Constitutively active cAMP receptor mutants dominantly inhibit receptor-mediated signaling pathways in Dictyostelium discoideum

Dictyostelium, a soil amoeba, is able to develop from free-living cells to multicellular fruiting bodies upon starvation using extracellular cAMP to mediate cell-cell communication, chemotaxis and developmental gene expression. The seven transmembrane G protein-coupled cAMP receptor-1 (cAR1) mediated responses, such as the activation of adenylyl cyclase and guanylyl cyclase, are transient, due to the existence of poorly understood adaptation mechanisms. For this dissertation, the powerful genetics of the Dictyostelium system was employed to study the adaptation mechanism of cAR1-mediated cAMP signaling as well as mechanisms intrinsic to cAR1 that regulate its activation. ^ We proposed that constitutively active cAR1 would cause constant adaptation, thus inhibiting downstream pathways that are essential for aggregation and development. Therefore, a screen for dominant negative cAR1 mutants was undertaken to identify constitutively active receptor mutants. Three dominant negative cAR1 mutants were identified. All appear to be constitutively active receptor mutants because they are constitutively phosphorylated and possess high affinity for cAMP. Biochemical studies showed that these mutant receptors prevented the activation of downstream effectors, including adenylyl and guanylyl cyclases. In addition, these cells also were defective in cAMP chemotaxis and cAR1-mediated gene expression. These findings suggest that the mutant receptors block development by constantly activating multiple adaptation pathways. ^ Sequence analysis revealed that these mutations (I104N, L100H) are clustered in a conserved region of the third transmembrane helix (TM3) of cAR1. To investigate the role of this region in receptor activation, one of these residues, I104, was mutated to all the other 19 possible amino acids. We found that all but the most conservative substitutions increase the receptor's affinity about 20- to 70-fold. However, only highly polar substitutions of I104, particularly basic residues, resulted in receptors that are constitutively phosphorylated and dominantly inhibit development, suggesting that highly polar substitutions not only disrupt an interaction constraining the receptor in its low-affinity, inactive state but also promote an additional conformational change that resembles the ligand-bound conformation. Our findings suggest that I104 plays a specific role in constraining the receptor in its inactive state and that substituting it with highly polar residues results in constitutive activation. ^

Molecular mechanism of the relaxin signaling pathways: Activation of cAMP, PI3K, and PKCzeta

Relaxin is a polypeptide hormone that has diverse effects on reproductive and non-reproductive tissues. Relaxin activates the G-protein coupled receptors, LGR7 and LRG8. Early studies described increased cAMP and protein kinase A activity upon relaxin treatment, but cAMP accumulation alone could not account for all of the relaxin-mediated effects. We utilized the human monocyte cell line THP-1 to study the mechanism of relaxin-stimulated CAMP production. ^ Relaxin treatment in THP-1 cells produces a biphasic time course in cAMP accumulation, where the first peak appears as early as 1–2 minutes with a second peak at 10–20 minutes. Selective inhibitors for phosphoinositide 3-kinase (P13K), such as wortmannin and LY294002, show a dose-dependent inhibition of relaxin-stimulated cAMP accumulation, specific for the second peak of the relaxin time course. Neither the effects of relaxin nor the inhibition of relaxin by LY294002 is mediated by the activity of phosphodiesterases. Furthermore, LY294002 blocks upregulation of vascular endothelial growth factor transcript levels by relaxin. ^ To further delineate relaxin signaling pathways, we searched for downstream targets of PI3K that could activate adenylyl cyclase (AC). Protein kinase C ζ (PKCζ) was a prime candidate because it activates types II and V AC. Chelerythrine chloride (a general PKC inhibitor) inhibits relaxin-induced cAMP production to the same degree as LY294002 (∼40%). Relaxin stimulates PKCζ translocation to the plasma membrane in THP-1, MCF-7, PHM1-31, and MMC cells, as shown by immunocytochemistry. PKCζ translocation is P13K-dependent and independent of cAMP production. Antisense PKCζ oligodeoxynucleotides (PKCζ-ODNs) deplete both PKCζ transcript and protein levels in THP-1 cells. PKCζ-ODNs abolish relaxin-mediated PKCζ translocation and inhibit relaxin stimulation of cAMP by 40%, as compared to mock and random ODN controls. Treatment with LY294002 in the presence of PKCζ-ODNs results in little further inhibition. Taken together, we present a novel role for PI3K and PKCζ in relaxin stimulation of cAMP and provide the first example of the PKCζ regulation of AC in an endogenous system. Furthermore, we have identified higher order complexes of AC isoforms and PKA anchoring proteins in attempts to explain the differential coupling of relaxin to cAMP and PI3K-signaling pathways in various cell types. ^

La política y la poética del CAMP

Fil: Amícola, José. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

La política y la poética del CAMP

Fil: Amícola, José. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

La política y la poética del CAMP

Fil: Amícola, José. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Snow height on sea ice and sea ice drift from autonomous measurements from buoy 2013S3, deployed at the Barneo ice camp 2013

Snow height was measured by the Snow Depth Buoy 2013S3, an autonomous platform, drifting on Arctic sea ice. This buoy was deployed at the Barneo ice camp 2013. The resulting time series describes the evolution of snow height as a function of place and time between 2013-04-09 and 2013-06-13 in sample intervals of 1 hour. The Snow Depth Buoy consists of four independent sonar measurements representing the area (approx. 10 m**2) around the buoy. The buoy was installed on multi year ice. In addition to snow height, geographic position (GPS), barometric pressure, air temperature, and ice surface temperature were measured. Negative values of snow height occur if surface ablation continues into the sea ice. Thus, these measurements describe the position of the sea ice surface relative to the original snow-ice interface. Differences between single sensors indicate small-scale variability of the snow pack around the buoy. The data set has been processed, including the removal of obvious inconsistencies (missing values). Records without any snow height may still be used for sea ice drift analyses.