ArticlePDF Available

Ecological assessment of different riverbank revitalisation measures to restore riparian vegetation in a highly modified river

Authors:

Abstract and Figures

Since anthropogenic activities have become concentrated along rivers, river regulations have strong-ly reduced the lateral connectivity by separating rivers from their floodplains. Consequently riparian habitat heterogeneity and the related species diversity are degrading, especially in highly modified prealpine rivers. Riverbank revitalisation measures aim at mitigating this degradation, but although river restoration projects have become widespread, little knowledge exists about their specific outcome, as standardised monitoring programs are missing. The aim of this study is to systematically compare vegetation change in response to three contrasting measures of bank diversification, i.e. embankment removal, sand input or gravel addition. Moreover, the influence of these measures on adjacent vegeta-tion is studied. Conclusions were drawn on the basis of three common goals of restoration projects: (i) improvement of vegetation structure, (ii) increase of species diversity, and (iii) characteristic species composition. The field work was done along River Inn northeast of Munich. Vegetation structure, species identity and cover as well as selected habitat variables were recorded in a stratified randomised sampling design; variation between measures was analysed using uni- and multivariate statistics. We detected great differences in the effect of the three measures two years after implementation. Embank-ment removal initiated highly dynamic habitats where plant establishment was difficult. The input of sand led to a rather homogenous species composition, at least partly because the habitats were produc-tive and therefore most likely will develop to tall reed stands or riparian forests. After gravel addition the restored sites remained relatively open, while riparian pioneer species could colonise. Vegetation structure and composition of adjacent reed stands were positively affected. The results indicate how restoration outcomes can vary depending on the specific measures chosen. This confirms the need for careful consideration of the pursued goals and site-specific conditions prior to implementation as well as long-term monitoring after implementation.
Content may be subject to copyright.
Tuexenia 35: xxx–xxx. Göttingen 2015.
doi: 10.14471/2015.35.005, available online at www.tuexenia.de
Ecological assessment of different riverbank revitalisation
measures to restore riparian vegetation in a highly
modified river
Ökologische Bewertung unterschiedlicher Uferstrukturierungsmaßnahmen
zur Renaturierung der Ufervegetation eines anthropogen geprägten Flusses
Katharina Strobl*, Anna-Lena Wurfer & Johannes Kollmann
Chair of Restoration Ecology, Technische Universität München, Emil-Ramann-Straße 6,
85354 Freising, Germany, katharina.strobl@tum.de; xxxxx@xxxx.de; jkollmann@wzw.tum.de
*Corresponding author
Abstract
Since anthropogenic activities have become concentrated along rivers, river regulations have strong-
ly reduced the lateral connectivity by separating rivers from their floodplains. Consequently riparian
habitat heterogeneity and the related species diversity are degrading, especially in highly modified
prealpine rivers. Riverbank revitalisation measures aim at mitigating this degradation, but although
river restoration projects have become widespread, little knowledge exists about their specific outcome,
as standardised monitoring programs are missing. The aim of this study is to systematically compare
vegetation change in response to three contrasting measures of bank diversification, i.e. embankment
removal, sand input or gravel addition. Moreover, the influence of these measures on adjacent vegeta-
tion is studied. Conclusions were drawn on the basis of three common goals of restoration projects: (i)
improvement of vegetation structure, (ii) increase of species diversity, and (iii) characteristic species
composition. The field work was done along River Inn northeast of Munich. Vegetation structure,
species identity and cover as well as selected habitat variables were recorded in a stratified randomised
sampling design; variation between measures was analysed using uni- and multivariate statistics. We
detected great differences in the effect of the three measures two years after implementation. Embank-
ment removal initiated highly dynamic habitats where plant establishment was difficult. The input of
sand led to a rather homogenous species composition, at least partly because the habitats were produc-
tive and therefore most likely will develop to tall reed stands or riparian forests. After gravel addition
the restored sites remained relatively open, while riparian pioneer species could colonise. Vegetation
structure and composition of adjacent reed stands were positively affected. The results indicate how
restoration outcomes can vary depending on the specific measures chosen. This confirms the need for
careful consideration of the pursued goals and site-specific conditions prior to implementation as well
as long-term monitoring after implementation.
Keywords: embankment removal, floodplain, gravel addition, monitoring, restoration, sand input
Erweiterte deutsche Zusammenfassung am Ende des Artikels
Manuscript received 26 November 2014, accepted 03 March 2015
Co-ordinating Editor: Norbert Hölzel
1
1. Introduction
River ecosystems are among the biologically most diverse ecosystems in the world
(WARD et al. 1999), and they provide important ecosystem services like flood mitigation,
nutrient exchange, drinking water supply and habitat provisioning (SCHOLZ et al. 2012). At
the same time river biodiversity and the associated ecosystem processes are negatively af-
fected (WARD et al. 1999), since anthropogenic activities have become concentrated in ripar-
ian zones (HABERSACK & PIÉGAY 2008). River regulations alter natural longitudinal and
lateral dynamics, which sustain high riverine habitat heterogeneity and species diversity
(WARD et al. 1999). Yet, as demonstrated by the Flood Pulse Concept (JUNK et al. 1989),
strong hydrological and ecological interconnections of rivers and their floodplains are the
basis for the functioning of riverine ecosystems.
Riparian habitats and communities are particularly affected by these changes, as rivers
and their floodplains have become separated by embankments and straightening (STAMMEL
et al. 2012). The riparian species richness generally decreases as habitat diversity gets lost
(WARD et al. 1999). Specialists like riparian pioneers are outcompeted by woody species
(KARRENBERG et al. 2002) or herbaceous perennials (ELLENBERG & LEUSCHNER 2010),
when connectivity and disturbance by floods are missing (TOCKNER et al. 1999). This often
results in a ‘single-channel’ morphology and straight bank lines with a dominance of monot-
onous tall reed stands dominated by herbaceous perennials, while there is a loss of diverse
open communities dominated by annual pioneers, which are the most threatened species in
floodplains (VON HEßBERG 2003).
In order to counteract these degradations, river restoration projects have increased expo-
nentially in the past years, including a large number of actions on riverbanks (BERNHARDT et
al. 2005). Nevertheless, although there is a large diversity of restoration measures, little is
known about their impact on flora, fauna and the surrounding landscape (BERNHARDT et al.
2005). This is mainly due to a lack of monitoring programs, which meet statistical and scien-
tific demands (CHAPMAN & UNDERWOOD 2000, BERNHARDT et al. 2005). Moreover, the
studies which fit scientific requirements focus mostly on the evaluation of the effectiveness
of single types of restoration measures in comparison to control sites (MÜLLER et al. 2014),
like removing bank fixation (JÄHNIG et al. 2009, JANUSCHKE et al. 2011), erosion control by
gravel addition (BARITEAU et al. 2013), or creation of new floodplain channels (SCHAICH et
al. 2010, STAMMEL et al. 2012). The publications, which compare the effects of different
types of restoration, focus mostly on aquatic organisms like fish and macroinvertebrates
(MÜLLER et al. 2014), or specific hydraulic aspects like the effect of embankment techniques
on biodiversity (CAVAILLÉ et al. 2013). In contrast, comparative studies take rarely into
account riparian vegetation, although it is a suitable indicator for restoration success (JÄHNIG
et al. 2009, JANUSCHKE et al. 2011). Plant species respond relatively fast to riverbank resto-
ration, due to effective dispersal or persistence in the soil seed bank (JÄHNIG et al. 2009), and
they are the first to indicate changes in abiotic conditions (ELLENBERG et al. 1992). As our
investigations as well as many monitoring programs are carried out only a few years after
restoration, riparian vegetation is a suitable indicator showing early developments.
Besides systematic comparative studies of contrasting types of restoration measures, it is
important to evaluate whether there are positive effects on adjacent vegetation and habitat
types. Even if some studies exist concerning the influence of land use on riparian forests
(cf. FERREIRA et al. 2005, FERNANDES et al. 2011), none of them deals with the specific
effects of restoration measures. However, such knowledge is of great practical relevance,
2
since it answers the question of possible positive effects of small-scale restoration measures
on larger areas. This is particularly important in highly modified rivers where space for
restoration measures is limited (DE NOOIJ et al. 2006).
The analysis of the restored communities often focuses on the presence of target species,
rare species or habitat specialists, and the absence of alien plants (HÖLZEL & OTTE 2001,
JÄHNIG et al. 2009, CAVAILLÉ et al. 2013, JANUSCHKE 2014). However, there is a problem
with defining target species in riparian vegetation, and a potential conflict between total
species diversity and presence of rare species, especially in ruderal sites of restored rivers.
Here we focus on the prealpine River Inn as suitable study system to better understand
the effects of contrasting measures that enhance natural dynamics and structural diversity of
riparian vegetation. The removal of embankment as well as the addition of gravel or sand
aim to (i) improve structural diversity, (ii) increase species diversity, and (iii) create a char-
acteristic species composition. The aim of our study is to compare these different revitalisa-
tion treatments (removal of embankment, sand input or gravel addition) by analysing vegeta-
tion change as indicator of restoration success. In addition, the influence of revitalisation
measures on adjacent vegetation types is investigated. We ask the following specific ques-
tions: 1) Is the removal of the embankment or sediment input better suited for increasing the
riparian diversity? 2) Does vegetation diversity (structure, small-scale variability, species
richness) in prealpine rivers respond differently when gravel or sand is added? 3) Can an
impact of the revitalisation measures be observed in adjacent vegetation?
2. Material and methods
2.1 Study area and revitalisation measures
The study area is located in the upper valley of the Bavarian Inn, ca. 60 km east from Munich, be-
tween the barrages Feldkirchen in the south (RW 4511890, HW 5313609, 440 m a. s. l.) and Gars in the
north (RW 4523404, HW 5335074, 412 m). The River Inn originates at about 2,500 m altitude in Swit-
zerland and flows into the Danube in Passau (300 m). Two thirds of its total length of 500 km is located
in the Alps resulting in a flow regime that is highly influenced by mountains.
In the study area, River Inn crosses the prealpine Inn-Chiemsee hilly region (Inn-Chiemsee-
Hügelland, MEYNEN et al. 1962), the end moraine and the Lower Inn Valley (Isar-Inn-Schotterplatten¸
MEYNEN et al. 1962). The studied river section is situated in the braided reach. It has a slope of
0.5-1.0‰ and its floodplain can be attributed to the group of (pre)alpine floodplains (gefällereiche
Flussaue der Alpen / Voralpen; KOENZEN et al. 2005). The natural substrate type of the river and its
floodplain is gravel (MEYNEN et al. 1962, KOENZEN 2005). According to ECKELMANN et al. (1996) this
grain fraction is round shaped and >2 mm. The mean discharge (1965–2012) is 221 m3 s-1 in winter and
490 m3 s-1 in summer in Wasserburg, which represents the centre of the investigated river section (LFU
2015). As many other European rivers the Inn is nowadays highly modified. A total of 24 barrages were
constructed; four of them located in the study area (Feldkirchen, Wasserburg, Teufelsbruck, Gars).
The barrages and other intensive hydro-engineering activities led to a loss of the natural river dy-
namics. The straightening caused a lowering of the riverbed and of the groundwater level (CONRAD-
BRAUNER 1994). Due to the construction of hydropower plants, the river carries almost no gravel
anymore, but mostly silt, sand and organic material (<2 mm; CONRAD-BRAUNER 1994). The mean
daily transport of suspended solid materials is 4.5 kg s-1. During flooding these fine sediments are
deposited along the riverbank, resulting in a strong reduction of floodplain dynamics, little turnover of
sand or gravel bars (CONRAD-BRAUNER 1994), and a disconnection between river and floodplain
(HABERSACK & PIÉGAY 2008).
3
In order to counteract these degradation processes, the revitalisation along River Inn aimed at im-
proving the ecological quality of the river and its floodplains as well as at increasing the natural dynam-
ics. Therefore, several restoration and revitalisation measures were carried out in 15 sites within a ca.
35 km long section of the river in winter 2012/13. For the purpose of this study only the riverbank
diversification measures were considered and solely their impact on riparian vegetation was studied.
They aimed at creating more diverse riparian habitats by adding or removing sediment. All sediments
originated from the study area to avoid introduction of non-native species and genotypes. In particular,
three measures can be distinguished: (i) embankment removal, (ii) sand input, or (iii) gravel addition.
i. Embankment removal consisted in the removal of constructed reinforcements or opening of natu-
rally fixed embankments by using excavators. The resulting open sites should facilitate subsequent
erosion. The substrate type favoured by this measure was mostly sand.
ii. Sand input was done in front of the bank lines. The sand originated from the digging of oxbow
lakes in the direct surroundings. It was deposited in form of piles of variable height (1.0–2.5 m) and
became eroded by river dynamics. The gravel cover in these sites was 0–10%.
iii. Gravel addition was also done in front of the straight or opened bank; the material was available
from local deposit. In most cases, gravel was introduced in form of flat groynes. The slope of these
sites is half as steep as the one of the two other measures. Gravel cover ranged from 70–100% in
these sites.
Three representative study sites were chosen for each of the three measure types. If more than three
sites were available, the choice was determined by accessibility. For the study of the adjacent vegeta-
tion types five locations were chosen, and reference sites were selected as a control for each of these
five sites. The references represent the regulated pre-restoration state and are located upstream from
each restored section. Thus, they are similar in terms of habitat conditions and exposed to similar dis-
turbance regimes, albeit without being affected by the restoration measure.
2.2 Study design and vegetation sampling
For the evaluation of floristic patterns, the survey was conducted on two spatial scales. On a small-
er scale, a map of riparian habitat types was obtained by studying aerial photographs of summer 2012.
As most of these pictures were taken prior to restoration, information was completed by more recent
pictures from GoogleEarth (GOOGLE INC. 2012) and verified in the field. Thus, homogenous structures
were delimited and assigned to three different categories. A predefined standard was established for the
mapping in order to prevent interpretation errors and to enable the reproducibility of the mapping:
Reed: herbaceous vegetation, which can be distinguished from shrubs by a different shade of green
and missing shadows;
Bare soil with pioneer vegetation: sparsely vegetated or vegetation free areas with clear characteris-
tics of exposed sediments;
We further distinguished between sand and gravel dominated bare soil habitats on aerial photo-
graphs if possible and verified it in the field.
On a larger scale, vegetation and abiotic variables were studied in the field using a stratified-
randomised sampling design. The different strata corresponded to the habitat types delineated on the
aerial photographs and described above. In each stratum five units were randomly selected at each
location. The randomisation was carried out in two steps for each stratum. Firstly the placement on the
longitudinal axis was randomly selected. Secondly the plot was again placed randomly on a transverse
line through the first selected point. In narrow vegetation stripes, the plots were located in the middle of
these strata, in order to avoid edge effects. The plot size was adapted to each habitat type in order to
meet the requirements of the minimum area (MÜLLER-DOMBOIS & ELLENBERG 1974). In reed zones
the plots measured 1.4 x 1.4 m, in pioneer vegetation 1.0 x 1.0 m.
We chose three locations for each measure type (embankment removal, addition of gravel, intro-
duction of sand) and five for reed and control plots, thus investigating 15 plots per measure type (3 x 5
plots) and 25 plots per treatment (5 x 5 plots). Thus, the study design resulted in a total of 95 sampling
plots.
4
The fieldwork was carried out between mid-June and early August 2014, when riparian vegetation
was most developed. The order of the study sites was random in order to compensate for phenological
differences between early and late sampling. Vegetation was recorded according to the BRAUN-
BLANQUET (1964) method, which was slightly modified to fit our purposes. The vegetation cover was
sampled instead of the abundance and number of individuals. The cover of each species, the proportion
of vegetation, moss, litter and bare ground were estimated, and the mean vegetation height was meas-
ured. Nomenclature of plant species followed BUTTLER & HAND (2008).
In addition, soil pH, distance to the riverbank and the slope of the riverbank were recorded. The pH
value of the soil was measured using pH-indicator strips following the protocol of ECKELMANN et al.
(1996). The slope of the riverbank was studied with a level instrument (Theis Tecomat 5/8’’); because
of the limited visibility, it could not be studied in reed zones. An orthogonal transect from the water-
front towards the plot until the forest or reed edge was established for each plot.
2.3 Conservation status and habitat specialism
Plants were identified as target species for pioneer vegetation or reed zones according to the classi-
fication of ELLENBERG et al. (1992). They were described as target species for pioneer vegetation on
bare soil habitats when attributed to one of the following phytosociological classes: Isoëto-Littorelletea
Br.-Bl. Et Vlieger in Vlieger 1937, Scheuchzerio-Caricetea nigrae xen 1937, Isoëto-Nanojuncetea
Br.-Bl. et Tx. ex Westhoff et al. 1946, Bidentetea tripartitae Tx. et al. ex von Rochow 1951 or Agrost-
ietea stoloniferae Oberdorfer et al. 1967 (= Polygono-Potentilletalia anserinae Tx. 1947).Species were
defined as target species for reed-zones when they were characteristic for the phytosociological class
Phragmito-Magnocaricetea Klika in Klika et Novák 1941, the orders Calystegietalia sepium Tx. ex
Moor 1958 or Molinietalia cearuleae W. Koch 1926 or the alliance Filipendulion ulmariae Segal ex
Lohmeyer in Oberd. et al. 1967. Species were called threatened when they were assigned to the catego-
ries 1, 2, 3 or V (V = likely to become endangered in the near future) in the Red List of Germany
(LUDWIG & SCHNITTLER 1996) or Bavaria (LFU 2003). Alien species were determined according to
the black list of invasive species (NEHRING et al. 2013), and the list of neophytes from the BFN (2014).
The definition of moisture indicating species was based on Ellenberg indicator values (ELLENBERG
et al. 1992). We calculated the median of the moisture value over all species to compare the average
moisture value of different vegetation units. In order to investigate whether the strategies of the riparian
vegetation differed between treatments, life-forms according to the classification of Raunkiaer
(MÜLLER-DOMBOIS & ELLENBERG 1974) were analysed. The amount of therophytes indicates the
disturbance regime, whereas the abundance of phanerophytes shows the regeneration of riparian forest.
2.4 Data analyses
Alpha-diversity was analysed directly via the number of species per plot as well as by the determi-
nation of the evenness index, in order to get information about the relative abundance of species. It was
calculated using the following equation:
=


where Hs is the alpha-diversity according to SHANNON (1948) and S is the total number of species.
Non-metric multidimensional scaling (NMDS) based on Bray-Curtis dissimilarities was computed
to visualise variation within and among types of measure. It aimed to investigate whether species com-
munities differ depending on the revitalisation measures. The appropriate number of dimensions was
determined by evaluating a scree plot choosing the number of axes, beyond which stress values do not
reduce considerably anymore (MCCUNE & GRACE 2002). Abiotic variables were subsequently overlaid
in the NMDS graph as explicating variables. Species used for emphasising results and statements could
clearly be assigned to one measure type on the ordination graphs. In order to test whether there are
significant differences in species composition PERMANOVA (permutational multivariate analysis of
variance; ANDERSON (2001) based on Bray-Curtis dissimilarities was applied.
5
Univariate statistics were investigated to test significant differences in the distribution of the
measures and to support the results of the multivariate analyses. The normality of the data and the
homogeneity of variances were tested using the Shapiro-Wilk test and the Levene test. In case of nor-
mality and homogeneity of variances a t-test was computed for pairwise comparisons and one-way
ANOVA for more than two variables (a posteriori Tukey-HSD). Yet the Mann-Whitney U test for
pairwise comparisons or the Kruskal-Wallis test (a posteriori Tamhane-T2) for multiple comparisons
was chosen if data were not normally distributed. Non-parametric Spearman-rank correlations (rho)
were calculated to test relations between different variables, since normality and homogeneity of vari-
ances could not be detected for all data.
The univariate statistics were carried out using the IBM SPSS Statistics 22 (IBM® 2013) software.
For multivariate analysis the statistical software program PCOrd (MCCUNE & MEFFORD 2011) was
used.
3. Results
3.1 Structural diversity
A total of 45 plots were analysed to compare the three types of riverbank revitalisation
measures: (i) embankment removal, (ii) sand input, and (iii) gravel addition. Vegetation
structure differed significantly between the three types of measure. The removal of the em-
bankment resulted in a significantly higher cover of bare soil (p < 0.001) in comparison to
sand input, whereas gravel addition showed intermediate values and no significant differ-
ences to the other types of measure. Vegetation cover and height were significantly lower on
plots with gravel than on those with sand (Fig. 1; p < 0.01, p < 0.001) and intermediate on
embankment removal. These results were also supported by the negative correlation of grav-
el cover with vegetation height (rho = -0.68, p < 0.01) and vegetation cover (rho = -0.64,
p < 0.01), as well as the positive correlation with the cover of bare soil (rho = 0.74,
p < 0.01).
3.2 Species diversity
In total 117 plant species were recorded. The median of the species number per plot after
embankment removal was 9 compared to 13 on sand and 10 on gravel. The species number
was significantly lower, when the embankment was removed than when sandy sediment was
added (Fig. 2; p < 0.05), even if the calculation of the evenness showed no significant differ-
ences between the three types of measure (p > 0.05). Both diversity indicators showed a
higher variance of values for the sites restored by embankment removal, while the other two
measures were more homogenous.
3.3 Species composition
The NMDS ordination showed clear differences in the species composition of the three
types of measure (Fig. 3) and PERMANOVA revealed that these differences are significant
(F = 3.80, p < 0.01). The NMDS ordination showed a clear distinction between sand and
gravel addition plots, where the species composition was mostly homogenous. However, the
plots recorded after removal of the embankment largely overlapped with the other two stud-
ied riverbank revitalisation measures. Their species composition was more variable.
6
Fig. 1. Comparison of vegetation cover (left) and vegetation height (right) for the three different types
of measure: embankment removal (black), sand input (dark grey) and gravel addition (light grey).
Gravel cover ranged 70–100% on sites with gravel addition, while it was between 010% on sites with
sand input and between 0–5% on sites with embankment removal. Different letters indicate significant
differences (p < 0.05; median; box, 25–75%; whiskers, min–max).
Abb. 1. Vergleich der Vegetationsdeckung (links) und der Vegetationshöhe (rechts) der drei Maßnah-
mentypen (vlnr): Uferanbruch (schwarz), Sandzugabe (dunkelgrau) und Kieszugabe (hellgrau). Die
Kiesdeckung betrug 70–100 % auf Flächen mit Kieszugabe, 0–10 % auf Flächen mit Sandzugabe und
0-5 % nach Uferanbruch. Unterschiedliche Buchstaben verweisen auf signifikante Unterschiede
(p < 0,05; Median; Box: 25–75 %; Whisker: Min–Max).
Fig. 2. Comparison of species number (left) and evenness (right) for the three different types of meas-
ure: embankment removal (black), sand input (dark grey) and gravel addition (light grey). Different
letters indicate significant differences (p < 0.05).
Abb. 2. Vergleich der Artenzahl (links) und des Evenness Index (rechts) der Maßnahmentypen Uferan-
bruch (schwarz), Sandzugabe (dunkelgrau) und Kieszugabe (hellgrau). Unterschiedliche Buchstaben
verweisen auf signifikante Unterschiede (p < 0,05).
7
Fig. 3. NMDS ordination based on Bray-Curtis dissimilarity for the comparison of species composition
of 15 plots sampled on three sites with embankment removal (grey crosses), 15 plots sampled on three
sites with sand input (grey circles) and 15 plots sampled on three sites with gravel addition (black
quadrats). It is based on the cover of 117 plant species and is visualised as a joint plot with environmen-
tal gradients represented as black vector lines (cutoff = 0.15; stress based on two dimensions: 0.18;
Monte-Carlo: p < 0.001). The vector lines of ‘vegetation height’ and ‘median moisture value’ as well as
‘distance to riverbank’ and ‘cover alien species’ overlap.
Abb. 3. NMDS Ordination basierend auf Bray-Curtis Unähnlichkeiten. Es wird die Artenzusammen-
setzung von je 15 Plots und je drei Standorten nach Uferanbruch (dunkelgraue Kreuze) nach
Sandzugabe (schwarze Kreise) und nach Kieszugabe (hellgraue Quadrate) verglichen. Die Ordination
basiert auf der Deckung von 117 Pflanzenarten und ist als ‚Joint Plot’ dargestellt, zusammen mit
Umweltgradienten, die hier als schwarze Vektorlinien angezeigt werden (cutoff = 0,15). Stresswert
basierend auf zwei Dimensionen: 0,18; Monte-Carlo: p < 0,001. Die Vektorlinien ‚Vegetationshöhe‘
und ‚Median Feuchtewert‘ sowie ‚Abstand zum Ufer‘ und ‚Deckung Neophyten‘ überschneiden sich.
Besides the variable heterogeneity, the three treatments could be distinguished by differ-
ent plant species. There was a significantly higher cover of therophyte species like Ara-
bidopsis arenosa, Arenaria serpyllifolia and Herniaria glabra on sites, where gravel was
added, compared to sites, where sand was added (p < 0.05). In addition, typical riparian plant
species like Clematis vitalba, Humulus lupulus and Solanum dulcamara were recorded on
sites with gravel addition (Fig. 4). Univariate statistics showed no significant difference in
the amount of pioneer target species (p > 0.05). On the NMDS graph (Fig. 4) all species
classified as target species for pioneer habitats were found in the centre of the graph on plots
with gravel and sand input. Sites after restoration by sand input were characterised by the
presence of pioneer species like Alopecurus aequalis, Isolepis setacea and Juncus inflexus
and those after gravel addition by species like Carex hirta, Juncus articulatus and Rumex
obtusifolius.
8
Fig. 4. NMDS ordination based on Bray-Curtis dissimilarity for the comparison of species composition
of 15 plots sampled on three sites with embankment removal (grey crosses), 15 plots sampled on three
sites with sand input (grey circles) and 15 plots sampled on three sites with gravel addition (black
quadrats). It is based on the cover of 117 plant species (stress based on two dimensions: 0.18; Monte-
Carlo: p < 0.001).
Abb. 4. NMDS Ordination basierend auf Bray-Curtis Unähnlichkeiten. Es wird die Artenzusammenset-
zung von je 15 Plots und je drei Standorten nach Uferanbruch (dunkelgraue Kreuze) nach Sandzugabe
(schwarze Kreise) und nach Kieszugabe (hellgraue Quadrate) verglichen. Die Ordination basiert auf der
Deckung von 117 Pflanzenarten. Stresswert basierend auf zwei Dimensionen: 0,18; Monte-Carlo:
p < 0,001.
Abbreviations: Acerpseu: Acer pseudoplatanus; Achimill: Achillea millefollium agg.; Alnuglut: Alnus glutinosa; Alnuinca: Alnus incana;
Alopaequ: Alopecurus aequalis; Arabaren: Arabidopsis arenosa; Arenserp: Arenaria serpyllifolia; Barbstri: Barbarea stricta; Beruerec: Berula
erecta; Betupend: Betula pendula; Bromerec: Bromus erectus; Calaepi g: Calamagrostis epigejos; Calapseu: Calamagrostis pseudophragmites;
Cardimpa: Cardamine impatiens; Cardpers: Carduus personata; Careelat: Carex el ata; Careflac: Carex flacca; Carehirt: Carex hirta; Carenigr:
Carex nigra; Careotru: Carex otrubae; Carepseu: Carex pseudocyperus; Centeryt: Centaurium erythraea; Chaeminu: Chaenorhinum minus;
Cirsarve: Cirsium arvense; Cirsoler: Cirsium oleraceum; Cirspalu: Cirsium palustre; Clemvita: Clematis vitalba; Conycana: Conyza canadensis;
Dactglom: Dactylis glomerata; Desccesp: Deschampsia cespitosa agg.; Echicrus: Echinochloa crus-galli; Eleopalu: Eleochari s palustris; Epilhirs:
Epilobium hirsutum; Epilparv: Epilobium parviflorum; Epiltetr: Epilobium tetragonum; Eq uiarve: Equisetum arvense; Equihyem: Equisetum
hyemale; Equipalu: Equisetum palustre; Erigacri: Erigeron acris; Erigannu: Erigeron annuus; Festrubr: Festuca rubra agg.; Filiulma: Filipendula
ulmaria; Fragvesc: Fragaria vesca; Galianis: Galium anisophyllon; Galimoll: Galium mollugo agg.; Gerarobe: Geranium robertianum; Hedeheli:
Hedera helix; Hernglab: Herniaria glabra; Hierpilo: Hieracium pilosella; Hierpilo: Hieracium piloselloides; Hippvulg: Hippuris vulgaris;
Humulupu: Humulus lupulus; Hypemacu: Hypericum maculatum; Hypeperf: Hypericum perforatum; Impaglan: Impatiens glandulifera; Isolseta:
Isolepis setacea; Juncarti: Juncus articulatus; Juncbulb: Juncus bulbosus; Junceffu: Juncus effusus; Juncinfl: Juncus inflexus; Junctenu: Jun cus
tenuis; Lycoeuro: Lycopus europaeus; Lythsali: Lythrum salicaria; Medilupu: Medicago lupulina; Melioffi: Melilotus officinalis; Mentaqua:
Mentha aquatica; Myosaqua: Myosoton aquaticum; Phalarun: Phalaris arundinacea; Phraaust: Phragmites australis; Planmajo: Plantago major
subsp. major; Poaannu: Poa annua; Poapalu: Poa palustris; Poaprat: Poa pratensis; Poatriv: Poa trivialis s. l.; Popunigr: Populus nigra; Poteanse:
Potentilla anserina; Poteerec: Potentilla erecta; Poteneum: Potentilla neumanniana; Prunvulg: Prunella vulgaris; Ranuacri: Ranunculus acris;
Ranurepe: Ranunculus repens; Reselute: Reseda lutea; Rhinglac: Rhinanthus glacialis; Roripalu: Rorippa palustris; Rubucaes: Rubus caesius;
Rumeobtu: Rumex obtusifolius; Saginodo: Sagina nodosal; Sagiproc: Sagina procumbens; Salialba: Salix alba; Saliauri: Salix aurita; Salicapr:
Salix caprea; Salicine: Salix cinerea s. l.; Salimyrs: Salix myrsinifolia; Salipurp: Salix purpurea; Salirube: Salix rubens; Salivimi: Salix viminalis;
Scronodo: Scrophularia nodosa; Scroumbr: Scrophularia umbrosa; Scutgale: Scutellaria galericulata; Seneaqua: Senecio aquaticus s. str.;
Silepalu: Silene palustris/ latifolia; Soladulc: Solanum dulcamara; Soncaspe: Sonchus asper; Sympoffi: Symphytum officinale s. str.; Taraoffi:
Taraxacum officinale agg.; Trifprat: Trifolium pratense; Tripmari: Tripleurospermum maritimum agg.; Tussfarf: Tussilago farfara; Typhlati:
Typha latifolia; Urtidioi: Urtica dioica s. l.; Verbdens: Verbascum densiflorum; Verbnigr: Verbascum nigrum; Verbthap: Verbascum thapsus;
Veroarve: Veronica arvensis; Verobecc: Veronica beccabunga; Verocate: Veronica catenata; Vicicrac: Vicia cracca s. str.
9
Plots with sand addition showed a significant higher median of moisture value than plots
with gravel input, revealing more moisture indicating species (p < 0.001). This result is
supported by the clear gradient in direction of ‘sand plots’ in the ordination graph (Fig. 3).
Furthermore, the amount of target species for reed stands was significantly higher on these
sites (p < 0.001) in comparison to the other measures. The NMDS ordination (Fig. 4)
showed that those are species like Carex elata, Lythrum salicaria and Phragmites australis.
None of the studied species groups could be exclusively attributed to the heterogeneous plots
after embankment removal. Thus, they were characterized by a significantly lower amount
of phanerophytes (p < 0.05).
There were no significant differences in univariate statistics in regard to the amount of
alien species (p > 0.05). Yet, the NMDS (Fig. 3) showed a distinct gradient of the cover of
alien species in the direction of two ‘gravel plots’ outlying the cluster. These two plots had a
comparatively higher cover (10 and 15%) of Impatiens glandulifera in proportion to their
main vascular plant cover (10 and 20% total cover).
3.4 Effect of restored riverbanks on adjacent reed stands
In order to detect the effects of structural bank diversification measures, 25 plots close to
restored riverbanks were compared to 25 plots in monotonous reed stands of regulated areas.
Although no significant differences in structural parameters could be found, there were
significant differences in species diversity. The species number per plot in restored areas had
a median of seven, which is significantly higher than in non-restored areas (four spp.;
p < 0.001). The evenness also revealed a significant higher diversity in restored areas
(p < 0.001).
In addition to differences in the species diversity, species composition varied significant-
ly between impact and control sites (PERMANOVA: F = 5.98, p < 0.001). The restored
areas were characterised by a significantly higher number of endangered species (p < 0.01)
and target species for reed stands (p < 0.01) like Carex elata, Equisetum palustre, Poa palus-
tris and Valeriana officinalis (Fig. 5). Although alien species (Conyza canadensis, Erigeron
annuus, Impatiens glandulifera) were found on both restored and unrestored sites, the cover
of alien plants was significantly higher on the control site (p < 0.05).
4. Discussion
4.1 Structural diversity
Our results showed that the removal of embankments and the addition of gravel are suit-
able measures to create open, sparsely vegetated areas. Our data revealed a lower vegetation
cover and height on these sites compared to those with addition of sand. It can be supposed
that these bare soil zones cannot be sustained on sites with sand input in absence of regular
natural disturbance or management. A high cover of reed species on these sites indicates fast
succession. This can have two explanations: Firstly, the sand used for creating the artificial
bank originated from the floodplain, so it can be suggested that it is nutrient-rich (FRIESE et
al. 2000) inducing high productivity. Secondly, the sand contains seeds that get activated
during disturbance (cf. HÖLZEL & OTTE 2001); these processes lead to dense and high vege-
tation cover, which is not suitable for riparian pioneer species.
10
Fig. 5. NMDS ordination based on Bray-Curtis dissimilarity for the comparison of species composition
of 25 plots sampled on five sites close to restored sites (black diamonds) and 25 plots sampled on five
non-restored control sites (grey triangles). It is based on the cover of 55 plant species and is visualised
as a joint plot with environmental gradients represented as red vector lines (cutoff = 0.15; stress
based on three dimensions: 0.10; Monte-Carlo: p < 0.05).
Abb. 5. NMDS Ordination basierend auf Bray-Curtis Unnähnlichkeiten. Es wird die Artenzusammen-
setzung von 25 Plots von fünf Standorten im direkten Umgriff der Renaturierungsmaßnahmen
(schwarze Rauten) verglichen mit 25 Kontrollflächen von fünf Standorten nicht-renaturierter
Flussabschnitte (graue Dreiecke). Die Ordination basiert auf der Deckung von 55 Pflanzenarten und
wird als ‚Joint Plot’ dargestellt, zusammen mit Umweltgradienten, die hier als rote Vektorlinien
angezeigt werden (cutoff = 0,15; Stresswert basierend auf drei Dimensionen: 0,10; Monte-Carlo:
p < 0,05).
11
Two years after restoration, the highly productive and dominant species can only hardly
settle under the circumstances created by gravel addition or embankment removal. The re-
moval of embankment structures leads to the development of instable banks with a dynamic
bare soil surface. It can be assumed that in general plant establishment is difficult due to
these sediment dynamics (WARD et al. 1999). This is shown by the significantly lower
amount of phanerophytes on these sites, for example. Though, even if in terms of habitat
creation these sites provide open spaces, it appears to be less suited for the development of
riparian vegetation.
Gravel introduction represents an intermediate situation with moderate species estab-
lishment leading to environmental conditions suitable for early-successional species, i.e.
nutrient-poor conditions, occasional inundation and frequent drought (VON HEßBERG 2003,
ELLENBERG & LEUSCHNER 2010). Thus, it increases the structural diversification in preal-
pine rivers by the establishment of another more open habitat type. Since gravel bars have
largely disappeared in the past decades, structural restoration measures should focus on their
reestablishment.
While considerable achievements could be obtained directly on measure sites for the
open structure, none of the studied measures revealed significant structural changes in the
adjacent reed zones. Nonetheless, this was not expected, because reed zones are naturally
characterised by a high and homogenous vegetation cover and height (ELLENBERG &
LEUSCHNER 2010). This implicates, that structural parameters are not a suitable indicator for
the monitoring of restoration impacts in these areas.
4.2 Species diversity
The results of our study indicated that sand and gravel input are more suitable measures
for an increase of species diversity than embankment removal. These results are following
the conclusions of JÄHNIG et al. (2009), who found out that gravel bars and loamy habitats
greatly increased species richness. Plots with embankment removal differ greatly in terms of
species diversity compared to the two other treatments. The reason for this might be the
difficult abiotic conditions only few species can deal with.
Concerning the regional diversity, ROSENZWEIG (1995) remarked a positive correlation
between the biotic diversity and habitat heterogeneity. As our results revealed very different
species compositions depending on the measures, we suggest that each measure leads to
another habitat type. In this case, implementing different revitalisation measures can increase
β-diversity. These findings follow the statements of WARD et al. (1999), who noticed that
regional diversity not only depends on the number of species per habitat, but also on the
number of habitats and the turnover between habitats. Compared to gravel input and em-
bankment removal the species composition of sand input is rather homogenous. Therefore, if
the creation of different habitats is defined as a goal and only one type of measure is imple-
mented, the input of sand cannot be recommended. To sum up, sand and gravel input are
most suitable for the enhancement of local species diversity, whereas the embankment re-
moval is more likely to increase the habitat diversity due to more heterogeneous species
compositions on these sites.
Furthermore, the results of this study showed that the implementation of structural diver-
sification measures enhances the species diversity of direct measure sites, but also the one of
the adjacent reed zones. Like JANUSCHKE et al. (2011) we recorded an increased α-diversity
in reed zones close to restoration sites in comparison to control sites. This could indicate
positive restoration effects by an easier colonisation due to a shorter distance to a diverse
12
species pool in restored areas (KAREIVA 1990). Nonetheless, this assumption cannot be ex-
clusively confirmed. Sites for revitalisation measures may have been chosen according to an
existing good conservation potential, whereas the control sites are situated upstream to the
revitalisation measures outside those better-preserved areas. Furthermore, the sites could
have been affected by disturbances during the implementation works and therefore support a
higher diversity. Intermediate disturbance events lead to a temporarily increase in species
diversity, because they create open spaces where other species can colonise, corresponding
to the well-known Intermediate Disturbance Hypothesis (CONNELL 1978).
4.3 Species composition
In our study, species composition greatly differs between all treatments as a result of a
successful creation of different habitat conditions. Moreover, our results showed that differ-
ent types of measures promote different species. The introduction of gravel leads to the
development of riparian pioneer species (therophytes and pioneer target species) shortly after
restoration. These results support the findings of JÄHNIG et al. (2009), who also described
that short-living taxa on gravel bars benefit from floodplain restoration. In floodplains,
where natural sediment deposition patterns are missing, gravel addition is an efficient means
to create open spaces that are suitable for many riparian species (RICHARDSON et al. 2007)
Nonetheless, the vegetation composition after gravel input can vary considerably. In our
results two plots differed greatly from the others due to a particularly high cover of Impati-
ens glandulifera. This may be problematic as invasive species can affect native species
communities if they reach high abundances (RICHARDSON et al. 2007), though HEJDA
& PEK (2006) argued that I. glandulifera does not considerably affect native species; it
merely influences the proportional cover of other dominant species like Urtica dioica. Ac-
cording to this assumption, the occurrence of I. glandulifera could be neglected and thus
rather be seen as one component of a partially new system (RICHARDSON et al. 2007).
Compared to the gravel introduction and embankment removal the input of sand was
more homogenous. Over all studied plots, the species composition was quite similar with
few outliers. In comparison with embankment removal, the level of disturbance was lower
due to more gentle slopes on these plots. Moisture indicating plants as well as pioneer spe-
cies cover was increased on these plots. HÖLZEL & OTTE (2001) suggested that riparian
species increase after seed bank mobilisation due to sediment relocation. Nonetheless, as we
also recorded a high number of phanerophytes and reed species, the succession of these sites
cannot be predicted two years after restoration. In the absence of sediment relocating floods,
some of these sites will develop into riparian forest or into reed stands. The fine sediment
with a high capacity of water retention provides good conditions for germination of riparian
tree species (KARRENBERG et al. 2002), at least when the abundance of competitive herbs is
low. Otherwise, the sites are more likely to support reed stands in the near future, especially
when competitive reed species are found in the direct surroundings. The measure of em-
bankment removal leads to a highly variable species composition. It increases dynamics,
which causes a high variability of habitats and species. Nonetheless, our results also indicate
that this measure is not suitable, if quick establishment of riparian pioneer species or the
development of riparian forest is aimed.
The species composition in the surroundings of restored river sections is positively af-
fected by revitalisation measures. Our results show a higher conservation value in these
areas, which is indicated by a higher amount of endangered species and target species for
reed stands on these plots. This observation can be due to a different species pool in the seed
13
bank or the immediate surroundings of restored and degraded river sections (HÖLZEL
& OTTE (2001). It could also be due to the reflection of methodological problems in the
sampling design. Indeed, plots may differ in other factors than restoration impact when using
a time for space substitution design. Indeed, HEJDA & PYŠEK (2006) discussed similar pat-
terns with the same kind of spatial design.
Finally, one must note, that our results represent only are a ‘snap shot’ of the restoration
state two years after measure implementation. After some years, the conservation value of
sites in the surrounding of restored river sections may diminish again. Sites after embank-
ment removal might flatten, facilitating species establishment on less dynamic habitats.
Succession towards dominant reed stands, indicated by the presence of Phalaris arundina-
cea and Phragmites australis, may also be observed on the now more open sites after gravel
input and embankment removal, as natural disturbances are missing in highly modified
rivers like the Inn. Though, fluvial dynamics are crucial for the maintenance of different
successional stages enhancing the overall species diversity (WARD et al. 1999). Therefore,
JANUSCHKE (2014) argues that a monitoring should not only evaluate, whether the desired
habitat types and species are initially present, but also verify, if they are maintained after a
longer time period. If then undesired vegetation change is observed, adaptive restoration
measures or management have to be considered.
4.4 Perspectives and implications for management
The three studied types of revitalisation measures for riverbank diversification greatly
differ in their development since implementation. For future projects, this means that differ-
ent measures should be accomplished according to the predefined goals. Gravel introduction
leads to open habitat structures where riparian pioneer species can establish. Due to high
nutrient levels and suitable moisture conditions the input of sand causes a comparatively fast
succession into either desirable riparian forest or monotonous reed stands. The removal of
embankment leads to the creation of highly dynamic habitats. This may be difficult for
plants, but can benefit reptiles, ground beetles or kingfishers.
In our study we showed that rare species, pioneer target species and other desirable ripar-
ian plants increase with the creation of open soil areas, which nowadays are also the most
threatened habitats in floodplains (VON HEßBERG 2003). Therefore, management efforts need
to guarantee the conservation of these early successional sites, as there is a lack of dynamics
in highly modified rivers. Our results show that succession is particularly fast on fine sedi-
ments, whereas restored gravel bars or reopened embankment are slower in succession and
can therefore be considered more sustainable. Possible management strategies to counteract
succession are soil-disturbance and biomass reduction, initiated for instance by grazing
(SCHAICH et al. 2010). As outcomes vary considerably depending on the type of measure,
our results emphasise how important careful planning, evaluation of site-specific conditions
and post-implementation monitoring and management can be.
Erweiterte deutsche Zusammenfassung
Einleitung Fließgewässer und ihre Auen gehören zu den artenreichsten Ökosystemen der Welt
(WARD et al. 1999). Mit der Intensivierung der anthropogenen Nutzung in Flussauen wurden Flüsse
zunehmend verbaut und ihre Gewässerstruktur sowie die natürliche Fließgewässerdynamik beeinträch-
tigt (HABERSACK & PIÉGAY 2008). Dabei sind das Auftreten regelmäßiger Störungen und eine intakte
laterale Konnektivität notwendig für den Artenreichtum der Aue (WARD et al. 1999). Besonders in den
14
stark verbauten Voralpenflüssen wird die Revitalisierung im Sinne einer Strukturverbesserung zur
Dynamisierung der Auen zu einer dringenden Notwendigkeit. Eine Studie von BERNHARDT et al.
(2005) belegt eine starke Zunahme von Renaturierungsprojekten an Flüssen. Standardisierte, langjähri-
ge Monitoringprogramme sind dabei bisher selten (CHAPMAN & UNDERWOOD 2000), aber unbedingt
nötig, um den Erfolg der Maßnahmen bewerten und zukünftige Projekte zielgerichteter durchführen zu
können. Ziel dieser Arbeit ist ein systematischer Vergleich unterschiedlicher Uferstrukturierungsmaß-
nahmen und die Untersuchung des Einflusses dieser Maßnahmen auf die Vegetation. Die abschließende
Bewertung erfolgte anhand von drei in Renaturierungsprojekten häufig verfolgten Zielen: (1) Verbesse-
rung der Vegetationsstruktur, (2) Erhöhung der Artenvielfalt und (3) charakteristische Artenzusammen-
setzung.
Material und Methoden Das Untersuchungsgebiet liegt an einem stark anthropogen überprägten
Fluss des bayerischen Voralpenlandes, dem Inn südlich und nördlich von Wasserburg. Dort wurden mit
dem Ziel der Dynamisierung des Flusses die Ufer umstrukturiert. Die durchgeführten Maßnahmen
lassen sich in drei Gruppen einteilen: Uferanbruch (Entsteinung, Aufbrechen), Kies- und Sandzugabe.
In einem stratifiziert-randomisierten Aufnahmedesign wurden gezielt die Vegetationsstruktur, die
Deckung der Arten und ausgewählte abiotische Größen (pH-Wert, Uferentfernung, Uferneigung) erho-
ben. Als Straten dienten die vorgefundenen Strukturtypen ‚Röhricht‘ und ‚Pionierfluren‘. Die Daten-
auswertung erfolgte anhand uni- und multivariater Analysen.
Ergebnisse Alle drei Maßnahmentypen unterschieden sich bezüglich der Vegetationsstruktur. Die
Rohbodendeckung war maximal nach Revitalisierung durch Uferanbruch. Die Vegetationshöhe und -
deckung am Flussufer waren am höchsten nach Zugabe von Sand. Die Probeflächen mit Uferanbruch
wiesen eine starke Streuung der Artenzahl auf, und auch die Diversität der angrenzenden Röhrichte war
erhöht. Alle drei Maßnahmen unterscheiden sich deutlich in ihrer Artenzusammensetzung, wobei erneut
die Maßnahme des Uferanbruchs eine sehr heterogene Entwicklung bewirkte. An Renaturierungsflä-
chen angrenzende Röhrichte zeigten eine veränderte Artenzusammensetzung im Vergleich mit Kon-
trollflächen.
Diskussion Zwei Jahre nach der Durchführung führten die drei untersuchten Maßnahmen zu gro-
ßen Unterschieden in der Vegetationsentwicklung. Durch die Entfernung der Uferbefestigung entstehen
dynamische Habitate, auf denen sich nur wenige Pflanzen etablieren. Wie auch in der Studie von JÄH-
NIG et al. (2009) führt die Kieszugabe zu einer vergleichsweise offenen Vegetationsstruktur, in der sich
auentypische Pionierarten ansiedeln. Auf Sandflächen stellt sich eine homogene Artenzusammenset-
zung ein; diese lässt sich zumindest teilweise durch die hohe Produktivität der Standorte erklären, die
sich vermutlich entweder in Richtung Röhricht (FRIESE et al. 2000) oder Auwald (KARRENBERG et al.
2002) entwickeln werden, jedenfalls wenn Störungsereignisse ausbleiben. Die beobachteten Entwick-
lungen zeigen die kurzfristige Reaktion der Auepflanzen auf die Uferstrukturierungsmaßnahmen. Für
eine abschließende Beurteilung der Wirksamkeit der Maßnahmen ist jedoch ein längerfristiges Monito-
ring nötig (JANUSCHKE 2014). Wenn die natürliche Dynamik des Flusses nicht ausreicht, müsste über
geeignete Managementstrategien zur Offenhaltung von Pionierstandorten nachgedacht werden.
Perspektiven für die Renaturierung Die Ergebnisse zeigen, wie unterschiedlich die Wirkungen
einzelner Renaturierungsmaßnahmen sein können. Dies unterstreicht, wie wichtig es ist, vor den Maß-
nahmen abzuwägen, welche Renaturierungsziele unter den gegebenen lokalen Bedingungen verfolgt
werden sollen. Nach Maßnahmendurchführung ist ein Langzeitmonitoring wünschenswert.
15
Acknowledgements
We are grateful to VERBUND Innkraftwerke GmbH and in particular Georg Loy for financial support,
insights into important data, access to the study sites and local support. We thank the landscape plan-
ning consultancies Dr. H. M. Schober (Gesellschaft für Landschaftsarchitektur mbH) and Aquasoli
Ingenieurbüro for providing information about the study site, and Dr. Melanie Müller (TU München,
Chair of Aquatic Systems Biology) for the cooperation, concerning the selection of study sites.
Supplements - im Text fehlt der Verweis???
Additional supporting information may be found in the online version of this article.
Zusätzliche unterstützende Information ist in der Online-Version dieses Artikels zu finden.
Supplement E1. List of species and frequency of occurrence on all surveyed plots.
Anhang E1. Artenliste und Frequenz des Vorkommens auf allen aufgenommenen Flächen.
References
ANDERSON, M.J. (2001): A new method for non-parametric multivariate analysis of variance. Austr.
Ecol. 26: 32–46.
BARITEAU, L., BOUCHARD, D., GAHNON, G., LEVASSEUR, M., LAPOINTE, S. & BÉRUBÉ, M. (2013): A
riverbank erosion control method with environmental value. – Ecol. Eng. 58: 384–392.
BERNHARDT, E.S., PALMER, M.A., ALLAN, J.D., ALEXANDER, G., BARNAS, K., BROOKS, S., CARR, J.,
CLAYTON, S., DAHM, C., FOLLSTAD-SHAH, J., GALAT, D., GLOSS, S., GOODWIN, P., HART, D.,
HASSETT, B., JENKINSON, R., KATZ, S., KONDOLF, G.M., LAKE, P.S., LAVE, R., MEYER, J.L.,
O’DONNELL, T.K., PAGANO, L., POWELL, B. & SUDDUTH, E.B. (2005): Synthesizing U.S. river res-
toration efforts. – Science 308 (5722): 636–637.
BFN = BUNDESAMT FÜR NATURSCHUTZ (2014): FloraWeb. Neophyten und Kulturpflanzen. URL:
http://www.floraweb.de/pflanzenarten/neophyten.html [accessed 2014–09–19].
BRAUN-BLANQUET, J. (1964): Pflanzensoziologie, Grundzüge der Vegetationskunde. 3. Aufl. – Sprin-
ger, Wien: 365 pp.
BUTTLER, K.P. & HAND, R. (2008): Liste der Gefäßpflanzen Deutschlands. – Kochia Beih. 2: 1–107.
CAVAILLÉ, P., DOMMANGET, F., DAUMERGUE, N., LOUCOUGARAY, G., SPIEGELBERGER, T., TABAC-
CHI, E. & EVETTE, A. (2013): Biodiversity assessment following a naturality gradient of riverbank
protection structures in French prealps rivers. – Ecol. Eng. 53: 23–30.
CHAPMAN, M.G. & UNDERWOOD, A.J. (2000): The need for a practical scientific protocol to measure
successful restoration. – Wetlands 19: 28–49.
CONNELL, J.H. (1978): Diversity in tropical rainforests and coral reefs. Sci. Total Environ.
199: 1302–1310.
CONRAD-BRAUNER, M. (1994): Naturnahe Vegetation im Naturschutzgebiet "Unterer Inn" und seiner
Umgebung. Eine vegetationskundlich-ökologische Studie zu den Folgen des Staustufenbaus. Bay-
erische Akademie für Naturschutz und Landschaftspflege: 175 pp.
DE NOOIJ, R.J.W., VERBERK, W.C.E.P., LENDERS, H.J.R., LEUVEN, R.S.E.W. & NIENHUIS, P.H.
(2006): The importance of hydrodynamics for protected and endangered biodiversity of lowland riv-
ers. Hydrobiologia 187: 153–162.
ECKELMANN, W., SPONAGEL, H., GROTTENTHALER, W., HARTMANN, K.-J., HARTWICH, R., JANETZKO,
P., JOISTEN, H., KÜHN, D., SABEL, K.-J. & TRAIDL, R. (1996): Bodenkundliche Kartieranleitung. Mit
103 Tabellen. 5. Aufl. Schweizerbart, Stuttgart: 438 pp.
ELLENBERG, H. & LEUSCHNER, C. (2010): Vegetation Mitteleuropas mit den Alpen in ökologischer,
dynamischer und historischer Sicht. 6. Aufl. Ulmer, Stuttgart: 1333 pp.
ELLENBERG, H., WEBER, H., DÜLL, R., WIRTH, V., WERNER, W. & PAULIßEN, D. (1992): Zeigerwerte
von Pflanzen in Mitteleuropa. Scr. Geobot. 18: 1–248.
16
FERNANDES, M.R., AGUIAR, F.C. & FERREIRA, M.T. (2011): Assessing riparian vegetation structure
and the influence of land use using landscape metrics and geostatistical tools. – Landsc. Urban Plan.
99: 166–177.
FERREIRA, M.T., AGUIAR, F.C. & NOGUEIRA, C. (2005): Changes in riparian woods over space and
time: Influence of environment and land use. – Forest Ecol. Manag. 212: 145–159.
FRIESE, K., WITTER, B., MIEHLICH, G. & RODE, M. (Ed.) (2000): Stoffhaushalt von Auenökosystemen.
Böden und Hydrologie, Schadstoffe, Bewertungen. Springer, Berlin: 434 pp.
GOOGLE INC. (2012): Google Earth. Version 6.2.2.6613.
HABERSACK, H. & PIÉGAY, H. (2008): 27 - River restoration in the Alps and their surroundings: past
experience and future challenges. In: HABERSACK, H., PIÉGAY, H. & RINALDI, M. (Ed.): Gravel
bed rivers VI. From process understanding to river restoration. Developments in earth surface pro-
cesses: 703–735. Elsevier Science & Technology, Amsterdam.
HEJDA, M. & PYŠEK, P. (2006): What is the impact of Impatiens glandulifera on species diversity of
invaded riparian vegetation? Biol. Conserv. 132: 143–152.
HÖLZEL, N. & OTTE, A. (2001): The impact of flooding regime on the soil seed bank of flood-
meadows. – J. Veg. Sci. 12: 209–2018.
IBM® (2013): IBM® SPSS® Statistics. Version 22.0.0.0. –.
JÄHNIG, S.C., BRUNZEL, S., GACEK, S., LORENZ, A.W. & HERING, D. (2009): Effects of re-braiding
measures on hydromorphology, floodplain vegetation, ground beetles and benthic invertebrates in
mountain rivers. – J. Appl. Ecol. 46: 406–416.
JANUSCHKE, K. (2014): River restorations. Morphological effects on colonization and succession of
aquatic and riparian organism groups. PhD. Thesis, Universität Duisburg-Essen: 113 pp.
JANUSCHKE, K., BRUNZEL, S., HAASE, P. & HERING, D. (2011): Effects of river restorations on riparian
mesohabitats, floodplain vegetation and carabid beetles. Biodiv. Conserv. 20: 3147–3164.
JUNK, W.J., BAYLEY, P.B. & SPARKS, R.E. (1989): The Flood Pulse Concept in river-floodplain sys-
tems. In: DODGE, D.P. (Ed.): Proceedings of the international Large River Symposium
(LARS): 110–127. Canadian Special Publication of Fisheries and Aquatic Sciences 106.
KAREIVA, P. (1990): Population dynamics in spatially complex environments: theory and data. – Philos.
Trans. Biol. Sci. 330: 175–190.
KARRENBERG, S., EDWARDS, P.J. & KOLLMANN, J. (2002): The life history of Salicaceae living in the
active zone of floodplains. Freshw. Biol. 47: 733–748.
KOENZEN, U. (2005): Fluss- und Stromauen in Deutschland: Typologie und Leitbilder. Ergebnisse des
F+E-Vorhabens "Typologie und Leitbildentwicklung für Flussauen in der Bundesrepublik Deutsch-
land" des Bundesamtes für Naturschutz: FKZ: 803 82 100. Bundesamt für Naturschutz, Bonn:
327 pp.
LFU = Landesamt für Umweltschutz (2003): Rote Liste gefährdeter Gefäßpflanzen Bayerns mit regio-
nalisierter Florenliste. – Schriftenr. Bayer. Landesamt Umweltschutz 165: 1–374.
LFU = BAYERISCHES LANDESAMT FÜR UMWELT (2015): Hauptwerte Pegel Wasserburg am
Inn. URL: http://www.gkd.bayern.de/fluesse/abfluss/stationen/statistik/index.php?thema=gkd&
rubrik=fluesse&produkt=abfluss&gknr=6&msnr=18003004 [accessed 2015–02–03].
LUDWIG, G. & SCHNITTLER, M. (1996): Rote Liste der Pflanzen Deutschlands. 224 pp.
MCCUNE, B. & GRACE, J.B. (2002): Analysis of ecological communities. MjM Software, Gleneden
Beach, Oregon, U.S.A.
MCCUNE, B. & MEFFORD, M.J. (2011): PC-ORD. Multivariate analysis of ecological data. Version 6.0.
MjM Software, Gleneden Beach, Oregon, U.S.A.
MEYNEN, E., SCHMITHÜSEN, J., GELLERT, J., NEEF, E., MÜLLER-MINY, H. & SCHULTZE, J.H. (Eds.)
(1962): Naturräumliche Gliederung Deutschlands. Band I. Selbstverlag, Bad Godesberg: xx pp.
MÜLLER, M., PANDER, J. & GEIST, J. (2014): The ecological value of stream restoration measures: An
evaluation on ecosystem and target species scales. – Ecol. Eng. 62: 129–139.
MÜLLER-DOMBOIS, D. & ELLENBERG, H. (1974): Aims and methods of vegetation ecology. John
Wiley & Sons, New York: 547 pp.
NEHRING, S., KOWARIK, I., RATITSCH, W.E.F. & ESSL, F. (Eds.) (2013): Naturschutzfachliche Invasivi-
tätsbewertung für die in Deutschland wild lebende gebietsfremde Gefäßpflanzen. – BfN Skripten
352: 1–202.
17
RICHARDSON, D.M., HOLMES, P.M., ESLER, K.J., GALATOWITSCH, S.M., STROMBERG, J.C., KIRKMAN,
S.P., PYŠEK, P. & HOBBS, R.J. (2007): Riparian vegetation: degradation, alien plant invasions, and
restoration prospects. Divers. Distrib. 13: 126–139.
ROSENZWEIG, M.L. (1995): Species diversity in space and time. Cambridge University Press, Cam-
bridge: 460 pp.
SCHAICH, H., RUDNER, M. & KONOLD, W. (2010): Short-term impact of river restoration and grazing
on floodplain vegetation in Luxembourg. Agric. Ecosyst. Environ. 139: 142–149.
SCHOLZ, M., MEHL, D., SCHULZ-ZUNKEL, C., KASPERIDUS, H.D., BORN, W. & HENLE, K. (2012):
Ökosystemfunktionen von Flussauen. Analyse und Bewertung von Hochwasserretention, Nährstoff-
rückhalt, Kohlenstoffvorrat, Treibhausgasemissionen und Habitat-funktion. – Naturschutz Biol.
Vielfalt 124: 1–258.
SHANNON, C.E. (1948): A mathematical theory of communication. Bell Syst. Tech. J. 27: 379–423,
623–656.
STAMMEL, B., CYFFKA, B., GEIST, J., MÜLLER, M., PANDER, J., BLASCH, G., FISCHER, P., GRUPPE, A.,
HAAS, F., KILG, M., LANG, P., SCHOPF, R., SCHWAB, A., UTSCHIK, H. & WEIßBROCK, M.
(2012): Floodplain restoration on the Upper Danube (Germany) by re-establishing water and sedi-
ment dynamics: a scientific monitoring as part of the implementation. River Syst. 20: 55–70.
TOCKNER, K., SCHIEMER, F., BAUMGARTNER, C., KUM, G., WEIGLAND, E., ZWEIMÜLLER, I. &
WARD, J. (1999): The Danube restoration project: Species diversity patterns River across connec-
tivity gradients in the floodplain system. – Regul. Rivers: Res. Manag. 15: 245–258.
VON HBERG, A. (2003): Landschafts- und Vegetationsdynamik entlang renaturierter Flussabschnitte
von Obermain und Rodach. PhD. Thesis, Universität Bayreuth: 252 pp.
WARD, J.V., TOCKNER, K. & SCHIEMER, F. (1999): Biodiversity of floodplain river ecosystems: eco-
tones and connectivity. – Regul. Rivers: Res. Manag. 15: 125–139.
18
... The aim of this study was to check for medium-term development of riparian vegetation comparing different measures on the River Inn in southern Germany, where previous assessments were available and allowed for repetition. We wanted to know if the positive trend observed 2 years after restoration by Strobl, Wurfer, and Kollmann (2015) still is detectable 2 years later or if the river shows a resilient development. On the basis of these observations, we suggest further actions in the sense of adaptive management to overcome restoration thresholds. ...
... The study design followed Strobl et al. (2015), who carried out the first monitoring 2 years after river bank restoration (2014). We considered three measures, each on three sites (in total nine sites: either gravel or sand addition or embankment removal; Table 1). ...
... As a control, we used unrestored riparian sections upstream of each study site, because no pre-restoration data exists, that is, a space-for-time substitution. Like Strobl et al. (2015), we applied a stratified randomized sampling design: ...
Article
River restoration is widely applied, although its effects are poorly understood, and degraded habitats might be difficult to improve. Moreover, there is a lack of monitoring as well as few systematic comparisons of restoration methods. This study presents results of a 4‐year monitoring on River Inn (southern Germany) investigating restoration by gravel or sand addition or embankment removal. The results were compared with reference sites that represent the pre‐restoration conditions. At the landscape scale, we analysed vegetation types based on aerial photographs, whereas at a smaller scale, we undertook vegetation surveys and evaluated species composition, growth, and life form, as well as the proportion of the target vegetation. After 4 years, the data indicated a “negative resilience” of the vegetation back to the state prior to restoration. The structural analysis revealed an extensive spread of reed at expense of bare soil. Thus, the species composition largely regressed to the pre‐restoration conditions, and neither annuals nor other pioneer species showed a long‐term benefit of river restoration. There were differences among the three restoration treatments after 2 years, but no longer after 4 years. However, the river restoration had three positive outcomes: (a) There was a temporary benefit for pioneer vegetation that most likely replenished the seed bank of the respective species, (b) the valuable reed communities showed resilience, and (c) the measures allowed some practical learning as expected for adaptive restoration.
... Therefore, in many economically developed countries, mechanical naturalization has been carried out by creating meanders and backwaters in previously straightened rivers and planting trees and bushes along the banks (Dai et al., 2022;Giergiczny et al., 2022;Strobl et al., 2015). In recent decades, a lot of efforts have been made to reduce the negative effects of dams and restore damaged fish populations by installing fishways and removing dams (Carlson et al., 2018;Magdaleno et al., 2018). ...
Conference Paper
Increasing environmental pollution and human intervention in nature today require the restoration, study, and monitoring of the positive effects on water quality in the restored rivers. Consequently, the main research questions arise: what are the main trends in river restoration impacting water quality and the watershed ecosystem? How does it contribute to the sustainable development of the environment? To answer these questions, this paper presents the results of the bibliometric analysis of papers from the Web of Science database and a keyword map of water quality in the restored rivers. The results of this study will help scientists and practitioners to monitor the restoration of the river ecosystem and its impact on water quality, and to choose further directions of river exploitation activity.
... Therefore, immediately after the natural disaster, 15 hectares of debris-covered pasture area were revegetated using two different commercial clover-grass seed mixtures and various revegetation measures aiming at the rapid reestablishment of pasture areas. There are several studies on restoration measures in heavily disturbed locations (Rydgren et al., 2011;Strobl et al., 2015). Numerous investigations have been made on primary succession on different substrate types (Rydin and Borgegard, 1988;Walker, 1989;Rebele, 1992;Chapin et al., 1994;Wiegleb and Felinks, 2001). ...
Article
Full-text available
In mountain regions, the likelihood of mudflows might increase due to climate change. Although mudflows are common worldwide and devastate agricultural land, virtually nothing is known about the revegetation of mudflow deposits for agricultural purposes. To provide recommendations for rapid revegetation of mountain pastures, 52 permanent plots (4 m × 4 m) on 20 revegetated mudflow deposits in the Nature Park Sölktäler were established. We evaluated different revegetation measures (seed addition alone or combined with application of straw, lime or cattle manure) two years after sowing using commercial clover-grass seed mixtures. Furthermore, 27 permanent plots on 15 unsown mudflow deposits were surveyed. Sowing seeds can considerably accelerate revegetation on siliceous mudflow deposits. Festuca rubra, Agrostis capillaris, Lolium perenne, Trifolium repens and Lotus corniculatus are particularly suitable for rapid grassland reestablishment, whereas Poa pratensis is not recommendable. A pure straw application should be avoided because it delays the revegetation success. Lime addition is not recommended because it can lead to an undesirable legume dominance if clover-grass seed mixtures are used for revegetation. The most effective measure for large-scale revegetation seems to be seed addition without additives. To facilitate revegetation on coarse-grained deposits, large rocks should be crushed using a stone mill.
... Viele Flüsse und Bäche haben uferbegleitende Wege, die für die Gewässerpflege angelegt wurden, aber zurückgebaut werden sollten zugunsten einer besseren Anbindung der Aue an das Fließgewässer. Dies kann geschehen unter anderem durch ein Entfernen der Ufer­ befestigung sowie ein Abflachen der Ufer, wodurch mehr Sedimentdynamik ermöglicht wird und neue Standorte für Pionierarten ent­ stehen ( Strobl et al. 2015 ...
Chapter
Full-text available
Fließgewässer und ihre Auen beherbergen eine große Lebensraumvielfalt aufgrund deutlicher ökologischer Gradienten im Flussverlauf und im Querprofil, verursacht durch Unterschiede der Wasser- und Sedimentdynamik. Fließgewässer gehören zu den am stärksten veränderten Ökosystemen Mitteleuropas. Bis auf einige Oberläufe und wenige Abschnitte der Mittel- und Unterläufe sind sie weitgehend umgestaltet worden. Wasserwirtschaftlicher Ausbau, Verschmutzung, Fragmentierung und Zerstörung von Habitaten sowie invasive Neophyten und Neozoen haben die Ökosystemprozesse und Lebensgemeinschaften zum Teil irreversibel beeinflusst. Zur Erfüllung der Wasserrahmenrichtlinie der EU sowie für eine Verbesserung des Hochwasserschutzes werden an vielen Flüssen Mitteleuropas Renaturierungsmaßnahmen durchgeführt. Dazu gehören Rückverlegung von Deichen, Verbesserung der Durchgängigkeit von Querbauwerken, Erhöhung von Restwassermengen und Kieszugabe. Dadurch werden manche Ökosystemfunktionen der Fließgewässer wiederhergestellt und einige Arten siedeln sich wieder an. Eine weitgehende Renaturierung der ursprünglichen Fluss- und Auendynamik ist aber aus Gründen der veränderten Landnutzung im Bereich der ehemaligen Aue und im Einzugsgebiet nicht mehr möglich.
... Therefore, a number of economically developed countries have accomplished mechanical naturalization, including regulated rivers having excavated meanders and backwaters not suitable to the bed, and pools and shoals forming with coastal areas being greeted with trees and shrubs [2][3]. The beds of regulated streams face spontaneous deformation processes [4][5]. ...
Article
Full-text available
The article deals with the auto-naturalization problems of regulated streams in Lithuania. Research on such streams overgrown with woody vegetation was conducted in the Neris River basin in the Baltic Highlands. We chose to investigate the most urbanized rough terrain area of southeastern Lithuania. The regulated streams found in this area include stretches with a relatively high reserve of hydraulic conductivity. Therefore, with reference to the Water Framework Directive for improving the ecological situation, we assessed the possibilities of promoting the naturalization process. The average density of woody vegetation on the investigated slopes of regulated streams is T = 1.26±0.20 items m⁻². The slopes with northeastern exposure point to the average density of woody vegetation counting TNE = 0.91 items m⁻², which is 2.42 times more than that observed on the slopes with eastern exposure and 2.30 times more than those with southern exposure (TS = 0.39 items m⁻²). Under the presence of the recent density of woody vegetation, hydraulic measurements established Manning’s roughness coefficient that varied from 0.030 to 0.094. The conducted simulation indicates that the studied stretches of regulated streams lose a margin of hydraulic conductivity when Manning’s roughness coefficient reaches a threshold of 0.060-0.080. Planning the naturalization of regulated streams is first offered in the stretches of higher slopes (S0>0.003), where the maintenance of the adequate roughness of the bed may assist in designing the overgrowth of both slopes with woody vegetation.
Article
Full-text available
Zusammenfassung: Im Bereich des Oberen Lechs (Tiroler Lech, Österreich) sind noch natürliche Wildflussbereiche mit ausgeprägten Kiesbettfluren erhalten. Der Tiroler Lech bietet damit eine der letztenMöglichkeiten, Diversität und Verbreitung von Alpenschwemmlingen an einem überwiegend natürlich erhaltenen Flussökosystem zu untersuchen. In den letzten Jahren wurden an mehreren Stellen Renaturierungen durchgeführt. Kurzlebige Pflanzengesellschaften, wie jene der Alpenschwemmlinge, zeigen rasch Erfolge von Renaturierungen an. Ziel der vorliegenden Arbeit war es, die Verbreitungsmuster von Alpenschwemmlingen mittels Aufnahmen von Vegetation und flussmorphologischen Parametern an natürlichen, verbauten und renaturierten Lechabschnitten zu untersuchen. Durch Markierungs- und Keimungsexperimente ausgewählter Arten wurde die Etablierungsfähigkeit der Alpenschwemmlinge überprüft. Am Tiroler Lech wurden 53 Arten mit (sub)alpiner Verbreitung gefunden. Natürlicher Ober- und Mittellauf wiesen eine höhere Diversität von Alpenschwemmlingen auf als verbaute Flächen. Ältere Renaturierungen (2005) ähnelten bereits den artenreichen natürlichen Abschnitten, während jüngere Flächen (2014) noch keinen Renaturierungserfolg zeigten. 2015 konnten 100 bis 85% der markiertenAlpenschwemmlinge wiedergefunden werden. Sie konnten sich reproduzieren und keimfähige Samen produzieren. Der Alpenschwemmlingsreichtum am Tiroler Lech ist einzigartig. Durch zukünftige Renaturierungen könnten noch mehr geeignete Flächen für Alpenschwemmlinge geschaffen werden. Summary: Propagules of (sub)alpine plants can be dispersed by water or avalanches and travel along rivers to the foothills of the mountains. They colonize at highly dynamic alluvions, which are mostly free of competition.At the upper Lech (Tyrolean Lech,Austria) there are still natural floodplains with well-developed gravel bars and characteristic vegetation. The Tyrolean Lech offers one of the last chances to study diversity and distribution of these plants in a natural preserved river ecosystem. During the past years, several restorations were implemented. Through the occurrence of (sub)alpine waterborne plants it is possible to estimate the success of restorations. The objective of this study was to investigate distribution patterns of (sub)alpine waterborne plants by recording vegetation surveys and river morphological parameters at several natural, regulated and restored areas of the Tyrolean Lech. Via marking and germination experiments, we tested the possibility of establishment for selected species. In total, 53 alpine and subalpine species were found along the Tyrolean Lech. The highest diversity occurred at the natural upper and middle course. At the regulated areas a lower number of Diversitätsalpine pioneers was present. Earlier restored areas of the Tyrolean Lech (2005) already showed similarities to the species rich natural areas, whereas no restoration success was found in younger areas (2014). In 2015 still 100 to 85% of the marked individuals were retrieved. Alpine pioneers were able to reproduce at the floodplains and to develop viable seeds. The Tyrolean Lech hosts a unique diversity of (sub)alpine waterborne plants. In the future, additional suitable areas could be created through restoration measures.
Article
Aquatic biological communities have directly undergone human-induced changes. Altered hydrological and morphological processes in running waters have caused the degradation of main habitats for biotas and have disturbed ecosystem functionality. The latest advances in river restoration concerned the rise in far-reaching hydromorphological restoration actions that have been implemented below dams to reverse well-known negative impacts of anthropogenic pressures. Some authors emphasized the enhancement of sediment supply and habitat diversity using gravel augmentation or bank erosion to restore morphodynamics, and thus improve biodiversity. We explored the Web of Science database for empirical research papers that specifically addressed such hydromorphological river restoration actions. Articles were examined using a text-content analysis tool to determine the major concepts or ideas they deal with. It has also been proved as useful in defining interrelationships and degree of interdisciplinary. Results showed that a low number of published scientific articles exist about such projects, mainly condensed in the North hemisphere. Divergent ecological issues were highlighted by the word co-occurrence networks: (i) gravel augmentation was used to improve spawning habitats for fish of economic interest whereas (ii) erodible corridor was designed to safeguard natural riparian systems, approaching morphological goals of channel widening. Overall, ecological responses were consistent with those expected, leading however rather to functional shifts than richness increase. Gravel augmentation or bank erosion were not usually combined with in-channel structure management. However, this might be an option to consider since the biological communities seem to be sensitive during first restorations with such combination. This review demonstrates the value of word co-occurrence networks in exploring a high number of previous publications, keys for formulating guidance to manage gravel augmentation or bank erosion along ecological purposes.
Article
Full-text available
Abstract JUNK, W. J., P. B. BAYLEY, AND R. E. SPARKS, 1989. The flood pulse concept in river-floodplain systems, p. 110-127. In D. P. Dodge [ed.] Proceedings of the International Large River Symposium. Can. Spec. Publ. Fish. Aquat. Sci. 106. The principal driving force responsible for the existence, productivity, and interactions of the major biota in river—floodplain systems is the flood pulse. A spectrum of geomorphological and hydrological conditions produces flood pulses, which range from unpredictable to predictable and from short to long duration. Short and generally unpredictable pulses occur in low-order streams or heavily modified systems with floodplains that have been leveed and drained by man. Because low-order stream pulses are brief and unpredictable, organisms have limited adaptations for directly utilizing the aquatic/terrestrial transition zone (ATTZ), although aquatic organisms benefit indirectly from transport of resources into the lotic environment. Conversely, a predictable pulse of long duration engenders organismic • adaptations and strategies that efficiently utilize attributes of the ATTZ. This pulse is coupled with a dynamic edge effect, which extends a "moving littoral" throughout the ATTZ. The moving littoral prevents prolonged stagnation and allows rapid recycling of organic matter and nutrients, thereby resulting in high productivity. Primary production associated with the ATTZ is much higher than that of permanent water bodies in unmodified systems. Fish yields and production are strongly related to the extent of accessible floodplain, whereas the main river is used as a migration route by most of the fishes. In temperate regions, light and/or temperature variations may modify the effects of the pulse, and anthropogenic influences on the flood pulse or floodplain frequently limit production. A local floodplain, however, can develop by sedimentation in a river stretch modified by a low head dam. Borders of slowly flowing rivers turn into floodplain habitats, becoming separated from the main channel by levées. The flood pulse is a "batch" process and is distinct from concepts that emphasize the continuous processes in flowing water environments, such as the river continuum concept. Flooclplains are distinct because they do not depend on upstream processing inefficiencies of organic matter, although their nutrient pool is influenced by periodic lateral exchange of water and sediments with the main channel. The pulse concept is distinct because the position of a floodplain within the river network is not a primary determinant of the processes that occur. The pulse concept requires an approach other than the traditional limnological paradigms used in lotic or lentic systems. Résumé JUNK, W. J., P. B. BAYLEY, AND R. E. SPARKS. 1989. The flood pulse concept in river-floodplain systems, p. 110-127. In D. P. Dodge [cd.] Proceedings of the International Large River Symposium. Can. Spec. Publ. Fish. Aquat. Sci . 106. Les inondations occasionnées par la crue des eaux dans les systèmes cours d'eau-plaines inondables constituent le principal facteur qui détermine la nature et la productivité du biote dominant de même que les interactions existant entre les organismes biotiques et entre ceux-ci et leur environnement. Ces crues passagères, dont la durée et la prévisibilité sont variables, sont produites par un ensemble de facteurs géomorphologiques et hydrologiques. Les crues de courte durée, généralement imprévisibles, surviennent dans les réseaux hydrographiques peu ramifiées ou dans les réseaux qui ont connu des transformations importantes suite à l'endiguement et au drainage des plaines inondables par l'homme. Comme les crues survenant dans les réseaux hydrographiques d'ordre inférieur sont brèves et imprévisibles, les adaptations des organismes vivants sont limitées en ce qui a trait à l'exploitation des ressources de la zone de transition existant entre le milieu aquatique et le milieu terrestre (ATTZ), bien que les organismes aquatiques profitent indirectement des éléments transportés dans le milieu lotique. Inversement, une crue prévisible de longue durée favorise le développement d'adaptations et de stratégies qui permettent aux organismes d'exploiter efficacement 1 'ATTZ. Une telle crue s'accompagne d'un effet de bordure dynamique qui fait en sorte que l'ATTZ devient un « littoral mobile'<. Dans ces circonstances, il n'y a pas de stagnation prolongée et le recyclage de la matière organique et des substances nutritives se fait rapidement, ce qui donne lieu à une productivité élevée. La production primaire dans l'ATTZ est beaucoup plus élevée que celle des masses d'eau permanentes dans les réseaux hydrographiques non modifiés. Le rendement et la production de poissons sont étroitement reliés à l'étendue de la plaine inondable, tandis que le cours normal de la rivière est utilisé comme voie de migration par la plupart des poissons.
Book
Full-text available
The standard textbook of Vegetation Ecology. A reprint (2002) is available from The Blackburn Press, Caldwell, New Jersey.
Article
Between 1992 and 1998, 55 km of riverbank on the Ottawa River was protected from erosion using rounded granular material of glaciofluvial origin from local gravel pits. The method did not require slope reprofiling or the installation of a key or geotextile. It allows for the slopes of the structure and the banks to reach an equilibrium state and relies on natural vegetation regrowth on the banks and embankments rather than bioengineering revegetation techniques. A follow-up was done in 2011 to assess its effectiveness. After fifteen years, the structures have halted erosion, blended into the local landscape and created a riparian ecotone. They quickly acquired a natural, gently sloping profile and recreated a sinuous shoreline dotted with sandy beaches. The follow-up also shows that the banks and structures are 80-90% covered by indigenous vegetation. Furthermore, this vegetation is as diverse as the natural vegetation seen on the unstabilized sections of riverbank. The work minimized damage to the riverbanks as it was done in winter so that shore ice could be used for access. This approach helped avoid interventions on the banks themselves and protected the existing vegetation. The availability of granular sources near the work site was a key criterion. Riverbank protection work of this scale is uncommon. This article discusses the effectiveness of the protection method and its environmental advantages and limitations. This method could prove to be an alternative to traditional rock-fill methods or bioengineering techniques, which are often quite complex and costly.
Article
The relationship between hydrological connectivity and species diversity patterns (alpha and beta diversity) of macrophytes, molluscs, odonates and amphibians was investigated in a semi-natural floodplain segment in the ‘Alluvial Zone National Park’ of the Danube River in Austria. Based on environmental variables, we distinguished four major channel types (inflow channel, parapotamal, plesiopotamal and palaeopotamal) that reflected a lateral connectivity gradient. In addition, a longitudinal environmental gradient along the parapotamal channel was found.Connectivity, rather than the surface area of individual floodplain water bodies, explained local species richness. Species diversity patterns varied among taxa: the highest species richness values for molluscs occurred in the parapotamal channels, for odonates in the para- and plesiopotamal channels, for macrophytes in the plesiopotamal channels and for amphibians in the palaeopotamal channels. Within the parapotamal channels, the species richness of odonates and amphibians increased moving upstream. Beta diversity displayed an almost inverse relationship with alpha diversity, with highest average values in isolated and fragmented floodplain channels. Habitat fragmentation favoured the beta diversity of most groups, although connectivity favoured the beta diversity of amphibians. The highest proportion of endangered species (mainly rheophilic forms) was found in the parapotamal channels.It is concluded that preservation of the high diversity of this alluvial flood plain would be more fully realised by reconstitution of fluvial dynamics and the associated connectivity gradients, rather than by restoration strategies for individual groups or endangered species. Copyright © 1999 John Wiley & Sons, Ltd.
Article
A high level of spatio-temporal heterogeneity makes riverine floodplains among the most species-rich environments known. Fluvial dynamics from flooding play a major role in maintaining a diversity of lentic, lotic and semi-aquatic habitat types, each represented by a diversity of successional stages. Ecotones (transition zones between adjacent patches) and connectivity (the strength of interactions across ecotones) are structural and functional elements that result from and contribute to the spatio-temporal dynamics of riverine ecosystems. In floodplain rivers, ecotones and their adjoining patches are arrayed in hierarchical series across a range of scales. At a coarse scale of resolution, fringing floodplains are themselves complex ecotones between river channels and uplands. At finer scales, patches of various types and sizes form habitat and microhabitat diversity patterns. A broad spatio-temporal perspective, including patterns and processes across scales, is needed in order to gain insight into riverine biodiversity. We propose a hierarchical framework for examining diversity patterns in floodplain rivers.
Article
Stream restoration is widely applied for conservation of freshwater ecosystems, but systematic comparisons on the effects of different techniques are rare. In this study, we systematically evaluated two types of gravel introduction, substratum raking and the placement of boulders in six streams. We compared indicator-based and multi-scale approaches that simultaneously assess effects on target species, different taxonomic groups and on ecosystem scale. Gravel introduction had by far the strongest effects on macroinvertebrates (increase of species density and numbers of individuals), periphyton (increase of cell numbers) and macrophytes (decrease of coverage, species numbers and biomass), followed by substratum raking. The placement of boulders had no significant long-term effects on aquatic communities. Over all investigated restoration treatments, fish community composition only changed significantly in 50% of the study rivers depending on the occurrence of species sensitive to the structures introduced by the restoration treatments. These were lithophilic, rheophilic and invertivorous fishes, comprising several species listed in the Red List of endangered species, which used the added 16–32 mm gravel as juvenile habitat. Areas with introduced gravel were also most frequently used by spawning Salmo trutta, Thymallus thymallus and Phoxinus phoxinus. In contrast, active bioindication using Salmo trutta eggs indicated that none of the restoration treatments was sufficient to enhance habitat conditions in deeper substratum layers throughout the egg incubation period. Our results suggest that instream restoration measures can contribute to freshwater biodiversity conservation, but reproductive success of species depending on long-term improvement of interstitial water quality cannot be achieved without considering catchment effects and natural substratum dynamics.