Response of nutrient cycles of an old-growth montane forest in Ecuador to experimental low-level nutrient amendments

Atmospheric nitrogen (N) and phosphorus (P) depositions are expected to increase in the tropicsrnas a consequence of increasing human activities in the next decades. Furthermore, a possiblernshortened El Niño Southern Oscillation cycle might come along with more frequent calcium (Ca)rndepositions on the eastern slope of the Ecuadorian Andes originating from Saharan dust. It isrncrucial to understand the response of the old-growth montane forest in Ecuador to increasedrnnutrient deposition to predict the further development of this megadiverse ecosystem.rnI studied experimental additions of N, P, N+P and Ca to the forest and an untreatedrncontrol, all in a fourfold replicated randomized block design. These experiments were conductedrnin the framework of a collaborative research effort, the NUtrient Manipulation EXperimentrn(NUMEX). I collected litter leachate, mineral soil solution (0.15 and 0.30 m depths), throughfallrnand fine litterfall samples and determined N, P and Ca concentrations and fluxes. This approachrnalso allowed me to assess whether N, P and/or Ca are limiting nutrients for forest growth.rnFurthermore, I evaluated the response of fine root biomass, leaf area index, leaf area and specificrnleaf area, tree diameter growth and basal area increment contributed from a cooperating group inrnthe Ca applied and control treatments.rnDuring the observation period of 16 months after the first fertilizer application, less thanrn10, 1 and 5% of the applied N, P and Ca, respectively, leached below the organic layer whichrncontained almost all roots but no significant leaching losses occurred to the deeper mineral soil.rnDeposited N, P and Ca from the atmosphere in dry and wet form were, on balance, retained in therncanopy in the control treatment. Retention of N, P and Ca in the canopy in their respectiverntreatments was reduced resulting in higher concentrations and fluxes of N, P and Ca inrnthroughfall and litterfall. Up to 2.5% of the applied N and 2% of the applied P and Ca werernrecycled to the soil with throughfall. Fluxes of N, P and Ca in throughfall+litterfall were higher inrnthe fertilized treatments than in the control; up to 20, 5 and 25% of the applied N, P and Ca,rnrespectively, were recycled to the soil with throughfall+litterfall.rnIn the Ca-applied plots, fine root biomass decreased significantly. Also the leaf area of thernfour most common tree species tended to decrease and the specific leaf area increasedrnsignificantly in Graffenrieda emarginata Triana, the most common tree species in the study area.rnThese changes are known plant responses to reduced nutrient stress. Reduced aluminium (Al)rntoxicity as an explanation of the Ca effect was unlikely, because of almost complete organocomplexationrnof Al and molar Ca:Al concentration ratios in solution above the toxicity threshold.rnThe results suggest that N, P and Ca co-limit the forest ecosystem functioning in thernnorthern Andean montane forests in line with recent assumptions in which different ecosystemrncompartments and even different phenological stages may show different nutrient limitationsrn(Kaspari et al. 2008). I conclude that (1) the expected elevated N and P deposition will bernretained in the ecosystem, at least in the short term and hence, quality of river water will not bernendangered and (2) increased Ca input will reduce nutrient stress of the forest.

On the cellular stress response to Staphylococcus aureus alpha-toxin

Staphylococcus aureus alpha-hemolysin was the first bacterial toxin recognized to form pores in the plasma membrane of eukaryotic cells. It is secreted as a water-soluble monomer that upon contact with target membranes forms an amphiphatic heptameric beta-barrel which perforates the bilayer. As a consequence, red cells undergo colloidosmotic lyses, while some nucleated cells may succumb to necrosis or programmed cell death. However, most cells are capable of repairing a limited number of membrane lesions, and then respond with productive transcriptional activation of NF-kB. In the present study, by using microarray and semiquantitative reverse transcriptase polymerase chain reaction (RT-PCR), data from a previously performed serial analysis of gene expression (SAGE) were extended and verified, revealing that immediate early genes (IEGs) such as c-fos, c-jun and egr-1 are strongly induced at 2-8 h after transient toxin treatment. Activating protein 1 (AP-1: c-Fos, c-Jun) binding activity was increased accordingly. As IEGs are activated by growth factors, these findings led to the discovery that -toxin promotes cell cycle progression of perforated cells in an EGFR-dependent fashion. Although the amount of c-fos mRNA rose rapidly after toxin treatment, c-Fos protein expression was observed only after a lag of about 3 h. Since translation consumes much ATP, which transiently drops after transient membrane perforation, the suspicion arised that membrane-perforation caused global, but temporary downregulation of translation. In fact, eIF2α became heavily phosphorylated minutes after cells had been confronted with the toxin, resulting in shutdown of protein synthesis before cellular ATP levels reached the nadir. GCN2 emerged as a candidate eIF2α kinase, since its expression rapidly increased in toxin-treated cells. Two hours after toxin treatment, GADD34 transcripts, encoding a protein that targets the catalytic subunit of protein phosphatase 1 (PP1) to the endoplasmic reticulum, were overexpressed. This was followed by dephosphorylation of eIF2α and resumption of protein synthesis. Addition of tautomycetin, a specific inhibitor of PP1, led to marked hyperphosphorylation of eIF2α and significantly reduced the drop of ATP-levels in toxin-treated cells. A novel link between two major stress-induced signalling pathways emerged when it was found that both translational arrest and restart were under the control of stress-activated protein kinase (SAPK) p38. The data provide an explanation for the indispensible role of p38 for defence against the archetypal threat of membrane perforation by agents that produce small transmembrane-pores.