Journal
BIOLOGY AND FERTILITY OF SOILS
Volume 50, Issue 1, Pages 191-196Publisher
SPRINGER
DOI: 10.1007/s00374-013-0838-y
Keywords
Acidification; Ammonium; Critical N load; Eutrophication; N deposition; Plant diversity; Soil faunal community
Categories
Funding
- Spanish Ministerio de Educacion y Ciencia [CGL-2009-11015]
- Autonomous Community of Madrid [REMEDINAL-2 S2009/AMB-1783]
- European Research Council under the European Community/ERC [242658]
- BIOCOM project
- Leverhulme Early Career Fellowship
- European Science foundation Nitrogen in Europe programme
- Percy Sladen Memorial Fund
- Natural Environment Research Council [ceh010010] Funding Source: researchfish
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Nitrogen (N) deposition is a major threat to the semiarid Mediterranean ecosystems. We simulated a gradient of N deposition (0, 10, 20 and 50 kg N ha(-1) year(-1) + 6.4 kg N ha(-1) year(-1) ambient deposition) in a Mediterranean shrubland from central Spain. In autumn 2011 (after 4 years of experimental duration), soil cores were taken to extract the soil fauna. Acari (45.54%) and Collembola (44.00%) were the most represented taxonomical groups, and their abundance was negatively related to soil pH. Simulated N deposition had an impact on the total number of individuals in soil as well as on Collembola and Pauropoda abundance. Collembola abundance increased with N loads up to 20 kg N ha(-1) year(-1) and then decreased. This response was attributed to soil acidification (between 0 and 20 kg N ha(-1) year(-1)) and increased soil ammonium (between 20 and 50 kg N ha(-1) year(-1)). Pauropoda were favoured by additions of 50 kg N ha(-1) year(-1), and it was the only taxonomical group whose abundance was exclusively related to N deposition, suggesting their potential as bioindicators. Contrary to predictions, there was a negative relationship between soil faunal abundance and plant diversity. In conclusion, soil faunal communities from semiarid Mediterranean ecosystems in central Spain seem to be primarily influenced by soil chemistry (mainly pH) but are also susceptible to increased N deposition. The main drivers of change under increased N deposition scenarios seem to be soil acidification and increased ammonium in soils where nitrate is the dominant mineral N form.
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