Nitrogen uptake during one year in subarctic plant functional groups and in microbes after long-term warming and fertilization

• Published in: Ecosystems
• Main Authors: Sørensen, Pernille Lærkedal, Michelsen, Anders, Jonasson, Sven Evert
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2008
• Subjects: Subarctic
• Online Access: https://curis.ku.dk/portal/da/publications/nitrogen-uptake-during-one-year-in-subarctic-plant-functional-groups-and-in-microbes-after-longterm-warming-and-fertilization(99e65790-f8e2-11dd-b219-000ea68e967b).html; https://doi.org/10.1007/s10021-008-9204-6

For the first time in an arctic long-term warming and fertilization experiment, the short-term (days) and longer-term (month and year) nitrogen (N) uptake and allocation in plants, microbes, and soil pools were studied, with 15 N-labeling of an organic nitrogen form, glycine. The long-term warming and fertilization had no marked effect on soil inorganic N content, but both dissolved organic N (DON) and plant biomass did increase after fertilization. Soil microbes initially immobilized most of the added 15 N, but in the following months, they lost two-thirds, while label concentration in plants increased. After a year, however, the 15 N recovered in microbes was still 10-fold higher than that in the plant biomass, showing the high importance of soil microbes in nutrient retention in arctic ecosystems, irrespective of the impact of long-term warming or fertilization. The effects of the treatments on the uptake of label by deciduous shrubs and evergreens paralleled that of their N pool sizes, suggesting that their N uptake potential was unaffected by long-term warming and fertilizer addition. Mosses and herbs had high uptake potential but in fertilized plots they took up less 15 N, that is, they were N saturated. The fraction of 15 N in microbes tended to decrease after fertilization, but this was an effect of higher N pool dilution after 1 month and a year, and not due to lower initial uptake. Although the concentration of soil inorganic N did not change after fertilization, both increased DON and the results of the 15 N label addition showed that the N availability in the ecosystem had increased. By contrast, warming had little effect on soil N pools and microbial 15 N uptake, and, hence, had no detectable effects on 15 N accumulation.