D. Tscherko et al., Effect of temperature on below-ground N-dynamics in a weedy model ecosystem at ambient and elevated atmospheric CO2 levels, SOIL BIOL B, 33(4-5), 2001, pp. 491-501
Model multispecies terrestrial communities composed of four trophic levels
(plants, herbivores, parasitoids, decomposers) were established in the Ecot
ron controlled environment facility. Two experimental runs enabled us to in
vestigate the effects of enhanced temperature on below-ground microbial pro
cesses (N-mineralisation. urease, arginine deaminase, protease activity and
potential denitrification) in both ambient and elevated (ambient +200 ppm)
CO2 atmospheres.
The enzyme activities involved in nitrogen cycling showed weak responses to
elevated temperature in both experimental runs. In the Ambient CO2 Run, pr
otease and arginine deaminase values tended to be lower in elevated tempera
ture; on the other hand, N-mineralisation, urease and denitrification enzym
e activity (DEA) were higher. In the Elevated CO2 Run, all microbial variab
les showed higher activities at elevated temperature, although only the res
ults for DEA and arginine deaminase were statistically significant. The int
eraction between higher temperature and elevated CO2 weakly affected root g
rowth and tissue C:N ratio, limiting feedbacks into the microbial community
.
Besides temperature and CO2, substrate availability, water stress and succe
ssional development regulated the response of the soil microbes. The supply
of organic carbon and nitrogen in the soil allowed plant growth and mainte
nance of the microbial population. Nitrogen competition between vegetation
and microbes restricted net microbial growth. The increase of dissolved org
anic carbon (DOC) at higher CO2, and temperature levels significantly favou
red DEA. The high water regime in the soil also favoured DEA and inhibited
oxidation of organic compounds. as indicated by low levels of enzyme activi
ty. Additionally, water stress decreased rooting density in the soil; this
resulted in negative feedback into microbial processes. We conclude that wa
ter stress and soil nitrogen deficiency caused an early levelling-off of bo
th microbial population growth and activity rates during the early part of
the model ecosystem's development. (C) 2001 Elsevier Science Ltd. All right
s reserved.