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PARENT SESSION
Organized Oral Session 48: Nitrogen cycling in terrestrial ecosystems: New insights from isotopes and experiments
Organizer(s): MC Mack, P Templer, and K Nadelhoffer
Thursday, August 11, 1:30 PM - 5:00 PM, Meeting Room 510b, Level 5, Palais des congrès de Montréal

Elevated CO2 increases plant foraging for soil resources: Evidence from a field 15N tracer experiment.

Holmes, William*,1, Zak, Donald1, Pregitzer, Kurt2, King, John2, Loya, Wendy2, Ellsworth, David1, 1 University of Michigan, Ann Arbor, MI2 Michigan Technological University, Houghton, MI

ABSTRACT- In north temperate forests, enhanced tree growth under elevated atmospheric CO2 could be limited by nutrient availability as well as tissue damage from O3 exposure. At the FACTS II FACE experiment in Wisconsin, elevated CO2 led to consistently greater NPP in aspen, aspen-birch and aspen-maple communities for several growing seasons. Elevated tropospheric O3 generally counteracted this response. Previous measurements of gross rates of N mineralization and immobilization suggested that elevated CO2 increased N availability to plants, whereas elevated O3 may have reduced N availability due to greater microbial N demand. To better assess treatment effects on plant N acquisition and ecosystem N cycling, we conducted an ecosystem scale 15N tracer experiment wherein we applied 15NH4Cl (0.015 g 15N/m2) directly to forest floor and sampled soil and biomass pools one year later. The majority of applied 15N (56-75%) was recovered in forest floor and soil organic matter. Preliminary analysis of leaves from aspen and aspen-birch communities indicates 15N recovery within canopy biomass increased under elevated CO2 (+68%) and elevated CO2 + O3 (+99%); recovery decreased under elevated O3 (-29%). Our results provide clear evidence that elevated CO2 increased the ability of plants to forage for soil N, which is likely the result of greater fine root production and greater exploitation of soil for resources.

Key words: nitrogen cycling, elevated CO2, ozone, FACE

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