|
2006
2005
2004
2003
2002
2001
2000
1999
1998
1997
1996
1995
1994
1993
1992
1991
ICOM 3
ICOM 2
ICOM 1
|
|
|
Bjork, RG; Klemedtsson, L; Molau, U; Harndorf, J; Odman, A; Giesler, R. 2007. Linkages between N turnover and plant community structure in a tundra landscape. PLANT AND SOIL. 294(1-2):247-261.
Address:
Bjork, RG, Univ Gothenburg, Dept Plant & Environm Sci, POB 461, S-40530
Gothenburg, Sweden
The spatial distribution of organic soil nitrogen (N) in alpine tundra
was studied along a natural environmental gradient, covering five plant
communities, at the Latnjajaure Field Station, northern Swedish
Lapland. The five communities (mesic meadow, meadow snowbed, dry heath,
mesic heath, and heath snowbed) are the dominant types in this region
and are differentiated by soil pH. Net N mineralization, net
ammonification, and net nitrification were measured using 40-day
laboratory incubations based on extractable NH4+ and NO3-.
Nitrification enzyme activity (NEA), denitrification enzyme activity
(DEA), amino acid concentrations, and microbial respiration were
measured for soils from each plant community. The results show that net
N mineralization rates were more than three times higher in the meadow
ecosystems (mesic meadow 0.7 mu g N g(-1) OM day(-1) and meadow snowbed
0.6 mu g N g(-1) OM day(-1)) than the heath ecosystems (dry heath 0.2
mu g N g(-1) OM day(-1), mesic heath 0.1 mu g N g(-1) OM day(-1) and
heath snowbed 0.2 mu g N g(-1) OM day(-1)). The net N mineralization
rates were negatively correlated to organic soil C/N ratio (r = -0.652,
P < 0.001) and positively correlated to soil pH (r = 0.701, P < 0.001).
Net nitrification, inorganic N concentrations, and NEA rates also
differed between plant communities; the values for the mesic meadow
were at least four times higher than the other plant communities, and
the snowbeds formed an intermediate group. Moreover, the results show a
different pattern of distribution for individual amino acids across the
plant communities, with snowbeds tending to have the highest amino acid
N concentrations. The differences between plant communities along this
natural gradient also illustrate variations between the dominant
mycorrhizal associations in facilitating N capture by the
characteristic functional groups of plants.
|
|
|