Oxidative DNA Damage Modulates Trinucleotide Repeat Instability Via DNA Base Excision Repair

Trinucleotide repeat (TNR) expansion is the cause of more than 40 types of human neurodegenerative diseases such as Huntington’s disease. Recent studies have linked TNR expansion with oxidative DNA damage and base excision repair (BER). In this research, we provided the first evidence that oxidative DNA damage can induce CAG repeat deletion/contraction via BER. We found that BER of an oxidized DNA base lesion, 8-oxoguanine in a CAG repeat tract, resulted in the formation of a CTG hairpin at the template strand. DNA polymerase β (pol b) then skipped over the hairpin creating a 5’-flap that was cleaved by flap endonuclease 1 (FEN1) leading to CAG repeat deletion. To further investigate whether BER may help to shorten an expanded TNR tract, we examined BER in a CAG repeat hairpin loop. We found that 8-oxoguanine DNA glycosylase removed the oxidized base located in the loop region of the hairpin leaving an abasic site. Apurinic/apyrimidinic (AP) endonuclease 1 then incised the 5’-end of the abasic site leaving a nick in the loop. This further converted the hairpin into an intermediate with a 3’-flap and a 5’-flap. As a 5’-3’ endonuclease, FEN1 cleaved the 5’-flap, whereas a 3’-5’ endonuclease, Mus81/Eme1, removed the 3’-flap. The coordination between FEN1 and Mus81/Eme1 ultimately resulted in removal of a CAG repeat hairpin attenuating or preventing TNR expansion. To further explore if pol β bypass of an oxidized base lesion, 5’,8-cyclodeoxyadenosine, may affect TNR instability, we examined pol β DNA synthesis in bypassing this base lesion and found that the lesion preferentially induced TNR deletion during BER and Okazaki fragment maturation. The repeat deletion was mediated by the formation of a loop in the template strand induced specifically by the damage. Pol β then skipped over the loop structure creating a 5’-flap that was efficiently removed by FEN1 leading to repeat deletion. Our study demonstrates that pol β-mediated BER plays an important role in mediating TNR deletion and removing a TNR hairpin to prevent TNR expansion. Our research provides a molecular basis for further developing BER as a target for prevention and treatment of neurodegenerative diseases caused by TNR expansion.

Delta 44/40 Ca, Mg/Ca and Sr/Ca record of Globigerinoides sacculifer and calculated temperatures and salinity changes of ODP Hole 165-999A

The delta18O values of planktonic foraminifera increased in the Caribbean by about 0.5? relative to the equatorial East Pacific values between 4.6 and 4.2 Ma as a consequence of the closure of the Central American Gateway (CAG). This increase in delta18O can be interpreted either as an increase in Caribbean sea surface (mixed layer) salinity (SSS) or as a decrease in sea surface temperatures (SST). This problem represents an ideal situation to apply the recently developed paleotemperature proxy delta44/40Ca together with Mg/Ca and d18O on the planktic foraminifer Globigerinoides sacculifer from ODP Site 999. Although differences in absolute temperature calibration of delta44/40Ca and Mg/Ca exist, the general pattern is similar indicating a SST decrease of about 2-3 8C between 4.4 and 4.3 Ma followed by an increase in the same order of magnitude between 4.3 and 4.0 Ma. Correcting the delta18O record for this temperature change and assuming that changes in global ice volume are negligible, the salinity-induced planktonic delta18O signal decreased by about 0.4? between 4.4 and 4.3 Ma and increased by about 0.9? between 4.3 and 4.0 Ma in the Caribbean. The observed temperature and salinity trends are interpreted to reflect the restricted exchange of surface water between the Caribbean and the Pacific in response to the shoaling of the Panamanian Seaway, possibly accompanied by a southward shift of the Intertropical Convergence Zone (ITCZ) between 4.4 and 4.3 Ma. Differences in Mg/Ca- and delta44/40Ca-derived temperatures can be reconciled by corrections for secular variations of the marine Mg/Ca[sw] and delta44/40Ca, a salinity effect on the Mg/Ca ratio and a constant temperature offset of ~2.5 °C between both SST proxy calibrations.

Age model and pollen analysis from site GIK16867 in the northern Angola Basin

Sporomorphs and dinoflagellate cysts from site GIK16867 in the northern Angola Basin record the vegetation history of the West African forest during the last 700 ka in relation to changes in salinity and productivity of the eastern Gulf of Guinea. During most cool and cold periods, the Afromontane forest, rather than the open grass-rich dry forest, expanded to lower altitudes partly replacing the lowland rain forest of the borderlands east of the Gulf of Guinea. Except in Stage 3, when oceanic productivity was high during a period of decreased atmospheric circulation, high oceanic productivity is correlated to strong winds. The response of marine productivity in the course of a climatic cycle, however, is earlier than that of wind vigour and makes wind-stress-induced oceanic upwelling in the area less likely. Monsoon variation is well illustrated by the pollen record of increased lowland rain forest that is paired to the dinoflagellate cyst record of decreased salinity forced by increased precipitation and run-off.

Pollen flux off Cape Blanc

Fluxes of airborne freshwater diatoms (FD), phytoliths (PH), and pollen grains (PO) collected with sediment traps off Cape Blanc, northwest Africa, from 1988 till 1991 are presented. Both continental rainfall variations and wind mean strength and direction play a key role in the temporal fluctuations of the fluxes of eolian traces in the pelagic realm. Drier conditions in Northern Africa in 1987 could have preceded the high lithogenic input and moderate FD flux in 1988. The PH peak in summer 1988 was probably caused by increased wind velocity. Wetter rainy seasons of 1988/89 might have promoted a significant pollen production in summer 1989, and FD in late 1989 and early 1990, as well as contributed to the reduction of the lithogenic flux in 1989/90. Decreased fluxes of FD, PH and PO, and higher contribution of the 6-11 µm lithogenic fraction in 1991 would mainly reflect minor intensity and decreased amount of continental trade winds. Air-mass backward trajectories confirm that the Saharan Air Layer is predominantly involved in the spring/summer transport. Trade winds play a decisive role in the fall/winter months, but also contribute to the transport during late spring/summer. Origin of wind trajectories does not support a direct relationship between transporting wind-layers and material source areas in Northern Africa. High winter fluxes of eolian tracers and high amount of trade winds with continental origin in summer warn against a simplistic interpretation of the seasonal eolian signal preserved in the sediments off Cape Blanc, and the wind layer involved in its transport.

Mineralogical, geochemical and magnetic signatures of surface sediments from the Canadian Beaufort Shelf and Amundsen Gulf (Canadian Arctic)

Mineralogical, geochemical, magnetic, and siliciclastic grain-size signatures of 34 surface sediment samples from the Mackenzie-Beaufort Sea Slope and Amundsen Gulf were studied in order to better constrain the redox status, detrital particle provenance, and sediment dynamics in the western Canadian Arctic. Redox-sensitive elements (Mn, Fe, V, Cr, Zn) indicate that modern sedimentary deposition within the Mackenzie-Beaufort Sea Slope and Amundsen Gulf took place under oxic bottom-water conditions, with more turbulent mixing conditions and thus a well-oxygenated water column prevailing within the Amundsen Gulf. The analytical data obtained, combined with multivariate statistical (notably, principal component and fuzzy c-means clustering analyses) and spatial analyses, allowed the division of the study area into four provinces with distinct sedimentary compositions: (1) the Mackenzie Trough-Canadian Beaufort Shelf with high phyllosilicate-Fe oxide-magnetite and Al-K-Ti-Fe-Cr-V-Zn-P contents; (2) Southwestern Banks Island, characterized by high dolomite-K-feldspar and Ca-Mg-LOI contents; (3) the Central Amundsen Gulf, a transitional zone typified by intermediate phyllosilicate-magnetite-K-feldspar-dolomite and Al-K-Ti-Fe-Mn-V-Zn-Sr-Ca-Mg-LOI contents; and (4) mud volcanoes on the Canadian Beaufort Shelf distinguished by poorly sorted coarse-silt with high quartz-plagioclase-authigenic carbonate and Si-Zr contents, as well as high magnetic susceptibility. Our results also confirm that the present-day sedimentary dynamics on the Canadian Beaufort Shelf is mainly controlled by sediment supply from the Mackenzie River. Overall, these insights provide a basis for future studies using mineralogical, geochemical, and magnetic signatures of Canadian Arctic sediments in order to reconstruct past variations in sediment inputs and transport pathways related to late Quaternary climate and oceanographic changes.

Metabolic signatures of Huntington's disease (HD): 1H NMR analysis of the polar metabolome in post mortem human brain

Huntington’s disease (HD) is an autosomal neurodegenerative disorder affecting approximately 5-10 persons per 100,000 worldwide. The pathophysiology of HD is not fully understood but the age of onset is known to be highly dependent on the number of CAG triplet repeats in the huntingtin gene. Using 1H NMR spectroscopy this study biochemically profiled 39 brain metabolites in post-mortem striatum (n=14) and frontal lobe (n=14) from HD sufferers and controls (n=28). Striatum metabolites were more perturbed with 15 significantly affected in HD cases, compared with only 4 in frontal lobe (P<0.05; q<0.3). The metabolite which changed most overall was urea which decreased 3.25-fold in striatum (P<0.01). Four metabolites were consistently affected in both brain regions. These included the neurotransmitter precursors tyrosine and L-phenylalanine which were significantly depleted by 1.55-1.58-fold and 1.48-1.54-fold in striatum and frontal lobe, respectively (P=0.02-0.03). They also included L-leucine which was reduced 1.54-1.69-fold (P=0.04-0.09) and myo-inositol which was increased 1.26-1.37-fold (P<0.01). Logistic regression analyses performed with MetaboAnalyst demonstrated that data obtained from striatum produced models which were profoundly more sensitive and specific than those produced from frontal lobe. The brain metabolite changes uncovered in this first 1H NMR investigation of human HD offer new insights into the disease pathophysiology. Further investigations of striatal metabolite disturbances are clearly warranted.

Evaluaci?n de la aplicaci?n de carb?n activado granular en la filtraci?n del agua clarificada del r?o Cauca

El constante deterioro de las fuentes h?dricas y su uso como recurso en el abastecimiento de agua para consumo humano han conllevado a la b?squeda de la optimizaci?n de los procesos de tratamiento de forma tal que se alcancen condiciones de agua segura con el menor riesgo posible de afectaciones a la salud de la poblaci?n. Es por esto que los sistemas de abastecimiento de agua potable han adoptado estrategias enmarcadas dentro de los planes de seguridad del agua mediante la reducci?n de la contaminaci?n en la fuente de abastecimiento, la remoci?n o reducci?n de diferentes contaminantes mediante los procesos de tratamiento y la prevenci?n de la contaminaci?n del agua en el sistema de almacenamiento y distribuci?n al usuario final. Al observar que la filtraci?n es una de las etapas m?s cr?ticas dentro del tratamiento por ser la ?ltima barrera f?sica para la remoci?n de part?culas presentes en el agua; se plante? este proyecto de grado para estudiar a escala de laboratorio el uso de carb?n activado granular en el proceso de filtraci?n de agua clarificada del Rio Cauca, con el fin de analizar la eficiencia de remoci?n de turbiedad y materia org?nica medida como UV254 y as? establecer el alcance de los valores l?mite recomendados por las entidades internacionales para la disminuci?n del riesgo microbiol?gico y el riesgo cr?nico que pueda estar asociado a la presencia de materia org?nica en el agua para consumo humano. Se emple? carb?n activado granular de origen bituminoso y arena en seis diferentes configuraciones como medio filtrante principal en la etapa de filtraci?n (50%CAG ? 50% Arena, 65% CAG ? 35% Arena, 75% CAG ? 25% Arena, 85% CAG ? 15% Arena, 90% CAG ? 10% Arena y 100% CAG). Se consider? adem?s una configuraci?n con antracita y arena (70% Antracita ? 30% Arena) para comparar el comportamiento de ambos materiales filtrantes en el tratamiento de agua resultante del proceso de clarificaci?n efectuado por la Planta de Tratamiento de Agua Potable Puerto Mallarino en la ciudad de Cali. Se emple? un sistema de filtraci?n en columnas con distribuci?n de agua mediante conducciones reguladas a un caudal constante de 12 mL/min. El efluente de cada unidad de filtros fue evaluado y comparado con el afluente mediante la medici?n de Color Aparente, Turbiedad, UV254, pH y Conductividad. Se obtuvo como resultado que la configuraci?n C5 con 90% de CAG y 10% Arena logr? una mayor estabilidad de la turbiedad obteniendo valores m?nimos por debajo de 2 UNT (MAVDT), 0.5 UNT (WHO) y 0.15 UNT (EPA) y aunque no tuvo diferencias significativas comparado con el filtro de Antracita y Arena, si present? un mejor desempe?o en la remoci?n de turbiedad debido al alcance de un mayor n?mero de datos por debajo de 0.3 UNT. En cuanto a la eficiencia de remoci?n de materia org?nica en el agua medida como UV254 se observaron mejores resultados para la configuraci?n C4 con 85% de CAG y 15% Arena y aunque las eficiencias de remoci?n de materia org?nica no fueron significativamente altas se observa claramente la ventaja que presenta el uso de CAG como medio filtrante adsorbente comparado con el medio convencional de Antracita y Arena. La obtenci?n de bajas eficiencias de remoci?n fue debido al contenido de material en suspensi?n ya que los filtros de CAG trabajaron en la retenci?n de dicho material afectando considerablemente la capacidad de adsorci?n. Mediante esta investigaci?n se comprob? que la selecci?n adecuada de las condiciones operacionales de los filtros de CAG puede generar agua comparativamente similar o superior a los filtros conformados con materiales convencionales como Antracita y arena. De igual forma, el uso de CAG como medio filtrante para el tratamiento de agua del Rio Cauca es un insumo que puede aportar a una posible estrategia para disminuir el riesgo microbiol?gico y el riesgo cr?nico asociado con el contenido de materia org?nica en el agua distribuida a la poblaci?n cale?a

The role of miRNAs in stroke

Stroke is currently one of the leading causes of death and disability worldwide. Despite recent advances in the treatment of stroke there is a major unmet clinical need for novel therapeutics for intervention. miRNAs are small coding RNAs which act to post-transcriptionally inhibit expression of genes. Emerging evidence has supported the view that miRNAs play an important role in the development and progression of ischaemic stroke, although understanding remains relatively poor. This research uses several models to investigate the effects of miRNAs in the context of stroke in vivo and in vitro, as well as assessment of patient serum samples in order to identify biomarkers for stroke. miR-29b was found to be significantly upregulated in SHRSP rat brain peri-infarct at 72h following stroke, and downregulated in ischaemic core at 24h and 72h following stroke, whilst miR-29c was significantly downregulated in remainder tissue at 24h following stroke and in infarct at 72h following stroke. The upreglation of miR-29b at 72h corresponded to a significant downregulation of miR-29 target genes MMP2, MMP9 and TGF-β1 in peri-infarct tissue at 72h following stroke. Modulation of miR-29b and miR-29c was achieved in a rat neuronal cell line but suppression of genes of interest was not observed following oxygen glucose deprivation. Several candidate miRNAs were then identified by microRNA Openarray analysis in stroke patient serum samples. Validation of these miRNAs was not demonstrated in the population studied, but assessment of these miRNAs in rat serum and isolated exosomes demonstrated that several of these miRNAs were significantly altered in SHRSP rats following stroke. Finally miR-21 was demonstrated to be significantly upregulated in SHRSP rat peri-infarct following stroke. This was associated with a change in miR-21 localization as determined by in situ hybridization. Modulation of miR-21 via the use of CAG-miR-21 mice demonstrated no difference in infarct size as measured by T2 -weighted MRI scan nor was any difference present in behavioural tests versus wild type. KO of miR-21 resulted in a reduction of survival rate compared with wild type. This thesis demonstrates that miR-29 and miR-21 are modulated following stroke in animal models, and these are potential candidates for therapeutic intervention in the future. Analysis of clinical samples has illustrated difficulties in the identification of serum miRNA profiles and suggests that looking at the exosomal component of serum may provide better information regarding miRNA profiles after stroke.