Mapeamento geológico-geomorfológico na região de Quirinópolis-GO

Geological and geomorphological mapping is an important tool for the characterization of physical environment, thus enabling the planning and use of areas more efficiently. This work represents a geological- geomorphologic mapping on the scale of 1:20.000 in the rural area of Quirinópolis – GO town, where outcrop rocks of Paraná Sedimentary Basin, specifically the Bauru Group. Through the methodology of analysis of integrated elements of the physical environment, it was possible to delineate geological- geomorphological five units, which were characterized as lithology, topography, soil conditions, and operating processes, and the development of weathering profiles bring of great importance for planning of land use as occupation thus avoiding further degradation of the physical environment

Medições de áreas por fotografias aéreas, em escala nominal, comparadas com a área obtida em fotografias com escalas corrigidas por meio de um SIG

Land use management has becoming a very important activity. Aerial photo interpretation is a basic resource and constitutes in a technique which enables infinite refining. Agricultural development and land use require a careful initial planning in order not only to protect them against superficial changing provoked by natural phenomenon but also to gradually develop its productive capacity. For the efficiency of land management, it is necessary to access correct and detailed information which can be available through aerial images of remote sensing. The use of vertical aerial photography through Remote Sensing has become more common in boundary survey projects, management and exploration, mainly because it substitutes, with lots of advantage, for cartographic bases, besides offering detailed characteristics, eliminating access difficulties in inaccessible areas, as well as facilitating a tridimensional view once it increases map efficiency and accuracy by combining field and laboratory work with photography interpretation. This work, using panchromatic aerial photography in nominal scale 1:25000 (1962), 1:45000 (1977) , and approximate nominal scale of 1:30.000, originating from aerial survey obtained in 2005, aimed at showing through the Geographic Information System (GIS) the possibility of developing a more complete and accurate analysis of the area values, obtained directly from photos without scale correction, and after comparing it with area values obtained from aerial photography with correct scale referred in IGC (Brazilian Cartography and Geography Institute) guidelines, resulting in an error coefficient which shows area differences through two proposed study. Considering the aerial photography in three different years: 1962, 1977 and 2005 it is possible to affirm that the 2005’s images presented lower values of area difference (43, 48 square meters) than determined area values in reference chart and the 2005’s colored images has facilitated the photo interpretation of the landscape, becoming accurate the confronting traces and among land owners and consequently offering precision during land marking.

Vegetation mapping in an area of Ombrophilous Dense Forest at Parque Estadual da Serra do Mar, São Paulo State, Brazil, and floristic composition of the tree component of some physiognomies*

This study aimed to map phytophysiognomies of an area of Ombrophilous Dense Forest at Parque Estadual da Serra do Mar and characterize their floristic composition. Photointerpretation of aerial photographs in scale of 1:35,000 was realized in association with field work. Thirteen physiognomies were mapped and they were classified as Montane Ombrophilous Dense Forest, Alluvial Ombrophilous Dense Forest or Secondary System. Three physiognomies identified at Casa de Pedra streamlet's basin were studied with more details. Riparian forest (RF), valley forest (VF), and hill forest (HF) presented some floristic distinction, as confirmed by Detrended Correspondence Analysis (DCA) and Indicator Species Analysis (ISA) conducted here. Anthropic or natural disturbances and heterogeneity of environmental conditions may be the causes of physiognomic variation in the vegetation of the region. The results presented here may be useful to decisions related to management and conservation of Núcleo Santa Virgínia forests, in general.

Di Poale Tzijon oif'n tzwelfṭen tzionisṭišen kongres : (1 - 14 sepṭember 1921 in Karlsbad) ; der tzunoifšṭel fun der praktzie

Digitalisat der Ausg. Win, 1921

Na 1 Nachlass Max Horkheimer, 601 - Philosophische und ökomonische Notizen und Referate; Extracta I; Referat Transcendentale Systematik (p. VII 1, 1-14 - VII 3)

Hans Hildebrandt, "Der Kunstunterricht an Hochschulen", Typoskript, 2 Blatt; "Das Wirtschaftsprinzip", Typoskript, 3 Blatt (GS 11, S. 13-16); "Betr. Scheler - Sombart", Manuskript, 2 Blatt; "Zur Psychologie des Denkens nach Benno Erdmann", Manuskript, 2 Blatt, davon 1 leer; "Zur Phänomenologie der Erkenntnis", Typoskript, 3 Blatt; "Zu Kants Kritik der Urteilskraft", Typoskript mir eigenhändigen Korrekturen, 5 Blatt (GS 11, S. 70-75); "Naturwissenschaftliche Methode und Erkenntnistheorie. Über Kant", Typoskript mit zahlreichen eigenhändigen Notizen, 2 Blatt; "Beantwortung der Frage: Was heißt vom Standpunkt des Transcendentalen Idealismus aus die Behauptung, daß die materielle Entwicklung der Entwicklung des Bewußtseins vorhergegangen ist?", Typoskript, 3 Blatt (GS 11, S. 17-21); "Sprache und Denken", Typoskript, 8 Seiten (GS 11, S. 119-132); "Psychologie und Erkenntnistheorie", Typoskript, 2 Blatt; "Zu David Hume", Typoskript, 3 Blatt; "Wie ist das Bewußtsein einer Mehrheit von Gegenständen möglich?", Typoskript, 6 Blatt; "Gegenstand der Psychologie nach Cornelius", Typoskript, 2 Blatt; "Psychologie und Philosophie bei Hume und Cornelius", Typoskript, 12 Blatt; "Das Wiedererkennen", Typoskript von 19.12.1919, 8 Blatt; Exzerpte über: Gustav Landauer, Arthur Wolfgang Cohn, Karl Vorländer, Friedrich Engels, Karl Kautsky, L. B. Boudin, Karl Marx, Arthur Schopenhauer, 1 Heft, Manuskript, 42 Blatt; Manuskript, 1 Heft, 13 Blatt, davon 1 leer;

Evaluation of long chain 1,14-alkyl diols in marine sediments as indicators for upwelling and temperature

Long chain alkyl diols form a group of lipids occurring widely in marine environments. Recent studies have suggested several palaeoclimatological applications for proxies based on their distributions, but also revealed uncertainties about their applicability. Here we evaluate the use of long chain 1,14-alkyl diol indices for reconstruction of temperature and upwelling conditions by comparing index values, obtained from a comprehensive set of marine surface sediments, with environmental factors like sea surface temperature (SST), salinity and nutrient concentrations. Previous cultivation efforts indicated a strong effect of temperature on the degree of saturation and the chain length distribution of long chain 1,14-alkyl diols in Proboscia spp., quantified in the diol saturation index (DSI) and diol chain length index (DCI), respectively. However, values of these indices in surface sediments show no relationship with annual mean SST of the overlying water. It remains unknown what determines the DSI, although our data suggests that it may be affected by diagenesis, while the relationship between temperature and DCI may be different for different Proboscia species. In addition, contributions of algae other than Proboscia diatoms may affect both indices, although our data provide no direct evidence for additional long chain 1,14-alkyl diol sources. Two other indices using the abundance of 1,14-diols vs. 1,13-diols and C30 1,15-diols have previously been applied as indicators for upwelling intensity at different locations. The geographical distribution of their values supports the use of 1,14 diols vs. 1,13 diols [C28 + C30 1,14-diols]/[(C28 + C30 1,13-diols) + (C28 + C30 1,14-diols)] as a general indicator for high nutrient or upwelling conditions.