L’océan côtier occupe une position clé dans le cycle du carbone et est exposé à l’acidification des océans. Une grande partie de matière organique(MO) marine et continentale est minéralisée dans les sédiments estuariens par des voies aérobies ou anaérobies. Cette minéralisation produit du carbone inorganique dissous (DIC), mais aussi de l’alcalinité totale(TA) pour la partie anoxique, ce qui tamponne les variations de pH du système et augmente la capacitéde l’eau de mer à absorber du CO2. Des mesures dans les sédiments du prodelta du Rhône ont montré que la minéralisation anoxique, surtout la sulfato-réduction, y est dominante et produit des forts flux de TA et de DIC. Proche de l’embouchure, c’est surtout la MO continentale qui est minéralisée et la fraction marine augmente vers le large. Une expérience d’acidification des sédiments de la baie de Villefranche-sur-mer a montré que l’acidification des océans cause la dissolution des carbonates ce qui tamponne le pH dans les sédiments. / Continental shelves are key regions for theglobal carbon cycle and particularly exposed to oceanacidification. A large part of organic matter (OM) ofcontinental and marine origin is mineralized in estuarinesediments following oxic and anoxic pathways.This mineralization produces dissolved inorganic carbon(DIC) leading to acidification of the bottom waters.Anoxic mineralization can produce total alkalinity(TA) that can contribute to buffer bottom water pHand increase the CO2 storage capacity of seawater. Measurementsin the sediments of the Rhˆone River prodeltashowed that anoxic mineralization, especially sulfate reduction,are the major pathways of OM mineralizationand create high DIC and TA fluxes. Land derived OMis mineralized close to the river mouth and marine OMtakes over on the shelf. An acidification experiment withsediment cores from the bay of Villefranche evidencedthat acidification causes carbonate dissolution at thesediment surface that buffers porewater pH.

Les résidus textiles archéologiques de l’Orient ancien sont rares. En Mésopotamie, la plupart des connaissances sur les textiles proviennent de textes cunéiformes. Fabriqués à partir de fibres animales ou végétales, les textiles sont périssables dans la plupart des environnements archéologiques. Un des principaux processus de préservation exceptionnelle de fibres archéologiques implique le contact avec un artefact métallique, ce phénomène est appelé « minéralisation ». Très peu de travaux ont été consacrés à l’étude approfondie des processus de minéralisation des textiles cellulosiques. Ce travail de doctorat a consisté à étudier à multi-échelles l’interaction entre substrat métallique à base cuivre et textile ancien, à partir d’échantillons provenant des sites archéologiques de Tello, de Nausharo et de Gonur-Depe (3e et 2e millénaire av. J.-C.). Le travail a permis de mettre en place une nouvelle méthodologie d’imagerie par microtomographie synchrotron de rayons X semi-quantitative afin de décrire la composition de ces systèmes complexes, hétérogènes et réactifs en 3d. Ces développements nous ont permis d’approfondir la description archéologique de ces textiles et de leur contexte d’enfouissement, en relation avec la question de leur production et de leur usage passés. Nous avons enfin abordé la description du système hybride fibres–produits de corrosion et la présence de signatures organiques dans ces systèmes hybrides altérés en vue de décrire les mécanismes à l’origine de leur conservation exceptionnelle. / Archaeological textile remains from the ancient East are rare. In Mesopotamia, most of the knowledge about textiles comes from cuneiform texts. Made from animal or vegetable fibres, textiles are perishable in most archaeological environments. One of the main processes of exceptional preservation of archaeological fibres involves contact with a metallic artefact, this phenomenon is called "mineralization". Very little work has been done on the in-depth study of the mineralization processes of cellulosic textiles. This PhD work consisted of a multi-scale study of the interaction between copper-base substrate and ancient textiles, based on samples from the archaeological sites of Tello, Nausharo and Gonur-Depe (3rd and 2nd millennium BC). The work made it possible to implement a new imaging methodology using synchrotron-based semi-quantitative X-ray microtomography to describe the composition of these complex, heterogeneous and reactive systems in 3d. These developments have allowed us to deepen the archaeological description of these textiles and their burial context in relation to the question of their production and use in past times. Finally, we discussed the description of the hybrid system of fibre-corrosion product and the presence of organic signatures in these altered hybrid systems in order to describe the mechanisms underlying their exceptional conservation.

Práce bude zaměřena na studium bakteriální degradace MCPP a BAM a na hledání vhodných bakteriálních kmenů.

<p> The "B" horizon at Tilt Cove occurs in subaqueous mafic volcanics near the base of the Silurian Cape St. John Group. It is 3 metres below a well-banded oxide iron formation ("A" horizon). </p> <p> Mineralization in the "B" horizon is analogous to that of the East Mine in that it is volcanogenic and has resulted in extensive chloritization of the footwall rocks, and in the deposition of banded sulphides or the replacement of the existing mafic volcanics by sulphides. There are differences in the geochemistry mineral textures and mineral types. The East Mine host volcanics are alkali depleted basaltic komatiites to magnesium theleiites. The horizon host volcanics are spillitized magnesium tholeiites. Samples of ore from the East Mine show well-developed colloform and framboidal textures. Pyrite, magnetite, hematite and chalcopyrite are the dominant minerals with minor sphalerite and accessory covellite. Samples from the horizon show relict colloform textures and framboids with less internal structure due to overgrowths. Atoll textures indicating extensive replacement are common. Pyrite is the dominant sulphide followed by sphalerite, chalcopyrite, accessory covellite and gold. The chalcopyrite occurs both as replacement of pyrite and exsolution in sphalerite. The most significant difference between samples from the East Mine and "B" horizon is the greater abundance of gold in the "B" horizon and its correlation with sphalerite. </p> / Thesis / Bachelor of Science (BSc)

No description available.

In the course of a little over a year, from January, 1950, to March, 1951, core samples of bottom sediments were collected at three different stations in the Dundas Marsh, Hamilton, Ontario. A number of the samples were analysed for total carbon content, bitumen, pectins, hemicelluloses, and cellulose and lignin content. This study is part of a larger investigated by the Department of Zoology to ascertain the relationships between the biological productivity in lakes and the rate of mineralization of the organic detritus in lake bottom sediments. / Thesis / Master of Science (MSc)

Environmental concerns about winter nitrogen (N) leaching loss limit the amount of biosolids applied to winter small grains in Virginia. Ten field studies were established 2012-2014 in Virginia to determine the agronomic and environmental feasibility of fall biosolids applications to soft red winter wheat (Triticum aestivum L.). Eight studies were located in the Coastal Plain physiographic province and two in the Ridge and Valley physiographic province. The effects of eight biosolids and urea N treatments on 1) biomass production at Zadoks growth stage (GS) 25-30, 2) soil inorganic N at GS 25-30, 3) soil mineralizable N at GS 25-30,4) N use efficiency (NUE) at GS 58, 5) grain yield, 6) end-of-season soil inorganic N, and 7) estimated N recovery were studied. Anaerobically digested (AD) and lime stabilized (LS) biosolids were fall applied at estimated plant available N (PAN) rates of 100 kg N ha⁻¹ and 50 kg N ha⁻¹. The 50 kg N ha⁻¹ biosolids treatments were supplemented with 50 kg N ha⁻¹ as urea in spring. Urea N was split applied at 0, 50, 100 and 150 kg N ha⁻¹, with 1/3 applied in fall and 2/3 in spring. Biomass at GS 25-30 increased with urea N rate and biosolids always resulted in equal or greater biomass than urea. Soil mineralizable N at GS 25-30 rarely responded to fall urea or biosolids N rate, regardless of biosolids type. Biosolids and urea applied at the agronomic N rate resulted in equal grain yield and estimated N recovery in soils where N leaching loss risk was low, regardless of biosolids type or application strategy. Lime stabilized biosolids and biosolids/urea split N application increased grain yield and estimated N recovery in soils with high or moderate N leaching loss risk. Therefore, AD and LS biosolids can be fall-applied to winter wheat at the full agronomic N rate in soils with low N leaching loss risk, while LS biosolids could be applied to winter wheat at the full agronomic N rate in soils with moderate or high N leaching loss risk. / Master of Science

Hyperthyroidism causes secondary osteoporosis through favoring bone resorption over bone formation, leading to bone loss with elevated bone fragility. Osteocytes that reside within lacunae inside the mineralized bone matrix orchestrate the process of bone remodeling and can themselves actively resorb bone upon certain stimuli. Nevertheless, the interaction between thyroid hormones and osteocytes and the impact of hyperthyroidism on osteocyte cell function are still unknown. In a preliminary study, we analyzed bones from male C57BL/6 mice with drug-induced hyperthyroidism, which led to mild osteocytic osteolysis with 1.14-fold larger osteocyte lacunae and by 108.33% higher tartrate-resistant acid phosphatase (TRAP) activity in osteocytes of hyperthyroid mice compared to euthyroid mice. To test whether hyperthyroidism-induced bone changes are reversible, we rendered male mice hyperthyroid by adding levothyroxine into their drinking water for 4 weeks, followed by a weaning period of 4 weeks with access to normal drinking water. Hyperthyroid mice displayed cortical and trabecular bone loss due to high bone turnover, which recovered with weaning. Although canalicular number and osteocyte lacunar area were similar in euthyroid, hyperthyroid and weaned mice, the number of terminal deoxynucleotidyl transferase–mediated deoxyuridine triphosphate nick end labeling (TUNEL)-positive osteocytes was 100% lower in the weaning group compared to euthyroid mice and the osteocytic TRAP activity was eightfold higher in hyperthyroid animals. The latter, along with a 3.75% lower average mineralization around the osteocyte lacunae in trabecular bone, suggests osteocytic osteolysis activity that, however, did not result in significantly enlarged osteocyte lacunae. In conclusion, we show a recovery of bone microarchitecture and turnover after reversal of hyperthyroidism to a euthyroid state. In contrast, osteocytic osteolysis was initiated in hyperthyroidism, but its effects were not reversed after 4 weeks of weaning. Due to the vast number of osteocytes in bone, we speculate that even minor individual cell functions might contribute to altered bone quality and mineral homeostasis in the setting of hyperthyroidism-induced bone disease. © 2022 The Authors. Journal of Bone and Mineral Research published by Wiley Periodicals LLC on behalf of American Society for Bone and Mineral Research (ASBMR).

Objetivos: Avaliar a estatura final, mineralização e marcadores de mineralização óssea de adultos com síndrome nefrótica (SN) idiopática corticossensível na infância e adolescência e analisar a influência da doença, suas comorbidades e do alvo de estatura no crescimento e mineralização destes pacientes. Casuística: Avaliamos a estatura final de 60 pacientes (41 masculinos e 19 femininos) com idade mínima de dezenove anos ou desenvolvimento genital P4G4 nos masculinos e menarca nos femininos portadores de SN corticossensível na infância e adolescência. Realizamos a densitometria óssea (DMO=g/cm2) em 26 destes pacientes e em 35 controles, com análise concomitante dos níveis séricos de 25 OH vitamina D3 (25(OH)D), Paratormônio (PTH), telopéptido carboxiterminal do colágeno tipo 1( (CTx), Propeptídeo Aminoterminal do Colágeno Tipo I (P1NP) e Osteocalcina (OC) Resultados: A idade média inicial dos 60 pacientes foi de 5a3m e final de 20a5m, com acompanhamento médio de 15a2m. A dose média de prednisona utilizada foi de 1264 mg/kg. O Zscore médio da estatura inicial (-0,60; SD: 1,0) e final (0,64; SD: 0,92), não diferiu significativamente (Teste T: p=0,72) entre si. O Zscore estatura na idade adulta se correlacionou significativamente apenas com o Zscore estatura inicial e com o Zscore alvo de estatura. Seis pacientes atingiram Zscore estatura < -2 na idade adulta e este achado demonstrou forte correlação com o Zscore estatura inicial e com o Zscore alvo de estatura. A DMO e Zscore DMO de L1L4, Cabeça do fêmur e do Fêmur total dos pacientes e controles não diferiram significativamente. 6 pacientes e 2 controles apresentaram Zscore DMO < -2 (massa óssea reduzida) enquanto 2 pacientes e 1 controle demonstraram , Zscore DMO < -2,5 (osteoporose). Pacientes com massa óssea reduzida receberam 2189 mg/kg de prednisona durante 13 anos e aqueles com osteoporose, 2510 mg/kg durante 14 anos. Estes valores, comparados com aqueles de pacientes com massa óssea normal, mostraram significância estatística (p=0,01). Não houve correlação significativa entre as demais variáveis analisadas e a DMO. Os marcadores 25(OH)D, PTH, CTx, P1NP e OC dos pacientes e controles não diferiram significativamente. Quando analisados em relação à doença e suas comorbidades, DMO e estatura final não apresentaram significação estatística. Conclusões: 1. Os valores de Zscore estatura inicial e final se correlacionaram fortemente com o alvo de estatura. 2. Não houve associação entre as características clinicas da doença e a aquisição do alvo de estatura, neste grupo de pacientes. 3. A massa óssea e os marcadores de mineralização dos pacientes não diferiram quando comparados aos controles. 4. Os 6 pacientes com massa óssea reduzida (2 com osteoporose) utilizaram dose total e tempo de uso da prednisona significativamente maior que aqueles com massa óssea adequada 5. Não houve correlação entre os níveis séricos dos marcadores de mineralização óssea e a doença e suas comorbidades, a estatura final e a DMO dos pacientes adultos com SN na infância e adolescência / Objectives: The aim of the present study was to evaluate the final height, bone mineral density (BMD) and bone mineralization markers of adults with steroid responsive Idiopathic Nephrotic Syndrome (NS) in childhood and adolescence and to examine the influence of the disease, its co-morbidities and the patients\' target height in the final height and mineralization results. Patients and Methods: We have analyzed initial and final anthropometric data of 60 patients (41 male and 19 females) and / or their records, with a minimum age of nineteen years or fully developed pubertal status (P4G4 in males and menarche in females). BMD (g/cm2) was evaluated in 26 patients and in 35 controls, with a concomitant analysis, of serum levels of 25-OH Vitamin D (25(OH)D), Parathyroid Hormone (PTH); C-terminal telopeptide of type I collagen (CTx) and aminoterminal propeptide of type 1 procollagen (P1NP) and Osteocalcin (OC) Results: Mean age at first consultation was 5.3 years (SD: 2.4 yrs) and at last consultation was 20.4 yrs (SD: 3.0 yrs). The mean cumulative dose of prednisone was 1254 mg/kg (SD: 831.39 mg/kg). The mean initial height SDS was -0.60; (SD: 1.0) the final height SDS was -0.64; (SD: 0.92), (t-test: p=0.72). The final height SDS showed correlated significantly only with the initial height SDS and the target height SDS. Six patients achieved a final height SDS <-2 and this finding showed a strong correlation to the initial height SDS and to the target height SDS in the male patients. The patients\' and control subjects L1L4 head of the femur and the total femur BMD and BMD SDS did not differ significantly. 6 patients and 2 control subjects showed a BMD SDS <-2 (low bone mass) while 2 patients and 1 control subjects showed a BMD SDS <-2.5 (osteoporosis). Patients with BMD SDS <-2 received 2189 mg / kg of prednisone over 13 years while those with a BMD SDS <-2.5 received 2510 mg / kg prednisone for 14 years (p = 0.01 vs BMD SDS -2 ). No other studied variable correlated significantly with BMD. The studied bone biomarkers showed similar results in patients and control subjects without a significant correlation with disease activity, co-morbidities, and BMD or height parameters. Conclusion: 1. the initial and final height SDS were strongly correlated to the height target. 2. INS and its co-morbidities did not prevent the patients to reach their target height 3. The patients\' BMD and bone mineralization markers did not differ when compared to controls. 4. The 6 patients with low bone mass (2 with osteoporosis) used a total dose of prednisone for a longer period of time in relation to those with an adequate BMD 5. There was no correlation between bone mineralization markers, disease activity and its co-morbidities, final height and BMD of adult patients with INS in childhood and adolescence

Objetivos: Avaliar a estatura final, mineralização e marcadores de mineralização óssea de adultos com síndrome nefrótica (SN) idiopática corticossensível na infância e adolescência e analisar a influência da doença, suas comorbidades e do alvo de estatura no crescimento e mineralização destes pacientes. Casuística: Avaliamos a estatura final de 60 pacientes (41 masculinos e 19 femininos) com idade mínima de dezenove anos ou desenvolvimento genital P4G4 nos masculinos e menarca nos femininos portadores de SN corticossensível na infância e adolescência. Realizamos a densitometria óssea (DMO=g/cm2) em 26 destes pacientes e em 35 controles, com análise concomitante dos níveis séricos de 25 OH vitamina D3 (25(OH)D), Paratormônio (PTH), telopéptido carboxiterminal do colágeno tipo 1( (CTx), Propeptídeo Aminoterminal do Colágeno Tipo I (P1NP) e Osteocalcina (OC) Resultados: A idade média inicial dos 60 pacientes foi de 5a3m e final de 20a5m, com acompanhamento médio de 15a2m. A dose média de prednisona utilizada foi de 1264 mg/kg. O Zscore médio da estatura inicial (-0,60; SD: 1,0) e final (0,64; SD: 0,92), não diferiu significativamente (Teste T: p=0,72) entre si. O Zscore estatura na idade adulta se correlacionou significativamente apenas com o Zscore estatura inicial e com o Zscore alvo de estatura. Seis pacientes atingiram Zscore estatura < -2 na idade adulta e este achado demonstrou forte correlação com o Zscore estatura inicial e com o Zscore alvo de estatura. A DMO e Zscore DMO de L1L4, Cabeça do fêmur e do Fêmur total dos pacientes e controles não diferiram significativamente. 6 pacientes e 2 controles apresentaram Zscore DMO < -2 (massa óssea reduzida) enquanto 2 pacientes e 1 controle demonstraram , Zscore DMO < -2,5 (osteoporose). Pacientes com massa óssea reduzida receberam 2189 mg/kg de prednisona durante 13 anos e aqueles com osteoporose, 2510 mg/kg durante 14 anos. Estes valores, comparados com aqueles de pacientes com massa óssea normal, mostraram significância estatística (p=0,01). Não houve correlação significativa entre as demais variáveis analisadas e a DMO. Os marcadores 25(OH)D, PTH, CTx, P1NP e OC dos pacientes e controles não diferiram significativamente. Quando analisados em relação à doença e suas comorbidades, DMO e estatura final não apresentaram significação estatística. Conclusões: 1. Os valores de Zscore estatura inicial e final se correlacionaram fortemente com o alvo de estatura. 2. Não houve associação entre as características clinicas da doença e a aquisição do alvo de estatura, neste grupo de pacientes. 3. A massa óssea e os marcadores de mineralização dos pacientes não diferiram quando comparados aos controles. 4. Os 6 pacientes com massa óssea reduzida (2 com osteoporose) utilizaram dose total e tempo de uso da prednisona significativamente maior que aqueles com massa óssea adequada 5. Não houve correlação entre os níveis séricos dos marcadores de mineralização óssea e a doença e suas comorbidades, a estatura final e a DMO dos pacientes adultos com SN na infância e adolescência / Objectives: The aim of the present study was to evaluate the final height, bone mineral density (BMD) and bone mineralization markers of adults with steroid responsive Idiopathic Nephrotic Syndrome (NS) in childhood and adolescence and to examine the influence of the disease, its co-morbidities and the patients\' target height in the final height and mineralization results. Patients and Methods: We have analyzed initial and final anthropometric data of 60 patients (41 male and 19 females) and / or their records, with a minimum age of nineteen years or fully developed pubertal status (P4G4 in males and menarche in females). BMD (g/cm2) was evaluated in 26 patients and in 35 controls, with a concomitant analysis, of serum levels of 25-OH Vitamin D (25(OH)D), Parathyroid Hormone (PTH); C-terminal telopeptide of type I collagen (CTx) and aminoterminal propeptide of type 1 procollagen (P1NP) and Osteocalcin (OC) Results: Mean age at first consultation was 5.3 years (SD: 2.4 yrs) and at last consultation was 20.4 yrs (SD: 3.0 yrs). The mean cumulative dose of prednisone was 1254 mg/kg (SD: 831.39 mg/kg). The mean initial height SDS was -0.60; (SD: 1.0) the final height SDS was -0.64; (SD: 0.92), (t-test: p=0.72). The final height SDS showed correlated significantly only with the initial height SDS and the target height SDS. Six patients achieved a final height SDS <-2 and this finding showed a strong correlation to the initial height SDS and to the target height SDS in the male patients. The patients\' and control subjects L1L4 head of the femur and the total femur BMD and BMD SDS did not differ significantly. 6 patients and 2 control subjects showed a BMD SDS <-2 (low bone mass) while 2 patients and 1 control subjects showed a BMD SDS <-2.5 (osteoporosis). Patients with BMD SDS <-2 received 2189 mg / kg of prednisone over 13 years while those with a BMD SDS <-2.5 received 2510 mg / kg prednisone for 14 years (p = 0.01 vs BMD SDS -2 ). No other studied variable correlated significantly with BMD. The studied bone biomarkers showed similar results in patients and control subjects without a significant correlation with disease activity, co-morbidities, and BMD or height parameters. Conclusion: 1. the initial and final height SDS were strongly correlated to the height target. 2. INS and its co-morbidities did not prevent the patients to reach their target height 3. The patients\' BMD and bone mineralization markers did not differ when compared to controls. 4. The 6 patients with low bone mass (2 with osteoporosis) used a total dose of prednisone for a longer period of time in relation to those with an adequate BMD 5. There was no correlation between bone mineralization markers, disease activity and its co-morbidities, final height and BMD of adult patients with INS in childhood and adolescence