title: Atmospheric CO2 and O3 alter the flow of 15N in developing forest ecosystems.
abstract: Anthropogenic O3 and CO2-induced declines in soil N availability could counteract greater plant growth in a CO2-enriched atmosphere, thereby reducing net primary productivity (NPP) and the potential of terrestrial ecosystems to sequester anthropogenic CO2. Presently, it is uncertain how increasing atmospheric CO2 and O3 will alter plant N demand and the acquisition of soil N by plants as well as the microbial supply of N from soil organic matter. To address this uncertainty, we initiated an ecosystem-level 15N tracer experiment at the Rhinelander (Wisconsin, USA) free air CO2-O3 enrichment (FACE) facility to understand how projected increases in atmospheric CO2 and 03 alter the distribution and flow of N in developing northern temperate forests. Tracer amounts of 15NH4+ were applied to the forest floor of developing Populus tremuloides and P. tremuloides-Betula papyrifera communities that have been exposed to factorial CO2 and O3 treatments for seven years. One year after isotope addition, both forest communities exposed to elevated CO2 obtained greater amounts of 15N (29%) and N (40%) from soil, despite no change in soil N availability or plant N-use efficiency. As such, elevated CO2 increased the ability of plants to exploit soil for N, through the development of a larger root system. Conversely, elevated O3 decreased the amount of 15N (-15%) and N (-29%) in both communities, a response resulting from lower rates of photosynthesis, decreases in growth, and smaller root systems that acquired less soil N. Neither CO2 nor 03 altered the amount of N or 15N recovery in the forest floor, microbial biomass, or soil organic matter. Moreover, we observed no interaction between CO2 and 03 on the amount of N or 15N in any ecosystem pool, suggesting that 03 could exert a negative effect regardless of CO2 concentration. In a CO2-enriched atmosphere, greater belowground growth and a more thorough exploitation of soil for growth-limiting N is an important mechanism sustaining the enhancement of NPP in developing forests (0-8 years following establishment). However, as CO2 accumulates in the Earth's atmosphere, future O3 concentrations threaten to diminish the enhancement of plant growth, decrease plant N acquisition, and lessen the storage of anthropogenic C in temperate forests.
authors.affiliation: School of Natural Resources & Environment, University of Michigan, Ann Arbor, Michigan 48109, USA. drzak@umich.edu
authors.forename: Donald R
authors.initials: DR
authors.lastname: Zak
authors.forename: William E
authors.initials: WE
authors.lastname: Holmes
authors.forename: Kurt S
authors.initials: KS
authors.lastname: Pregitzer
mesh_terms: D018533:Biomass; D002245:Carbon Dioxide / Q000494:pharmacology*; D017753:Ecosystem; D009584:Nitrogen / Q000378:metabolism*; D009587:Nitrogen Isotopes; D010126:Ozone / Q000494:pharmacology*; D018517:Plant Roots / Q000187:drug effects / Q000254:growth & development / Q000378:metabolism; D032107:Populus / Q000187:drug effects* / Q000254:growth & development / Q000378:metabolism; D012987:Soil / Q000032:analysis / Q000592:standards; D012988:Soil Microbiology
chemical_list: D009587:Nitrogen Isotopes; D012987:Soil; D002245:Carbon Dioxide; D010126:Ozone; D009584:Nitrogen