Symbiotic fungi's role in providing nitrogen to host plants is well-studied in tundra at Toolik Lake, Alaska, but little-studied in the adjoining boreal forest ecosystem. Along a 570 km north-south transect from the Yukon River to the North Slope of Alaska, the .15 N content was strongly reduced in ectomycorrhizal and ericoid mycorrhizal plants including Betula, Salix, Picea mariana (P. Mill.) B.S.P., Picea glauca Moench (Voss), and ericaceous plants. Compared with the . 15 N content of soil, the foliage of nonmycorrhizal plants (Carex and Eriophorum) was unchanged, whereas content of the ectomycorrhizal fungi was very much higher (e.g., Boletaceae, Leccinum and Cortinarius). It is hypothesized that similar processes operate in tundra and boreal forest, both nitrogen-limited ecosystems: (i) mycorrhizal fungi break down soil polymers and take up amino acids or other nitrogen compounds; (ii) mycorrhizal fungi fractionate against .15 N during production of transfer compounds; (iii) host plants are accordingly depleted in .15 N; and (iv) mycorrhizal fungi are enriched in . 15 N. Increased N availability for plant roots or decreased light availability to understory plants may have decreased N allocation to mycorrhizal partners and increased d. 15 N by 3%-4% for southern populations of Vaccinium vitis-idaea L. and Salix. Fungal biomass, measured as ergosterol, correlated strongly with soil organic matter and attained amounts similar to those in temperate forest soils.Key words: mycorrhizal fungi, .15 N, nitrogen cycling, symbiosis, nitrogen isotopes.RĂ©sumĂ© : Le rĂŽle des champignons symbiotiques dans l'apport en azote des hĂŽtes est bien Ă©tudiĂ© dans la toundra, au lac Toolik, en Alaska, mais peu Ă©tudiĂ© dans l'Ă©cosystĂšme adjacent que constitue la forĂȘt borĂ©ale. Le long des 570 km du transect nord-sud allant de la riviĂšre Yukon au versant nord de l'Alaska, le d. 15 N Ă©tait fortement rĂ©duit chez les plantes ectomycorhizes et mycorhizes Ă©ricoĂŻdes, notamment Betula, Salix, Picea mariana (P. Mill.) B.S.P., Picea glauca Moench (Voss) et les Ă©ricacĂ©es. Le feuillage des plantes non mycorhizes (Carex et Eriophorum) demeure inchangĂ© en fonction du contenu du sol en . 15 N, alors que le contenu des champignons ectomycorhizes est beaucoup plus Ă©levĂ© (e.g., BolĂ©tacĂ©es, Leccinum et Cortinarius). On a supposĂ© que des processus similaires opĂšrent dans la toundra et la forĂȘt borĂ©ale, deux Ă©cosystĂšmes limitĂ©s en azote : (i) les champignons mycorhizes scindent les polymĂšres du sol et incorporent les acides aminĂ©s ou les autres composĂ©s azotĂ©s; (ii) les champignons mycorhizes favorisent le .15 N lors du transfert des composĂ©s; (iii) les plantes hĂŽtes sont consĂ©quemment appauvries en . 15 N; et (iv) les champignons mycorhizes sont enrichis en . 15 N. La disponibilitĂ© accrue de l'azote pour les racines des plantes ou la plus faible disponibilitĂ© de lumiĂšre pour les plantes en sous-Ă©tage peut avoir diminuĂ© la portion d'azote allouĂ©e aux partenaires des mycorhizes et augmentĂ© le d. 15 N de 3%-4% chez les populations de Vaccinium vit...