Reise-Protokoll der Reichstagsdeputation nach Innsbruck: Deputations-Mitglieder: 1. Herr Franz Schmitt, für Nieder-Oesterreich ...: Die drei sub 3 bis 5 verzeichneten Deputations-Mitglieder reiseten Montags den 31. Juli 1848 ...

Welsch (Projektbearbeiter): Eingehende Schilderung der Reise einer Reichstagsdeputation nach Innsbruck (31. Juli - 9. August 1848) anläßlich der bevorstehenden Rückkehr Kaiser Ferdinands I. nach Wien

Rede, gehalten bei dem Trauerg[o]ttesdienst zum Gedächtniss des seligen Freiherrn Wilhelm Carl von Rothschild in der Synagoge zu Lübeck, am Sonntag, den 14. Schwat 5661 (3. Febr. 1901), Nachm. 4 Uhr

von S. Carlebach

Molecular consequences of the loss of 3'→5' exonuclease activity of DNA polymerases delta and epsilon

The DNA replication polymerases δ and ϵ have an inherent proofreading mechanism in the form of a 3'→5' exonuclease. Upon recognition of errant deoxynucleotide incorporation into DNA, the nascent primer terminus is partitioned to the exonuclease active site where the incorrectly paired nucleotide is excised before resumption of polymerization. The goal of this project was to identify the cellular and molecular consequences of an exonuclease deficiency. The proofreading capability of model system MEFs with EXOII mutations was abolished without altering polymerase function.^ It was hypothesized that 3'→5' exonucleases of polymerases δ and ϵ are critical for prevention of replication stress and important for sensitization to nucleoside analogs. To test this hypothesis, two aims were formulated: Determine the effect of the exonuclease active site mutation on replication related molecular signaling and identify the molecular consequences of an exonuclease deficiency when replication is challenged with nucleoside analogs.^ Via cell cycle studies it was determined that larger populations of exonuclease deficient cells are in the S-phase. There was an increase in levels of replication proteins, cell population growth and DNA synthesis capacity without alteration in cell cycle progression. These findings led to studies of proteins involved in checkpoint activation and DNA damage sensing. Finally, collective modifications at the level of DNA replication likely affect the strand integrity of DNA at the chromosomal level.^ Gemcitabine, a DNA directed nucleoside analog is a substrate of polymerases δ and ϵ and exploits replication to become incorporated into DNA. Though accumulation of gemcitabine triphosphate was similar in all cell types, incorporation into DNA and rates of DNA synthesis were increased in exonuclease defective cells and were not consistent with clonogenic survival. This led to molecular signaling investigations which demonstrated an increase in S-phase cells and activation of a DNA damage response upon gemcitabine treatment.^ Collectively, these data indicate that the loss of exonuclease results in a replication stress response that is likely required to employ other repair mechanisms to remove unexcised mismatches introduced into DNA during replication. When challenged with nucleoside analogs, this ongoing stress response coupled with repair serves as a resistance mechanism to cell death.^

IV Jornadas de Graduados - Jóvenes Investigadores : La Plata, Facultad de Humanidades y Ciencias de la Educación de la UNLP, 3 a 5 de octubre de 2012

Fil: Cairo, María Emilia. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

IV Jornadas de Graduados - Jóvenes Investigadores : La Plata, Facultad de Humanidades y Ciencias de la Educación de la UNLP, 3 a 5 de octubre de 2012

Fil: Cairo, María Emilia. Universidad Nacional de La Plata. Facultad de Humanidades y Ciencias de la Educación; Argentina.

Particle camera and settling chamber measurements at site PC (GeoB11834-3) and SC (GeoB12914-4) off Cape Blanc/Mauritania

Particles sinking out of the euphotic zone are important vehicles of carbon export from the surface ocean. Most of the particles produce heavier aggregates by coagulating with each other before they sink. We implemented an aggregation model into the biogeochemical model of Regional Oceanic Modelling System (ROMS) to simulate the distribution of particles in the water column and their downward transport in the Northwest African upwelling region. Accompanying settling chamber, sediment trap and particle camera measurements provide data for model validation. In situ aggregate settling velocities measured by the settling chamber were around 55 m d**-1. Aggregate sizes recorded by the particle camera hardly exceeded 1 mm. The model is based on a continuous size spectrum of aggregates, characterised by the prognostic aggregate mass and aggregate number concentration. Phytoplankton and detritus make up the aggregation pool, which has an averaged, prognostic and size dependent sinking. Model experiments were performed with dense and porous approximations of aggregates with varying maximum aggregate size and stickiness as well as with the inclusion of a disaggregation term. Similar surface productivity in all experiments has been generated in order to find the best combination of parameters that produce measured deep water fluxes. Although the experiments failed to represent surface particle number spectra, in the deep water some of them gave very similar slope and spectrum range as the particle camera observations. Particle fluxes at the mesotrophic sediment trap site off Cape Blanc (CB) have been successfully reproduced by the porous experiment with disaggregation term when particle remineralisation rate was 0.2 d**-1. The aggregation-disaggregation model improves the prediction capability of the original biogeochemical model significantly by giving much better estimates of fluxes for both upper and lower trap. The results also point to the need for more studies to enhance our knowledge on particle decay and its variation and to the role that stickiness play in the distribution of vertical fluxes.

Ladderane lipid analysis and pore water and sediment chemistry of sediment cores from the continental shelf and slope off northwest Africa

The presence and abundance of anaerobic ammonium-oxidizing (anammox) bacteria was investigated in continental shelf and slope sediments (300-3000 m water depth) off northwest Africa in a combined approach applying quantitative polymerase chain reaction (q-PCR) analysis of anammox-specific 16S rRNA genes and anammox-specific ladderane biomarker lipids. We used the presence of an intact ladderane monoether lipid with a phosphocholine (PC) headgroup as a direct indicator for living anammox bacteria and compared it with the abundance of ladderane core lipids derived from both living and dead bacterial biomass. All investigated sediments contained ladderane lipids, both intact and core lipids, in agreement with the presence of anammoxspecific 16S rRNA gene copies, indicating that anammox occurs at all sites. Concentrations of ladderane core lipids in core top sediments varied between 0.3 and 97 ng g**-1 sediment, with the highest concentrations detected at the sites located on the shelf at shallower water depths between 300 and 500 m. In contrast, the C20 [3]-ladderane monoether-PC lipid was most abundant in a core top sediment from 1500 m water depth. Both anammox-specific 16S rRNA gene copy numbers and the concentration of the C20 [3]-ladderane monoether-PC lipid increased downcore in sediments located at greater water depths, showing highest concentrations of 1.2 x 10**8 copies g**-1 sediment and 30 pg g**-1 sediment, respectively, at the deepest station of 3000 m water depth. This suggests that the relative abundance of anammox bacteria is higher in sediments at intermediate to deep water depths where carbon mineralization rates are lower but where anammox is probably more important than denitrification.