There are differences in some monitoring methods
on both sides henceforth (e.g. on the Hungarian side the similarity index and
the ecological analysis of terrestrial plant communities is not evaluated; reed
communities on the Slovak side are not observed in such a detail like on the
Hungarian side; the monitoring of Ephemeroptera, Trichoptera and Odonata on the
Slovak side is based on aquatic larvae observation, while on the Hungarian side
it reside in observation of imagines), however, further unification is ongoing.
Abiotic conditions, which influence the growth and
development of plant and animal communities in the evaluated area on both sides
of the Danube, in 2003 can be characterised as follows:
Unusual flow rate
regime in the Danube characterised the hydrological year 2003. Higher
discharges were typical in the winter period till end of January, while
since March till the end of vegetation period average and significantly
below the average flow rates were characteristic.
Although the
initial conditions for optimal start of vegetation growth were almost
reached at the beginning of vegetation period in 2003, intensive
deterioration of moisture conditions in following months was registered.
Rich precipitations, together with high flow rates in the Danube allowed
saturation of soils, however lack of precipitation in the whole vegetation
period caused significant decrease of soil moisture in the area.
Higher long
lasting air temperatures often accompanied this extremely dry weather in the
period from May to September. Because of low flow rates the water
temperature in the Danube frequently reached the highest values in the
period of last 40 years.
The amount of
organic matter brought by floods in 2002 allowed a general increase of
coverage of nitratophilous plants in the whole inundation area.
In the relatively
short period of monitoring numerous meteorological records were registered
in both, positive and negative senses. Impact of these conditions could be
demonstrated on flow rates, soil moisture, and consecutively on development
of vegetation.
7.1. Phytocoenology
The left side river branch system
The changes of biota on the monitoring area No. 2600 are
caused by gradual long-term drying up of the locality, which was already
observed since seventies of the twentieth century. The observed phytocoenoses
develops relatively favourable, which could be explained by increase of soil
moisture after two strong floods in 2002. Similar phenomenon was registered at
the beginning of vegetation period in 2003, owing to the high flow rates in
2003. The development of every three layers of phytocoenoses was relatively
favourable. No premature defoliation or mosaic loosening of coverage in the herb
layer occurred in the summer period. The extremely dry weather was visible on
dry and declined individuals of nettle in August only. Only the increase of
species diversity and rising number of invasive species reflect the tendency of
gradual changing of community towards more xerophilous one.
Monitoring areas No. 2603 and 2604 are situated downstream of
the intake structure to left side river branch system, thanks to what the
moisture conditions have not changed significantly after damming the Danube and
high water level can be kept in the river branches too. Some change was recorded
in the flood regime of the region and in case of the monitoring area No. 2603
attention should be aimed also to changes caused by the drainage effect of the
Danube.
Phytocoenological monitoring on the monitoring area No. 2603
(TMP 9A) was restarted in 2002 in the five-year-old cultivated poplar stand
after an interruption in the period 1998-2001 due to cut out. The gradual
development of the stand in the second year was shown in increase of the tree
layer coverage and decrease of ruderal and nitrophilous species in the summer
aspect. Decrease of species number and coverage of the herb layer in the summer
period was caused by long-term drought.
The plant communities on monitoring area No. 2604 are stable.
Life form changes after floods in 2002 and fluctuation of several factors of the
ecological analysis, which are not caused by hydropower station operation,
testify the dynamic development of the softwood phytocoenoses.
Monitoring areas No. 2608 and 2609 are situated in a region
where the backwater effect upstream the confluence of the tailrace channel and
the Danube old riverbed significantly decreases the impact of diversion.
Although the situation in this area is relatively stable (particularly at
monitoring area No. 2609), the solution of the water regime should not be
underestimated. In case of long lasting low and average flow rates in the Danube
the area becomes vulnerable. Premature defoliation of willows and fading and
drying of plant species was registered during the extremely dry summer period in
2003, accompanied with high temperatures and low ground water level due to long
lasting low flow rates. On the monitoring area No. 2609 well-preserved willow
stand is present, typical for softwoods. Dry weather conditions did not affect
the phytocoenoses in 2003. However, the spring dominance of Aster lenceolatus,
accompanied with simultaneous retreat of protected species Leucojum aestivum
is an atypical phenomenon.
The reference monitoring area No. 2612 is situated downstream
the confluence of the tailrace channel and the Danube old riverbed, where the
direct impact of the Gabčíkovo waterworks is insignificant. In spite of
unfavourable moisture conditions in 2003 the development of transitive
floodplain forest was relatively favourable. Strong spreading of nitrophilous
species was registered in the evaluated year because of new sediment layer rich
in organic matter, brought by two floods during previous year.
The right side river branch system
The evaluation of plant and reed communities monitoring on
the Hungarian side is based on data of summer aspect. According to the obtained
results it can be stated that changes of vegetation in the observed area are
slow and not significant in last years. Interannual differences in
meteorological conditions do not alter the vegetation to such an extent that
could be detectable by field investigation methods used in the frame of joint
monitoring. In 2003 according to the phytocoenological studies slight
significant increase in species richness was recorded, however the rise from the
point of view of coverage values was not significant. Average values of leaf
area were lower in comparison to the previous year, while no clear tendency
appeared in this variable for the reed stands. The vegetation of oxbow lakes had
regenerated where water supply created sufficiently high water level. Since the
water level in Mosoni Danube was artificially kept stable the ground water table
depth stabilised, thus no vegetation change appeared that could be attributed to
the diversion of the Danube. A number of seminatural willow stands grow at the
banks of the Danube old riverbed, however, several willow forests has been
replaced by hardwood plantations on the drying floodplain.
Field observations indicate high regeneration potential for
wetland vegetation. Artificial wetlands are rapidly and spontaneously colonized
(or recolonized) by characteristic wetland species. The bank of Lipót lake is a
good example for this. This indicates a quick regeneration for floodplain
vegetation if the water recharge for an oxbow lake, for a river branch or for
even a complete tributary system could be provided artificially by distributing
sufficient water in the area. The influence of high water table level and
temporary inundation on vegetation is much pronounced if these occur from April
to September than during the rest of the year.
7.2. Terrestrial molluscs
The left side river branch system
The process of drying out in the area of monitoring site No.
2600, which was recorded in previous decades, speeded up after diverting the
Danube. The terrestrial mollusc’s community had stabilized at medium
degradation level of the original community of dryer softwoods type. Temporary
decrease of further hygrophilous species was registered during the dry summer.
In the year 2002 the monitoring of terrestrial malakocoenose
in the original monitoring site “9A” of the monitoring area No. 2603 was
restarted. It was temporarily moved to the monitoring site “9B” due to cut
out of forest stand. High degree of similarity was noted between the two
sub-sites and the composition of malakocoenoses in 2002 was comparable with the
state before the damming. During the dry year 2003 the malakocoenose got an
atypical structure, with dominance of two ecologically different species
(semisteppe and hygrophilous forest species). The gradual development of the
tree layer will lead to decrease of microclimate fluctuations in next years,
which can be reflected on the stabilisation of the malakocoenose.
Permanent presence of natural wetland community of
terrestrial molluscs can be observed on the monitoring site No. 2604.
Polyhygrophilous and hygrophilous forest species remain dominant. The drought in
2003 was reflected in the decrease of abundance only.
According to the monitoring results in 2003 the
malakocoenoses on monitoring site No. 2608 is moving towards the xerophilous
type. The expected decrease of non-original species after the flood in August
2002 was not confirmed, moreover further decrease of hygrophilous species was
registered due to unfavourable moisture conditions in 2003. The high species
diversity, atypical for wetland communities, maintains as well. Hydrotechnical
solution of water supply for this part of inundation seems to be necessary.
The changes of water regime in the area of monitoring site
No. 2609 after diverting the Danube are minimal thanks to the backwater effect.
The unfavourable moisture conditions in 2003 were shown by irregular occurrence
of several polyhygrophilous species and by significant decrease of abundance,
mainly during the summer sampling. Penetration of xenocenous (alien) species was
not registered.
The hydrological regime of the area downstream the confluence
of the Danube old riverbed and the tailrace channel was not changed. The
malakocoenose of monitoring site No. 2612 consist of species wit various
ecological demands from polyhygrophilous to eurytopic species. Wide species
diversity was created by mixing of communities from diversified surroundings
during regular floods. The lack of moisture in 2003 was shown in decrease of
species number and their abundance during the summer.
The right side river branch system
The terrestrial molluscs community in the inundation area as
well in the flood-protected area is intact. The decrease in the number of
individuals of the terrestrial molluscs in the year 2003 is an unfavourable
phenomenon. On the other hand, the proliferation of Lithoglyphus naticoides,
the occurrence of Unio crassus and the regular presence of Palidilhia
oshanovae should be regarded as a favourable trend of change. The settlement
of the species Planorbis carinatus and Gyraulus riparius in the
side branches was recorded.
7.3. Aquatic macrophytes
The Danube
In the Danube old riverbed two Hungarian monitoring sites are
situated (No. 2 and 7). The old riverbed has not provided favourable conditions
for development of macrophyte communities before damming the Danube.
The monitoring area No. 2 is in the main riverbed downstream
of the bottom weir, where the flow rate prevents creating of macrophyte
communities. The monitoring site No. 7 is separated from the Danube old riverbed
by shoreline vegetation of Salicetum triandrae and Scirpo-Phragmitetum.
Due to its intensive spreading the part of water area was isolated and it had a macrophyte
community rich in species in the last years.
The left side river branch system
The state of macrophyte community on the monitoring area No.
2603 is determined by the water supply through the intake structure since 1993.
Macrophytes in deep arms with flowing water mainly occur along the line
structures, where they are protected from the strong current. Their stands were
wash out by strong floods in 2002, and their regeneration was not registered in
2003. Only one isolated submerged species was recorded along the line structure.
The results of macrophyte monitoring in the dead arm of
monitoring area No. 2604, since restarting the macrophyte monitoring
(1999-2002), are comparable with findings before damming the Danube. The marshy
lake is bordered by a reed stand of the association Phragmitetum communis,
the open water area is almost fully covered by Ceratophyllum demersum, in
the littoral endangered aquatic and marshy species occur.
The region of monitoring area No. 2608 is characterised by
existence of depressions. Due to the regular flooding of the surface they are
occupied by species of wet and very wet biotopes, which suffer water level
fluctuation and flooding.
The observed river arm on monitoring site No. 2612 was
influenced by extremely low water level in 2003. Dense stands of species not
directly depending on aquatic environment dominate due to very frequent
occurrence of limose ecophase.
The right side river branch system
The discharges supplied into the active floodplain were
similar to discharges in previous years. The species composition in last years
is stable, however some quantitative changes were noticeable. In the deep slower
flowing water of Csákanyi river arm (monitoring site No. 9) the macrophytes
stand extended. The water of Schisler oxbow (monitoring site No. 4) is shallow
and nearly stagnant. In the river arm algae growth occurred and rhizophytic
macrophyte species were present in small groups in last years.
Due to permanent water supply the hydrological conditions of
the flood-protected area (monitoring sites No. 6, 8) remained unchanged in last
years. The number of observed macrophytes species remained unchanged as well.
7.4. Aquatic molluscs
The Danube
The evaluation of the aquatic molluscs’ community in the
Danube in 2003 is based on the data provided by both the Slovak and Hungarian
Party (Slovak observation sites are situated at rkm 1841, 1817 and 1804,
Hungarian observation sites are situated at rkm 1831 and 1824). Based on
observations it can be stated that the molluscs’ community in the Danube is
stable. The malakocoenose is characterised by dominance of rheophilous species
during the whole observed period, although a slight increase of species
number indifferent to the flow velocity was observed after damming the Danube.
The left side river branch system
The aquatic molluscs’ community in the river branch system
on the Slovak side is monitored on areas No. 2603 and 2604.
Because of connection of the river branch at monitoring site
No. 2603 with the neighbouring river arms and the Danube, high species diversity
of community can be continuously observed, which consist mainly of stagnicolous
and indifferent species. Changes in the community after floods in the previous
year were not registered.
The connection of isolated community of aquatic molluscs on
the monitoring area No. 2604 (since last big flood in 1991) was temporarily
restored during the floods in 2002. Increase of species richness and abundance
was registered in the molluscs community. However, regarding the wide food
offer, the community of aquatic molluscs could be richer in species and number
of individuals.
The right side river branch system
No significant changes in malakofauna of the right side river
arm system were recorded in 2003. Stable occurrence of some species in the river
branch system should be regarded positively.
7.5. Dragonflies (Odonata)
The left side river branch system
The species composition of dragonflies’ community on the
Slovak side during the whole observed period is rather poor.
Monitoring of dragonflies in the monitoring area No. 2600 was
in 2002 restored in a gravel pit, which is filled up with Danube water and
had muddy-gravel bottom. The newly formed biotope was not overgrew by
macrophytes yet and the dragonflies’ community was poor. More significant
settling of this biotope by dragonflies can be expected in the following years.
The abiotic conditions of aquatic biotopes on the monitoring
area No. 2603 was not changed since introducing the water supply to the river
branch system (in 1993). Stabilisation of odonatocoenose mainly consisting of
rheophilous and semirheophilous species was registered since then. The raised
values of species number and abundance in 2003 probably reflect the reaction of
the community to antropic influences (forest cultivation).
Moderately rich dragonfly community on monitoring site No.
2604 remains on similar level as in 2002, in spite of the dry vegetation period
in 2003. Flooding and washing out of the dead arm in previous year slowed down
its natural gradual degradation.
The sampling site on monitoring area No. 2608 was moved due
to unfavourable biotope conditions for dragonflies’ communities. Although the
abiotic conditions of the newly chosen site were favourable, irregular
occurrence of one rare species was registered only in 2003.
Monitoring of odonatocoenose on the monitoring area No. 2612
was moved to neighbouring river arm with more favourable conditions for
dragonflies’ occurrence in 2002. The dragonflies’ community in 2003 had
relatively high species richness and consisted of species of eutrophic water
bodies and semireophilous species, however with low abundance.
The right side river branch system
The species composition of odonatocoenoses of regularly
monitored sites has stabilised during last years. The recorded number of species
in 2003 was 36.
7.6. Crustaceans (Cladocera, Copepoda)
The Danube
Evaluation of development of Cladoceras and Copepods
communities is based on the results of the Slovak side (monitoring site No. 2600
and 2608). The stabilised conditions of the Danube old riverbed allow formation
of the stable communities of Cladoceras and Copepods. Actual spreading of the
macrovegetation in the river influences their development in the respective
year. Their species diversity was rather high in the evaluated year; even the
proportion of euplanktonic and tychoplanktonic species was comparable with the
pre-dam state.
The left side river branch system
The state of Cladoceras community in the river arm on
monitoring area No. 2603 was relatively stable during last years, however this
state is not comparable with the pre-dam period. The difference is in lower
species diversity and the occurrence of euplanktonic species, which formed the
main part of this community before the damming, became insignificant. Similar
changes were observed in the Copepods community as well. The euplanktonic
species were displaced by gradual spreading of macrophytes, however their
repeated dominance was recorded in 2003 (probably due to wash out of macrophytes
in previous year).
The gradual overgrowing of the dead river arm on the
monitoring area No. 2604 causes changes in Cladoceras community, where loss of
dominance of euplanktonic species going on. The rate of phytophilous species and
species settling biotopes rich in organic detritus increases. The temporary
interconnection of the river arm during floods in previous years did not stop
this tendency. Similar changes in Copepods community have significantly lower
intensity. Only fluctuation of abundance of present species within the dominant
euplanktonic group of species is registered.
Following the temporary interruption of the permanent
dominance of euplanktonic Cladocera species on monitoring sites No. 2608 in 2001
and 2002, the proportion of euplanktonic and tychoplanktonic species reaches the
pre-dam state again. The Copepods community did not show significant fluctuation
during the whole observed period.
The water level of the isolated river arm on monitoring site
No. 2612 was very low in 2003 due to unfavourable hydrological and
meteorological conditions. Therefore significant dominance of tychoplanktonic
species was registered in Cladoceras and Copepods communities, which occurrence
in the pre-dam period was very poor. Due to the extreme hydrological conditions
the species richness of Cladoceras community was poor, while the species
diversity of Copepodas community remained relatively rich.
The right side river branch system
The development of planktonic crustaceans in the Schisler arm
(monitoring site No. 4) and in the Zátonyi Danube (monitoring site No. 5) was
similar to the previous years. In 2003 significant decrease of species number
was observed in the Lipót oxbow (monitoring site No. 6), where several species
dependent on macrophytes was not observed. Increase of species diversity was
registered in the Csákányi river arm (monitoring site No. 9) in the inundation
area, but the species density was low, except one tychoplanktonic phytophilous
Cladocera species.
The Cladoceras and Copepods communities were characteristic
by maximum abundance during the spring period in 2003. Probably because of the
extremely unfavourable hydrological condition the species densities in summer
and autumn were low, while the maximal density in the previous year was
registered in autumn. The most frequent species were Bosmina longirostris
and Chydorus sphaericus, like in the previous year.
7.7. Caddisflies and Mayflies (Trichoptera, Ephemeroptera)
There are differences in the mayflies (Ephemeroptera) and
caddisflies (Trichoptera) taxocoenoses monitoring methods used by the Slovak and
Hungarian Party. On the Slovak side the larvae of mayflies and caddisflies
living in the water are observed, while on the Hungarian side the flying
imagines are monitored. The Hungarian Party did not carry out sampling of
caddisflies communities in 2003; evaluation of the amassed biological material
was performed only.
The Danube
Changes of ecological conditions in the Danube old riverbed
resulted in changes in mayflies and caddisflies’ communities. The monitoring
results on the Slovak side (monitoring sites No. 2600, 2603 and 2608) indicate
presence of very poor mayflies community. However, the presence of further
species can be expected in the deeper part of the river, where gravel bottom bed
occurs. The mayflies community was represented by semirheophilous and
rheophilous species, while only one species in the caddisflies community,
belonging to the filtrator group, was registered in last years. The occurrence
of the species indicate the gradual decrease scrapers, spread in the Danube due
to changes in food offer after diversion of the Danube.
The differences in the mayflies community registered by the
Hungarian side during the last year in the upper and middle part of the Danube
old riverbed were balanced in 2003. Rich appearance of eutrophic water mayfly
species was recorded on both sampling sites (Rajka and Szőgye). The monitoring
of mayflies based on flying imagines shows the existence of richer community,
than is represented by results obtained by the Slovak Party, which are based on
insect larvae. While the Slovak Party indicate the presence of rheophilous and
semirheophilous species, imagines observed on the Hungarian side give evidence
of several stagnant water species, which settle the Danube old riverbed.
The left side river branch system
The mayflies and caddisflies communities in the left side
river branch system are generally characterised by low species diversity and low
number of individuals of present species. This statement is valid for every
monitored river arm in the left side inundation area (monitoring sites No. 2603,
2604, 2608 and 2612).
The mayflies and caddisflies communities in the river arm of
monitoring area No. 2603 in 2003 consisted of irregularly present species from
semirheophilous to stagnicolous type. The forest cut out in river arm
surroundings did not influenced the development of the community for the
present.
After a moderate increase of species diversity in the
mayflies community on the monitoring site No. 2604 in 2002, only larvaes of two
stagnicolous species were registered in 2003. Regeneration of caddisflies
community, after its absence in 2000 and 2001) did not occurred in 2002 and
2003, not even after favourable hydrological (floods) in 2002. In 2003 only one
species was registered, which was bound to macrophytes.
The presence of mayflies and caddisflies communities on the
monitoring site No. 2608 was irregular in the last period. No larvae were found
in 2002 and 2003. Moving of the monitoring site within the complex monitoring
area seems to be necessary.
The mayflies’ community in the monitoring area No. 2612 is
represented by single stagnicolous species during last years, which was
accompanied by further species of eutrophic water bodies in 2003. The presence
of caddisflies community in individual years and individual samples was
irregular. Occurrence of one species of filtrator type was registered in the
summer sample only in 2003.
The right side river branch system
Different results in monitoring of mayflies and caddisflies
on the Slovak and Hungarian side have been reached in the river branch system
too.
The species diversity and the abundance of mayflies’
species on the Hungarian side are significantly higher in long-term. High
species diversity was observed on the monitoring site at Mosoni Danube near
Feketeerdő again. The Ephoron virgo, liking river branches with silted
bottom, was the dominant species in 2003. The mayflies community is
characterised by high stability. Mass occurrence of mayfly of eutrophic water
bodies (Caenis horaria) persist in the Lipót marsh, along with lower
number of other species. Species composition changes were registered in the
individual years as well.
No caddisflies observation was performed in 2003, however
according to the evaluation of amassed biological material of several years it
can be stated that composition of caddisfly communities basically did not
changed. According to the observation of flying imagines the caddisfly
communities in the Szigetköz region are very rich, which is proved by high
species number and high number of individuals (51 species was determined).
Rheophilous species preserves its dominance; population of several other
characteristic species are stabilised as well. Based on the caddisflies
communities’ development and composition the water bodies of Szigetköz region
are in a good state.
7.8. Fish (Osteichtyes)
The ichtyofauna monitoring on both sides is carried out by
electro-fishing (with moderate high power-output apparatus – 600 W). In 2002
very high power-output electro-fishing boat was alternatively used in the Danube
by the Hungarian Party (10000 W). The mentioned apparatus has higher range and
therefore allows observation of deeper parts of water. Due to the different
species-selectivity of the mentioned methods, the obtained results are not
directly comparable with the data of previous years, therefore the Hungarian
Party in 2003 used the medium power-output apparatus again. The methods of
electro-fishing have limited range and they are species-selective, therefore
they cannot give complete results.
The Danube
The evaluation is based on Slovak observation results on
monitoring areas No. 2600 and 2608 and Hungarian observation results on
monitoring sides No. 10 and 11. In general it can be stated that the fish
community in the Danube old riverbed is stabilised. After diversion of the
Danube decrease of the number of rheophilous species was recorded; eurytopic
species replaced them. Significant changes of the relatively rich species
composition were not registered during last years. Fluctuation of species number
and abundance in individual samples could by assigned to different hydrological
conditions at the time of sampling (different flow rates). Results of last years
are influenced by difficult access to the shoreline, due to spreading of
littoral willow stands.
The left side river branch system
The ecological conditions in the river branch system at Bodíky
(monitoring area No. 2603) have changed after introducing the water supply in
1993. The ichtyocoenose of the area is characteristic by stability in last
years, with the dominance of eurytopic species. The positive impact of floods in
previous year was observed in immediate significant increase of species
diversity, which remained on the same level in 2003 as well.
The long-term isolation of the monitoring area No. 2604
resulted in decrease of species diversity of the dead river arm. However,
moderate increase of species number and abundance as well was registered in last
years, what is explained by the absence of overwarming of the water body and by
floods in 2002. However, in 2003, due to unfavourable meteorological and
hydrological conditions, low species diversity and abundance was registered in
the ichtyocoenose.
The ichtyocoenose on the monitoring area No. 2608 is observed
on two partial monitoring sites in the river branch system (upwards and
downwards from the Foki weir), which differs in their connection with the
Danube. The monitoring site upwards from Foki weir is permanently connected with
the Danube, particularly during higher flow rates. The fish community is stable,
with high species diversity and abundance as well as, with dominance of
eurytopic species. While in 2002 occurrence of rheophilous species was
characteristic, significant spreading of limnophilous species was registered in
2003 due to extremely low flow rates. The connection with the main riverbed was
lost in the river arm downwards from Foki weir since damming the Danube. Only
temporary reconnection occurs during big floods. After floods in 2002 temporary
increase of species diversity and abundance was registered, however the
ichtyocoenose in 2003 consisted of several mainly eurytopic species. The
occurrence of rheophilous species was insignificant.
The development of ichtyocoenose on monitoring area No. 2612
depends on the hydrological regime of the Danube. The area is situated
downstream the confluence of the tailrace channel and the Danube old riverbed
and is not influenced by the flow rate discharged into the old riverbed. The
connection with the Danube is restored only during big floods on the Danube
(1991, 2002). During the ten years long isolation it almost lost its spawning
function, which was accompanied by significant decrease of fish species and
number of individuals (to 3-4 limnophilous species). The connection with the
Danube was temporarily restored during floods in 2002. Due to this significant
increase of species diversity and abundance was registered. Besides limnophilous
species the eurytopic ones became dominant. In consequence of the unfavourable
hydrologic conditions in 2003 the species diversity and abundance of individuals
returned to the level recorded before floods in 2002. However, the dominance of
eurytopic species remained.
The right side river branch system
The ichtyocoenose on the Hungarian side is monitored on two
monitoring sites in the inundation area (No. 4 and 9)and on two monitoring sites
in the flood protected area (No. 5 and 12).
The ichtyofauna of the Schisler river arm restored after its
artificial reconnection with Csákányi Danube in 1997. The species number
radically increased, the species richness of the fish community is moderately
rich at present. Eurytopic fish species were dominant in 2003. Limnophilous
species occurred in the middle part of the river arm, however rheophilous fish
species was found in the connection channel as well.
The state of ichtyofauna in Csákányi Danube (monitoring
site No. 9) in last years (since introduction the water supply in 1995) was
comparable with the community found before the damming. The macrophytes
vegetation retreated due to continuous water supply and the limnophilous fish
species were replaced by rheophilous ones. A slight decrease of species
diversity can indicate the tendency of silting of the river bottom at the
sampling site, however this cannot be generalised to the whole river arm system.
After introduction of the water supply to the monitoring site
No. 5 – Lipót marsh regeneration of ichtyofauna is observed. Eurytopic
species were dominant. The species richness of this site is significant and
balanced at present.
The hydrological conditions of Gazfűi Danube (monitoring
site No. 12) are equal since introducing the water supply of the flood-protected
area. Moderate species richness characterised the stabilised ichtyofauna, which
consisted of eurytopic and limnophilous species. The eurytopic species Rutilus
rutilus remain dominant.
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Fig. 7-1 Monitoring network of observation objects agreed in the frame of the
Joint monitoring
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