Mean above-ground biomass of plant communities of floodplain meadows. The analyses are means for Estonia representing seminatural hay meadows in 1978-19812
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
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
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 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]
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]
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
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
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
|Above-ground biomass, mean for community type|
|Dry floodplain meadow||150||80|
|Moderately moist floodplain meadow||150–250||200|
|Moist floodplain meadow||150–300||230|
|Wet floodplain meadow with tall grasses||80–200 (300)||250|
|Wet floodplain meadow with tall sedges||200–250||260|
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
|Floodplain meadow type|
English description in Truus & Tõnisson, 1998
St.Dev in parentheses)
|Moderately moist||493 (240)|
|Wet with tall sedges||742 (70.3)|
|Floodplain marsh||376 (100.9)|
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
|Floodplain meadow type|
English description in Truus & Tõnisson, 1998
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)|
of grasslands can lead to dominance (in some cases to almost monospecies communities) of tall herbs like
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]
Rinne, L. (1927). Sooheinamaa toodangu kahanemisest väetuse puudusel. Eesti Sooparanduse Seltsi teated, Vol.8&9, 3–15. [In Estonian]
|Dry standing biomass|
St.Dev. in parentheses
|England and Wales||~ 200||Wheeler & Shaw, 1991, Fig. 1|
|England and Wales||~ 200|
|England and Wales||~ 200|
|England and Wales||~ 300|
|England and Wales||Rich-fen meadow||~ 500|
|England and Wales||~ 600|
|England and Wales||~ 700|
|England and Wales||~ 850|
|England and Wales||~ 1200|
|England and Wales||~ 1300|
|England and Wales||~ 1500|
|England and Wales||Tall herb fen||~ 1750|
|England and Wales||900–1200||Smith et al., 1985|
|England and Wales||700–1200|
|Siberia, Russia||200||Pjavtšenko, 1967|
|Switzerland||152–231||Venterink & Vittouz, 2008|
|Netherlands||~ 300–400||Van der Hoek & Sýkora, 2006|
|Estonia||50||Data from 1977-19802|
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.
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