Ana Isabel Rodrigues - Academia.edu (original) (raw)
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Papers by Ana Isabel Rodrigues
Tetrahedron: Asymmetry, 2008
Tetrahedron: Asymmetry, 2008
Phytotherapy Research, 2008
Marine Drugs, 2004
... (00351)-21-7165141, Fax (00351) 21-7168100, E-mail: helena.gaspar@ineti.pt ... of fungal infe... more ... (00351)-21-7165141, Fax (00351) 21-7168100, E-mail: helena.gaspar@ineti.pt ... of fungal infections found in most countries, affecting skin, hair and nails [10]. While (+)-curcuphenol inhibited the growth of the fungi A. ramosa, A. niger, B. cinerea, C. ...
Journal of Separation Science, 2008
Journal of Molecular Catalysis A: Chemical, 2006
Journal of Ethnopharmacology, 2004
Applied Spectroscopy, 2002
Summary In recent years chemical analysis has been established as a significant contributor to sc... more Summary
In recent years chemical analysis has been established as a significant contributor to science-based archaeology. The present work is a first
approach to the study of chemical and mineralogical composition of pigments used in archaeological rupestrian arts of Vão Grande site,
included in Lajeado Complex in Tocatins State, Brazil. Representative pigments micro-samples were removed from rock paintings and substrate
rock. The characterization of the pigments was carried out by micro X-ray diffraction (μ-XRD) and Fourier transform infrared microspectroscopy
(μ-FTIR).
Riassunto
Questo lavoro è un primo approccio allo studio della composizione chimica e mineralogica dei pigmenti utilizzati nel sito archeologico di arte
rupestre di Vão Grande, facente parte del complesso di Lajeado nello Stato di Tocatins, Brasile. Micro-campioni dei pigmenti sono stati rilevanti
dalle pitture rupestri e dal substrato di roccia. La caratterizzazione dei pigmenti è stata condotta con microdiffrazione dei raggi-X (μ-XRD) e
microspettroscopia a infrarossi a trasformata di Fourier (μ-FTIR).
A petrographic and isotopic study of a stalagmite from Los Postes cave, located at the Natural Mo... more A petrographic and isotopic study of a stalagmite from Los Postes cave, located at the Natural Monument “Cuevas de Fuentes de León”, Spain, was carried out in order to assess Holocene climate changes in the landscape of this region. The stalagmite consists of calcite, but also contains small clasts of quartz, plagioclase, zircon, "terra rossa", limestone, iron oxides and hydroxides and clay minerals. In the stalagmite, calcite columnar textures tend to yield the lowest δ18O and δ13C values, and their growth should reflect relatively slow but constant drip rates. On the other hand, layers with columnar microcrystalline and radial-acicular textures show the highest δ18O and δ13C values and are related to a decrease in the drip rate. Layers formed by aggregates of detrital materials, cemented with micrite, are associated to low drip rates or even dryness periods. However, the detrital components should have entered in the system due to torrentional transport processes. The δ18O and δ13C values co-vary, ranging from -5.17 ‰ to -2.57 ‰ and from -9.34 ‰ and -4.95 ‰, respectively. The petrographic and isotopic data point to a outset of a more dry and warm period at ca. 2.6 ka BP, with δ18O and δ13C values higher than -3.75 ‰ and -6.80 ‰, respectively, which could led to a predominance of C4 plants over C3.
Tetrahedron: Asymmetry, 2008
Tetrahedron: Asymmetry, 2008
Phytotherapy Research, 2008
Marine Drugs, 2004
... (00351)-21-7165141, Fax (00351) 21-7168100, E-mail: helena.gaspar@ineti.pt ... of fungal infe... more ... (00351)-21-7165141, Fax (00351) 21-7168100, E-mail: helena.gaspar@ineti.pt ... of fungal infections found in most countries, affecting skin, hair and nails [10]. While (+)-curcuphenol inhibited the growth of the fungi A. ramosa, A. niger, B. cinerea, C. ...
Journal of Separation Science, 2008
Journal of Molecular Catalysis A: Chemical, 2006
Journal of Ethnopharmacology, 2004
Applied Spectroscopy, 2002
Summary In recent years chemical analysis has been established as a significant contributor to sc... more Summary
In recent years chemical analysis has been established as a significant contributor to science-based archaeology. The present work is a first
approach to the study of chemical and mineralogical composition of pigments used in archaeological rupestrian arts of Vão Grande site,
included in Lajeado Complex in Tocatins State, Brazil. Representative pigments micro-samples were removed from rock paintings and substrate
rock. The characterization of the pigments was carried out by micro X-ray diffraction (μ-XRD) and Fourier transform infrared microspectroscopy
(μ-FTIR).
Riassunto
Questo lavoro è un primo approccio allo studio della composizione chimica e mineralogica dei pigmenti utilizzati nel sito archeologico di arte
rupestre di Vão Grande, facente parte del complesso di Lajeado nello Stato di Tocatins, Brasile. Micro-campioni dei pigmenti sono stati rilevanti
dalle pitture rupestri e dal substrato di roccia. La caratterizzazione dei pigmenti è stata condotta con microdiffrazione dei raggi-X (μ-XRD) e
microspettroscopia a infrarossi a trasformata di Fourier (μ-FTIR).
A petrographic and isotopic study of a stalagmite from Los Postes cave, located at the Natural Mo... more A petrographic and isotopic study of a stalagmite from Los Postes cave, located at the Natural Monument “Cuevas de Fuentes de León”, Spain, was carried out in order to assess Holocene climate changes in the landscape of this region. The stalagmite consists of calcite, but also contains small clasts of quartz, plagioclase, zircon, "terra rossa", limestone, iron oxides and hydroxides and clay minerals. In the stalagmite, calcite columnar textures tend to yield the lowest δ18O and δ13C values, and their growth should reflect relatively slow but constant drip rates. On the other hand, layers with columnar microcrystalline and radial-acicular textures show the highest δ18O and δ13C values and are related to a decrease in the drip rate. Layers formed by aggregates of detrital materials, cemented with micrite, are associated to low drip rates or even dryness periods. However, the detrital components should have entered in the system due to torrentional transport processes. The δ18O and δ13C values co-vary, ranging from -5.17 ‰ to -2.57 ‰ and from -9.34 ‰ and -4.95 ‰, respectively. The petrographic and isotopic data point to a outset of a more dry and warm period at ca. 2.6 ka BP, with δ18O and δ13C values higher than -3.75 ‰ and -6.80 ‰, respectively, which could led to a predominance of C4 plants over C3.