OOS 49-3 - Molybdenum limitation of tropical nitrogen fixation: A widespread phenomenon?

Friday, August 10, 2007: 8:40 AM
C3&4, San Jose McEnery Convention Center
Alexander R. Barron, Chemistry, Carleton College, Northfield, MN, Anne Kraepiel, Geosciences, Princeton University and Lars Hedin, Ecology and Evolutionary Biology, Princeton University, Princeton, NJ

Nitrogen (N) fixation, the biologically mediated conversion of atmospheric N2 to plant-available NH4+, is the primary natural input of N to ecosystems with implications for plant growth and ecosystem-atmosphere carbon exchange from local to global scales.  While there has been progress in understanding N fixation in marine ecosystems, we know comparably little about factors that control this process in terrestrial ecosystems.  Tropical forests are of particular concern as they contribute roughly one third of N fixed on land, harbor one third of land primary production, and play a critical role in the Earth's climate system.  Here we report direct experimental demonstration that the soil micronutrient molybdenum (Mo) controls heterotrophic N fixation in tropical forests that grow on weathered soils.  We show that, in lowland Panamanian forests, N fixation increased in response to long-term fertilization with either phosphorus (P) or micronutrients, but decreased in response to N.  Direct additions confirmed that the trace-element molybdenum (Mo) caused the micronutrient effect.  Analyses further showed that Mo contamination of the P fertilizer may act as a "hidden treatment" that adequately explains the observed P effect.   Our findings constitute the first-ever experimental observation that Mo can limit N fixation in tropical forests, and suggest that Mo in P fertilizer may cause Mo limitation of fixation to be mistaken for P limitation.

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