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

L’ostéoarthrose (OA) est une pathologie de forte incidence affectant les articulations. Elle est caractérisée principalement par une dégradation du cartilage articulaire, un déséquilibre au niveau du remodelage osseux et une sclérose de l’os sous-chondral. L’étiologie de cette pathologie reste encore méconnue, cependant il semble de plus en plus que tous les tissus composant l’articulation soient affectés dans cette pathologie. L’importance du rôle de l’os dans le développement de l’OA est incontestable et représente donc une cible thérapeuthique intéressante. Des études effectuées par tomodensitométrie ont démontré une structure et une organisation anormales du tissu osseux des patients OA. Parallèlement, les cultures primaires d’ostéoblastes (Ob) humains OA issus de l’os sous-chondral démontrent un phénotype altéré et une faible minéralisation in vitro. La signalisation Wnt, essentielle dans l’embryogenèse, a montré avoir un rôle clé dans la régulation de l’ostéogenèse en régulant notamment la différenciation terminale des Ob. Le facteur de croissance transformant-β1 (TGF-β1), un facteur agissant notamment sur la prolifération et sur le début de la différenciation des Ob, est surexprimé par les Ob OA et pourrait moduler cette signalisation. Aussi, deux populations de patients OA peuvent être différenciées in vitro par la production de prostaglandines E2 (PGE2) par leurs Ob et les PGE2, dans une étude sur le cancer colorectal, ont montré moduler la signalisation Wnt. Notre hypothèse de travail est que l’activation de la voie de signalisation Wnt/β-caténine est diminuée dans les Ob OA. Cette diminution est responsable de la sous-minéralisation et de l’altération du phénotype des Ob humains OA. Par ailleurs, DKK2, dont l’expression est contrôlée par TGF-β1, est responsable de la diminution de l’activité Wnt/β-caténine et les PGE2 peuvent en partie corriger cette situation. L’objectif général de cette étude est d’une part, de démontrer le rôle de TGF-β1, DKK2 et de PGE2 sur l’altération de la signalisation Wnt/β-caténine et d’autre part, de démontrer le lien entre TGF-β1 et DKK2 et l’effet de ces derniers sur le phénotype des Ob. Dans cette étude on a montré que la signalisation canonique Wnt est altérée dans les Ob OA et que cela était responsable de l’altération du phénotype des Ob OA. On a montré, parmi les acteurs de la signalisation Wnt, que l’expression de l’antagoniste Dickkopf-1 (DKK1) était relativement similaire entre les Ob OA et normaux contrairement à celle de l’antagoniste DKK2 qui était augmentée et à celle de l’agoniste Wnt7B qui était diminuée dans les Ob OA. On a également montré que les PGE2 pouvaient potentialiser l’activité de la signalisation Wnt dans les Ob OA. L’inhibition de DKK2 a permis d’augmenter l’activité de la signalisation Wnt et de corriger le phénotype anormal ainsi que d’augmenter la minéralisation des Ob OA. L’inhibition de TGF-β1, un facteur aussi surexprimé dans les Ob OA, a également permis la correction du phénotype et l’augmentation de la minéralisation dans les Ob OA. L’inhibition de TGF-β1 a aussi menée à l’inhibition de DKK2. Le contraire ne fût pas observé démontrant ainsi la régulation de DKK2 par TGF-β1. En conclusion, la signalisation canonique Wnt est diminuée dans les Ob OA et cela est dû au niveau élevé de DKK2 dans ces Ob. TGF-β1 régule positivement DKK2 et donc la surexpression de TGF-β1 entraîne celle de DKK2 ce qui a pour conséquences d’altérer le phénotype des Ob. Les PGE2 ont aussi montré pouvoir potentialiser l’activité de la signalisation Wnt et auraient donc un rôle positif. Ensemble, ces données suggèrent que ces altérations au niveau des Ob OA pourraient être responsables de la structure osseuse anormale observée chez les patients OA. / Osteoarthritis (OA) is a disease affecting joints and it has a very strong incidence in the population. It is characterized by articular cartilage degradation, an abnormal bone remodelling cycle and subchondral bone sclerosis. The aetiology of this disease is still unknown although OA is now considered as a joint disease involving all the tissues of the joint. The importance of bone in OA pathogenesis is now considered as fundamental and thus bone represent an interesting target for treatments. Tomodensitometric studies have shown an abnormal structure and organisation of the bone tissue of OA patients. In parallel, primary human OA osteoblast (Ob) cultures grown from the tibiofemoral subchondral bone show an abnormal phenotype and a reduced mineralization in vitro. The Wnt signalling pathway, known primarily for its important role in embryogenesis, is of utmost importance in osteogenesis and it has been shown to regulate terminal Ob differentiation. Transforming growth factor-β1 (TGF-β1), known to act on proliferation and on early phases of the differentiation of Ob, is overexpressed by OA Ob and could also modulate the Wnt signalling activity. Furthermore, two populations of OA patients can be discriminated in vitro by the production of prostaglandins E2 (PGE2) of their Ob. In a study on colorectal cancer, PGE2 was shown to modulate the canonical Wnt signalling pathway. Our hypothesis is that canonical Wnt signalling is diminished in OA Ob. This reduction is responsible for the poor mineralization and the abnormal phenotype of human OA Ob. Furthermore, DKK2, overexpressed in OA Ob and whose expression is controlled by TGF-β1, is responsible for the diminution of Wnt signalling activity, and PGE2 can partly correct this situation. The general goal of this study is twofold: 1) to demonstrate the role of TGF-β1, DKK2 and of PGE2 in the Wnt signalling activity; 2) to demonstrate the link between TGF-β1 and DKK2 and their effect on the abnormal OA Ob phenotype. We have shown in this study that the canonical Wnt signalling pathway is altered in OA Ob and that this was responsible for the altered phenotype observed in OA Ob. Also, we have shown that among the mediators of the Wnt signalling pathway, the expression of antagonist Dickkopf-1 (DKK1) was similar between OA and normal Ob. In contrast, the antagonist DKK2 was overexpressed and the expression of the agonist Wnt7B was low in OA Ob. Moreover, PGE2 increased Wnt signalling activity in OA Ob. The inhibition of DKK2 expression also increased Wnt signalling activity and corrected the abnormal phenotype along with increasing the mineralization of OA Ob. The inhibition of TGF-β1 expression, also overexpressed in OA Ob, also resulted in the correction of the phenotype and increased the mineralization of OA Ob. Inhibiting TGF-β1 expression also led to DKK2 inhibition. As the contrary was not observed, this demonstrated that TGF-β1 could regulate DKK2 expression. To conclude, Wnt signalling is reduced in OA Ob and this is due to elevated DKK2 levels in these cells. High levels of TGF-β1 in OA Ob increased DKK2 expression which could be responsible, at least partially, for their altered phenotype. PGE2 was shown to also increase Wnt signalling activity in OA Ob. Taken together these data suggest that such alterations in OA Ob could be responsible for the abnormal bone structure observed in OA patients.

Les gisements de sulfures massifs encaissés dans les massifs hercyniens marocains des Jebilets et Guemassa sont de type (VMS) déformés et métamorphisés. Il manque toutefois une évaluation de la contribution de cette déformation à leur structuration actuelle, et l’éventuel impact de celle-ci sur le plan économique et en termes d’exploration. Par conséquent, cette contribution vise principalement à définir le contexte structural de ces minéralisations, en vue d’en déduire un modèle structural relatif au VMS de Hajjar.Le VMS de Hajjar, appartenant au domaine des Guemassa (Meseta occidentale). Il est encaissé dans des terrains d’origine volcanosédimentaire composés de pélites, de grès et de lentilles et barres calcaires intrudés par des sills et dykes felsique et basique. Les principaux corps volcaniques correspondent aux dômes rhyolitiquesLe gisement de Hajjar est composé de 3 corps minéralisés : le corps principal (CP), le corps Nord-Est (CNE) et les corps ouest et extrême ouest descenderie (CWD, CEWD). Le gisement de Hajjar est affecté par un seul plan XY d’aplatissement subvertical de directions N0 à N45. L’encaissant et les corps sulfurés présentent les mêmes assemblages métamorphiques silicatés, qui présentent soit une texture granoblastique « statique » lorsque la déformation est faible, soit des caractéristiques prés à syn-tectoniques lorsque la schistosité est fortement exprimée. La texture, les formes des biotites et d'andalousites (± cordiérite suspectée) sont typiques du métamorphisme de contact HT / BP des faciès de cornéennes. L'assemblage syntectonique est composé de quartz + chlorite + micas blancs (± calcite), et remplace partiellement les anciennes biotites et andalousites. Les données de surface du bloc N'Fis montrent la présence d'un seul plan XY subvertical orienté N130. Les biotites du métamorphisme de contact sont allongées parallèlement à la schistosité. L’ensemble des données indiquent que le VMS de Hajjar et le bloc N'Fis sont affectés par une seule schistosité qui est synchrone d’un métamorphisme de contact de HT / BP. La virgation importante de la schistosité des affleurements d'Imarine au VMS de Hajjar est dû à une importante zone de cisaillement - transpressive de direction ENE-WSW. Près de la mine Hajjar, une telle zone de cisaillement à l’échelle régionale est reconnue pour la première fois, et constitue une caractéristique structurale-clé du district de Hajjar.La minéralisation de Hajjar est fortement déformée et métamorphisée. Elle est affectée par le plissement, la schistosité et la mylonitisation dans un contexte cisaillant. Les structures minéralisées stratiformes sous forme de rubans riches en pyrrhotite précèdent clairement la déformation et le métamorphisme de contact. D’autres structures minéralisés riche en (Zn, Cu, Pb) présentent un rubanement tectonique issu de la remobilisation par fluide de la minéralisation précoce Le stade précoce est caractérisé par la précipitation de la pyrrhotite, pyrite, arsénopyrite, sphalérite et la galène, alors que le stade syncinématique constitue l’événement concentrateur majeur caractérisé par la dissolution et la recristallisation de la paragenèse précoce avec un enrichissement en Zn, Cu. Le stade tardif post-cinématique est responsable la néoformation de sulfures, à savoir la chalcopyrite, la pyrite et quelques traces de sphalérite.Nous avons mis en évidence un épaississement tectonique dans les zones de charnières. Le métamorphisme pré à syntectonique favorise le comportement ductile et la recristallisation des sulfures (Po, Cpy et Sph). Les veines triangulaires polymétalliques à l'extrémité des lentilles de sulfures massifs sont le témoin d'une remobilisation hydrothermale assistée par un fluide pendant la déformation. L’ensemble de nos études débouche sur la proposition d’un modèle 3D tectonométamorphique pour le VMS des Guemassa et des propositions pour rechercher des extensions de la minéralisation. / The massive sulphide deposits hosted in the Moroccan Hercynian massifs of Jebilets and Guemassa are Volcanogenic Massive Sulfide (SMV), deformed and metamorphosed. However, an assessment of the contribution of this deformation to their current structure and the eventual impact on the economy and in terms of exploration is missing. Therefore, this contribution aims mainly to define the structural context of these mineralizations, in order to deduce a structural model relating to Hajjar's VMS.The VMS of Hajjar, belonging to the domain of Guemassa (Western Meseta). It is hosted in volcanosedimentary terrain composed of pelites, sandstones and lentils and limestone bars intruded by felic and basic sills and dykes. The main volcanic bodies correspond to the rhyolitic plugs.The Hajjar deposit is composed of 3 mineralized bodies: main body (CP); north-eastern body (CNE); western body (CWD) and extreme western body(CEWD.). The Hajjar deposit is affected by a single XY plane of subvertical flattening of directions N0 to N45. The host rock and sulphide bodies have the same silicate metamorphic assemblages, which exhibit either a "static" granoblastic texture when the strain is low or pre to syn-tectonic features when the foliation is strongly expressed. The texture shapes, and aggregates of the biotite and andalousite (± suspected cordierite) are typical of HT/LP “contact” metamorphism in the hornfels facies. The syn-tectonic assemblage is composed of quartz + chlorite + white micas (± calcite) and partially replaced the former biotite and andalousite blasts. The data from the N’Fis block show the occurrence of a single sub-vertical XY plane oriented N130. The biotites of contact metamorphism are elongated parallel to the foliation. These data imply that the Hajjar MSD and the N’Fis block are affected by a single foliation which encompasses a HT/LP contact metamorphism. The significant inflexion of foliation from Imarine outcrops to Hajjar VMS is due to major right-lateral ENE-trending transpressive shear zone at Hajjar. Near the Hajjar mine, such a regional shear zone is recognized for the first time, and is a structural key feature of the Hajjar district.The mineralization of Hajjar is strongly deformed and metamorphosed. It is affected by folding, foliation and mylonitic bands within a regional scale shear zone. Structures such as pyrrhotite-rich ribbons clearly pre-date the deformation and the HT/LP contact metamorphism. The early stage is characterized by the precipitation of pyrrhotite, pyrite, arsenopyrite, sphalerite, and galena, whereas the synkinematic stage constitutes major concentrator event characterized by the dissolution and recrystallization of early paragenesis with enrichment in Zn, Cu. The late post-kinematic stage is responsible for the neoformation of sulphides, namely chalcopyrite, pyrite and some traces of sphalerite.We have demonstrated a tectonic thickening within the fold hinge zone. pre-syntectonic metamorphism favors ductile behavior and sulfide recrystallization (Po, Cpy, and Sph). The polymetallic veins argue for hydrothermal fluid-assisted remobilization during deformation. All of our studies lead to the proposal of a 3D tectono-metamorphic model for the VMS of Guemassa and proposals to search extensions of the mineralization.

Le gisement de Tocantinzinho est situé sur la province aurifère de Tapajós et est le plus grand gisement d'or de la province, avec 53,9 tonnes d'or estimées. Sa formation commence par un magmatisme granodioritique autour de 2005 Ma, suivi d'un magmatisme granitique. Le granite Tocantinzinho est composé de deux faciès principaux (syenogranite - 1996± 2Ma; monzogranite 1989±1 Ma), des corps d’aplite et de pegmatite, qui suggère un magmatisme enrichie en fluide et mis en place à faible profondeur. Intrusifs dans ces roches, des dykes d'andésite (1998±8Ma) ont des fragments de granite et des mélanges entre les 2 magmas suggèrent un magmatisme à la fois continu et polyphasé. Il est proposé que les premiers dykes d’andésite se sont mis en place alors que le granite n’était pas entièrement cristallisé (mingling) et les derniers lors des stades de déformation à l’état solide du granite. Utilisant la courbe de refroidissement, un âge minimum de 1975 Ma a été estimé pour l’andésite. Les taux de refroidissement des roches plutoniques varient de 3,6 à 14,7°C/Ma, avec une moyenne de 7,5°C/Ma, suggérant que les processus d'exhumation verticale sont faibles. La géométrie allongée du granite ainsi que la tectonique syn-magmatique de l'andésite corroborent la prédominance des mouvements horizontaux. L’affinité calc-alcaline fortement potassique et des anomalies en niobium définissent deux configurations possibles pour le cadre géotectonique: arc continental de type Andin ou Post-collisionnel. Compte tenue la relation génétique entre magmatisme, cisaillement décrochant et les faibles taux de refroidissement, l’environnement post-collisionnel est plus probable. Cela ensemble avec les âges nous permettent de comparer ces roches avec celles de la Suite Intrusive Creporizão (1997-1957Ma). La dacite (1992 ± 2 Ma) recoupe les autres roches, cependant, la signature géochimique comparable aux roches anorogéniques suggère qu’elle appartient à une série magmatique distinct. La zone minéralisée est limitée par deux failles majeures senestres de direction N100°-130E°. Le granite Tocantinzinho et les roches hypo-volcaniques déformées sont dans ce couloir, altérées par de fluides hydrothermaux et minéralisées pendant deux phases tectoniques distinctes. La première est caractérisée par des brèches et des microfractures remplies par muscovite (1864±5Ma) et pyrite, associées à de faibles teneur d’or (<1,5ppm) restreintes au granite. La deuxième phase a été contrôlée par le cisaillement décrochant senestre normal générant des fentes de tension et des brèches remplies par quartz, chlorite, calcite, albite, rutile, pyrite, galène, sphalérite, chalcopyrite et or. La teneur en or peut atteindre jusqu'à 70 ppm dans les veines riches en sulfures. Ces structures de remplissage syntectonique sont parallèles entre elles et orientées N30-60°E. Deux hypothèses ont été proposées pour expliquer la genèse du gisement: la première considère une relation génétique entre magmatisme et minéralisation au moins pour le premier stage de minéralisation selon un modèle porphyrique et la seconde alternative considère une réactivation des failles préexistantes par une tectonique transtensive liée au magmatisme Maloquinha (ca. 1880Ma) pour les deux stades minéralisateurs. Les deux phases dans les deux hypothèses, ont été classées comme des minéralisations de type magmato-hydrothermale qui pourraient être classées soit comme des systèmes d'or liés à l'intrusion. De nouveaux travaux sur le terrain et en laboratoire seraient nécessaires pour identifier et caractériser la nature et la source des fluides hydrothermaux, pour dater la minéralisation et mieux comprendre le rôle des roches hypo-volcaniques. Toutefois, les premiers résultats, et notamment le rôle fondamental du contrôle tectonique pour la minéralisation sont très significatifs et peuvent aider de manière conséquente à l'établissement des programmes d'exploration et d'exploitation futurs. / The Tocantinzinho deposit is located on the Tapajós Gold Province and is the largest gold deposit within Province, with 53,9 tons of gold. Its formation begins with a granodioritic magmatism around 2005Ma, followed by a granitic magmatism 10 Ma latter. The Tocantinzinho granite is composed by two main facies, syenogranite (1996±2Ma) and monzogranite (1989±1Ma), and by aplite and pegmatite bodies, suggesting a fluid-rich magmatism at shallow depth. Andesite dikes (1998±8Ma) are intrusive in both rocks. Sharp fragments of those rocks along contacts and minor mingling with granitic magma suggest a multiphase magmatism at distinct timing. The first dikes have intruded within granite when it was crystalizing, thus a minimum age of 1975Ma was estimated. Cooling rates of plutonic rocks vary from 3.6 to 14.7°C/Ma, with an average of 7.5°C/Ma, suggesting vertical exhumation processes were minor. The elongated geometry of granite along with sin-magmatic strike-slip tectonics of andesite corroborate the predominance of horizontal movements. Geochemical analysis show high-K calk-alkaline affinity and niobium anomaly indicator of two possible geotectonic settings for these rocks: Andean-type continental arc or post-collisional one. Considering the genetic relationship between magmatism, strike-slip faults, and low cooling rates, a post-collisional setting is more likely. The geochemical signature, ages and style of tectonism allow us to compare those rocks with the ones from Creporizão Intrusive Suite (1997-1957Ma). Dacite dikes (1992±2Ma) cut across all other rocks, but the temporal relationship among them remains misunderstood, due to the geochemical signature similar to the anorogenic rocks, suggesting it belongs to a distinct and latter magmatic series. Indeed, the dated zircons were probably inherited from host rocks. The mineralized area is restricted to a domain constrained by two major sinistral strike-slip N100°-130E°E faults that comprises the Tocantinzinho granite and sub-volcanic rocks, which were hydrothermally altered, brittle deformed and mineralized during two phases. The first one is characterized by breccias and microfractures infilled with muscovite (1864±5Ma) and pyrite, which contains low gold grades and are restricted to the Tocantinzinho granite. The second phase was controlled by strike-slip and normal tectonics generating tension gashes veins and pull apart breccias infilled with quartz, chlorite, calcite, albite, rutile, pyrite, galena, sphalerite, chalcopyrite, and gold. The gold grade can reach up to 70 ppm in some sulfide-rich veins. These structures are parallel and mainly trends N30-60°E, showing textures and orientated minerals typical of syn-tectonic infilling. Based on petrographical features and argon ages two hypothesis were proposed for the ore genesis: the first one consider a genetic relationship between magmatism and ore fluids for first mineralization stage and the second hypothesis consider a reactivation of pre-existing faults by an extensional tectonism related to the Maloquinha Intrusive Suite magmatism (ca.1880Ma) for this phase. The second mineralization phase is considered as formed as consequence of tectonic reactivation at ca. 1880Ma, in both hypothesis. Both phases in both hypothesis were classified as magmatic-hydrothermal ore mineralization and might be classified as intrusion-related gold systems. However, new field works are important in order to identify and characterize the nature and source of hydrothermal fluids, as well as ore dating and new geochemical and geochronological data of sub-volcanic rocks are imperative to better understand the genesis and evolution of the Tocantinzinho gold deposit. Such results, strongly linked to the fact that the tectonic control seem significant, may help for future exploration and exploitation programs.

A compostagem é uma solução inteligente para a destinação final de resíduos orgânicos. O presente trabalho baseou-se na hipótese de que é possível, por meio da aplicação de compostos orgânicos ao solo, alcançar patamares de produção agrícola equivalentes aos obtidos pela adubação nitrogenada mineral. O experimento foi realizado em vasos com Brachiaria brizantha cv. Marandu em dois solos, um de textura argilosa e outro de textura média. Objetivou-se avaliar a dose de nitrogênio (N) proveniente de composto de lixo, composto de lodo de esgoto e composto de lodo de dejetos suínos que fosse equivalente à dose de 150 mg dm-3 de N proveniente da adubação nitrogenada mineral. Para isso, as doses de composto orgânico foram determinadas com base nas frações de mineralização de N, estimadas em 30, 15 e 7%. Assim, para a obtenção de 150 mg dm-3 de N mineralizado, foram aplicadas doses de, respectivamente, 500, 1.000 e 2.143 mg dm-3 de N total, provenientes dos compostos orgânicos. Foram realizados três cortes no capim Marandu, sendo mensurados, a cada corte, o teor de clorofila, o número de folhas e de perfilhos, a área foliar, a biomassa e o teor de N total da parte aérea das plantas. Os resultados foram submetidos à análise de variância, teste de médias e análise de regressão. Foi possível, por meio dos compostos orgânicos, obter resultados de adubação nitrogenada equivalentes, e até superiores, aos obtidos pela adubação mineral, dependendo do tipo de composto, a dose aplicada e a escala temporal. De modo geral, os tratamentos com composto de lodo de esgoto, a partir da dose 1.000 mg dm-3 de N, foram superiores ao com adubação mineral no primeiro corte, equivalentes no segundo corte, e superiores no terceiro corte do capim Marandu. A quantidade de N liberada ao sistema por meio dos compostos de lixo e de lodo de dejetos suínos chegou aos patamares dos tratamentos com adubação mineral no segundo corte, na dose 2.143 mg dm-3 e no terceiro corte, na dose 1.000 mg dm-3 de N. As frações de mineralização de N que geraram resultados mais próximos aos da adubação nitrogenada mineral foram, em média, de 15% para o composto de lodo de esgoto e de 7% para os compostos de lixo e de lodo de dejetos suínos / Composting is a smart final destination for organic residues. The present work was based in the hypothesis that it is possible to obtain similar agricultural productivity levels applying organic compounds on soil in comparison with mineral nitrogen application. The experiment was conducted in pots with Brachiaria brizantha cv. Marandu in two soil types, with clay and sandy clay loam texture. The objective was to evaluate if estimated doses of nitrogen (N) from waste compost, sewage sludge compost and and pig manure compost, when applied on the soil, was equivalent to 150 mg dm-3 of mineral Nitrogen fertilizer. The doses of organic composts applied were based in estimations of N mineralized of 30, 15 and 7%, correspondent, respectively, to doses of 500, 1000 and 2143 mg dm-3 of total N. The grass was harvested three times, on each time the chlorophyll level, the number of leaves, number of branches, leaf area, biomass and total N were measured in the aerial part of the plants. The results were submitted to variance analysis, and regression analysis. It was possible, trough the N fertilization by organic composts, to obtain similar and even superior results, in comparison to the mineral N, depending on type of compost, the applied dose and the time frame. The treatment with sewage sludge compost in the dose of 1000 mg dm-3 of N was superior to the mineral N in the first harvest, similar in the second and superior in the third harvest of the grass. The waste and pig manure composts reached similarity with the mineral fertilization in the second harvest, in the dose of 2143 mg dm-3, and in the third harvest, in the dose of 1000 mg dm-3 of N. The mineralization fractions of N found for the composts that were the most similar the mineral fertilization were, in average, of 15% for the sewage sludge compost and 7% for the waste and pig manure compost

Este estudo in vitro teve como objetivo avaliar os efeitos moleculares do TGF-&beta;1, com diferentes períodos de suplementação, sobre a formação do fenótipo osteogênico das células MC3T3-E1, comparando-os com células tratadas com AA+&beta;-GP suplementados com Dex e/ou TGF-&beta;1, sem e com a neutralização dos receptores de TGF-&beta;1. A expressão gênica do próprio TGF-&beta;1 e Smad3 foram analisadas, bem como, a diferenciação das células osteogênicas e a biomineralização. As células tratadas com TGF-&beta;1 sem neutralização de receptores apresentam efeito inibitório nos estágios mais avançados da diferenciação dos osteoblastos e da biomineralização in vitro, mas expressarem alguns marcadores importantes envolvidos na mineralização. Observaram-se nódulos de mineral em todos os tratamentos das células que tiveram os receptores de TGF-&beta;1 neutralizados, mas houve uma diminuição na expressão de alguns genes. Os resultados confirmam a complexidade da via de sinalização do TGF-&beta;1, mostrando que existem lacunas para que seja entendido o mecanismo dessa molécula na biologia osteoblástica. / This in vitro study aimed to evaluate the molecular effects of TGF-&beta;1, with different supplementation time periods on the establishment of MC3T3-E1 cells, comparing with cells treated with AA+&beta;-GP supplemented with Dex and/or TGF-&beta;1, without or with neutralization of TGF-&beta;1 receptors. The gene expression of the TGF-&beta;1 and Smad3 were analyzed, as well as the osteoblast differentiation and biomineralization. The cells treated with TGF-&beta;1 without neutralization of receptors have had inhibitory effect on some important stages of osteoblast differentiation and biomineralization in vitro, but expressed some important mineralization markers. Mineral nodules were observed in all treatments of cells with their TGF-&beta;1 receptors neutralized, but there was a decrease in the expression of some important genes. The results confirm the complexity of the pathway signaling of TGF-&beta;1, showing that there are gaps for understand the mechanisms of this molecule in the biology of osteoblasts.

A adição ao solo de resíduo vegetal de elevada relação C/N no sistema \"cana crua\", afeta o equilíbrio entre os processos de entrada e saída do N no sistema solo-planta-atmosfera. Assim, a presença da palhada modifica o agrossistema fazendo-se necessários ajustes no manejo da fertilização nitrogenada. Nesse sentido, quatro estudos foram desenvolvidos com os seguintes objetivos: (i) Avaliar as características produtivas e nutricionais da cultura da cana-de-açúcar de modo a identificar a fonte e a dose de N de maior eficiência agronômica; (ii) Quantificar a recuperação do N proveniente do fertilizante pela cana-de-açúcar; (iii) avaliar o potencial de inibição do íon cloreto na nitrificação no solo; (iv) avaliar as taxas de mineralização e imobilização do N-fertilizante e a sua interação com o Nnativo do solo. Em campo, foi conduzido um experimento em Latossolo Vermelho distróficocom cana-de-açúcar. O delineamento experimental foi o de blocos casualizados, com quatro repetições e nove tratamentos, com as fontes nitrogenadas: sulfato de amônio, YaraBela NitromagTM, nitrato de amônio e ureia na dose de 100kg ha-1 de N, cloreto de amônio, nas doses de N: 50, 100, 150 e 200 kg ha-1, e controle. Foram instaladas microparcelas com aplicação das fontes marcadas no isótopo 15N na dose de 100 kg ha-1 de N. Os fertilizantes nitrogenados foram aplicados manualmente, sobre a palhada. Posteriormente, amostras do solo coletadas previamente foram incubadas aerobiamente por um período de 21 dias. O delineamento experimental foi o inteiramente casualizado com quatro repetições e os tratamentos constaram da combinação de sulfato de amônio ou cloreto de amônio, na dose de 100 mg kg-1 de nitrogênio, com cloreto de potássio na dose de 100 ou 200 mg kg-1 de cloro. Avaliou-se, também, doses de cloreto de amônio (50, 100 e 200 mg kg-1 de N). As formas de N-mineral foram determinadas por meio de sistema de análise por injeção em fluxo. Amostras de solo foram, também, incubadas aerobiamente por um período de 20 semanas. O delineamento experimental foi o inteiramente casualizado com três repetições e seis tratamentos, constituindo-se um fatorial 3x2 (Namídico, N-amoniacal ou sem N versus com ou sem resíduo de cana). As fontes nitrogenadas (enriquecidas com 2% em átomos de 15N) foram aplicadas superficialmente no solo na dose de 100 mg kg-1 de N e o resíduo de cana-de-açúcar incorporado na dose de 5,2 g kg-1. O fornecimento de doses de N na forma de cloreto de amônio resultou em decréscimo de produtividade de colmos e açúcar. As fontes nítrico/amoniacais promoveram maior atividade da enzima redutase do nitrato nas folhas da cana-de-açúcar, porém, não apresentaram influência no acúmulo total de N. O aproveitamento do N-fertilizante pela cana-de-açúcar foi da ordem de 60% nos estádios iniciais, reduzindo-se para aproximadamente 20% próximo à fase de maturação. O íon cloreto reduziu a concentração de nitrato no solo devido a ação do ânion na reação de nitrificação. A incorporação de resíduo de cana-de-açúcar ao solo promoveu maiores taxas de imobilização do N e a aplicação de sulfato de amônio resultou em maior mineralização do N nativo do solo comparado a ureia. / The addition of plant residue with high C/N ratio to the soil in a \"green cane\" system affects the balance of input/output processes of N in a soil-plant-atmosphere system. Thus, the presence of straw modifies the agroecosystem requiring adjustments in management of nitrogen fertilization. Accordingly, four studies were developed to: (i) evaluate the nutritional and productive characteristics of sugarcane crops to identify the source and N rates of greater agronomic efficiency; (ii) quantify the sugarcane N recovery from fertilizers; (iii) assess the potential inhibition of chloride ion in reaction to soil nitrification, (iv) evaluate mineralization and immobilization rates of fertilizer-N and their interaction with the native soil N. We conducted a field experiment on a Typic Hapludox with sugarcane, in the 2009/2010 harvest. The experimental design was a randomized block with four replications and nine treatments with nitrogen sources: ammonium sulfate, YaraBela NitromagTM, ammonium nitrate and urea at 100 kg N ha-1, ammonium chloride at N doses: 50, 100, 150 and 200 kg ha-1 and control. Microplots were installed with application of nitrogen sources labeled 15N at 100 kg N ha-1. Nitrogen fertilizers were applied manually over straw. Subsequently, previously collected soil samples were incubated aerobically for 21 days. The experimental design was completely randomized with four replications and the treatments consisted of ammonium sulfate or ammonium chloride at 100 mg N kg-1 with potassium chloride at a chlorine dose 100 or 200 mg kg-1. We also evaluated doses of ammonium chloride (50, 100, and 200 mg N kg-1). Forms of mineral-N were determined by Flow Injection Analysis (FIA) system. Soil samples were incubated aerobically for 20 weeks. The experimental design was completely randomized with three replications and six treatments, comprising a 3x2 factorial (amidic-N, ammonium- N or without N versus with or without cane residue). Nitrogen sources (enriched with 2 atom% 15N) were applied to the soil surface at a N dose of 100 mg kg-1 and residue sugarcane incorporated at 5.2 g kg-1. The N supply in ammonium chloride form resulted in decreased yield of sugar and stalks. Nitric-ammonium sources promoted higher activity of nitrate reductase in sugarcane leave; however, they did not affect total N accumulation. The sugarcane recovery of fertilizer-N was approximately 60% in early stages, dropping to about 20% near the maturity stage. The chloride ion reduced nitrate concentration in soil due to the anion action in the nitrification reaction. The sugarcane residue incorporation to the soil showed higher N immobilization rates and the use of ammonium sulfate resulted in higher N mineralization rates of native soil N compared to urea.

Cette thèse visait l’étude des micro-environnements géochimiques créés par la présence de l’herbier de Zostera noltei et de son réseau racinaire dans le Bassin d’Arcachon ainsi que ses effets 1) sur l’écologie des foraminifères benthiques, un groupe d’organismes présent en grand nombre dans les sédiments et dont l’influence sur les cycles biogéochimiques reste mal connue et 2) sur les espèces chimiques et les flux benthiques associés. Pour y répondre, une stratégie multidisciplinaire a été mise en place. L’étude écologique des foraminifères benthiques à l’échelle centimétrique, conduite dans des sédiments avec et sans végétation en février et juillet 2011, a montré la présence de trois espèces majeures aux métabolismes spécifiques. L’herbier de Zostera noltei semble influencer la densité et la profondeur de vie des espèces calcaires hétérotrophe (Ammonia tepida) et mixotrophe (Haynesina germanica), présentes près de la surface des sédiments. La troisième espèce (Eggerella scabra), au métabolisme anaérobie encore inconnu, est retrouvée sur au moins 7 cm de sédiment et semble préférer le carbone organique issu de la dégradation de l’herbier. En surface, la contribution des foraminifères à la reminéralisation aérobie a été évaluée à 7 % soit 5 fois plus que lors des études précédentes dans d’autres environnements marins. La présence de l’herbier influence également la géochimie du sédiment où des structures enrichies en fer dissous et appauvries en sulfure sont observables en 2D grâce aux gels DET-DGT développés ici. Le phosphate dissous semble dépendre de la demande des zostères et est observé à forte concentration uniquement sous forme de spots. Une tranche de sédiment, prélevée en vis-à-vis du gel DET-DGT visait la réalisation de cartes de la phase solide et de la densité des foraminifères. Bien que ce travail reste inachevé, des méthodes comme la micro-fluorescence et la micro-tomographie aux rayons X donnent des perspectives prometteuses. De nouvelles voies de recherches ont ainsi été ouvertes grâce à des méthodologies innovantes combinant physiologie, écologie et géochimie. / This thesis aimed to study the geochemical microenvironments created by Zostera noltei meadows and its root system in Arcachon Basin and to evaluate the effect of these microenvironments 1) on living benthic foraminifera ecology, a group of organisms present in large densities in sediment which impact on marine biogeochemical cycles remain poorly known and 2) on the chemical species and associated benthic fluxes. To fulfill these objectives, a multidisciplinary strategy was developed. The study of benthic foraminiferal ecology at centimeter scale, conducted in sediments with or without vegetation in February and July 2011, has shown the presence of three major species with specific metabolisms. Zostera noltei meadows seem to influence the densities and the living depth of heterotrophic (Ammonia tepida) and mixotrophic (Haynesina germanica) calcareous species, present in the sediment surface. The third species (Eggerella Scabra), which anaerobic metabolism is still to discover, is found throughout the sedimentary column and seems to prefer the organic matter coming from the degradation of the seagrass. In surface sediment, the contribution of these three species to aerobic remineralization was estimated at 7%, i.e. 5 times more than the maximum rates previously recorded in marine environments. The presence of the seagrass also influences geochemistry where enriched iron and depleted sulfide structures are observable in 2D thanks to DET-DGT gels developed here. Dissolved phosphorus depended on seagrass uptake and was highly concentrated only as scattered spots. A slice of sediment, taken face to face with the DET-DGT gel, was also conducted during this study aiming to map the solid phase and foraminiferal density. Despite this work is still in progress, methods such as X-ray microfluorescence and microtomography showed promising perspectives. New research pathways have been opened through technological developments and innovative approaches combining physiology, ecology, and geochemistry.

O cinturão Fíngoè é uma unidade tectônica do Supercontinente Gondwana Oeste composta por rochas supracrustais formadas há aproximadamente 1.33 Ga. Essas rochas são portadoras de mineralizações de Au, Cu, Zn, Pb e Fe. Com cerca de 150 km de comprimento, e orientado WSW-ENE, este cinturão estende-se desde o Monte Atchiza a oeste até cerca de 30 km para leste da vila de Fíngoè no norte de Moçambique e consiste de uma extensa variedade de rochas metassedimentares e metavulcânicas. O cinturão Fíngoè apresenta especialização metalogenética para Au e Cu, que já foram explotados no passado em diversos locais. Muitos destes registros estão associados com magnetita e malaquita. Atualmente trabalhos de prospecção e pesquisa mineral têm sido realizados pela empresa de mineração African Queen Mines Ltda, através do projeto denominado de King Solomons, localizado na parte central do mesmo. A geologia da área abrangida pelo prospecto Mankombiti, mostra uma predominância de rochas carbonáticas, granitos e gabros. As rochas carbonáticas são consideradas importantes na gênese de depósitos tipo skarn e depósitos de substituição de metais de base e Au devido à sua natureza fortemente reativa. Os dados geocronológicos realizados neste trabalho indicaram uma idade precisa para a rocha intrusiva granítica associada à mineralização de 1079,1 ± 8,2 Ma, que poderia ser a idade da formação do skarn e consequentemente desta mineralização. Entretanto a idade obtida para o processo de alteração hidrotermal que afetou o gabro, na ordem de 657 ± 36 Ma e a idade modelo Pb-Pb sugerida pelo modelo de Stacey e Kramers (1975) para a calcopirita da mineralização principal de 725 Ma, sugerem que a mineralização, do prospecto Mankombiti é neoproterozóica. Para melhor entendimento dos processos que estiveram envolvidos na formação deste depósito skarn, duas hipóteses são consideradas: (i) poderia ser admitida a presença de corpos graníticos intrusivos em 700 Ma, situados em profundidade, que não foram ainda caracterizados, como responsáveis pela fonte de calor necessária, (ii) pode ser admitida ocorrência de um evento distensional em 700 Ma que produziria um adelgaçamento da litosfera e a consequente ascensão da astenosfera, produzindo uma elevação do fluxo térmico gerando os fluidos mineralizantes necessários. / The Fíngoè belt is a tectonic unit of West Gondwana Supercontinent, comprised of supracrustal rocks formed at approximately 1.33 Ga. These rocks are carriers of Au, Cu, Zn, Pb and Fe mineralization. With about 150 km long and oriented WSW- ENE, this belt extends from west of the Atchiza Mount to about 30 km east of the Fíngoè village in the north Mozambique, and consists of an extensive variety of metasedimentary and metavolcanic rocks. The Fíngoè metallogenic belt provides specialization for Au and Cu, which have been exploited in the past in various locations. Many of these records are associated with magnetite and malachite. Currently, the prospecting and mineral exploration have been conducted by the African Queen Mines Ltd mining company, through a project called the King Solomons, located in the central part of it. The geology of the studied area shows a predominance of carbonate rocks, granites and gabbros. The carbonate rocks are considered important in the genesis of the skarn deposits type and deposits of replacement for base metals and Au due to its highly reactive nature. The geochronological data performed in this work indicate a precise age of the 1079.1 ± 8.2 Ma for the intrusive granitic rock associated with mineralization, which could be interpreted as the age of the skarn and consequently of the mineralization. However the age obtained for the hydrothermal alteration that affected the gabbro at about 657 ± 36 Ma and the Pb-Pb model age suggested by the model of Stacey and Kramers (1975) for primary chalcopyrite mineralization at 725 Ma, suggesting that the mineralization of the Mankombiti prospectus was developed during the Neoproterozoic time. For understanding the processes that were involved in the skarn-type mineralization processes, two hypotheses are here considered: (i) could be admitted the presence of i ntrusive granitic rocks at 700 Ma, situated in depth, which have not yet been characterized, as responsible for the heat source required, (ii) may be admitted occurrence of an extensional event at 700 Ma to produce a thinning of the lithosphere and the uplift of the asthenosphere, producing high thermal flows generating the mineralization fluids.

Submitted by Biblioteca de Pós-Graduação em Geoquímica BGQ (bgq@ndc.uff.br) on 2017-09-04T17:31:07Z No. of bitstreams: 1 TESE_Viviane Figueiredo Souza versão final.pdf: 1973892 bytes, checksum: 8b1ac31fbe25c8a6584e68f8e3b8ff71 (MD5) / Made available in DSpace on 2017-09-04T17:31:07Z (GMT). No. of bitstreams: 1 TESE_Viviane Figueiredo Souza versão final.pdf: 1973892 bytes, checksum: 8b1ac31fbe25c8a6584e68f8e3b8ff71 (MD5) / Conselho Nacional de Desenvolvimento Científico e Tecnológico / Universidade Federal Fluminense. Instituto de Química. Programa de Pós-Graduação em Geoquímica, Niterói, RJ / O nitrogênio (N) é um elemento imprescindível para todos os organismos do nosso planeta, entretanto o composto nitrogenado mais abundante, o gás dinitrogênio (N2), é assimilável apenas por poucos micro-organismos. Isso torna o N limitante, refletindo na sua disponibilização via mineralização de matéria orgânica (MO) e a nitrificação, que produzem amônio (NH4+) e nitrato (NO3-), respectivamente. Em solos, esses processos são regulados por fatores como conteúdo de MO e água no solo, pH e temperatura. Em ecossistemas florestais, tropicais e boreais, esses processos são muito relevantes e ainda pouco estudados, principalmente em áreas de floresta secundária sob influência de manejo. A mudança de uso do solo causa alterações na ciclagem e disponibilidade do N, nos fatores reguladores, e na emissão de óxido nitroso (N2O), um gás de efeito estufa. Padrões de recuperação florestal são bastante distintos entre diferentes florestas tropicais, como visto para floresta de Mata Atlântica e Amazônica, com taxas de mineralização em florestas jovens (10 anos) muito elevadas na Amazônia (20,9 μg N g-1 SWD d-1) e mais baixas na Mata Atlântica (3,2 μg N g-1 SWD d-1). Já a nitrificação teve um padrão semelhante, com baixas taxas em ambas as florestas jovens (0,6 6,8 μg N g-1 SWD d-1 na Mata Atlântica e Amazônia, respectivamente), o que indica uma ciclagem de N conservativa, evitando perdas via emissão de gás e lixiviação de NO3-. Entretanto, a emissão de N2O em área de restauração na Mata Atlântica foi maior do que na pristina (22 e 2,5 μg N2O-N g-1 SWD h-1, respectivamente) devido à maior temperatura do solo que estimula os processos microbianos produtores de N2O. Em termos de floresta pristina, a taxa de nitrificação foi bastante distinta entre a floresta de Mata Atlântica e Amazônica (0,08 e 15,9 μg N2O-N g-1 SWD h-1, respectivamente). Isso evidencia os diferentes fatores reguladores de cada região tropical, como regime de chuvas, composição vegetal, tipos de solo, etc. Em florestas boreais, foi visto que o conteúdo de MO e água do solo e o pH do solo são os principais reguladores, limitando a disponibilidade de N em florestas bem drenadas dominadas por coníferas, em comparação com florestas pouco drenadas dominadas por turfa. Dessa forma, verificamos que a mineralização e, principalmente, a nitrificação, são processos muito relevantes no controle de N, e mesmo em ecossistemas diferentes, os fatores reguladores muitas vezes são os mesmos. Isso evidencia a necessidade de mais estudos acerca da dinâmica do N nesses ambientes, principalmente em florestas em restauração / Nitrogen (N) is an essential element for all organisms; however, the most abundant nitrogen compound, dinitrogen (N2), is assimilable only by a few microorganisms. This makes N limiting, which reflects in its availability via organic matter (OM) mineralization and nitrification, which produce ammonium (NH4+) and nitrate (NO3-), respectively. In soils, these processes are regulated by factors such as OM and soil water content, pH and temperature. In forest ecosystems, tropical and boreal, these processes are very relevant and still poorly understood, especially in secondary forest previously deforested. The land use change causes alterations in cycling and availability of N, regulating factors, and emission of nitrous oxide (N2O), a greenhouse gas. Forest recovery patterns are quite distinct among different rainforests, as seen for Atlantic and Amazon rainforest, with very high levels of mineralization in young forests (10 years) in Amazonia (20.9 μg N2O-N g-1 SWD h-1) and low in the Atlantic Forest (3.2 μg N2O-N g-1 SWD h-1). Nitrification had a similar pattern between them, with low rates in both young forests (0.6 and 6.8 μg N2O-N g-1 SWD h-1 in the Atlantic and Amazon forest, respectively), indicating a conservative N cycling, avoiding losses through gas emission and NO3- leaching. However, the N2O emission in restoration area in the Atlantic Forest was higher than in pristine (22 and 2.5 μg N2O-N g-1 SWD h-1, respectively) due to the higher soil temperature, which stimulates microbial production of N2O. In terms of pristine forest, the nitrification rate was very different between the Atlantic forest and Amazonian forest (0.08 and 15.9 μg N2O-N g-1 SWD h-1, respectively), showing the different regulatory factors of each tropical region, such as rainfall regime, vegetal composition, soil types, etc. In boreal forests, OM, soil water content and soil pH were the main regulators, limiting the availability of N in conifer-dominated well-drained forests compared to peat-dominated poorly drained forests. In this way, we verified that mineralization and, mainly, nitrification are very relevant processes in the control of N, and even in extremely different ecosystems, the regulating factors are often the same. This evidences the need for more studies about N dynamics in these environments, especially in restoration forests