Generierung und Transduktion wachstumsnegativer Signale durch den Contactinhibin-Rezeptor

Generierung und Transduktion wachstumsnegativer Signale durch den Contactinhibin-RezeptorDie kontaktabhängige Wachstumshemmung, Kontaktinhibition, basierend auf der Interaktion von Contactinhibin (Ci) und seinem Rezeptor (CiR), reguliert das Zellwachstum. Ziel dieser Arbeit war die Aufklärung der Signalweiterleitung über den CiR.Der transformierende Wachstumsfaktor TGF-beta führt in den meisten Zelltypen wie die Kontaktinhibition zum Zellzyklusstopp in der G1-Phase. Um mögliche Interaktionen der beiden Signalkaskaden zu untersuchen, wurden humane Keratinozyten (HaCaT) mit einem dominant-negativen TGF-beta-Rezeptor Typ II stabil transfiziert. Das Ausschalten des TGF-beta-Signalweges resultierte in einer erhöhten Sättigungsdichte und Aufhebung der Kontaktinhibition. Die durch Kontaktinhibition induzierte Zunahme der Expression der TGF-beta-mRNA bestätigte die mögliche Interaktion der beiden Signalwege.In einem weiteren Ansatz sollte die Proteinkinase C (PKC) als möglicher Second Messenger der Kontaktinhibition untersucht werden. Die Herunterregulierung der PKC-Isoformen alpha, delta, epsilon und mu nach Langzeit-Behandlung mit 12-O-Tetradecanoylphorbol-13-acetat führte in humanen Fibroblasten (FH109) zu einer Reduktion der Kontaktinhibition. Nur durch Inkubation mit dem spezifischen Inhibitor der delta-Isoform Rottlerin konnte die Kontaktinhibition vollständig aufgehoben werden. Eine Beteiligung der PKC-delta in die Kontaktinhibition wurde dadurch bestätigt, daß sowohl die Stärke ihrer Proteinexpression als auch ihre intrazelluläre Verteilung über Zell-Zellkontakte reguliert wurde. Außerdem führte die transiente Transfektion von Maus-Fibroblasten, NIH3T3, mit einer dominant-negativen Mutante der PKC-delta zu einem transformierten Phänotyp.

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.