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Estimation of Above-Ground Biomass of Wetlands

Written By

Laimdota Truus

Submitted: 27 October 2010 Published: 06 September 2011

DOI: 10.5772/18390

From the Edited Volume

Biomass and Remote Sensing of Biomass

Edited by Islam Atazadeh

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1. Introduction

Despite global importance of wetlands, estimations of their production and biomass have received little attention (Campbell et al., 2000). This chapter concentrates on analysis of the composition and above-ground biomass of floodplain grasslands and fen vegetation in the Northern forest zone. Both vegetation types were extensively used for hay and/or grazing up to the middle of the 20th century, and abandoned later.

Systematic biomass estimations were conducted in the 1970s–1980s (Estonian data from 1977–1980; most data from Canada from 1972–1978 (Campbell et al., 2000)) when they were feasible for agricultural use. Papers on vegetation production and above-ground biomass of wetlands are quite scarce nowadays. Biomass has sometimes been measured for developing community structure theories, e.g. Zobel & Liira (1997) included some wet grasslands into analysis of richness vs biomass relationship. Still, some thorough reviews can be found like an overview of biomass of rich fen types in South England and Wales by Wheeler & Shaw (1991). New interest in the subject has risen in the context of biomass use for bioenergy production (e.g. Rösch et al., 2009).

Many plant species cannot survive without special accommodation to wetland conditions. The composition of wetland vegetation is mostly controlled by the wetland water level (WL) (Bootsma & Wassen, 1996; Hájková et al., 2004; Barry et al., 2008). Wilcox & Nichols (2008) and Ilomets et al. (2010) found that the diversity and habitat value of plant communities depend on the wetland WL and the water level amplitude between dry and wet seasons (WLA). In fens with a constantly high WL rhizome-spreading graminoids and herbs dominate, while drainage and fluctuating WL support high tussock-forming graminoids.

A specific feature of both floodplain grassland and fen vegetation is high patchiness due to variations in WL and WLA caused by microtopography (Liira et al., 2009). Tussocks, formed by herbaceous plants or tree stumps, locally increase the habitat variability even more (Liira et al., 2009; Ilomets et al., 2010).

Total biomass of wetland vegetation is significantly affected by three main factors: the N:P ratio, total nutrient supply and morphological and physiological traits of plants (Güsewell, 2005). Biomass variations are higher on moister sites such as wet floodplain grasslands (Truus & Puusild, 2009) and fens (Ilomets et al., 2010). The height and coverage of tussocks increases with denser or deeper drainage. About 52% of the vascular plant species variance occurs due to four environmental variables: amplitude of WL (between spring flooding and midsummer dry period), midsummer WL, mire water pH and electrical conductivity (Ilomets et al., 2010).

Truus & Puusild (2009) found strong relation of the above-ground biomass with the management regime but not with the variations in site conditions on wet and moist floodplain grasslands. Wilson & Keddy (1986), Moore & Keddy (1989) and Garica et al. (1993) detected general hump-back relationship between species richness and biomass, but it has also been shown that a high number of factors can complicate prediction of species richness from community biomass (Gough et al., 1994).


2. Factors affecting wetland productivity and species richness

2.1. Relationship between species richness and biomass

The relation between plant species richness and biomass was first discussed by Grime (1973, 1979) and Al-Mufti et al. (1977) when describing general hump-back relationship between species density and community biomass. According to these authors, maximum species richness can be found at medium values of biomass. Later, this relation has been approved (Wheeler & Giller, 1982) or denied (Gough et al., 1994). In the development of this theory Zobel & Liira (1997) attributed species richness to the plant ramet density.

Gough et al. (1994) established correlation between environmental conditions and species richness but not between biomass and environmental conditions. Therefore, the influence of environmental conditions on species richness could not be assumed strictly from biomass. Wheeler & Giller (1982), Boyer & Wheeler (1989) and Wheeler & Shaw (1991) recorded differences in biomass– species richness relation between community types (low-sedge low-productive fen, productive tall-sedge and reed fen, and fertile site communities with strong domination of Filipendula ulmaria or Molinia cerulea).

According to Gough et al. (1994), two types of processes operate in the species richness–productivity relation on wetlands:

  • At low levels of productivity, species richness is primarily limited by the ability of the species to survive the abiotic conditions. In this range increase in productivity reflects a decrease in the harshness of the environment.

  • At higher levels of community productivity, the decline in richness is believed to be related in some way to a greater degree of competitive exclusion with increasing productivity. For wetlands this relation was revealed by Wheeler & Giller (1982). Examining herbaceous fen vegetation, they found that species richness was negatively correlated to above-ground biomass.

Wet meadows are poorer in species than those on mineral soil. Two reasons could be pointed out:

  • Hard environmental stress that excludes several plant species.

  • The absence of management leading to domination of tall plants and accumulation of dead biomass on soil surface (Truus, 1998).

Strong correlation has been found in fens between the height and coverage of the tussock-forming graminoid Molinia cerulea in fens with fluctuating WL and midsummer WL minimum (Ilomets et al., 2010).

In general, relationship of species richness and above-ground biomass is complex and hardly predictable, especially for wetlands.

2.2. Limitations of productivity

2.2.1. Flood, water level and water level amplitude

On floodplain meadows the duration and intensivity of flooding serve as environmental determinants of plant species selection. Riverine floodwater pulses provide water, nutrient-rich material and sediments to floodplain wetlands, but flood pulses also act as a natural disturbance by removing biomass, scouring sediments and delivering turbid waters (Bayley & Guimond, 2009). Riparian ecosystems are among the most diverse systems on the world’s continents (Nilsson et al., 1997). The intensity of natural processes taking place on floodplains is variable, depending on the properties of the river and shore. Estonian rivers are usually small and floodplains narrow. Thereby most riverborn nutrients settle on the 50 m wide belt close to the river channel

Pork, K. (1984). Jõeluhtade looduslikus seisundis säilitamisest. In: Looduskaitse ja põllumajandus. Kumari, E., Randalu, I. & Hang, V. (Eds.). Academy of Sciences of the E.S.S.R, 58–70. [In Estonian]

where productive high-growing vegetation develops. An exception is South Estonia where luxorious sandy sediments form rapidly desiccating low-productivity dry floodplain meadows.

The species composition of spring fen communities is mainly influenced by groundwater chemistry, especially pH, electrical conductivity and mineral richness (Hájek et al., 2002). It is unknown whether these factors affect species richness and the amount of above-ground biomass (Hájkova & Hájek, 2003).

2.2.2. Water and soil chemistry and nutrient availability

Water and soil chemistry and nutrient availability to plants are among the important factors controlling the diversity of wetland vegetation.

Floods bring extra nutrients to floodplain grasslands. Thus there is no N and P deficit and vegetation is luxorious. Management of grasslands removes nutrients from soil and biomass production decreases. Without management, however, annual biomass production increases.

Fens are characterized by high concentrations of cations in soil and water. The concentration of Ca, Fe, N, P and K in plants varies along the poor–rich fen vegetation gradient from poor Sphagnum-fens to calcareous fens, and from sedge-moss fens to forb-rich wet meadows (Rozbrojová & Hájek, 2008). The same study showed that the fertility gradient was largely independent of the poor–rich (pH/calcium) gradient. Nutrient limitations of fens are complicated: species in one community can have different limitations (Rozbrojová & Hájek, 2008). Low-productivity fen communities that support more rare species (Wassen et al., 2005) are rather P- or K- (co)limited, or limited by different environmental conditions (Rozbrojová & Hájek, 2008).

2.2.3. Management

Due to nutrient supply by floodwater, the soil of floodplain meadows is rich in nutrients and biomass productivity is high. The amounts of nutrients brought by floods is comparable to quantities taken away with the harvest or/and cattle grazing. Clipping increase species richness and shoot density but decrease above-ground biomass, thus creating more favourable conditions for more plant species. Bakker (2007) demonstrated that cutting reduces the vigour of tall competitive species, allowing smaller species coexist. Nowadays most of the floodplain meadows are left unmanaged. Hay is mown only in restricted areas for the purposes of environmental protection.

In comparison with other meadow types above-ground biomass production is lower on dry floodplain meadows and higher on floodplain marshes. Productivity is variable in all floodplain meadow community types depending on species composition (Table 1). On wet meadows the site moisture conditions are greatly responsible for plant ecological traits. On permanently wet sites both tussock-forming and mat-forming graminoids dominate while herbs dominate where soil WL drops down at least in summer (Fig. 1). Comparison of Estonian data from the period of regular management (Table 1) with the period of abandonment (Tables 2 and 3) showed that productivity had risen due to accumulation of plant nutrients on unmanaged meadow soils. Above-ground biomass varied threefold, depending on the management regime (Table 3). Liira et al. (2009) also noticed that management lowered canopy height but revealed differences in functional trait structure in more detail.

Falinska (1991, 1995) described two stages in the after-abandonment vegetation succession in Cirsium rivularis phytocoenosis on wet grassland. The initial stage of the succession lasted about 9 years: half of 142 plant species retreated but 12 species became dominant and a macroforb meadow community (Lysimachio vulgaris–Filipenduletum) meadow with mosaic structure, including species like Filipendula ulmaria, Carex cespitosa, C. acutiformis, Lythrum salicaria and Lysimachia vulgaris, was formed. During the following 15 years a specific spatial complex developed, consisting of meadow and herbaceous communities and willow shrub aggregations with the first tree species. Next the Circaeo-Alnetum woodland community appeared. The succession exhibits differentiation of the horizontal structure – increase in patchiness, and differentiation of the vertical structure – plant height started to increase immediately after management stopped and most of the above-ground biomass moved higher from the near-surface position.

Figure 1.

Life-form distribution on Soomaa (West Estonia) wet and moist floodplain meadows

The species composition and duration of this vegetation change depend on climatic and trophic conditions and hydrology, also on the ecological trait of plants and availability of diaspores. General trends, however, are: decrease in species richness, change in species composition, increase in vegetation height and above-ground biomass, and finally replacement of the herbaceous community by woodland. Re-location of most of the biomass to a higher level in the community as described by Falinska (1991, 1995) takes place if herbs dominate – on wet meadows at a drier site. No comparable data about composition and biomass change are available due to abandonment of seminatural hay lands and pastures. Just general trends in vegetation change can be followed.

Floodplain meadow type
English description of classification in Truus & Tõnisson, 1998
Plant community Above-ground biomass
(g m-2)
Above-ground biomass, mean for community type
(g m-2)
Dry floodplain meadow SesleriaFestucetum ovinaea 150 80
SeslerioNardetum 40
ThymoFestucetum 30–100
SieglingoNardetum 40–80
AnthoxanthoAgrostetum 40–100
GalioAgrostetum tenuis 50–150
Moderately moist floodplain meadow Agrostetum giganteae 150–250 200
DeschampsioFestucetum rubrae 100–300
Alopecuretum pratensis 150–380
Moist floodplain meadow CirsioPolygonetum bistortae 150–300 230
FilipenduloGeranietum palustris 200–400
DeschampsietoCaricetum caespitosae 100–250
ElytrigietoAlopecuretum arundinacei 150–300
Wet floodplain meadow with tall grasses Stellario-Deschampsietum 80–200 (300) 250
Phalaroidetum 150–500
Wet floodplain meadow with tall sedges Caricetum distichae 200–250 260
Caricetum acutae 100–450
Caricetum rostrato-vesicariae 100–450
Floodplain marshes Seslerio-Caricetum paniceae 40–100 125
Caricetum paniceo-nigrae 50–150
Caricetum diandro-nigrae 50–180
Caricetum cespitoso-appropinquatae 100–200
Caricetum elatae 80–300

Table 1.

Mean above-ground biomass of plant communities of floodplain meadows. The analyses are means for Estonia representing seminatural hay meadows in 1978-19812

Analysis of life-form distribution on Estonian floodplain meadows in periods with different management showed an increased proportion of tall herbs and graminoids instead of low herbs and graminoids in the 1960s when these areas were mostly regularly mown and the end of the 1990s when they were out of use (Fig. 2). The proportion of tall tussock-forming graminoids did not change. On floodplain grasslands these plants inhabit depressions with a higher water table and thereby were absent even in the former period.


3. Above-ground biomass

3.1. Methods for standing crop estimation

Wheeler & Shaw (1991) calculated above-ground biomass as the biomass increment between April and September. In regions with a dormant season for herbaceous plants in winter, above-ground biomass (that also represents production per year) is in its maximum in the middle of summer, but before abundant flowering. In wetlands different flowering times can be noticed: the sedges usually stop growing and flower in May and June (Leht, 1999) while common reed continues growing up to the August. In all cases, biomass samples were air-dried before measuring. Standing biomass measured in its maximum is usually equalized with production.

3.2. Above-ground biomass of floodplain meadows

In the period of regular management, mean values for above-ground biomass of Estonian floodplain meadows measured from 80 to 260 g m-2, varying largely between community types and even communities2. On unmanaged floodplain meadows those values are more than twice higher (Tables 2 and 3). Zobel & Liira (1997) presented biomass values from 300 to 600 g m-2 for West Estonian floodplain meadows of Sauga, Vaskjõe and Kasari (the lowest value on a dry site). High standard deviation in Tables 2 and 3 shows high variability of floodplain meadows vegetation discussed earlier. For comparison, in the Czech Republic Molinio-Arrhenetheretea above-ground biomass in a moist floodplain meadow was 300–350 g m-2 (Joyce, 2001). Values of above-ground biomass from the earlier (with regular hay cutting; Table 1) and later (without management; Tables 2 and 3) periods show an increase in standing crop that can be explained as a result of management cessation. Standing biomass also varied threefold (from 263 to 763 g m-2) on floodplains in Soomaa, West Estonia (Truus & Puusild, 2009).

Floodplain meadow type
English description in Truus & Tõnisson, 1998
Above-ground biomass
(g m-2,
St.Dev in parentheses)
Dry 458 (148.6)
Moderately moist 493 (240)
Moist 350 (448.3)
Wet (no data)
Wet with tall sedges 742 (70.3)
Floodplain marsh 376 (100.9)

Table 2.

Mean above-ground biomass on the Kloostri landscape transect, West Estonia. Previous hay-meadow, abandoned over 15 years

Truus & Puusild (2009) studied the distribution of ecological groups (graminoids, herbs, low and tall growth-form) in relation to management cessation. The ecological group composition turned towards tussock-forming plants but the most obvious change was the increase in vegetation height (Fig. 2).

Unmanaged wetlands are dominated by powerful species (Wheeler & Giller, 1982; Truus, 1998; Truus & Puusild, 2009). On sites with a permanently high groundwater level Deschampsia cespitosa or Carex cespitosa form high tussocks while low-growing tussocks (Nardus stricta, Festuca ovina) spread on dry or moist managed grasslands. The abandonment

Floodplain meadow type
English description in Truus & Tõnisson, 1998
Above-ground biomass
(g m-2,
St.Dev in parentheses)
Moist, regularly mown 572 (692.3)
Moist, mown, recently abandoned 333 (167.5)
Moist, unmown but mowing reintroduced 380 (178.2)
Moist, unmown over 15 years 763 (627.5)
Wet, regularly mown 263 (108.0)
Wet, mown, recently abandoned 516 (165.9)
Wet, unmown, but mowing reintroduced 452 (398.7)
Wet, unmown over 15 years 447 (86.4)

Table 3.

Mean above-ground biomass on moist and wet floodplain meadows with different management regimes in Soomaa, West Estonia.

Figure 2.

Proportions of the most frequent growth-forms on floodplain meadows in periods of extensive management (first half of the 20th century) and unmanagement (end of the 1990s)

of grasslands can lead to dominance (in some cases to almost monospecies communities) of tall herbs like Filipendula ulmaria. The coverage and height of tussocks of Molinia cerulea increase on rich fen meadows (Ilomets et al., 2010).

3.3. Biomass of fens

Fen vegetation presented in Table 4 is highly variable and the biomass values vary between locations. The above-ground biomass values for low-growing vegetation range from 50 to 500 g m-2 and from 600 to 1750 g m–2 for both tall graminoids and tall herbs. For comparison, in Canada and adjacent USA mean above-ground biomass was 337 ± 142 g m-2 for fens and bogs, and 924 ± 463 g m-2 for marshes and swamps (Campbell et al., 2000).

No recent data are available on biomass production on fens in Estonia. The data from 1977–1980 (Table 4) gives very low values (50 g m-2) for above-ground biomass of fen meadows. The utilization of fen meadows grew in Estonia at the beginning of the 20th century. An experiment from 1922–1926 showed the yield of 140 to 450 g m-2 from unfertilized fen meadows.

Rinne, L. (1927). Sooheinamaa toodangu kahanemisest väetuse puudusel. Eesti Sooparanduse Seltsi teated, Vol.8&9, 3–15. [In Estonian]

. It was also mentioned that during the experiment hay production was related to weather conditions but decreased year by year (probably because of experimental hay cutting).

Location Vegetation community Dry standing biomass
(g m-2)
St.Dev. in parentheses
England and Wales SchoenoJuncetum ~ 200 Wheeler & Shaw, 1991, Fig. 1
England and Wales AcrocladioCaricetum ~ 200
England and Wales PotentilloCaricetum ~ 200
England and Wales PeucedanoPhragmitetum ~ 300
England and Wales Rich-fen meadow ~ 500
England and Wales CladioMolinietum ~ 600
England and Wales PeucedanoPhragmitetum ~ 700
England and Wales AngelicoPhragmitetum ~ 850
England and Wales CicutoPhragmitetum ~ 1200
England and Wales Phragmites consociation ~ 1300
England and Wales Glyceria maxima community ~ 1500
England and Wales Tall herb fen ~ 1750
England and Wales Phalaris arundinacea community 900–1200 Smith et al., 1985
England and Wales Glyceria maxima community 700–1200
Siberia, Russia Carex–dominating fen 200 Pjavtšenko, 1967
Switzerland Saxifraga hirculus fen 152–231 Venterink & Vittouz, 2008
Netherlands Molinietalia fen ~ 300–400 Van der Hoek & Sýkora, 2006
Estonia DrepanocladoSchoenetum 50 Data from 1977-19802
Estonia Seslerio–Caricetum paniceae 50

Table 4.

Above-ground biomass of fens with highly variable composition in different regions


4. Conclusions

Vegetation of floodplain meadows and fens varies depending on the environmental (soil, water) conditions and management regime. Both vegetation types have been in economic use but a great part of them is in the successional stage due to abandonment.

On low-productive sites plant species richness is primarily limited on abiotic conditions (WL, WLA, mineral content of soil and water, availability of plant nutrients).

The main limitation in highly productive sites is competition for light. Tall graminoids or herbs compete out low-growing plants, enabling even the development of monospecies vegetation.

The management status determines plant species richness and the above-ground biomass production. Above-ground standing biomass varied threefold due to management cessation on West Estonian floodplain grassland. Widespread cessation of management on seminatural meadows is a key for interpretation of different above-ground biomass values from different periods. Fen vegetation is probably more sensitive to above-ground biomass cutting than floodplain grassland vegetation.

It is complicated to predict species richness from community biomass, and biomass (or production) from site conditions.

Values of above-ground biomass increase from north to south but the geographical latitude (availability of photosynthetic radiation) is not as strong determinant for biomass production of wet grasslands as the local hydrological, nutritional and management status.



This research was financed by the Estonian Ministry of Education and Research (targeted funding project No. 0280009s07). The author is indebted to Anne Noor for linguistic help.


  1. 1. Al-Mufti M. M. Sydes C. L. Furness S. B. Grime J. P. Band S. R. 1977 A quantitative analysis of shoot phenology and dominance in herbaceous vegetation J. Ecol., 65 759 EOF 0000-0010i313577
  2. 2. Barry M. J. Andreas B. K. De Szalay F. A. 2008 Long-term plant community changes in managed fens in Ohio, USA Aquat. Conserv., 18 392 EOF 407 EOF 1099-0755
  3. 3. Bayley S. E. Guimond J. K. 2009 Aboveground biomass and nutrient limitation in relation to river connectivity in montane floodplain marshes Wetlands 29 4 1243 EOF 1254 EOF 0277-5212
  4. 4. Bootsma M. C. Wassen M. J. 1996 Environmental conditions and fen vegetation in three lowland mires Vegetatio 127 173 EOF 1385-0237
  5. 5. Boyer M. L. H. Wheeler B. D. 1989 Vegetation patterns in spring-fed calcareous fens: calcite precipitation and constraints on fertility J. Ecol., 77 597 EOF 0000-0010i313577
  6. 6. Campbell C. Vitt D. H. Halsey L. A. Campbell I. D. Thormann M. N. Bayley S. E. 2000 Net primary production and standing biomass in northern continental wetlands. Information report NOR-X-369. Canadian Forest Service, Northern Forestry Centre, 0704-7673Canada
  7. 7. Falinska K. 1991 Plant demography and vegetation succession. Kluwer Academic Publishers, 0-79231-060-8Boston, London
  8. 8. Falinska K. 1995Genet disintegration in Filipendula ulmaria: consequences for population dynamics and vegetation succession. J. Ecol. 83 0000-0010i313577
  9. 9. Garcia L. V. Maranon T. Moreno A. Clemente L. 1993Above-ground biomass and species richness in a Mediterranean salt marsh. J. Veg. Sci., 4 1100-9233
  10. 10. Gough L. Grace J. B. Taylor K. L. 1994The relationship between species richness and community biomass: the importance of environmental variables. Oikos, 70 0030-1299
  11. 11. Grime J. P. 1973Competitive exclusion in herbaceous vegetation. Nature, 242 0028-0836
  12. 12. Grime J. P. 1979 Plant strategies and vegetation processes. Wiley & Sons Ltd, 04719920U.K.
  13. 13. Güsewell S. 2005Responses of wetland graminoids to the relative supply of nitrogen and phosphorus. Plant Ecol., 176 1385-0237
  14. 14. Hájek M. Hekera P. Hájkova P. 2002Spring fen vegetation and water chemistry in the West Carpathian flysh zone. Folia Geobot., 37 1211-9520
  15. 15. Hájkova P. Hájek M. 2003Species richness and above-ground biomass of poor and calcareous spring fens in the flysh Weat Carpathians, and their relationship to water and soil chemistry. Preslia, 75 0032-7786
  16. 16. Hájková P. Wolf P. Hájek M. (2004). Environmental factors and Carpathian spring fen vegetation: the importance of scale and temporal variation, Ann. Bot. Fenn., Vol.41, 249-262, ISSN 0003-3847
  17. 17. Ilomets M. Truus L. Pajula R. Sepp K. 2010Species composition and structure of vascular plants and bryophytes on the water level gradient within a calcareous fen in North Estonia. Est. J. Ecol., 59 1 1736-7549
  18. 18. Joyce C. 2001The sensitivity of a species-rich flood-meadow plant community to fertilizer nitrogen: the Lužnice river floodplain, Czech Republic. Plant Ecol., 155 1385-0237
  19. 19. Leht M. . Ed. 1999 Eesti taimede määraja. EPMÜ ZBI, Eesti Loodusfoto, 998583027Tartu, Estonia (In Estonian)
  20. 20. Liira J. Issak M. Jõgar Ü. Mändoja M. Zobel M. 2009Restoration management of a floodplain meadow and its cost-effectiveness- The results of a 6-year experiment. Ann. Bot. Fen., 46 0003-3847
  21. 21. Moore D. R. J. Keddy P. A. 1989The relationship between species richness and standing crop in wetlands: The importance of scale. Vegetatio, 79 1406-0914
  22. 22. Moore D. R. J. Keddy P. A. Gaudet C. L. Wisheu I. 1989Conservation of wetlands: do infertile wetlands deserve a higher priority? Biol. Conserv., 47 0006-3207
  23. 23. Nilsson C. Jansson R. Zinko U. (1997 1997Long-term responses of river-margin vegetation to water-level regulation. Science, 276 0036-8075
  24. 24. Pjavtšenko N. I. 1967O produktivnosti bolot Zapadnoi Sibiri. Rastitelnõje Resursõ. 3 4 0033-9946In Russian)
  25. 25. Rozbrojová Z. Hájek M. 2008Changes in nutrient limitation of spring fen vegetation along environmental gradients in the West Carpathians. J. Veg. Sci., 19 1100-9233
  26. 26. Rösch C. Skarka J. Raab K. Stelzer V. 2009Energy production from grassland- Assessing the sustainability of different process chains under German conditions. Biomass and Bioenergy, 33 0961-9534
  27. 27. Smith S. J. Ridge I. Morris R. M. 1984The biomass potential of seasonally flooded wetlands. In: Proceedings of Bioenergy’ 84 World Conference, 15 21June 1984 in Goteborg, Sweden, The Bioenergy Council, 190-195, 978-0-85334-351-6Stockholm, Sweden
  28. 28. Zobel K. Liira J. 1997A scale-independent approach to the richness vs biomass relationship in ground-layer plant communities, Oikos. 80 0030-1299
  29. 29. Truus L. Puusild E. 2009Species richness, biomass production and recent vegetation changes of Estonian floodplain grassland. Pol. J. Ecol., 57 1 1505-2249
  30. 30. Truus L. Tõnisson A. 1998The ecology of floodplain grasslands in Estonia. In: European Wet Grasslands: Biodiversity, Management and Restoration, C.B. Joyce & P.M. Wade, (Eds.), 49 60John Wiley & Sons Ltd, 0-47197-619-9U.K.
  31. 31. Truus L. 1998Influence of management cessation on reedbed and floodplain vegetation on the Kloostri floodplain meadow in the delta of the Kasari River, Estonia. Proc. Estonian Acad. Sci. Biol. Ecol., 47 1 1406-0914
  32. 32. Van der Hoek D. Sýkora K. V. 2006Fen-meadow succession in relation to spatial and temporal differences in hydrological and soil conditions, Appl. Veg. Sci., 9 1402-2001
  33. 33. Wassen M. J. Barendregt A. Palczynski A. De Smidt J. T. De Mars H. 1990The relationship between fen vegetation gradients, groundwater flow and flooding in an undrained valley mire at Biebrza, Poland, J. Ecol., 78 0000-0010i313577
  34. 34. Wassen M. J. Venterink H. O. Lapshina E. D. Tanneberger F. 2005Endangered plants persist under phosphorus limitation, Nature, 437 22 0028-0836
  35. 35. Venterink O. H. Vittoz P. 2008Biomass production of the last remaining fen with saxifraga hirculus in Switzerland is controlled by nitrogen availability, Botanica Helvetica, 118 0253-1453
  36. 36. Wheeler B. D. Shaw S. C. 1991Above-ground crop mass and species richness of the principal types of herbaceous rich-fen vegetation of lowland England and Wales, J. Ecol., 79 0000-0010i313577
  37. 37. Wheeler B. D. Giller K. E. 1982Species richness of herbaceous fen vegetation in Boardland, Norfolk in relation to the quantity of above-ground plant material, J. Ecol., 70 0000-0010i313577
  38. 38. Wilcox D. A. Nichols S. J. 2008The effect of water-level fluctuations on vegetation in a Lake Huron wetland, Wetlands, 28 2 0277-5212
  39. 39. Wilson S. D. Keddy P. A. 1986Species competitive ability and position along a natural stress/disturbance gradient, Ecology, 67 0012-9658


  • Pork, K. (1984). Jõeluhtade looduslikus seisundis säilitamisest. In: Looduskaitse ja põllumajandus. Kumari, E., Randalu, I. & Hang, V. (Eds.). Academy of Sciences of the E.S.S.R, 58–70. [In Estonian]
  • Rinne, L. (1927). Sooheinamaa toodangu kahanemisest väetuse puudusel. Eesti Sooparanduse Seltsi teated, Vol.8&9, 3–15. [In Estonian]

Written By

Laimdota Truus

Submitted: 27 October 2010 Published: 06 September 2011