AQUATIC MACROPHYTES AND THEIR USE AS ECOLOGICAL...
Transcript of AQUATIC MACROPHYTES AND THEIR USE AS ECOLOGICAL...
Romanian Journal of Aquatic Ecology 1.1 (2011)
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AQUATIC MACROPHYTES AND THEIR USE AS ECOLOGICAL
STATUS INDICATORS IN RESTORATION PROJECTS
IN THE DANUBE DELTA (ROMANIA)Erika SCHNEIDER-BINDER 1
Keywords: Romania, Danube Delta, aquatic macrophytes, quality indicators,
filtering function, restoration, monitoring as success control.
Abstract
The present study provides an introduction to the aquatic plants and their
communities occurring in three restored areas of the Danube Delta - Babina, Cernovca
and Popina. Given that the aquatic vegetation is very sensitive to physical and chemical
parameter changes it perfectly suits as indicator in the evaluation of alterations owing to
restoration measures. These evaluations consist in changes regarding the hydrological
regime, water circulation, water exchange, sedimentation processes, nutrient content
and filter function. The presence of aquatic plants of the Hydrocharition alliance such
as Greater bladderwort (Utricularia vulgaris), Frogbit (Hydrocharis morsus ranae)
or Waster soldier (Stratiotes aloides) in those spots along the reed area borders where
clear, filtered water seeps in substantiates the re-established filter function in the restored
areas.
ZUSAMMENFASSUNG: Gewässermakrophyten und ihre Verwendung als
Indikatoren des ökologischen Zustandes in Renaturierungsprojekten im Donau-Delta
(Rumänien).
In vorliegender Arbeit werden die Wasserpflanzen und ihre Gesellschaften aus
drei renaturierten Gebieten Babina, Cernovca und Popina im Donau-Delta vorgestellt. Da
die Wasserpflanzen auf Änderungen der physikalischen und chemischen Parameter sehr
sensibel reagieren, können sie zur Bewertung von Veränderungen nach erfolgten
Renaturier-ungsmaßnahmen dienen. Dabei geht es um die Bewertung von Veränderungen
des hydrologischen Regimes, von Wasser-zirkulation, Wasseraustausch, Sedimenta-
tionsprozessen, Nährstoffgehalt und Filterfunktion. Wasserpflanzen des Verbandes
Hydrocharition wie beispielsweise Wasserschlauch (Utricularia vulgaris), Froschbiss
(Hydrocharis morsus ranae) oder Krebsschere (Stratiotes aloides), die am Rande von
Schilfflächen dort vorkommen, wo klares, gefiltertes Wasser heraustritt, belegen die
Wiederherstellung der Filterfunktion in den renaturierten Gebieten.
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Rezumat: Macrofite acvatice şi folosirea lor ca indicatori ai stării ecologice în
proiecte de restaurare în Delta Dunării (România).
Lucrarea prezintă macrofitele acvatice şi comunităţile lor din trei arii situate în
nord-estul Deltei Dunării: Babina, Cernovca şi Popina, în care au fost implementate
măsuri de reconstrucţie ecologică. Deoarece macrofitele acvatice reacţionează foarte
sensibil la schimbarea parametrilor fizici şi chimici, pot fi utilizate pentru evaluarea
schimbărilor în urma măsurilor de reconstrucţie ecologică aplicate. Evaluarea se referă la
schimbări în regimul hidrologic, circulaţia apei, procese de sedimentare, conţinutul de
nutrienţi şi refacerea funcţiei de filtru a stufului. Macrofite acvatice din alianţa
Hydrocharition ca de exemplu otrăţelul de baltă (Utricularia vulgaris), broscariţă
(Hydrocharis morsus-ranae) şi foarfeca de apă (Stratiotes aloides), care s-au reinstalat în
bordura stufului acolo unde apa iese limpede şi filtrată, dovedesc refacerea funcţiei de
filtru în zonele renaturate.
Introduction
The Danube Delta presents a diversified network of water bodies including water
courses and standing waters of varying sizes. The water courses consist in the main
branches of the Danube river, large secondary natural branches, large channels that flow
into secondary branches, small and narrow channels connecting the lakes, smaller
streams, the so called “gârla” and “japse”, temporary water courses, flood channels or
channels characterized by anthropogenic impacts such as dragging and artificial canals
that were cut through the reeds. A large variety of standing waters of various sizes and
depths exists between the branches of the delta in the large reed areas. They consist in
reed-surrounded, isolate lakes, connected to smaller or larger water courses, temporary
small standing waters and artificial standing waters such as fishponds.
The hydrological regime, hydro-morphological processes and trophic conditions
of these waters constitute the basis for a large diversity of aquatic macro- and
microhabitats, which in their turn form the basis for the settling of various aquatic
macrophytes and their communities. The habitats are differentiated by their spatial
structure and the species composition of the macrophyte communities, offering niches to
many macroinvertebrate and fish species. Ecological gradients do exist between the
various types of water bodies and also within individual water bodies where the
repartition of macrophytes follows ecological gradients in dependence of their width,
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depth, flow velocity and turbidity. The latter is in relation with the connection to the
Danube branch categories (direct connection, secondary and third connection category).
Given that the aquatic vegetation is very sensitive to natural changes, the
fluctuations of environmental factors and changes owing to anthropogenic impacts such
as rectifications, the construction of new canals, dykes and further hydraulic measures, it
is well suited as status indicator for changes in water quality and physical parameters in
consequence of restoration works.
In recent times water macrophytes have been increasingly used for the evaluation
of the trophic condition (Oosterberg & Staraş, 2000; Penning et al., 2008; Coops &
Hanganu, 2000) and the determination of physical parameters (Schneider, 2009). The
present study discusses the use of water macrophytes for the purpose of an ecological
status evaluation of water bodies in three project areas of the Danube Delta prior to and
after restoration. The macrophytes act as success control element for the monitoring of
changes occurring in the ecological condition after the measures were implemented (water
flow, filtering capacity, sediments).
Among the project areas, Babina and Cernovca were abandoned agricultural
polders characterized by destroyed, arid reed areas with increasing salinity. The third
area, Popina, consisted in an abandoned fishpond, a disturbed wetland that had been cut
off from the water dynamics of the Danube River and was subject in some parts to silting
and increasing salinity (Lagendijk & Schneider, 2000). Before hydrotechnical measures
were taken the area was a characteristic wetland area with standing and running waters.
The construction of dams transformed all former small water courses into standing
waters.
Among these three areas Babina was the first to be reconnected to the water
dynamics of the Danube River in 1994 and was followed in 1996 by Cernovca (Marin &
Schneider, 1997; Staraş, 2000; Schneider et al., 2008). The third area, Popina, was opened
subsequent to preliminary studies and technical plannings in the year 2000 (Schneider et
al., 2004) and has been monitored in 2000 at its opening as well as in 2001. Given that
wetland areas and aquatic vegetation could be found on Popina island, even though not
homogeneously and of varying quality, running waters being not existent, the objective
was to find out to which extent water circulation and water exchange had been re-
established by the reconnection to the Danube and how aquatic macrophytes had adapted
to these changes.
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Materials and Methods
Due to multiannual samplings taken in a determined network of sampling sites in
the restoration areas Babina, Cernovca and Popina in the North-eastern Danube Delta/
Chilia branch the following elements became provable within the frame of the monitoring
programme: recolonisation of species depending on the hydrological regime, abundance-
dominance value fluctuations of individual species on various sites of the restored areas
over several years and changes in the abundance-dominance values of plant communities
(Schneider et al., 2008).
The samples were taken within the frame of field studies and along with studies
conducted on macrozoobenthos, phyto- and zooplankton. The samples and the physical-
chemical measurements were taken in 23.-24. VII 1996, 29.-30 VI 1997, 1.-4 VI 1998,
18.-22 VI 1999, 23.-24 VI 2000 and 20 VI 2001 for the island polders Babina and
Cernovca, with a number of verifications in 2005, and in 1999, 2000 and 2001 for
Popina.
The sampling sites were determined to include all types of water bodies
(Lagendijk & Schneider, 2000; Schneider et al., 2004, Schneider et al., 2008).
The permanent waters are composed of a network of artificial canals, natural
former branches, smaller water courses, the so-called „Gârla“ and the shallow
depressions of varying extent that are connected to them, some kind of shallow
lakes. Considering their connectivity the waters had to be evaluated differently.
Besides selective samplings, data have also been collected in the circumference of
the sampling spots to allow a large-scale vegetation recording. Moreover, data on
the vegetation occurring alongside a number of water transects have been collected
all the same to allow a more concise registration along ecological gradients. The
collection of the aquatic vegetation data has been effected by means of the methods
for the evaluation of species abundance, dominance and sociability according to
Braun-Blanquet (1964). The yearly controls of the sampling spots allowed to draw
comparisons and made it also possible to show the development trends of the
vegetation under the changed physical and chemical parameters subsequent to
restoration measures. The improvement of water circulation, water exchange and
flashing was monitored one year following the opening on the basis of the abundance
of existing salinity indicators as well as by the recording of further indicator species
for running waters.
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Results and Discussions
The Babina and Cernovca area
After the reflooding of the two agricultural polders Babina and Cernovca, site-
specific species and plant communities developed rapidly in strong relation with the
restoration of the hydrological regime and the water quality. Along with the flooding a
shifting from dry towards a humid, moist and constantly water-covered area took place.
Depending on the ground level, the recorded data differed as a result of duration, height,
period and frequency of the floods respectively of the depth of the water bodies.
Characteristic species for running waters have been observed at the opening spots
just as species characteristic of running waters with a high to low turbidity, they are
represented by the pondweeds Potamogeton pectinatus, Potamogeton nodosus and
locally also by Potamogeton crispus. Species characteristic of running and more or less
clear waters such as the submerged form of Sagittaria sagittifolia and Sparganium
emersum. Potamogeton pectinatus occur in the oulet areas, even though they have a large
ecological amplitude and are present in clear to extremely turbid running and standing
waters. In some canals of the opened polder’s centre the pondweeds Potamogeton
crispus and Potamogeton pectinatus have been observed as well, the first being the only
water macrophyte species which persisted in the some canals of the polder before
opening.
Table 1. Evolution of water macrophyte diversity in the restored polder Babina;p = present, d = dominant.
SpeciesYear
1994 1995 1996 1997 1998 1999 2000 2001 2005Aldrovandavesiculosa . . . . . p . . .
Alismalanceolatum . p . p . . . . .
Alismaplantago-aquatica . p p p . . p p p
Azollafiliculoides . d d d p d . . p
Ceratophyllumdemersum . d d d d d d p p
Characontraria . . . . d . . . .
Charaglobularis . . . p d d . p .
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Table 1 continuing.Charavulgaris . . . . p . . p .
Elodeacanadensis . . . . . d p p p
Elodeanutalii . . . . d d p p p
Hydrocharismorsus-ranae . d d p p d d d d
Lemnaminor p p p p d p p p p
Lemnatrisulca . p p p p d p p p
Myriophyllumspicatum . p d d d d p p p
Najas marina . . . d . . . . pNupharluteum . . . . . . . . .
Nymphaeaalba . d d p d d d d d
Nymphoidespeltata . d d . p d . . p
Polygonumamphibium p p d p p p p p p
Potamogetonberchtoldii . . . . p . . . .
Potamogetoncrispus p p p d d d p p p
Potamogetonlucens . p p d d d d d d
Potamogetonnodosus . p p p d p p p p
Potamogetonpectinatus . p p . p d p p p
Potamogetonperfoliatus . . . p . . . . p
Potamogetontrichoides . . . p d d d p p
Ranunculuscircinatus . . p . d p p p p
Ranunculustrichophyllus . . d . . . p p .
Sagittariasagittifolia . p p d . . p d d
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Table 1 continuing.Salvinianatans d d d d d d d d d
Sparganiumemersum . . . d p p p p d
Spirodelapolyrhiza . d d p p p p p d
Stratiotesaloides . p d d d d d d d
Trapanatans . p p d d d d d d
Utriculariavulgaris . . . p d d d d p
Veronicaanagallis-aquatica . p p . p p d p .
Wolffiaarrhiza . p . . p p . . .
Zannichelliapalustris L.ssp. pedicellata
. p p p p d p d p
Numberofspecies
4 23 23 25 29 28 26 28 28
The development of water macrophytes and their communities in the
opened Babina polder became clearly apparent already in 1995 with broad covers of
fringed water-lily (Nymphoides peltata) in the northern area with shallow waters and
a high sediment load, the species being an indicator in shallow, eutrophic waters
with siltation processes and medium turbidity. In the first year after opening, covers
of floating macrophytes such as swimming fern (Salvinia natans), giant duckweed
(Spirodela polyrhiza) and common waterlens (Lemna minor) have also developed
and are characteristic of moderate eutrophic to eutrophic waters with medium
turbidity. Small areas were covered with European white water lily (Nymphaea
alba), characteristic of clear, moderate eutrophic to eutrophic waters. The rapid
re-establishment of the species can only be explained by the existence of the
rootstocks which survived on the bottom of the drained polder area for a period of
about twelve years, from the construction of the dams and the drainage measures
up to the reconnection of the area to the water dynamics of the Danube River (Table
1).
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A similar situation has been observed in the Cernovca polder openend two years
later in 1996. In this area the White water lily (Nymphaea alba) developed also in
proximity of floating species such as Salvinia natans, Giant duckweed (Spirodela
polyrhiza) and Common waterlens (Lemna minor). The latter arrived in the area with the
inflowing water and was among the first settlers after the reflooding (Table 2).
The gradual recovery of the reed area’s filter function has been observed from the
second year following the opening. First signs of a beginning filtering capacity of the
reed could be documented by the presence of small stands of Frogbit (Hydrocharis
morsus ranae) along the borders of small rushes consisting of the Bulrush Typha
angustifolia, Water-archer (Sagittaria sagittifolia) and Sparganium ramosum. The
Greater bladderwort (Utricularia vulgaris) settled in Babina along the borders of the
main canal CC2 from 1997, in those places where clear and filtered water seeped in from
the reed stands. These species occurring only in clear meso-eutrophic and eutrophic
waters are perfect indicators for the recovery of the reed’s filtering function in the
restored area and mark a distinct belt along the reed border, as does Frogbit (Hydrocharis
morsus ranae).
In the subsequent year 1998 the Greater Bladderwort already showed higher
abundance and dominance values (Table 2). In some lateral channels where the Water
soldier (Stratiotes aloides) builds broad covers, the Greater bladderwort occurred very
frequently as well. The sporadic occurrence of Aldrovanda vesiculosa together with
Greater Bladderwort Utricularia vulgaris in clear waters along the borders of a reed
stand is remarkable and shows as well the recovered filter function of the reed areas.
A similar evolution has been observed in Cernovca polder in 1997 and 1998, i. e.
the second and the third year following the opening and re-flooding. The Frogbit
(Hydrocharis morsus ranae) covered larger areas already in 1997. The recovery of the
filter function has been proven by the occurrence as well as abundance and dominance of
the Greater baldderwort (Utricularia vulgaris) and the development of large stands of
Water soldier (Stratiotes aloides). Greater baldderwort, Water soldier and Frogbit occur
together with the submerged floating Lemna trisulca in clear, moderate eutrophic waters,
they are very characteristic indicators of a good water quality.
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Table 2. Evolution of water macrophyte diversity in the restored areas ofCernovca Island; p = present, d = dominant.
SpeciesYears
1996 1997 1998 1999 2000Azolla filiculoides . d . p pCeratophyllum demersum . d d d dChara hispida . . d . pElodea canadensis . . . p dElodea nutalii . p . . dHydrocharis morsus-ranae . d d d dLemna gibba . . . . pLemna minor p p p p pLemna trisulca . p d p dMyriophyllum spicatum - d p d dMyriophyllum verticillatum . . . p pNajas minor . p . . .Nuphar luteum . p p p pNymphaea alba . d d d pPolygonum amphibium p p p p .Potamogeton crispus p p p p pPotamogeton lucens . d p d dPotamogeton pectinatus . d d d pPotamogeton trichoides . p d d dRanunculus aquatilis . . p . .Ranunculus circinatus . . p p .Salvinia natans . d p p dSpirodela polyrhiza . . d p pStratiotes aloides . d d d dTrapa natans . p p p dUtricularia vulgaris . p d d dVallisneria spiralis . . p . .Zannichelia palustris . . p p d
Number of species 3 19 22 22 23
The distribution of water macrophyte associations in both artificial main and
lateral canals and in the lakes of Babina and Cernovca occurred as a function of pH-
values - the differentiation depending on water salinity, nutrient content of the water,
suspended load and involved water transparency, flow velocity, water depth and
involved water respectively channel bed warming and subsoil (sandy, silty).
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The following water macrophyte associations have been recorded in the Babina
and Cernovca restoration area:
Lemnion minoris R. Tx 55 / Duckweed communities
- Lemno-Spirodeletum polyrhizae (Kalkofer 15) W. Koch 54 em. Müll. et Görs 60
- Lemnetum minoris (Oberd. 57) Müller et Görs 60
Hydrocharition Rübel 33 / Frogbit communities
The group of frogbit-associations is bound to clear, moderately nutrient-rich water
sections.
- Spirodelo-Salvinietum natantis Slavnic 1956
- Lemno-Azolletum filiculoidis Br.-Bl. 1915
- Lemno-Utricularietum vulgaris Soó (1928) 1938
- Hydrocharitetum morsus-ranae van Langendonck 1935
- Stratiotetum aloidis Nowinski 1930 em. Midjian 1933
facies with Utricularia vulgaris
Salvinia natans occurs predominantly and in some years (2005) it shapes the
autumnal aspect of the canals and other waters that are covered for their major parts by
this species. Azolla filiculoides occurs unsteadily. Given its tolerance against a moderate
salinity in waters and soils it has been recorded mainly in the western part of Babina and
Cernovca islands, where soil salinization has indeed been reduced as a result of the
reconnection to the Danube river, it is, however, still existent. In some places the species
forms also large carpets in the restoration area of Popina fishpond (2000, 2001).
Stonewort (Chara) – Associations
- Chara globularis community
Chara globularis has been registered in the western part of Babina at the end of canal
CC2 as a species developing dominant stands. In some parts they were closely interlaced
with stands of Ranunculus circinatus in waters with light salinity. In shallow waters they
could also be found in loose stands of sea club-rush (Bolboscheonus maritimus). Their
characteristic sites have changed following the opening and re-flooding of the polder as a
result of intensified cattle and pig grazing (and related to this an increasing
eutrophication) and the species disappeared as from 1998 even though it occurred en
masse before.
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Potamion eurosibiricum Koch 26 p. p. / Submerged pondweed - communities
- Potamogetonetum perfoliati W. Koch 1926 em. Pass. 1964.
- Parvopotameto-Zannichellietum palustris (Baumann 1921) W. Koch 1926, facies
with Ranunculus circinatus
- Potamogetonetum lucentis Hueck 1931
- Potamogetonetum pectinati Horvatic 1931
- Potamogetono - Najadetum marinae (Oberd. 1957) Fukarek 1961
- Ceratophylletum demersi (Soó 1927) Hild 1956
- Najadetum marinae Fukarek 1961
- Elodeetum nutalii Ciocârlan et al., 1997
- Potamogetonetum trichoidis Freitag et al., 1956
- Potamogetonetum crispi Soó 1927
Nymphaeion Oberd. 1957 (Potamion eurosibiricum W. Koch 1926 p. p. /
Group of water lily communities
- Nymphoidetum peltatae (All. 22) Bellot 1951
- Trapetum natantis Müll. et Görs 1960
- Myriophyllo-Nupharetum luteae W. Koch 1926
- Nymphaeetum albae Vollmar 1947
- Myriophyllum spicatum-community
The Popina fishpond area.
Due to the relatively young alluvial land and the topography of the area with
respect to the mean water level of the Danube River, the Popina areas EC 21 and EC 22
are dominated by a characteristic vegetation which is called „balta“. It is characterised by
a mixture of reed vegetation and open water bodies with varying depths and extensions.
Large areas are covered by emerged and submerged macrophytes and small parts of
higher river embankments and dunes with semiaquatic and terrestrial vegetation.
Depending on the Danube River’s water level, the depressions of the western
part of Popina EC 22 that are dominated by Bolboschoenus maritimus and Juncus
maritimus also act as temporary waters, when the Danube water level exceeds the mean
level. During flood periods these temporary waters are colonised by water macrophytes
such as Utricularia vulgaris and Charophytes, as was the case in 2000 and also in 2001.
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Even though large areas are characterized by more or less uniform reeds, the
area’s vegetation shows a high diversity of different types of species and plant
communities. This is due to the various ecological conditions depending on microrelief,
soil and hydrological regime (surface and groundwater dynamics), that have
unfortunately been subject to changes owing to hydrotechnical constructions in the area.
Small differences in the relief level lead to visible changes in the repartition of the
vegetation. In the area of Popina Polder EC 21 and 22 the following plant communities
have been identified:
Lemnion minoris R. Tx 55 / Duckweed communities
- Lemno-Spirodeletum polyrhizae (Kalkofer 15) W. Koch 54 em. Müll. et Görs 60
- Lemnetum minoris (Oberd. 57) Müller et Görs 60
Hydrocharition Rübel 33 / Frogbit communities
- Spirodelo-Salvinietum natantis Slavnic 1956
- Hydrocharitetum morsus-ranae van Langendonck 1935
- Stratiotetum aloidis Nowinski 1930 em. Midjian 1933
- Lemno-Utricularietum vulgaris Soó (1928) 1938 facies with Aldrovanda vesiculosa
- Lemno-Azolletum filiculoidis Br.-Bl. 1915
Stonewort (Chara) – Associations
- Charetum asperae Corillion 1957
- Charetum contrariae Corillion 1957
Potamion eurosibiricum Koch 26 p. p. / Submerged pondweed – communities- Potamogetonetum trichoidis Freitag et al., 1956
- Potamogetonetum lucentis Hueck 1931
- Potamogetonetum pectinati Horvatic 1931
- Parvopotameto-Zannichellietum palustris (Baumann 1921) W. Koch 1926
facies with Ranunculus circinatus
- Potamogetonetum nodosi (Soó 1960) Segal 1964
- Potamogetonetum crispi Soó 1927
- Ceratophylletum demersi (Soó 1927) Hild 1956 facies with Ranunculus circinatus
- Elodeetum canadensis Eggler 1973
- Hippuris vulgaris community
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Nymphaeion Oberd. 1957 (Potamion eurosibiricum W. Koch 1926 p. p. / Group of
water lily communities
- Nymphoidetum peltatae (All. 22) Bellot 1951 facies with Hippuris vulgaris
- Myriophyllum spicatum-community
- Nymphaeetum albae Vollmar 1947
- Myriophyllo-Nupharetum W. Koch 1926
- Ranunculetum circinati community
The most diversified vegetation may be found in the south-western part of the
Popina EC 22 area. The ecological gradients from dry to wet, fresh to salty on different
soil types exemplified by cross sections are demonstrating very impressively the mosaic
patterns and a high diversity of species in relatively small areas.
Aquatic macrophytes are represented by more or less eutrophic plant
communities characteristic of different types of water bodies, standing or running
waters, clear or turbid, fresh or lightly saline, with various depth and extension,
bordered or mixed with patches of reeds. Due to these facts the aquatic vegetation
includes a wide range of different types of water macrophyte communities, locally
in small-scale mosaic patterns. Utricularia vulgaris occurs in clear and
mesotrophic-eutrophic waters. Further occurring, vulnerable species are the water
macrophytes Hippuris vulgaris, Stratiotes aloides and Trapa natans. Among the
endangered species and rare in the whole delta is Aldrovanda vesiculosa which occurs
in EC 22.
The reed vegetation is represented more frequently in the southern polder
EC 22 and more rarely in EC 21 owing to the destruction of the reed beds in EC 21 at
the moment of the fishpond construction. In polder EC 22 the reed’s function
as biological filter shows through the abundant occurrence of species that are
characteristic of clear, deep waters on organic soils. The same is true for EC
21. Utricularia vulgaris, Myriophyllum verticillatum, Lemna trisulca, Hydrocharis
morsus ranae and Hippuris vulgaris. Charophytes (Chara contraria, Chara
aspera) settle in clear shallow water areas and occur in the southern part of the both
polders.
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In general the water macrophytes are represented mainly by communities
characterstic of eutrophic spots or slowly running waters. The large areas covered
by Nymphoides peltata in EC 21 and 22 indicate eutrophic waters with changing
water levels, the species being well adapted to these changes can also survive in
the summer time (i. e. the Danube River’s low water levels) and persist in semiterrestrial
conditions. The big quantity of biomass in the large open shallow waters and the
lacking water circulation will lead to increasing organic deposits and to a progressive
silting of area.
The courses of small old water channels („gârla“) are partly well contoured by the
presence and abundance of Stratiotes aloides. They constitute a first step towards a
development of swimming reeds, the so called „plaur“.
Generally higher pH values in the northern polder EC 21 compared to the
southern polder EC 22 becomes apparent by the dominance and high abundance of
Myriophyllum spicatum covering large areas, i. e. a species occurring in waters with high
pH values (s. Ellenberg et al., 1991). Highly abundant in EC 21 is also Ranunculus
circinatus, characteristic just as Myriophyllum spicatum in calcareous and extremely
basic waters (s. Krausch, 1996).
Potamogeton pectinatus occurs with a broader ecological amplitude. The species
is sporadically present in standing clear waters with high pH values and a high nutrient
content even though rather in running waters, as is the case in the surrounding canal of
Popina and Cardon, where turbidity is high owing to its sediment content. This species
occurs only along the borders of Popina polder in the Chilia branch.
Dyked areas without any direct connection to the channels or to the Danube
River branches show a higher salinity. This is apparent in the area situated between
the dyke adjacent to Popina channel and the former protecting dyke of the
village Sfistofca. This area with its changed hydrological regime, in connection
with a high evaporation rate owing to the studied area’s continental climate type,
is characterized by settlements of communities with increasingly characteristic
halophilous, polyhalin and also eurihalin species. On the water-side, next to the
Popina channel the community of Carex distans (lightly halophilous conditions
present) dominates on sites where salinity is well-balanced thanks to fresh water
floodings.
Romanian Journal of Aquatic Ecology 1.1 (2011)
59
Potamogeton pectinatus occurring on larger areas around the openings after
the reconnection to the water dynamics of the Danube River and the occurrence
of Potamogeton nodosus reflect an improved water flow into the opened polder area.
The better water exchange was also documented by a decreasing salinity in the
northern polder area. However, applied merely during one vegetation period
following the restoration measures as element of success control, monitoring
documents only a first step towards an improvement and does not depict the long-term
evolution in the area.
Water macrophytes can be used as quality indicators of physical and
chemical parameters, for ater dynamics (circulation, exchange, velocity, sedimentation),
filtering capacity, nutrient content and salinity. The reaction of macrophytes to
changes following restoration measures can be used for the evaluation of restoration
successes.
The reconnection of abandoned agricultural polders areas of Babina and also of
Cernovca and the restoration of the wetlands functions were documented by the
recolonisation of water macrophytes and their communities with different indicator
values.
The repartition of the water macrophytes and their communities is obviously and
strongly interdependent with flow velocity, turbidity and nutrient input in the restored
areas.
Species characterised by a broad ecological amplitude such as for example
Potamogeton pectinatus are among the first re-settlers, so are free floating species,
species that enter in the area with the water flow. The diasporas of rooted
macrophytes that occurred in the first colonisation phase survived in the studied area’s
soil.
The shorter the area’s period as drained polder, the more rapidly the
restoration process of characteristic plant communities could occur. This can also
be documented in comparison with the two islands Babina and also Cernovca. The
species diversity grows rapidly over the first two years and stabilizes in the third and
forth year.
Rom. J. Aquat. Ecol. 1.1 (2011); E. Schneider - Aquatic macrophytes and restoration, pp. 45-62
60
Fig. 1 - Restoration area Popina fishponds (EC21 and EC22).
Romanian Journal of Aquatic Ecology 1.1 (2011)
61
The reed’s filtering function developed right from the start and became
clearly apparent with the occurrence of species such as for example Utricularia
vulgaris and Hydrocharis morsus ranae that develop small belts along the reed borders
in sites were the water is flowing into the channels after being filtered by the restored
reed. The growing abundance-dominance of these species provides evidence of a well
operating filter system. In particular the characteristic species of the Hydrocharition
alliance are quality indicators for an intact ecological status, i. e. clear, moderately
eutrophic or euthrophic-mezotrophic waters. Along the borders of canals showing this
type of vegetation they also serve as indicators of a good filtering capacity of the areas
reeds.
The decrease in salinity became evident with the parallel decrease of dominant
species such as Azolla filiculoides, Zannichellia palustris serving as indicators of a light
water salinity.
The first opening in the circular dam on the crossing point with the dam
between EC 21 and EC 22 in the Popina area has improved the ecological situation in
the polders but this was not enough to ensure the water circulation and exchange in the
area.
The site-specific biodiversity which is conditioned by the hydrological regime
can only be preserved in the long term by the maintenance of water circulation and water
exchange. For this reason the reactivation of the old water courses, i. e. the „gârla“ on
Babina, Cernovca and Popina islands, had a crucial effect on the area’s ecological
functioning.
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Author1 Erika SCHNEIDER-BINDER
[email protected], [email protected]
KIT-Karlruhe Institute of Technology -
Univerity of Land Baden-Württemberg and
Research Center of Helmholtz Society
Department WWF Auen-Institut,
Josefstrasse 1,
76437 Rastatt /Germany