Voyage dans les provinces de Rio de Janeiro et de Minas Geraes

As Voyages... são estudos completos, abrangendo todos os aspectos das regiões percorridas; servem de subsídio ao estudo das condições de vida no Brasil no século passado. "Fonte primordial de informações sobre os prédios coloniais do Rio de Janeiro, Minas Gerais, São Paulo, Santa Catarina e Goiás. Poucas obras no gênero atingem o valor de Saint-Hilarire. São clássicas e indispensáveis para o estudo do sul do Brasil, antes da Independência" segundo Borba de Moraes

Voyage au Bresil : ou l'on trouve la description du pays, de ses productions, de ses habitants, et de la ville et des provinces de san-salvatore et porto-seguro, avec une table correcte des latitudes et longitudes des ports de la cote du bresil, ainsi qu'un tableau du change, etc

Voyage au Brésil narra a experiência de observar a vida e os costumes dos habitantes do Brasil e oferece um registro cheio de interesse sociológico e até científico. Segundo Rubens Borba de Moraes, " é obra valiosíssima sobre a Bahia colonial", sendo esta edição mais preciosa que a inglesa de 1805. A obra foi traduzida também para o alemão. Afonso de Taunay resume e comenta o livro de Lindley em Aventuras de Thomas Lindley.

Sertum palmarum brasiliensium, ou, Relation des palmiers nouveaux du Brésil : découverts, décrits et dessinés d'après nature

A história Bibliográfica de Sertum palmarum brasiliensium... é a seguinte: em 1900, o Deputado Federal por São Paulo, D. Augusto César Miranda Azevedo, apresentou ao Congresso Nacional uma emenda à proposta orçamentária para 1901, autorizando o Poder Executivo "a mandar imprimir na Imprensa Nacional o texto e as estampas da monografia sobre palmeiras do botânico brasileiro Dr. João Barbosa Rodrigues..." Entretanto, a autorização não pôde ser efetivada porque a Imprensa Nacional não dispunha de equipamento para a reprodução de estampas. Em 1901, o Senador pelo Estado do Pará, Dr. Lauro Sodré, apresentou emenda à proposta orçamentária para 1902, cuja lei estabeleceu no art. 6º : "é o Governo autorizado a mandar imprimir na Europa ou em país onde houver mais vantagem, a obra Sertum palmarum..., abrindo para tal fim o necessário crédito, e de acordo com o autor". O crédito -- duzentos contos de réis -- foi finalmente, aberto o Decreto nº 4.428, de 12 de junho de 1902, assinado por Campos Sales e referendado por Sabino Barroso, Ministro da Justiça. A obra foi impressa em Bruxelas sob a direção do próprio Barbosa Rodrigues, que, para esse fim ali se demorou nove meses. Trata-se de trabalho gráfico de primeira ordem, tanto pela reprodução colorida das estampas, como pelo texto e encadernação.

Les Portugais d'Amérique : souvenirs historiques de la guerre du Brésil en 1635 : contenant un tableau intéressant des moeurs et usages des tribus sauvages, des détails instructifs sur la situation des colons dans cette partie du nouveau-monde : ouvrage destiné a la jeunesse

Illustré de 12 dessins impremés en 2 couleurs

Les jeunes face au marché du travail en France: entre difficultés d´insertion et stratégies de pénétration

En une génération, entre 1975 et 1995, le paysage du marché du travail auquel les jeunes font face a radicalement changé.

Traité général des pesches : et histoire des poissons qu'elles fournissent tant pour la subsistance des hommes que pour plusieurs autres usages qui ont rapport aux arts et au commerce. [3 volumes bound in 2 parts in folio]

Early illustrated book about fish, fishing and fisheries by one of the preeminent scientific investigators of the French enlightenment. This work deals extensively with the species of fish found in Europe and beyond, their habits and habitats, techniques and equipment used in fishing and fish processing, and many other aspects of these endeavours. Roughly 185 engraved plates illustrate the text. The scans for this version come from 3 volumes bound in two parts in folio.

Voyage au Brésil / M. et Mme. Agassiz ; abrégé sur la traduction de F. Vogeli par J. Belin-de Launay et contenant une Carte e 16 gravures sur bois

Jean Louis Rodolphe Agassiz foi professor e naturalista suíço naturalizado americano. Nasceu em Motiers, em 28 de maio de 1807, e morreu em Cambridge, em 1873. Estudou em Universidades suíças e alemãs, doutorando-se em Medicina, em Munique, em 1830. Em 1846, fixou-se nos Estados Unidos, onde lecionou em Harvard, e, em 1861, tornou-se cidadão americano. O estudo e a classificação de espécies de peixes brasileiros despertou-lhe o interesse pelo Brasil e , em 1865, chegou ao País à frente de uma expedição científica, que ficou conhecida como Thayer Expedition, custeada pelo milionário americano Nathanael Thayer e patrocinada pelo Imperador D. Pedro II. Permaneceu no País por quinze meses, explorando o Rio Amazonas e o interior cearense, período em que classificou 1.800 espécies da fauna ictiológica. Dessa viagem, resultou o livro A journey in Brasil. Seus estudos de Zoologia e Paleontologia, assim como os dos glaciares da Europa e da América, tornaram-se célebre. A obra científica de Agassiz é constituída por mais de quatrocentos volumes.

Memoires de monsieur du Guay-Trouin, lieutenant general des armees navales de France, et commandeur de l'ordre royal & militaire de Saint Louis

Notas tipográficas retiradas de Brunet, v. 2, col. 1780.

Second mémoire présenté par les Etats Unis du Brésil au gouvernement de la Confédération Suisse, arbitre choisi selon les stipulations du Traité conclu a Rio de Janeiro, le 10 Avril 1897, entre le Brésil et la France : frontières entre le Brésil et la Guyane Française

Nota de conteúdo : V.1. Memoire en reponse aux allegations de la France, accompagne de quelques cartes -- V. 2-3. Documents accompagnes de notes explicatives ou rectificatives, 1. ptie, 1536-1713 ; 2. ptie, 1713-1896 -- V. 4. Texte original de documents traduits dans les tomes 2 et 3 -- V. 5. Album : fac-simile de quelques documents reproduits aux tomes 2, 3 et 4 -- V. 6. Atlas : contenant 86 cartes.

Kommentar zum Worm-et-al.-Artikel„Impacts of Biodiversity Loss on Ocean Ecosystem Services“: erschienen im Wissenschaftsmagazin Science, Vol. 314, am 3. November 2006

Folgende Kernbehauptungen bzw. Hypothesen werden in dem Worm-et-al.-Artikel aufgestellt: -Der Verlust an Biodiversität (Artenzahl) in einem Meeresgebiet reduziert tief greifend seine Produktivität und seine Stabilität in Stressperioden, hervorgerufen u.a. durch Überfischung und Klimaänderung. -Die Zahl der kollabierten Arten nimmt zu. Dieser Trend projeziert den Kollaps aller wildlebenden Arten und Bestände, die gegenwärtig befischt werden, auf das Jahr 2048. -Diese Entwicklung ist zum gegenwärtigen Zeitpunkt reversibel, denn das Meer besitzt noch ein großes Potential sich zu regenerieren. Dazu ist aber mehr Umweltschutz notwendig.

Voyage au Brésil, dans les années 1815, 1816 et 1817

Ouvrage enrichi d'un superbe atlas, compose de 41 planches gravées en taille-douce, et de trois carte.

Histogénèse et structure de la glande hermaphrodite d'Helix pomatia (Linn.)

(PDF contains 267 pages)

Nourriture et santé dans la médecine grecque ancienne

Presentado en el IIe Colloque International de l'IEHA: « Un aliment sain dans un corps sain ». Perspectives historiques - «Healthy Food in a Healthy Body», organizado por el Institut Européen d'Histoire de l'Alimentation y celebrado en Tours los días 14 y 15 de diciembre de 2002.

Seismic structure above and below the core-mantle boundary

Seismic structure above and below the core-mantle boundary (CMB) has been studied through use of travel time and waveform analyses of several different seismic wave groups. Anomalous systematic trends in observables document mantle heterogeneity on both large and small scales. Analog and digital data has been utilized, and in many cases the analog data has been optically scanned and digitized prior to analysis.

Differential travel times of S - SKS are shown to be an excellent diagnostic of anomalous lower mantle shear velocity (V s) structure. Wavepath geometries beneath the central Pacific exhibit large S- SKS travel time residuals (up to 10 sec), and are consistent with a large scale 0(1000 km) slower than average V_s region (≥3%). S - SKS times for paths traversing this region exhibit smaller scale patterns and trends 0(100 km) indicating V_s perturbations on many scale lengths. These times are compared to predictions of three tomographically derived aspherical models: MDLSH of Tanimoto [1990], model SH12_WM13 of Suet al. [1992], and model SH.10c.17 of Masters et al. [1992]. Qualitative agreement between the tomographic model predictions and observations is encouraging, varying from fair to good. However, inconsistencies are present and suggest anomalies in the lower mantle of scale length smaller than the present 2000+ km scale resolution of tomographic models. 2-D wave propagation experiments show the importance of inhomogeneous raypaths when considering lateral heterogeneities in the lowermost mantle.

A dataset of waveforms and differential travel times of S, ScS, and the arrival from the D" layer, Scd, provides evidence for a laterally varying V_s velocity discontinuity at the base of the mantle. Two different localized D" regions beneath the central Pacific have been investigated. Predictions from a model having a V_s discontinuity 180 km above the CMB agree well with observations for an eastern mid-Pacific CMB region. This thickness differs from V_s discontinuity thicknesses found in other regions, such as a localized region beneath the western Pacific, which average near 280 km. The "sharpness" of the V_s jump at the top of D", i.e., the depth range over which the V_s increase occurs, is not resolved by our data, and our data can in fact may be modeled equally well by a lower mantle with the increase in V_s at the top of D" occurring over a 100 krn depth range. It is difficult at present to correlate D" thicknesses from this study to overall lower mantle heterogeneity, due to uncertainties in the 3-D models, as well as poor coverage in maps of D" discontinuity thicknesses.

P-wave velocity structure (V_p) at the base of the mantle is explored using the seismic phases SKS and SPdKS. SPdKS is formed when SKS waves at distances around 107° are incident upon the CMB with a slowness that allows for coupling with diffracted P-waves at the base of the mantle. The P-wave diffraction occurs at both the SKS entrance and exit locations of the outer core. SP_dKS arrives slightly later in time than SKS, having a wave path through the mantle and core very close to SKS. The difference time between SKS and SP_dKS strongly depends on V_p at the base of the mantle near SK Score entrance and exit points. Observations from deep focus Fiji-Tonga events recorded by North American stations, and South American events recorded by European and Eurasian stations exhibit anomalously large SP_dKS - SKS difference times. SKS and the later arriving SP_dKS phase are separated by several seconds more than predictions made by 1-D reference models, such as the global average PREM [Dziewonski and Anderson, 1981] model. Models having a pronounced low-velocity zone (5%) in V_p in the bottom 50-100 km of the mantle predict the size of the observed SP_dK S-SKS anomalies. Raypath perturbations from lower mantle V_s structure may also be contributing to the observed anomalies.

Outer core structure is investigated using the family of SmKS (m=2,3,4) seismic waves. SmKS are waves that travel as S-waves in the mantle, P-waves in the core, and reflect (m-1) times on the underside of the CMB, and are well-suited for constraining outermost core V_p structure. This is due to closeness of the mantle paths and also the shallow depth range these waves travel in the outermost core. S3KS - S2KS and S4KS - S3KS differential travel times were measured using the cross-correlation method and compared to those from reflectivity synthetics created from core models of past studies. High quality recordings from a deep focus Java Sea event which sample the outer core beneath the northern Pacific, the Arctic, and northwestern North America (spanning 1/8th of the core's surface area), have SmKS wavepaths that traverse regions where lower mantle heterogeneity is pre- dieted small, and are well-modeled by the PREM core model, with possibly a small V_p decrease (1.5%) in the outermost 50 km of the core. Such a reduction implies chemical stratification in this 50 km zone, though this model feature is not uniquely resolved. Data having wave paths through areas of known D" heterogeneity (±2% and greater), such as the source-side of SmKS lower mantle paths from Fiji-Tonga to Eurasia and Africa, exhibit systematic SmKS differential time anomalies of up to several seconds. 2-D wave propagation experiments demonstrate how large scale lower mantle velocity perturbations can explain long wavelength behavior of such anomalous SmKS times. When improperly accounted for, lower mantle heterogeneity maps directly into core structure. Raypaths departing from homogeneity play an important role in producing SmKS anomalies. The existence of outermost core heterogeneity is difficult to resolve at present due to uncertainties in global lower mantle structure. Resolving a one-dimensional chemically stratified outermost core also remains difficult due to the same uncertainties. Restricting study to higher multiples of SmKS (m=2,3,4) can help reduce the affect of mantle heterogeneity due to the closeness of the mantle legs of the wavepaths. SmKS waves are ideal in providing additional information on the details of lower mantle heterogeneity.