Encontrados 4 documentos, a visualizar página 1 de 1
Neudesin is involved in anxiety behavior : structural and neurochemical correlates
Novais, Ashley da Cruz; Ferreira, Ana C.; Marques, Fernanda; Pêgo, José M.; Cerqueira, João; Pereira, Ana Carla David; Campos, Filipa L.Neudesin (also known as neuron derived neurotrophic factor, Nenf) is a scarcely studied putative non-canonical neurotrophic factor. In order to understand its function in the brain, we performed an extensive behavioral characterization (motor, emotional, and cognitive dimensions) of neudesin-null mice. The absence of neudesin leads to an anxious-like behavior as assessed in the elevated plus maze (EPM), light/d...
Whole blood transfusion in small animals: indications and effects
Godinho-Cunha,Luís F; Ferreira,Rui M. R. F; Silvestre-Ferreira,Ana CTransfusion therapy is a major resource that can improve the patient's capability to overcome the underlying disease. However, the effects of whole blood infusion, and how they affect the patient's outcome, are not yet clear. For this study, a protocol was developed in order to monitor a group of 15 animals (9 dogs, 6 cats) that received a total of 19 transfusions; 3 animals received more than one transfusion e...
Chemical composition of gahnite and degree of pegmatitic fractionation in the B...
Soares,Dwight R.; Beurlen,Hartmut; Ferreira,Ana C.M.; da-Silva,Marcelo R.R.Gahnite electron probe microanalyses from three pegmatites (Mirador, Capoeira and Quintos) of the Borborema Pegmatitic Province in northeastern Brazil allowed to determine molar compositions ranging from 86.22 to 95.41 mol% gahnite (ZnAl2O4), 1.51 to 6.62 mol% hercynite (Fe2+Al2O4), 0.11 to 5.89 mol% spinel (MgAl2O4), 1.48 to 2.74 mol% galaxite (MnAl2O4), and Zn/FeTotal atomic ratios ranging from 11.53 to 60.87...
Chemical and mineralogical characterization of elbaites from the Alto Quixaba p...
Ferreira,Ana C.M.; Ferreira,Valderez P.; Soares,Dwight R.; Vilarroel-Leo,Hugo S.The Alto Quixaba pegmatite, Seridó region, northeastern Brazil, is a 60º/80ºSW-trending subvertical dike discordantly intruded into biotite schists of the Upper Neoproterozoic Seridó Formation. It has three distinct mineralogical and textural zones, besides a replacement body that cuts the pegmatite at its central portion and in which occur, among other gem minerals, colored elbaites. Elbaites usually occur as ...
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