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Leaf 15N abundance of subarctic plants provides field evidence that ericoid, ectomycorrhizal and non-and arbuscular mycorrhizal species access different sources of soil nitrogen

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Abstract

The natural abundance of the nitrogen isotope 15, δ15N, was analysed in leaves of 23 subarctic vascular plant species and two lichens from a tree-line heath at 450 m altitude and a fellfield at 1150 m altitude close to Abisko in N. Sweden, as well as in soil, rain and snow. The aim was to reveal if plant species with different types of mycorrhizal fungi also differ in their use of the various soil N sources. The dwarf shrubs and the shrubs, which in combination formed more than 65% of the total above-ground biomass at both sites, were colonized by ericoid or ectomycorrhizal fungi. Their leaf δ15N was between−8.8 and−5.5‰ at the heath and between−6.1 and −3.3‰ at the fellfield. The leaf δ15N of non- or arbuscular mycorrhizal species was markedly different, ranging from −4.1 to −0.4‰ at the heath, and from −3.4 to+2.2‰ at the fellfield. We conclude that ericoid and ectomycorrhizal dwarf shrubs and shrubs utilize a distinct N source, most likely a fraction of the organic N in fresh litter, and not complexed N in recalcitrant organic matter. The latter is the largest component of soil total N, which had a δ15N of −0.7‰ at the heath and +0.5‰ at the fellfield. Our field-based data thus support earlier controlled-environment studies and studies on the N uptake of excised roots, which have demonstrated protease activity and amino acid uptake by ericoid and ectomycorrhizal tundra species. The leaves of ectomycorrhizal plants had slightly higher δ15N (fellfield) and N concentration than leaves of the ericoids, and Betula nana, Dryas octopetala and Salix spp. also showed NO sup-inf3 reductase activity. These species may depend more on soil inorganic N than the ericoids. The δ15N of non- or arbuscular mycorrhizal species indicates that the δ15N of inorganic N available to these plants was higher than that of average fresh litter, probably due to high microbial immobilization of inorganic N. The δ15N of NH sup+inf4 -N was +12.3‰ in winter snow and +1.9‰ in summer rain. Precipitation N might be a major contributer in species with poorly developed root systems, e.g. Lycopodium selago. Our results show that coexisting plant species under severe nutrient limitation may tap several different N sources: NH sup+inf4 , NO sup-inf3 and organic N from the soil, atmospheric N2, and N in precipitation. Ericoid and ectomycorrhizal fungi are of major importance for plant N uptake in tundra ecosystems, and mycorrhizal fungi probably exert a major control on plant δ15N in organic soils.

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References

  • Abuzinadah RA, Read DJ (1988) Amino acids as nitrogen sources for ectomycorrhizal fungi. Utilization of individual amino acids. Trans Br Mycol Soc 91:473–479

    Google Scholar 

  • Allen SE (1989) Chemical analysis of ecological materials, 2nd edn. Blackwell, Oxford, pp 126–127

    Google Scholar 

  • Atkin OK, Villar R, Cummins WR (1993) The ability of several high arctic plants to utilize nitrate nitrogen under field conditions. Oecologia 96:239–245

    Google Scholar 

  • Berendse F, Jonasson S (1992) Nutrient use and nutrient cycling in northern ecosystems. In: Chapin FS III, Jefferies RL, Reynolds JF, Shaver GR, Svoboda J (eds) Arctic ecosystems in a changing climate. An ecophysiological perspective. Academic Press, San Diego, pp 337–356

    Google Scholar 

  • Blaschke H (1991) Multiple mycorrhizal associations of individual calcicole host plants in the alpine grass-heath zone. Mycorrhiza 1:31–34

    Google Scholar 

  • Bledsoe C, Klein P, Bliss LC (1990) A survey of mycorrhizal plants on Truelove Lowland, Devon Island, N.W.T., Canada. Can J Bot 68:1848–1856

    Google Scholar 

  • Callaghan TV, Headley AD, Lee JA (1991) Root function related to morphology, life history and ecology of tundra plants. In: Atkinson D (ed) Plant root growth. An ecological perspective. Blackwell, Oxford, pp 311–340

    Google Scholar 

  • Chapin FS III, Moilanen L, Kielland K (1993) Preferential use of organic nitrogen for growth by a nonmycorrhizal arctic sedge. Nature 361:150–153

    Google Scholar 

  • Delwiche CC, Steyn PL (1970) Nitrogen isotope fractionation in soils and microbial reactions. Environ Sci Technol 4:929–935

    Google Scholar 

  • Dhillon SS (1994) Ectomycorrhizae, arbuscular mycorrhizae and Rhizoctonia sp. of alpine and boreal Salix spp. in Norway. Arct Alp Res 26:304–307

    Google Scholar 

  • Downs MR, Nadelhoffer KJ, Mellillo JM, Aber JD (1993) Foliar and fine root nitrate reductase activity in seedlings of four forest tree species in relation to nitrogen availability. Trees 7:233–236

    Google Scholar 

  • Grannhall U, Selander H (1973) Nitrogen fixation in a subarctic mire. Oikos 24:8–15

    Google Scholar 

  • Gu B, Alexander V (1993) Estimation of N2 fixation based on differences in the natural abundance of 15N among freshwater N2-fixing and non-N2-fixing algae. Oecologia 96:43–48

    Google Scholar 

  • Handley LL, Raven JA (1992) The use of natural abundance of nitrogen isotopes in plant physiology and ecology. Plant Cell Environ 15:965–985

    Google Scholar 

  • Handley LL, Daft MJ, Wilson J, Scrimgeour CM, Ingleby K, Sattar MA (1993) Effects of ecto- and VA-mycorrhizal fungi Hydnagium carneum and Glomus clarum on the δ15N and δ13C values of Eucalyptus globulus and Ricinus communis. Plant Cell Environ 16:375–382

    Google Scholar 

  • Handley LL, Odee D, Scrimgeour CM (1994) δ15N and δ13C patterns in savanna vegetation: dependence on water availability and disturbance. Funct Ecol 8:306–414

    Google Scholar 

  • Havström M, Callaghan TV, Jonasson S (1993) Differential growth responses of Cassiope tetragona, an arctic dwarfshrub, to environmental perturbations among three contrasting high-and subarctic sites. Oikos 66:389–402

    Google Scholar 

  • Högberg P (1990) 15N natural abundance as a possible marker of the ectomycorrhizal habit of trees in mixed African woodlands. New Phytol 115:483–486

    Google Scholar 

  • Högberg P, Alexander IJ (1995) Roles of root symbioses in African woodland and forest: evidence from 15N abundance and foliar analysis. J Ecol 83:217–224

    Google Scholar 

  • IVL (1993) Luft-och nederbördskemiska stationsnätet inom PMK. Rapport fran verksamhet 1992. Institutet för vatten-och luftvardsforskning L93/186, Box 47086, 402 58 Göteborg, Sweden

  • Jonasson S, Havström M, Jensen M, Callaghan TV (1993) In situ mineralization of nitrogen and phosphorus of arctic soils after perturbations simulating climatic change. Oecologia 95:179–186

    Google Scholar 

  • Jonasson S, Vestergaard P, Jensen M, Michelsen A (1995) Effects of carbohydrate amendments on nutrient partitioning plant and microbial performance of a grassland-shrub ecosystem. Oikos (in press)

  • Kielland K (1994) Amino acid absorbtion by arctic plants: implications for plant nutrition and nitrogen cycling. Ecology 75:2373–2383

    Google Scholar 

  • Kohls SJ, van Kessel C, Baker DD, Grigal DF, Lawrence DB (1994) Assessment of N2 fixation and N cycling by Dryas along a chronosequence within the forelands of the Athabasca Glacier, Canada. Soil Biol Biochem 26:623–632

    Google Scholar 

  • Kohn LM, Stasovski E (1990) The mycorrhizal status of plants at Alexandra Fiord, Ellesmere Island, Canada, a high arctic site. Mycologia 82:23–35

    Google Scholar 

  • Körner C (1989) The nutritional status of plants from high altitudes. A worldwide comparison. Oecologia 81:379–391

    Google Scholar 

  • Ledgard SF (1989) Nutrition, moisture and rhizobial strain influence isotopic fractionation during N2 fixation in pasture legumes. Soil Biol Biochem 21:65–68

    Google Scholar 

  • Melillo JM, Aber JD, Linkins AE, Ricca A, Fry B, Nadelhoffer KJ (1989) Carbon and nitrogen dynamics along the decay continuum: Plant litter to soil organic matter. Plant Soil 115: 189–198

    Google Scholar 

  • Michelsen A, Sprent JI (1994) The influence of vesicular-arbuscular mycorrhizal fungi on the nitrogen fixation of nurserygrown Ethiopian acacias estimated by the 15N natural abundance method. Plant Soil 160:249–257

    Google Scholar 

  • Michelsen A, Jonasson S, Sleep D, Havström M, Callaghan TV (1995a) Shoot biomass, δ13C, nitrogen and chlorophyll responses of two arctic dwarf shrubs to in situ shading, nutrient application and warning simulating climatic change. Oecologia (in press)

  • Michelsen A, Schmidt IK Jonasson S, Dighton J, Jones HE, Callaghan TV (1995b) Inhibition of growth, and effects on nutrient uptake of arctic graminoids by leaf extracts-allelopathy or resource competition between plants and microbes? Oecologia (in press)

  • Miller OK Jr (1982) Mycorrhizae, mycorrhizal fungi and fungal biomass in subalpine tundra at Eagle Summit, Alaska. Holarct Ecol 5: 125–134

    Google Scholar 

  • Nadelhoffer KJ, Fry B (1988) Controls on natural nitrogen-15 and carbon-13 abundances in forest soil organic matter. Soil Sci Soc Am J 52:1633–1640

    Google Scholar 

  • Nadelhoffer KJ, Giblin AE, Shaver GR, Linkins AE (1992) Microbial processes and plant nutrient availability in arctic soils. In: Chapin FS III, Jefferies RL, Reynolds JF, Shaver GR, Svoboda J (eds) Arctic ecosystems in a changing climate. An ecophysiological perspective. Academic Press, San Diego, pp 281–300

    Google Scholar 

  • Pate JS, Stewart GR, Unkovich M (1993) 15N natural abundance of plant and soil components of a Banksia woodland ecosystem in relation to nitrate utilization, life form, mycorrhizal status and N2-fixing abilities of component species. Plant Cell Environ 16:365–373

    Google Scholar 

  • Read DJ (1993) Plant-microbe mutualisms and community structure. In: Schulze ED, Mooney HA (eds) Biodiversity and ecosystem function. (Ecological studies, vol 99) Springer, Berlin Heidelberg New York, pp 181–203

    Google Scholar 

  • Read DJ, Haselwandter K (1981) Observations on the mycorrhizal status of some alpine plant communities.New Phytol 88:341–352

    Google Scholar 

  • Read DJ, Leake JR, Langdale AR (1989) The nitrogen nutrition of mycorrhizal fungi and their host plants. In: Boddy L, Marchant R, Read DJ (eds) Nitrogen, phosphorus and sulphur utilization by fungi. Cambridge University Press, Cambridge, UK, pp 181–204

    Google Scholar 

  • Schulze ED, Chapin FS III, Gebauer G (1994) Nitrogen nutrition and isotope differences among life forms at the northern treeline of Alaska. Oecologia 100:406–412

    Google Scholar 

  • Shearer G, Kohl DH (1989) Estimates of N2 fixation in ecosystems: the need for and basis of the 15N natural abundance method. In: Rundel PW, Ehleringer JR, Nagy KA (eds) Stable isotopes in ecological research. Springer, Berlin Heidelberg New York, pp 343–374

    Google Scholar 

  • Shearer G, Duffy J, Kohl DH, Commoner B (1974) A steady state model of isotopic fractionation accompanying nitrogen transformation in soil. Soil Sci Soc Am Proc 38:315–322

    Google Scholar 

  • Statistical Analysis Systems Institute (1988) SAS/STAT Users Guide, Release 6.03. SAS Institute, Cary, NC

    Google Scholar 

  • Stewart GR, Pate JS, Unkovich M (1993) Characteristics of inorganic nitrogen assimilation of plants in fire-prone Mediterranean-type vegetation. Plant Cell Environ 16:351–363

    Google Scholar 

  • Sutton MA, Pitcairn CER, Fowler D (1993) The exchange of ammonia between the atmosphere and plant communities. Adv Ecol Res 24:301–393

    Google Scholar 

  • Väre H, Vestberg M, Eurola S (1992) Mycorrhiza and root-associated fungi in Spitsbergen. Mycorrhiza 1:93–104

    Google Scholar 

  • Virginia RA, Delwiche CC (1982) Natural 15N abundance of presumed N2-fixing and non-N2-fixing plants from selected ecosystems. Oecologia 54: 317–325

    Google Scholar 

  • Vitousek PM, Shearer G, Kohl DH (1989) Foliar 15N natural abundance in Hawaiian rainforests: patterns and possible mechanisms. Oecologia 54:317–325

    Google Scholar 

  • Voroney RP, Winter JP, Beyaert RP (1993) Soil microbial biomass C and N In: Carter MR (ed) Soil sampling and methods of analysis. Lewis, Boca Raton, pp 277–286

    Google Scholar 

Download references

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Michelsen, A., Schmidt, I.K., Jonasson, S. et al. Leaf 15N abundance of subarctic plants provides field evidence that ericoid, ectomycorrhizal and non-and arbuscular mycorrhizal species access different sources of soil nitrogen. Oecologia 105, 53–63 (1996). https://doi.org/10.1007/BF00328791

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