Nitrogen deposition threatens species richness of grasslands across Europe

Evidence from an international survey in the Atlantic biogeographic region of Europe indicates that chronic nitrogen deposition is reducing plant species richness in acid grasslands. Across the deposition gradient in this region (2-44 kg N ha⁻¹ yr⁻¹) species richness showed a curvilinear response, with greatest reductions in species richness when deposition increased from low levels. This has important implications for conservation policies, suggesting that to protect the most sensitive grasslands resources should be focussed where deposition is currently low. Soil pH is also an important driver of species richness indicating that the acidifying effect of nitrogen deposition may be contributing to species richness reductions. The results of this survey suggest that the impacts of nitrogen deposition can be observed over a large geographical range.     

Diagnostic indicators of elevated nitrogen deposition

Tissue N content of mosses, which has been shown to be an indicator of enhanced N, was studied at a range of locations dominated either by wet or dry deposited and oxidised and reduced forms of N. Tissue N responded differently to wet and dry deposited N. For a 1 kg ha(-1) y(-1) increase in N deposition, tissue N increased by 0.01% at wet deposition sites but by 0.03% at sites dominated by dry deposited NH3. Tissue N at wet deposition sites responded more to concentrations of NO3- and NH4+ in precipitation (r(2) 0.63) than to total N deposition (r(2) 0.27), concentration explaining 66% of the variation in tissue N, wet deposition 33%. The study clearly concludes that tissue N concentration in mosses provides a good indication of N deposition at sites where deposition is dominated by NH3, and is also valuable in identifying vegetation exposed to large concentrations of NH4+ or NO3-, in wet deposition dominated areas, such as hilltops and wind exposed woodland edges.     

A NEW METHOD FOR SAMPLING SNOW MELT AND RAINFALL IN FORESTS1

ABSTRACT: Monitoring snow melt rates in high elevation, high snowfall forest stands is difficult mechanically and often impossible due to winter inaccessibility. A method for continuous unattended measurements of melt rate is described. With individual lysimeter pans connected to a common collector, any reasonable number of pans can be installed at each site.     

Ultrastructural and biochemical studies of intracellular metal-binding patterns in kidney tubule cells of the scallop Placopecten magellanicus following prolonged exposure to cadmium or copper

Sea scallops Placopecten magellanicus, which had been trawl-collected in late November, 1982 off the Rhode Island, USA coast, were exposed to 20 g of Cd or Cu per liter for a period of seven weeks in a flowing seawater system. Metal analyses of kidneys from both groups indicated uptake of both metals, although the tissue concentrations of Cd declined markedly in the Cu-treated scallops. The ultrastructural appearance of tubule cells of kidneys from Cd-exposed scallops was indistinguishable from controls. In contrast, tubule cells from scallops exposed to Cu showed marked cellular degeneration with loss of concretions. These ultrastructural changes were associated with significant reductions in renal isocitrate dehydrogenase activity in the Cu-treated scallops. Elemental analyses conducted on the kidney concretions and on the cytosolic metal-binding proteins of Cd-exposed scallops showed a 6-to 7-fold increase in Cd content of both these metalsequestering compartments, with concomitant changes in Zn, Mn, and Cu content. Loss of the concretions from Cu-treated scallops precluded analysis of this compartment, but Cu sequestration within cytosolic metal-binding proteins was associated with marked reductions of Zn and Cd from these proteins, suggesting disruption of this cellular mechanism for control of divalent metal cations. These findings support the hypothesis that toxic metal perturbation of normal homeostatic mechanisms that control divalent metal cation bioavailability is important factor in mediating cell injury from these agents.     

Uptake of 55Fe from contaminated sediments by the polychaete Nereis diversicolor

The polychaete Nereis diversicolor O. F. Müller was exposed to marine sediments which had been contaminated with ⁵⁵Fe either through the testing of nuclear devices or by the release of liquid waste effluent from a nuclear fuel reprocessing plant. The amount of ⁵⁵Fe taken up reached a concentration in the worms about 6% of the concentration in both types of sediment. Bioavailability of ⁵⁵Fe was shown to depend on its concentration in sediment and not on sediment type, stable iron concentration, or the source of contamination. N. diversicolor may not extract from sediment the same fraction of ⁵⁵Fe as does 0.1N HCl and caution should be exercised in using such measurements to represent the bioavailable fraction.     

An investigation of the impact of afforestation on stream-water chemistry in the Loch Dee catchment, SW Scotland

The impact of conifer afforestation on stream-water chemistry was investigated in the acidified catchment of Loch Dee, SW Scotland. Long-term trends in stream-water chemistry were evaluated during a period of forest growth from age 6 to 17 years. A significant increase was observed for pH (0.2 units) and a significant decline for aluminium (0.05 mg litre(-1)), sulphate (1.2 mg litre(-1)) and nitrate (0.02 mg litre(-1)) concentrations. The long-term decrease in stream-water acidity was ascribed to the marked reductions in sulphur depositions during the 1970s and early 1980s. There was no evidence that this response had been attenuated by afforestation, the improvements in stream-water chemistry being of a similar magnitude to those recorded in nearby moorland lochs and exceeding that in an adjacent moorland-catchment stream. The lack of a clear forest acidification effect is consistent with deposition-model estimates which show the increased scavenging of occult and dry deposition by the growing forest to be small at this site (相似文献   

Changes in the atmospheric deposition of acidifying compounds in the UK between 1986 and 2001

Emissions of a precursor of acidity in precipitation, sulphur dioxide (SO2), declined in the UK and the EU (15) by 71% and 72%, respectively, between 1986 and 2001, while nitrous oxide emissions declined by about 40%. Acidity in UK precipitation and the deposition of sulphate in precipitation halved during this period, but reductions were larger in the English Midlands than at the west coast and in high rainfall areas (>2000 mm). There is evidence that the smaller reductions in sulphur deposition in the west and south are due in part to shipping sources of SO2. Reductions in sulphur dry deposition (74%) are larger than in wet deposition (45%), due to changes in the canopy resistance to dry deposition. For reduced nitrogen, there has been a small (10%) reduction in emissions and deposition, while for oxidized nitrogen, a substantial reduction in emissions (40%) occurred but wet deposition of nitrate changed by less than 10%.     

Trace metal monitoring of pelagic organisms from the open Mediterranean Sea

During the periods 1974–75 and 1977 mixed microplankton and individual species of macrozooplankton and nekton were sampled from a number of areas in the mediterranean Sea in order to establish baseline levels of selected trace elements in pelagic species from the open Mediterranean. Trace elements analyzed were Ag, As, Cd, Co, Cs, Cu, Fe, Hg, Mn, Rb, Sc, Se, V, and Zn. Variability for concentrations of many of the trace elements was high, and broadly speaking if trace element concentrations in all species examined from any one area in the Mediterranean are considered, no general regional differences in element levels were evident. On the other hand, metal concentrations in certain individual pelagic species did suggest limited regional variations. No significant differences between metal concentrations in organisms collected in 1974–75 and 1977 were noted. For most of the elements, similar data for the same species collected in other years do not exist, therefore at present it is not possible to establish temporal trends for metals in pelagic Mediterranean organisms. Comparison of these results with data reported for similar species from other oceanic regions suggests that metal levels in open ocean organisms are no higher in the Mediterranean than elsewhere. It is concluded that long-term, open ocean ecological monitoring programmes, while useful and possible to carry out technically, may be severely limited by the high costs of shiptime and lack of long-term commitment and financial support from both national and international bodies.     

A field study of the generation of nitrate in a hill cap cloud

A field experiment to investigate the formation of nitrate as an airstream passes through a hill cap cloud has been performed at the UMIST field station on Great Dun Fell. It has been shown that the aerosol nitrate concentration increased by about 0.5 microg m(-3) as the airstream passed through the cloud during the night. At sunrise the nitrate production disappeared. It is suggested that the most likely mechanism for this nitrate production was due to the solution of N2O5 and NO3 formed from the reaction of NO2 with O3. These higher oxides build up overnight in the absence of short wave radiation to photolyse them. Other possible mechanisms of nitrate production are also discussed.     

Field scale N2O flux measurements from grassland using eddy covariance

In order to assess nitrous oxide (N₂O) emissions from typical intensively managed grassland in northern Britain fluxes were measured by eddy covariance using tuneable diode laser absorption spectroscopy from June 2002 to June 2003 for a total period of 4000 h. With micrometeorological techniques it is possible to obtain a very detailed picture of the fluxes of N₂O at field scale (10³–10⁴ m²), which are valuable for extrapolation to regional scales. In this paper three of the four fertilizer applications were investigated in detail. N₂O emissions did not always show a clear response. Hourly fluxes were very large immediately after the June 2002 nitrogen fertilizer application, peaking at 2.5 mg N₂O–N m^–2 s^–1. Daily fluxes were averaging about 300 ng N₂O m^–2 s^–1 over the 4 days following fertilizer application. The response of N₂O emissions was less evident after the August fertilization, although 2 days after fertilizer application an hourly maximum flux of 554 ng N₂O–N m^–2 s^–1 was registered. For the rest of August the flux was undetectable. The differences between fertilization events can be explained by different environmental conditions, such as soil temperature and rainfall. A fertiliser-induced N₂O emission was not observed after fertilizer application in March 2003, due to lack of rainfall. The total N₂O flux from June 2002 to June 2003 was 5.5 kg N₂O–N ha^–1y^–1, which is 2.8% of the total annual N fertilizer input.