Common genetic loci influencing plasma homocysteine concentrations and their effect on risk of coronary artery disease.

BACKGROUND: The strong observational association between total homocysteine (tHcy) concentrations and risk of coronary artery disease (CAD) and the null associations in the homocysteine-lowering trials have prompted the need to identify genetic variants associated with homocysteine concentrations and risk of CAD. OBJECTIVE: We tested whether common genetic polymorphisms associated with variation in tHcy are also associated with CAD. DESIGN: We conducted a meta-analysis of genome-wide association studies (GWAS) on tHcy concentrations in 44,147 individuals of European descent. Polymorphisms associated with tHcy (P < 10(-8)) were tested for association with CAD in 31,400 cases and 92,927 controls. RESULTS: Common variants at 13 loci, explaining 5.9% of the variation in tHcy, were associated with tHcy concentrations, including 6 novel loci in or near MMACHC (2.1 Ã- 10(-9)), SLC17A3 (1.0 Ã- 10(-8)), GTPB10 (1.7 Ã- 10(-8)), CUBN (7.5 Ã- 10(-10)), HNF1A (1.2 Ã- 10(-12)), and FUT2 (6.6 Ã- 10(-9)), and variants previously reported at or near the MTHFR, MTR, CPS1, MUT, NOX4, DPEP1, and CBS genes. Individuals within the highest 10% of the genotype risk score (GRS) had 3-μmol/L higher mean tHcy concentrations than did those within the lowest 10% of the GRS (P = 1 Ã- 10(-36)). The GRS was not associated with risk of CAD (OR: 1.01; 95% CI: 0.98, 1.04; P = 0.49). CONCLUSIONS: We identified several novel loci that influence plasma tHcy concentrations. Overall, common genetic variants that influence plasma tHcy concentrations are not associated with risk of CAD in white populations, which further refutes the causal relevance of moderately elevated tHcy concentrations and tHcy-related pathways for CAD.

A genetic risk score combining 32 SNPs is associated with body mass index and improves obesity prediction in people with major depressive disorder.

BACKGROUND: Obesity is strongly associated with major depressive disorder (MDD) and various other diseases. Genome-wide association studies have identified multiple risk loci robustly associated with body mass index (BMI). In this study, we aimed to investigate whether a genetic risk score (GRS) combining multiple BMI risk loci might have utility in prediction of obesity in patients with MDD. METHODS: Linear and logistic regression models were conducted to predict BMI and obesity, respectively, in three independent large case-control studies of major depression (Radiant, GSK-Munich, PsyCoLaus). The analyses were first performed in the whole sample and then separately in depressed cases and controls. An unweighted GRS was calculated by summation of the number of risk alleles. A weighted GRS was calculated as the sum of risk alleles at each locus multiplied by their effect sizes. Receiver operating characteristic (ROC) analysis was used to compare the discriminatory ability of predictors of obesity. RESULTS: In the discovery phase, a total of 2,521 participants (1,895 depressed patients and 626 controls) were included from the Radiant study. Both unweighted and weighted GRS were highly associated with BMI (P <0.001) but explained only a modest amount of variance. Adding 'traditional' risk factors to GRS significantly improved the predictive ability with the area under the curve (AUC) in the ROC analysis, increasing from 0.58 to 0.66 (95% CI, 0.62-0.68; χ(2) = 27.68; P <0.0001). Although there was no formal evidence of interaction between depression status and GRS, there was further improvement in AUC in the ROC analysis when depression status was added to the model (AUC = 0.71; 95% CI, 0.68-0.73; χ(2) = 28.64; P <0.0001). We further found that the GRS accounted for more variance of BMI in depressed patients than in healthy controls. Again, GRS discriminated obesity better in depressed patients compared to healthy controls. We later replicated these analyses in two independent samples (GSK-Munich and PsyCoLaus) and found similar results. CONCLUSIONS: A GRS proved to be a highly significant predictor of obesity in people with MDD but accounted for only modest amount of variance. Nevertheless, as more risk loci are identified, combining a GRS approach with information on non-genetic risk factors could become a useful strategy in identifying MDD patients at higher risk of developing obesity.

La educación para la salud como objeto de estudio histórico : proyecto de investigación

Objetivo: El objetivo es presentar el proyecto de investigación cuyo propósito es conocer la evolución de la Educación para la salud (EpS) desde la antigüedad hasta la época contemporánea, con el fin de identificar y comprender la génesis y construcción de la disciplina. Método: Se trata de un estudio cualitativo histórico enmarcado en el paradigma interpretativo etnohistórico y hermenéutico. Los pilares básicos en que se enmarca conceptualmente, son la Educación, la Persona, grupo o comunidad y la Salud. El espacio social, es aquel en que los grupos sociales vivían y el estructural-temporal, las épocas históricas: prehistoria, antigüedad (culturas antiguas y clásicas), edad media, renacimiento y contemporánea hasta pasada la Guerra Civil española (1940). El sujeto de estudio es la EpS a partir de los elementos que la conforman: el concepto de salud, las creencias, los conocimientos sanitarios, las intervenciones y los recursos educativos para la salud de les personas y los grupos sociales en cada una de las épocas históricas a estudio. Las fuentes utilizadas son las indirectas, materiales-arqueológicas y culturales: verbales (escritas) y no verbales (semiológicas/audiovisuales) y las no seriadas. La recogida de información a través de técnicas de investigación histórica cualitativa: la observación y análisis documental bibliográfico, iconográfico de archivos, prensa, publicaciones oficiales, textos bibliográficos y técnicas textuales-filosóficas: análisis de contenido y crítica histórica. El análisis de la información será cronológico y mediante una clasificación por temáticas y periodos históricos.

Predictive ability of heel quantitative ultrasound for incident fractures: an individual-level meta-analysis.

UNLABELLED: The relationship between bone quantitative ultrasound (QUS) and fracture risk was estimated in an individual level data meta-analysis of 9 prospective studies of 46,124 individuals and 3018 incident fractures. Low QUS is associated with an increase in fracture risk, including hip fracture. The association with osteoporotic fracture decreases with time. INTRODUCTION: The aim of this meta-analysis was to investigate the association between parameters of QUS and risk of fracture. METHODS: In an individual-level analysis, we studied participants in nine prospective cohorts from Asia, Europe and North America. Heel broadband ultrasonic attenuation (BUA dB/MHz) and speed of sound (SOS m/s) were measured at baseline. Fractures during follow-up were collected by self-report and in some cohorts confirmed by radiography. An extension of Poisson regression was used to examine the gradient of risk (GR, hazard ratio per 1 SD decrease) between QUS and fracture risk adjusted for age and time since baseline in each cohort. Interactions between QUS and age and time since baseline were explored. RESULTS: Baseline measurements were available in 46,124 men and women, mean age 70 years (range 20-100). Three thousand and eighteen osteoporotic fractures (787 hip fractures) occurred during follow-up of 214,000 person-years. The summary GR for osteoporotic fracture was similar for both BUA (1.45, 95 % confidence intervals (CI) 1.40-1.51) and SOS (1.42, 95 % CI 1.36-1.47). For hip fracture, the respective GRs were 1.69 (95 % CI, 1.56-1.82) and 1.60 (95 % CI, 1.48-1.72). However, the GR was significantly higher for both fracture outcomes at lower baseline BUA and SOS (p < 0.001). The predictive value of QUS was the same for men and women and for all ages (p > 0.20), but the predictive value of both BUA and SOS for osteoporotic fracture decreased with time (p = 0.018 and p = 0.010, respectively). For example, the GR of BUA for osteoporotic fracture, adjusted for age, was 1.51 (95 % CI 1.42-1.61) at 1 year after baseline, but at 5 years, it was 1.36 (95 % CI 1.27-1.46). CONCLUSIONS: Our results confirm that quantitative ultrasound is an independent predictor of fracture for men and women particularly at low QUS values.

Relationship between obesity and the risk of clinically significant depression: Mendelian randomisation study.

BACKGROUND: Obesity has been shown to be associated with depression and it has been suggested that higher body mass index (BMI) increases the risk of depression and other common mental disorders. However, the causal relationship remains unclear and Mendelian randomisation, a form of instrumental variable analysis, has recently been employed to attempt to resolve this issue. AIMS: To investigate whether higher BMI increases the risk of major depression. METHOD: Two instrumental variable analyses were conducted to test the causal relationship between obesity and major depression in RADIANT, a large case-control study of major depression. We used a single nucleotide polymorphism (SNP) in FTO and a genetic risk score (GRS) based on 32 SNPs with well-established associations with BMI. RESULTS: Linear regression analysis, as expected, showed that individuals carrying more risk alleles of FTO or having higher score of GRS had a higher BMI. Probit regression suggested that higher BMI is associated with increased risk of major depression. However, our two instrumental variable analyses did not support a causal relationship between higher BMI and major depression (FTO genotype: coefficient -0.03, 95% CI -0.18 to 0.13, P = 0.73; GRS: coefficient -0.02, 95% CI -0.11 to 0.07, P = 0.62). CONCLUSIONS: Our instrumental variable analyses did not support a causal relationship between higher BMI and major depression. The positive associations of higher BMI with major depression in probit regression analyses might be explained by reverse causality and/or residual confounding.

Association between parental history and genetic risk scores for coronary heart disease prediction: The population-based CoLaus study.

BACKGROUND AND AIMS: Parental history (PH) and genetic risk scores (GRSs) are separately associated with coronary heart disease (CHD), but evidence regarding their combined effects is lacking. We aimed to evaluate the joint associations and predictive ability of PH and GRSs for incident CHD. METHODS: Data for 4283 Caucasians were obtained from the population-based CoLaus Study, over median follow-up time of 5.6 years. CHD was defined as incident myocardial infarction, angina, percutaneous coronary revascularization or bypass grafting. Single nucleotide polymorphisms for CHD identified by genome-wide association studies were used to construct unweighted and weighted versions of three GRSs, comprising of 38, 53 and 153 SNPs respectively. RESULTS: PH was associated with higher values of all weighted GRSs. After adjustment for age, sex, smoking, diabetes, systolic blood pressure, low and high density lipoprotein cholesterol, PH was significantly associated with CHD [HR 2.61, 95% CI (1.47-4.66)] and further adjustment for GRSs did not change this estimate. Similarly, one standard deviation change of the weighted 153-SNPs GRS was significantly associated with CHD [HR 1.50, 95% CI (1.26-1.80)] and remained so, after further adjustment for PH. The weighted, 153-SNPs GRS, but not PH, modestly improved discrimination [(C-index improvement, 0.016), p = 0.048] and reclassification [(NRI improvement, 8.6%), p = 0.027] beyond cardiovascular risk factors. After including both the GRS and PH, model performance improved further [(C-index improvement, 0.022), p = 0.006]. CONCLUSION: After adjustment for cardiovascular risk factors, PH and a weighted, polygenic GRS were jointly associated with CHD and provided additive information for coronary events prediction.

Seismic characterization of heterogeneous sedimentary and fractured rocks based on Biot's theory of poroelasticity

Understanding and quantifying seismic energy dissipation, which manifests itself in terms of velocity dispersion and attenuation, in fluid-saturated porous rocks is of considerable interest, since it offers the perspective of extracting information with regard to the elastic and hydraulic rock properties. There is increasing evidence to suggest that wave-induced fluid flow, or simply WIFF, is the dominant underlying physical mechanism governing these phenomena throughout the seismic, sonic, and ultrasonic frequency ranges. This mechanism, which can prevail at the microscopic, mesoscopic, and macroscopic scale ranges, operates through viscous energy dissipation in response to fluid pressure gradients and inertial effects induced by the passing wavefield. In the first part of this thesis, we present an analysis of broad-band multi-frequency sonic log data from a borehole penetrating water-saturated unconsolidated glacio-fluvial sediments. An inherent complication arising in the interpretation of the observed P-wave attenuation and velocity dispersion is, however, that the relative importance of WIFF at the various scales is unknown and difficult to unravel. An important generic result of our work is that the levels of attenuation and velocity dispersion due to the presence of mesoscopic heterogeneities in water-saturated unconsolidated clastic sediments are expected to be largely negligible. Conversely, WIFF at the macroscopic scale allows for explaining most of the considered data while refinements provided by including WIFF at the microscopic scale in the analysis are locally meaningful. Using a Monte-Carlo-type inversion approach, we compare the capability of the different models describing WIFF at the macroscopic and microscopic scales with regard to their ability to constrain the dry frame elastic moduli and the permeability as well as their local probability distribution. In the second part of this thesis, we explore the issue of determining the size of a representative elementary volume (REV) arising in the numerical upscaling procedures of effective seismic velocity dispersion and attenuation of heterogeneous media. To this end, we focus on a set of idealized synthetic rock samples characterized by the presence of layers, fractures or patchy saturation in the mesocopic scale range. These scenarios are highly pertinent because they tend to be associated with very high levels of velocity dispersion and attenuation caused by WIFF in the mesoscopic scale range. The problem of determining the REV size for generic heterogeneous rocks is extremely complex and entirely unexplored in the given context. In this pilot study, we have therefore focused on periodic media, which assures the inherent self- similarity of the considered samples regardless of their size and thus simplifies the problem to a systematic analysis of the dependence of the REV size on the applied boundary conditions in the numerical simulations. Our results demonstrate that boundary condition effects are absent for layered media and negligible in the presence of patchy saturation, thus resulting in minimum REV sizes. Conversely, strong boundary condition effects arise in the presence of a periodic distribution of finite-length fractures, thus leading to large REV sizes. In the third part of the thesis, we propose a novel effective poroelastic model for periodic media characterized by mesoscopic layering, which accounts for WIFF at both the macroscopic and mesoscopic scales as well as for the anisotropy associated with the layering. Correspondingly, this model correctly predicts the existence of the fast and slow P-waves as well as quasi and pure S-waves for any direction of wave propagation as long as the corresponding wavelengths are much larger than the layer thicknesses. The primary motivation for this work is that, for formations of intermediate to high permeability, such as, for example, unconsolidated sediments, clean sandstones, or fractured rocks, these two WIFF mechanisms may prevail at similar frequencies. This scenario, which can be expected rather common, cannot be accounted for by existing models for layered porous media. Comparisons of analytical solutions of the P- and S-wave phase velocities and inverse quality factors for wave propagation perpendicular to the layering with those obtained from numerical simulations based on a ID finite-element solution of the poroelastic equations of motion show very good agreement as long as the assumption of long wavelengths remains valid. A limitation of the proposed model is its inability to account for inertial effects in mesoscopic WIFF when both WIFF mechanisms prevail at similar frequencies. Our results do, however, also indicate that the associated error is likely to be relatively small, as, even at frequencies at which both inertial and scattering effects are expected to be at play, the proposed model provides a solution that is remarkably close to its numerical benchmark. -- Comprendre et pouvoir quantifier la dissipation d'énergie sismique qui se traduit par la dispersion et l'atténuation des vitesses dans les roches poreuses et saturées en fluide est un intérêt primordial pour obtenir des informations à propos des propriétés élastique et hydraulique des roches en question. De plus en plus d'études montrent que le déplacement relatif du fluide par rapport au solide induit par le passage de l'onde (wave induced fluid flow en anglais, dont on gardera ici l'abréviation largement utilisée, WIFF), représente le principal mécanisme physique qui régit ces phénomènes, pour la gamme des fréquences sismiques, sonique et jusqu'à l'ultrasonique. Ce mécanisme, qui prédomine aux échelles microscopique, mésoscopique et macroscopique, est lié à la dissipation d'énergie visqueuse résultant des gradients de pression de fluide et des effets inertiels induits par le passage du champ d'onde. Dans la première partie de cette thèse, nous présentons une analyse de données de diagraphie acoustique à large bande et multifréquences, issues d'un forage réalisé dans des sédiments glaciaux-fluviaux, non-consolidés et saturés en eau. La difficulté inhérente à l'interprétation de l'atténuation et de la dispersion des vitesses des ondes P observées, est que l'importance des WIFF aux différentes échelles est inconnue et difficile à quantifier. Notre étude montre que l'on peut négliger le taux d'atténuation et de dispersion des vitesses dû à la présence d'hétérogénéités à l'échelle mésoscopique dans des sédiments clastiques, non- consolidés et saturés en eau. A l'inverse, les WIFF à l'échelle macroscopique expliquent la plupart des données, tandis que les précisions apportées par les WIFF à l'échelle microscopique sont localement significatives. En utilisant une méthode d'inversion du type Monte-Carlo, nous avons comparé, pour les deux modèles WIFF aux échelles macroscopique et microscopique, leur capacité à contraindre les modules élastiques de la matrice sèche et la perméabilité ainsi que leur distribution de probabilité locale. Dans une seconde partie de cette thèse, nous cherchons une solution pour déterminer la dimension d'un volume élémentaire représentatif (noté VER). Cette problématique se pose dans les procédures numériques de changement d'échelle pour déterminer l'atténuation effective et la dispersion effective de la vitesse sismique dans un milieu hétérogène. Pour ce faire, nous nous concentrons sur un ensemble d'échantillons de roches synthétiques idéalisés incluant des strates, des fissures, ou une saturation partielle à l'échelle mésoscopique. Ces scénarios sont hautement pertinents, car ils sont associés à un taux très élevé d'atténuation et de dispersion des vitesses causé par les WIFF à l'échelle mésoscopique. L'enjeu de déterminer la dimension d'un VER pour une roche hétérogène est très complexe et encore inexploré dans le contexte actuel. Dans cette étude-pilote, nous nous focalisons sur des milieux périodiques, qui assurent l'autosimilarité des échantillons considérés indépendamment de leur taille. Ainsi, nous simplifions le problème à une analyse systématique de la dépendance de la dimension des VER aux conditions aux limites appliquées. Nos résultats indiquent que les effets des conditions aux limites sont absents pour un milieu stratifié, et négligeables pour un milieu à saturation partielle : cela résultant à des dimensions petites des VER. Au contraire, de forts effets des conditions aux limites apparaissent dans les milieux présentant une distribution périodique de fissures de taille finie : cela conduisant à de grandes dimensions des VER. Dans la troisième partie de cette thèse, nous proposons un nouveau modèle poro- élastique effectif, pour les milieux périodiques caractérisés par une stratification mésoscopique, qui prendra en compte les WIFF à la fois aux échelles mésoscopique et macroscopique, ainsi que l'anisotropie associée à ces strates. Ce modèle prédit alors avec exactitude l'existence des ondes P rapides et lentes ainsi que les quasis et pures ondes S, pour toutes les directions de propagation de l'onde, tant que la longueur d'onde correspondante est bien plus grande que l'épaisseur de la strate. L'intérêt principal de ce travail est que, pour les formations à perméabilité moyenne à élevée, comme, par exemple, les sédiments non- consolidés, les grès ou encore les roches fissurées, ces deux mécanismes d'WIFF peuvent avoir lieu à des fréquences similaires. Or, ce scénario, qui est assez commun, n'est pas décrit par les modèles existants pour les milieux poreux stratifiés. Les comparaisons des solutions analytiques des vitesses des ondes P et S et de l'atténuation de la propagation des ondes perpendiculaires à la stratification, avec les solutions obtenues à partir de simulations numériques en éléments finis, fondées sur une solution obtenue en 1D des équations poro- élastiques, montrent un très bon accord, tant que l'hypothèse des grandes longueurs d'onde reste valable. Il y a cependant une limitation de ce modèle qui est liée à son incapacité à prendre en compte les effets inertiels dans les WIFF mésoscopiques quand les deux mécanismes d'WIFF prédominent à des fréquences similaires. Néanmoins, nos résultats montrent aussi que l'erreur associée est relativement faible, même à des fréquences à laquelle sont attendus les deux effets d'inertie et de diffusion, indiquant que le modèle proposé fournit une solution qui est remarquablement proche de sa référence numérique.

Filosofi

Samlingen med signum HB IIa finns vid huvudbiblioteket och innehåller filosofisk litteratur till och med år 1999. Vid Humanistiska biblioteket finns dessutom en samling filosofisk litteratur i anslutning till ämnet Filosofi. Stommen till akademibibliotekets filosofiska samlingar ligger i donationer. Några donatorer från äldre tid kan nämnas, som hovrättsauskultant Harry Streng, FM Kurt Reuter, prof. Rolf Lagerborg, teol.dr. Eric Hammarberg, prof. J.V.Tallqvist och fil.dr. Arne Törnudd. Friexemplar som erhållits från och med 1919 samt inköp kompletterar samlingen vid huvudbiblioteket. Den filosofiska litteraturen vid huvudbiblioteket söks med sökfunktionen Signum och söktermen HB IIa medan återvinning av litteratur tryckt före 1980 görs genom manuell sökning i huvudbibliotekets systematiska kortkatalog. Retroaktiv inmatning i databasen Alma gör att också litteratur tryckt 1830 t.o.m. 1979 med tiden blir sökbar i Alma. Från och med år 2000 ingår den filosofiska litteraturen vid huvudbiblioteket i en numerus currens-samling.

Alandica

Samlingen med signum HB Saml. Alandica finns vid huvudbiblioteket och innehåller litteratur som på något sätt berör landskapet Åland, politiskt, naturvetenskapligt, socialt, historiskt, litterärt osv. Stommen till Alandica-samlingen kommer från det historiska bibliotek som statsarkivarie Reinhold Hausen samlade och donerade till akademibiblioteket. I Hausens stora historiska bibliotek ingick en omfattande specialsamling om Åland som han använde som underlag för sina bibliografier över Åland publicerade i samlingsverken Åland VI, VII, IX och X. Bibliografierna omfattar tiden ända fram till 1936. Av särskilt intresse i Hausens samling är det material som handlar om ålandsfrågan, speciellt kan nämnas talrika särtryck av artiklar i tidskrifter och övertryck från tidningar, även utländska. Utom katalogiserat material finns det också endel okatalogiserat småtryck. Samlingen Alandica har kontinuerligt vuxit genom bibliotekets friexemplarsrätt. En del material har kommit som gåvor, t.ex. material från Ålands lagting. Samlingen innehåller också administrativt material som inte enskilt katalogiseras, exempelvis Ålands författningssamling och olika årsberättelser, verksamhetsberättelser och budgeter. Biblioteket strävar efter att bevaka den utländska utgivningen av alandica och kompletterar samlingen genom inköp. Återvinning av material görs i databasen Alma med sökfunktionen Signum och söktermen HB Saml. Alandica. En kortkatalog med alandica tryckt mellan 1830 och 1979 är i det närmaste retrokatalogiserad till Alma.

Konstvetenskap - arkitektur

En större samling konstvetenskaplig litteratur finns vid huvudbiblioteket och av den handlar några tusen volymer om arkitektur och arkitekturhistoria, om arkitekter och deras verk samt om olika typer av byggnader såsom offentliga byggnader, bostadshus, villor, slott osv. Av särskilt intresse är att det finns mycket litteratur om kyrko- och klosterbyggnader både i Sverige och i Finland. Vid Humanistiska biblioteket finns litteratur om arkitektur i samband med ämnet Konstvetenskap. En del av den äldre litteraturen om arkitektur har förvärvats genom bokdonationer, som exempel ett antal arkitekturhistoriska samlingsverk från arkitekt Carl-Folke Collianders sterbhus på 1950-talet. Återvinning av litteratur om arkitektur tryckt före 1980 görs genom manuell sökning i huvudbibliotekets systematiska kortkatalog, där samlingen med har signum HB IVd2. Retroaktiv inmatning i databasen Alma gör att all konstvetenskaplig litteratur tryckt mellan 1830 och 1979 med tiden blir sökbart i Alma med sökfunktionen Signum och söktermen HB IVd. Från och med år 2000 ingår huvudbibliotekets litteraturen om arkitektur i en numerus currens-samling.

Konstvetenskap - bildhuggarkonst

En större samling konstvetenskaplig litteratur finns vid huvudbiblioteket och av den handlar ungefär femhundra volymer om bildhuggarkonst. Vid Humanistiska biblioteket finns konstvetenskaplig litteratur i anslutning till ämnet Konstvetenskap. Bokdonationer både från Sverige och från Finland kompletterar det som biblioteket erhållit genom sin friexemplarsrätt från år 1919. Återvinning av litteratur om bildhuggarkonst tryckt före 1980 görs genom manuell sökning i huvudbibliotekets systematiska kortkatalog, där litteraturen om bildhuggarkonst har signum IVd3. Retroaktiv inmatning i databasen Alma gör att all konstvetenskaplig litteratur tryckt mellan 1830 och 1979 vid huvudbiblioteket med tiden blir sökbar i Alma med sökfunktionen Signum och söktermen HB IVd. Från och med år 2000 ingår huvudbibliotekets konstvetenskapliga litteratur i en numerus currens-samling.

Konstvetenskap - grafisk konst

En större samling konstvetenskaplig litteratur finns vid huvudbiblioteket och av den handlar ungefär 600 volymer om grafisk konst. Vid Humanistiska biblioteket finns konstvetenskaplig litteratur i anslutning till ämnet Konstvetenskap. Bokdonationer både från Sverige och från Finland kompletterar det som biblioteket erhållit genom sin friexemplarsrätt efter 1919. Återvinning av litteratur tryckt före 1980 görs genom manuell sökning i huvudbibliotekets systematiska kortkatalog, där litteraturen om grafisk konst har signum IVd5. Retroaktiv inmatning i databasen Alma gör att konstvetenskaplig litteratur tryckt mellan 1830 och 1979 med tiden blir sökbar i Alma med sökfunktionen Signum och söktermen HB IVd. Från och med år 2000 ingår huvudbibliotekets konstvetenskapliga litteratur i en numerus currens-samling.

Konstvetenskap - målarkonst

En större samling konstvetenskaplig litteraturmed finns vid huvudbiblioteket och av den handlar ett par tusen volymer om målarkonst. Vid Humanistiska biblioteket finns konstvetenskaplig litteratur i anslutning till ämnet Konstvetenskap. Bokdonationer både från Sverige och från Finland kompletterar det som biblioteket erhållit genom sin friexemplarsrätt efter 1919. Återvinning av litteratur tryckt före 1980 görs genom manuell sökning i huvudbibliotekets systematiska kortkatalog, där litteraturen om målarkonst har signum IVd4. Retroaktiv inmatning i databasen Alma gör att all konstvetenskaplig litteratur tryckt mellan 1830 och 1979 med tiden blir sökbar i Alma med sökfunktionen Signum och söktermen HB IVd. Från och med år 2000 ingår huvudbibliotekets konstvetenskapliga litteratur i en numerus currens-samling.

Kyrkohistoria

Samlingen med signum HB IIc3 finns vid huvudbiblioteket och innehåller litteratur om kyrkohistoria. Vid Teologiska biblioteket finns mycket kyrkohistorisk litteratur. Kyrkohistorisk litteratur har ingått i talrika boksamlingar som genom åren donerats till akademibiblioteket. Återvinning av litteratur om kyrkohistoria tryckt före 1980 görs genom manuell sökning i huvudbibliotekets systematiska kortkatalog. Retroaktiv inmatning i databasen Alma gör att också kyrkohistorisk litteratur tryckt mellan 1830 och 1979 med tiden blir sökbar i Alma med sökfunktionen Signum och söktermen HB IIc3. Från och med år 2000 ingår den kyrkohistoriska litteraturen vid huvudbiblioteket i en numerus currens-samling.