Considerações sobre a globalização e seus efeitos sobre o trabalho infantil

Inclui bibliografia

Bibliografía especializada sobre Traducción e Interpretación: la revista MonTI (Universidades de Alicante, Jaume I y València) (2009-2015)

Este artículo bibliográfico propone una panorámica de MonTI (Monografías de Traducción e Interpretación), una revista académica anual nacida en 2009 y publicada conjuntamente por las tres universidades públicas que ofrecen un grado en Traducción e Interpretación en la Comunidad Autónoma Valenciana.

Strasbourg, France, 1734 (Raster Image)

This layer is a georeferenced raster image of the historic paper map entitled: Strasbourg ville ancienne celebre et tres fortifieé [sic] du Roy. de France dans la Basse Alsace sur le Rhin = Strasburg eine Uhralte sehr Berühmte u. nun auch ungemein fortificirte Statt dem König in Franckr gehörig in Unter Elsas am Rhein ligend, gravée aux depens de Matth. Seutter, S.C.M. Geogr. à Augsb. = verfertigt u. verlegts M. Seutter, I.R.K. ; Ioh. Thomas Kraus., delin. It was published by M. Seutter in 1734. Scale [ca. 1:11,853]. Covers Strasbourg, France. Map in French and German. The image inside the map neatline is georeferenced to the surface of the earth and fit to the 'European Datum 1950 UTM Zone 32N' coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, drainage, built-up areas and selected buildings, fortification, ground cover, and more. Includes note, ill., and a view. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

Juzʼ fīhi aḥādīth Abī ʻAbd Allāh al-Ḥusayn ibn Yaḥyá ibn ʻAyyāsh ... al-Tūnī ʻan shuyūkhih : manuscript, [12--?]

Bound with ʻAlī ibn al-Ḥasan ibn ʻAsākir, Kitāb al-Arbaʻīn al-buldānīyah, and other hadith collections.

Developing an underlying inflation gauge for China. Bruegel Working Paper 2014/11, 9 October 2014

This paper develops a new underlying inflation gauge (UIG) for China which differentiates between trend and noise, is available daily and uses a broad set of variables that potentially influence inflation. Its construction follows the works at other major central banks, adopts the methodology of a dynamic factor model that extracts the lower frequency components as developed by Forni et al (2000) and draws on the experience of the People’s Bank of China in modelling inflation.

(Table T1) Strontium isotopic composition and ages of limestone samples from ODP Hole 180-1118A

Limestone from Unit VI (857.1-859.15 meters below seafloor) collected at Site 1118 contains a planktonic foraminiferal fauna indicating a latest Miocene to early Pliocene age. Globorotalia tumida is recorded in Sample 180-1118A-68R-4, 46-48 cm, indicating an early Pliocene (N18) age at this level (J. Resig, pers. comm., 2000). Based on their known range in the western Papuan Basin, the presence of (rare) Lepidocyclina and common Amphistegina in some samples suggests that abundant shallow-water bioclastic debris present in these limestones may be reworked from older, possibly middle or early late Miocene sediments. Four samples were selected for whole-rock strontium isotopic analysis to further investigate this possibility. A petrographic examination of samples analyzed was also conducted.

(Table 1) Bulk and clay mineralogy at DSDP Leg 66 Holes

During Leg 66 eight sites on an active margin transect off southern Mexico were drilled in order to determine the nature of ocean-continent transition across a subduction zone. Present outcrops of Mesozoic to Precambrian basement at the coast intruded by Mesozoic magmas within only 65 km of the Middle America Trench axis indicate truncation of the continental margin, tectonic removal of an accretionary zone, and consumption of ocean sediments and crust by subduction.

Solar radiation over and under sea ice during the POLARSTERN cruise ARK-XXVI/3 (TransArc) in summer 2011

Arctic sea ice has declined and become thinner and younger (more seasonal) during the last decade. One consequence of this is that the surface energy budget of the Arctic Ocean is changing. While the role of surface albedo has been studied intensively, it is still widely unknown how much light penetrates through sea ice into the upper ocean, affecting sea-ice mass balance, ecosystems, and geochemical processes. Here we present the first large-scale under-ice light measurements, operating spectral radiometers on a remotely operated vehicle (ROV) under Arctic sea ice in summer. This data set is used to produce an Arctic-wide map of light distribution under summer sea ice. Our results show that transmittance through first-year ice (FYI, 0.11) was almost three times larger than through multi-year ice (MYI, 0.04), and that this is mostly caused by the larger melt-pond coverage of FYI (42 vs. 23%). Also energy absorption was 50% larger in FYI than in MYI. Thus, a continuation of the observed sea-ice changes will increase the amount of light penetrating into the Arctic Ocean, enhancing sea-ice melt and affecting sea-ice and upper-ocean ecosystems.