Ectomycorrhizal impacts on plant nitrogen nutrition: Emerging isotopic patterns, latitudinal variation and hidden mechanisms

Abstract

Ectomycorrhizal (EcM)-mediated nitrogen (N) acquisition is one main strategy used by terrestrial plants to facilitate growth. Measurements of natural abundance nitrogen isotope ratios (denoted as δ15N relative to a standard) increasingly serve as integrative proxies for mycorrhiza-mediated N acquisition due to biological fractionation processes that alter 15N:14N ratios. Current understanding of these processes is based on studies from high-latitude ecosystems where plant productivity is largely limited by N availability. Much less is known about the cause and utility of ecosystem δ15N patterns in the tropics. Using structural equation models, model selection and isotope mass balance we assessed relationships among co-occurring soil, mycorrhizal plants and fungal N pools measured from 40 high- and 9 low-latitude ecosystems. At low latitudes 15N-enrichment caused ecosystem components to significantly deviate from those in higher latitudes. Collectively, δ15N patterns suggested reduced N-dependency and unique sources of EcM 15N-enrichment under conditions of high N availability typical of the tropics. Understanding the role of mycorrhizae in global N cycles will require reevaluation of high-latitude perspectives on fractionation sources that structure ecosystem δ15N patterns, as well as better integration of EcM function with biogeochemical theories pertaining to climate-nutrient cycling relationships.