LRP1 modulates APP trafficking and APP metabolism within compartments of the secretory pathway. Increased AICD generation is ineffective in nuclear translocation and transcriptional activation

LRP1 modulates APP trafficking and metabolism within compartments of the secretory pathway The amyloid precursor protein (APP) is the parent protein to the amyloid beta peptide (Abeta) and is a central player in Alzheimer’s disease (AD) pathology. Abeta liberation depends on APP cleavage by beta- and gamma-secretases. To date, only a unilateral view of APP processing exists, excluding other proteins, which might be transported together and/or processed dependent on each other by the secretases described above. The low density lipoprotein receptor related protein 1 (LRP1) was shown to function as such a mediator of APP processing at multiple steps. Newly synthesized LRP1 can interact with APP, implying an interaction between these two proteins early in the secretory pathway. Therefore, we wanted to investigate whether LRP1 can mediate APP trafficking along the secretory pathway, and, if so, whether it affects APP processing. Indeed, we demonstrate that APP trafficking is strongly influenced by LRP1 transport through the endoplasmic reticulum (ER) and Golgi compartments. LRP1-constructs with ER- and Golgi-retention motifs (LRP-CT KKAA, LRP-CT KKFF) had the capacity to retard APP trafficking at the respective steps in the secretory pathway. Here, we provide evidence that APP metabolism occurs in close conjunction with LRP1 trafficking, highlighting a new role of lipoprotein receptors in neurodegenerative diseases. Increased AICD generation is ineffective in nuclear translocation and transcriptional activity A sequence of amyloid precursor protein (APP) cleavages gives rise to the APP intracellular domain (AICD) together with amyloid beta peptide (Abeta) and/or p3 fragment. One of the environmental factors identified favouring the accumulation of AICD appears to be a rise in intracellular pH. This accumulation is a result of an abrogated cleavage event and does not extend to other secretase substrates. AICD can activate the transcription of artificially expressed constructs and many downstream gene targets have been discussed. Here we further identified the metabolism and subcellular localization of the constructs used in this well documented gene reporter assay. We also co-examined the mechanistic lead up to the AICD accumulation and explored possible significances for its increased expression. We found that most of the AICD generated under pH neutralized conditions is likely that cleaved from C83. Furthermore, the AICD surplus is not transcriptionally active but rather remains membrane tethered and free in the cytosol where it interacts with Fe65. However, Fe65 is still essential in AICD mediated transcriptional transactivation although its exact role in this set of events is unclear.

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.