Caspase-mediated cleavage of the exosome subunit PM/Scl-75 during apoptosis

Recent studies have implicated the dying cell as a potential reservoir of modified autoantigens that might initiate and drive systemic autoimmunity in susceptible hosts. A number of subunits of the exosome, a complex of 3'→5' exoribonucleases that functions in a variety of cellular processes, are recognized by the so-called anti-PM/Scl autoantibodies, found predominantly in patients suffering from an overlap syndrome of myositis and scleroderma. Here we show that one of these subunits, PM/Scl-75, is cleaved during apoptosis. PM/Scl-75 cleavage is inhibited by several different caspase inhibitors. The analysis of PM/Scl-75 cleavage by recombinant caspase proteins shows that PM/Scl-75 is efficiently cleaved by caspase-1, to a smaller extent by caspase-8, and relatively inefficiently by caspase-3 and caspase-7. Cleavage of the PM/Scl-75 protein occurs in the C-terminal part of the protein at Asp369 (IILD369↓G), and at least a fraction of the resulting N-terminal fragments of PM/Scl-75 remains associated with the exosome. Finally, the implications of PM/Scl-75 cleavage for exosome function and the generation of anti-PM/Scl-75 autoantibodies are discussed.

Endocytic trafficking and oligodendroglial exosome secretion in axon-glia communication and myelination

Oligodendrocytes form specialized plasma membrane extensions which spirally enwrap axons, thereby building up the myelin sheath. During myelination, oligodendrocytes produce large amounts of membrane components. Oligodendrocytes can be seen as a complex polarized cell type with two distinct membrane domains, the plasma membrane surrounding the cell body and the myelin membrane. SNARE proteins mediate the fusion of vesicular cargoes with their target membrane. We propose a model in which the major myelin protein PLP is transported by two different pathways. VAMP3 mediates the non-polarized transport of newly synthesized PLP via recycling endosomes to the plasma membrane, while transport of PLP from late endosomes/lysosomes to myelin is controlled by VAMP7. In the second part of the thesis, the role of exosome secretion in glia to axon signaling was studied. Further studies are required to clarify whether VAMP7 also controls exosome secretion. The thesis further focused on putative metabolic effects in the target neurons. Oligodendroglial exosomes showed no obvious influences on neuronal metabolic activity. Analysis of the phosphorylation levels of the neurofilament heavy subunit revealed a decrease in presence of oligodendrocytes, indicating effects of oligodendroglial exosomes on the neuronal cytoskeleton. Finally, candidates for kinases which are possibly activated upon influence of oligodendroglial exosomes and could influence neuronal survival were identified.

Temporal and Spatial Coexistence of Archaeal and Bacterial amoA Genes and Gene Transcripts in Lake Lucerne

Despite their crucial role in the nitrogen cycle, freshwater ecosystems are relatively rarely studied for active ammonia oxidizers (AO). This study of Lake Lucerne determined the abundance of both amoA genes and gene transcripts of ammonia-oxidizing archaea (AOA) and bacteria (AOB) over a period of 16 months, shedding more light on the role of both AO in a deep, alpine lake environment. At the surface, at 42 m water depth, and in the water layer immediately above the sediment, AOA generally outnumbered AOB. However, in the surface water during summer stratification, when both AO were low in abundance, AOB were more numerous than AOA. Temporal distribution patterns of AOA and AOB were comparable. Higher abundances of amoA gene transcripts were observed at the onset and end of summer stratification. In summer, archaeal amoA genes and transcripts correlated negatively with temperature and conductivity. Concentrations of ammonium and oxygen did not vary enough to explain the amoA gene and transcript dynamics. The observed herbivorous zooplankton may have caused a hidden flux of mineralized ammonium and a change in abundance of genes and transcripts. At the surface, AO might have been repressed during summer stratification due to nutrient limitation caused by active phytoplankton.

THE DOMAINS OF THE CATALYTIC SUBUNIT OF THE EUKARYOTIC RNA DEGRADING EXOSOME, RRP44P, HAVE DISTINCT FUNCTIONS

The exosome is a 3’ to 5’ exoribonuclease complex that consists of ten essential subunits. In the cytoplasm, the exosome degrades mRNA in a general mRNA turnover pathway and in several mRNA surveillance pathways. In the nucleus, the exosome processes RNA precursors to form small, stable, mature RNA species, including rRNA, snRNA, and snoRNA. In addition to processing these RNAs, the nuclear exosome is also involved in degrading aberrantly processed forms of these RNAs, and others, including mRNA. The 3’ to 5’ exoribonuclease activity of the exosome is contributed by the RNB domain of the only catalytically active subunit, Rrp44p, a member of the RNase II family of enzymes. In addition to the RNB domain, Rrp44p consists of three putative RNA binding domains and has an uncharacterized N-terminus, which includes a CR3 region and PIN domain. In an effort to characterize the cellular functions of the domains of Rrp44p, this study identified a second nuclease active site in the PIN domain. Specifically, the PIN domain exhibits endoribonuclease activity in vitro and is essential for exosome function. Further analysis of the nuclease activities of Rrp44p indicate a role for the exoribonuclease activity of Rrp44p in the cytoplasmic and nuclear exosome. This work has also characterized the CR3 region of Rrp44p, a region that has not yet been characterized in any other protein. This region is needed for the majority, if not all, of the cytoplasmic exosome functions as well as for interaction with the exosome. The CR3 region, along with a histidine residue in the N-terminus of Rrp44p, may coordinate a zinc atom. Preliminary evidence supports a role for this coordination in exosome function. Further investigation, however, is needed to determine the molecular dependence of the exosome on the CR3 region of Rrp44p. Despite its initial discovery thirteen years ago, the essential function of Rrp44p, and the exosome, is not yet known. The studies presented here, however, indicate that the essential function of Rrp44p and the exosome is in the nucleus and depends on the nuclease activities of Rrp44p.

Phototaxis signaling by the membrane complex of archaeal sensory rhodopsins and their transducers

Sensory rhodopsins I and II (SRI and SRII) are visual pigment-like phototaxis receptors in the archaeon Halobacterium salinarum. The receptor proteins each consist of a single polypeptide that folds into 7 $\alpha$-helical membrane-spanning segments forming an internal pocket where the chromophore retinal is bound. They transmit signals to their tightly bound transducer proteins, HtrI and HtrII, respectively, which in turn control a phosphotransfer pathway modulating the flagellar motors. SRI-HtrI mediates attractant responses to orange-light and repellent responses to UV light, while SRII-HtrII mediates repellent response to blue light. Experiments were designed to analyze the molecular processes in the SR-Htr complexes responsible for receptor activation, which previously had been shown by our laboratory to involve proton transfer reactions of the retinylidene Schiff base in the photoactive site, transfer of signals from receptor to transducer, and signaling specificity by the receptor-transducer complex.^ Site-directed mutagenesis and laser-flash kinetic spectroscopy revealed that His-166 in SRI (i) plays a role in the proton transfers both to and from the Schiffbase, either as a structurally critical residue or possibly as a direct participant, (ii) is involved in the modulation of SIU photoreaction kinetics by HtrI, and (iii) modulates the pKa of Asp-76, an important residue in the photoactive site, through a long-distance electrostatic interaction. Computerized cell tracking and motion analysis demonstrated that (iv) His-166 is crucial in phototaxis signaling: a spectrum of substitutions either eliminate signaling or greatly perturb the activation process that produces attractant and repellent signaling states of the receptor.^ The signaling states of SRI are communicated to HtrI, whose oligomeric structure and conformational changes were investigated by engineered sulfhydryl probes. It was found that signaling by the SRI-HtrI complex involves reversible conformational changes within a preexisting HtrI dimer, which is likely accomplished through a slight winding or unwinding of the two HtrT monomers via their loose coiled coil association. To elucidate which domains of the Htr dimers confer specificity for interaction with SRI or SRII, chimeras of HtrI and HtrII were constructed. The only determinant needed for functional and specific interaction with SRI or SRII was found to be the four transmembrane segments of the HtrI or HtrII dimers, respectively. The entire cytoplasmic parts of HtrI and HtrII, which include the functionally important signaling and adaptation domains, were interchangeable.^ These observations support a model in which SRI and SRII undergo conformational changes coupled to light-induced proton transfers in their photoactive sites, and that lateral helix-helix interactions with their cognate transducers' 4-helix bundle in the membrane relay these conformational changes into different states of the Htr proteins which regulate the down-stream phosphotransfer pathway. ^

The Role of the Arched Helicases in Exosome-Mediated Function

RNA processing and degradation are two important functions that control gene expression and promote RNA fidelity in the cell. A major ribonuclease complex, called the exosome, is involved in both of these processes. The exosome is composed of ten essential proteins with only one catalytically active subunit, called Rrp44. While the same ten essential subunits make up both the nuclear and cytoplasmic exosome, there are nuclear and cytoplasmic exosome cofactors that promote specific exosome functions in each of the cell compartments. To date, it is unclear how the exosome distinguishes between RNA substrates. We hypothesize that compartment specific cofactors may promote the substrate specificity of the exosome. In this work, I characterize several cofactors of the exosome, both nuclear and cytoplasmic. First, I describe the arch domain, which is a unique domain in a nuclear and a cytoplasmic cofactor of the exosome. Specifically, I show that the arch domain of the nuclear exosome cofactor, Mtr4, is required for specific exosome-mediated activities and overlaps functionally with the exosome-associated exonuclease, Rrp6. Further, I show that the arch domain of Ski2 is required for the degradation of normal and aberrant mRNAs. Additionally, this work describes in detail the Mtr4 domains involved in the physical association with other RNA processing proteins. Further, I characterize the minimal Mtr4-binding region in a third exosome cofactor, Trf5. Understanding how exosome cofactors synergistically promote exosome function will provide us a better understanding of how the exosome complex precisely regulates its catalytic activities. As described here, cofactors play a major role in determining the substrate specificity of the nuclear and cytoplasmic exosome. Moreover, specific accessory domains, which are not involved in the catalytic function of the cofactor, are required for substrate targeting of the eukaryotic RNA exosome.

Development of bacterial and archaeal communities in erupted subsurface muds at the Håkon Mosby mud volcano

The microbial oxidation of methane controls the emission of the greenhouse gas methane from the ocean floor. However, some seabed structures such as mud volcanoes have leaky microbial methane filters and can be important sources of methane. We investigated the disturbance and recovery of a methanotrophic mud volcano microbiome (Håkon Mosby mud volcano, 1250 m water depth), to assess time scales of community succession and function in the natural deep-sea environment. We analyzed 10 surface and 5 subsurface sediment samples across HMMV mud flows from most recently discharged subsurface muds towards old consolidated muds as well as one reference site (REF) located approximately 0.5 km outside of the HMMV. Surface samples were obtained in 2003, 2009 and 2010. The surface of the new mud flows at the geographical center was sampled in 2009 and 2010. Around 100 m south of the center, we sampled more consolidated aged muds in 2003 and 2010. Old mud flows were sampled around 300 m southeast and 100 m north of the geographical center in 2003, 2009 and 2010. Surface sediment samples (0-20 cm) were recovered either by TV-guided Multicorer or by push cores using the remotely operated vehicle Quest (Marum, University Bremen). Subsurface sediments of all zones (>2 m below sea floor) were obtained in 2003 by gravity corer. After recovery, sediments were immediately subsampled in a refrigerated container (0°C) and further processed for biogeochemical analyses or preserved at -20°C for later DNA analyses. Our study show that freshly erupted muds hosted heterotrophic deep subsurface communities, which were replaced by surface communities within a few years of exposure. Aerobic methanotrophy was established at the top surface layer within less than a year, followed by anaerobic methanotrophy, sulfate reduction and finally thiotrophy. Our data indicate that it takes decades in cold environments before efficient methanotrophic communities establish to control methane emission. The observed succession provides insights to the response time of complex deep-sea communities to seafloor disturbances.