Does nitrogen deposition affect soil microfungal diversity and soil N and P dynamics in a high Arctic ecosystem?

• Published in: Global Change Biology
• Main Authors: Robinson, C H, Saunders, P W, Madan, N J, Pryce-Miller, E J, Pentecost, A
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2004
• Subjects: Antarctic; Arctic; Greenland; Antarc*; Iceland; Shannon
• Online Access: https://kclpure.kcl.ac.uk/portal/en/publications/does-nitrogen-deposition-affect-soil-microfungal-diversity-and-soil-n-and-p-dynamics-in-a-high-arctic-ecosystem(9ce18a26-7318-4920-8e74-35f5327d0c1a).html; https://doi.org/10.1111/j.1529-8817.2003.00793.x; http://www.scopus.com/inward/record.url?scp=3242738169&partnerID=8YFLogxK

In a high Arctic polar semidesert ecosystem (ambient N deposition c. 0.1 g N m(-2) a(-1)), the effects of N enrichment on the diversity of soil microfungi and on N content and availability in organic and mineral soils were determined. Three N (total: 0, 0.5, 5 g N m(-2) a(-1)) and two P (total 0, 1 g m(-2) a(-1)) treatments were applied, since P may limit response to N in this ecosystem. Organic and mineral soils were sampled in June and August in the second year of treatment for microfungi, pH, moisture content, and total N and P. In the third year, soils were resampled for extractable and total N and P. The fungi isolated were typical of high pH soils in the High Arctic and Antarctic. The species richness and diversity of soil microfungi were very low, with ranges as follows: Shannon diversity, 0.56-1.5; richness, 2-6; evenness, 0.79-0.9. There was no significant effect of treatment on the frequency of occurrence of different taxa of soil microfungi. Time of sampling also had no significant impact on fungal assemblages, although different, more diverse communities were isolated from organic, rather than mineral, soils. Nitrate-N in organic soil decreased significantly when P was added alone, but not when P and N were added together. Addition of 0.5 g N m(-2) a(-1), a rate deposition already occurring in Greenland and Iceland, appeared to exceed N demand even when P limitation was relieved. There was no apparent soil acidification as a result of the N treatments.