US EPA

6972974 

Journal Article 

Nitrogen Isotopes in Soils and Plants of Tundra Ecosystems in the Khibiny Mountains 

Makarov, MI; Buzin, IS; Tiunov, AV; Malysheva, TI; Kadulin, MS; Koroleva, NE; , 

2019 

Yes 

Eurasian Soil Science
ISSN: 1064-2293
EISSN: 1556-195X 

PLEIADES PUBLISHING INC 

MOSCOW 

1195-1206 

10.1134/S1064229319100077 

WOS:000491515600005 

The isotopic composition of nitrogen in soils and plants may be an indicator of transformation of its compounds and sources of N nutrition of plants. Natural N-15 abundance (delta N-15) was determined in soils (the total, ammonium, and nitrate nitrogen) and in plant leaves and roots of four tundra ecosystems in the Khibiny Mountains. The studied soils (Folic Leptic Entic Podzol and Leptosols) significantly differ in N availability, and plants are represented by the species, forming ectomycorrhiza, ericoid mycorrhiza, and arbuscular mycorrhiza, as well as by the species, which usually do not form a mycorrhiza. The range of delta N-15 in soil inorganic compounds is from -16.2 parts per thousand in nitrates to +6.4 parts per thousand in ammonium, which reflects the correlation between the activities of N-mineralization and nitrification and delta N-15-, as well as a potentially strong effect on the isotopic composition of nitrogen in plants. The value of delta N-15 in plant leaves and roots changes in a narrower range (from -7.3 to +2.4 parts per thousand), which may be related to N uptake from different sources and to fractionation of N isotopes during N assimilation. Roots are N-15-enriched in comparison with leaves in most of the studied plant species, which corresponds to the concept of mycorrhiza participation in N nutrition of plants. Regardless of the type of mycorrhizal symbiosis, the difference in delta N-15 between roots and leaves of most plant species decreases contrary to N availability in soils.