1000 resultados para Discours sur le châtiment corporel
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Mode of access: Internet.
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Mémoires sur la Bastille, et sur la détention de l'auteur, par Linguet.--De l'insurrection parisienne, et de la prise de la Bastille, discours historique, par Dusaulx.--Récit fidèle, non publié jusqu'à ce jour, de la prise de la Bastille, le 14 juillet, 1789, par un ancien officier au régiment des gardes-françaises.
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"Ouvrages cité dans les deux discours sur l'Histoire littéraire de la France au XIVe siècle": t.2, p. [299]-369.
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Cette thèse examine les pratiques architecturales et les dynamiques identitaires chez les Podokwo, Muktele et Mura des monts Mandara (Cameroun). Elle s’organise autour de l’hypothèse-cadre selon laquelle la logique pratique et fonctionnelle de la construction, de l’extension et de la transformation d’une maison évolue en tandem avec des considérations d’ordre symbolique, notamment la production des sentiments ethniques (Hodder, 1982) et la quête du prestige social à l’intérieur de la communauté (Duncan, 1982 ; Roux, 1976). En partant de l’approche développée par des auteurs comme Ian Hodder (2012, 2006, 1999, 1982), Daniel Miller (2010, 2007, 2005, 2001, 1987), et Christophey Tilley (2010, 2006, 2004, 2002, 1999), je montre comment la maison, à travers ses multiples usages, devient porteuse de plusieurs appartenances identitaires à un niveau sociétal et individuel (Bromberger, 1980). Pour cela, j’ai porté mon attention, non seulement sur ce que les individus font avec la maison, mais aussi sur la manière dont celle-ci construit à son tour l’identité des individus (Miller, 2001 : 119). J’ai par ailleurs centrée mon analyse autour de quelques évènements clés survenus dans l’histoire des Podokwo, des Muktele et des Mura, en particulier la descente en plaine (1963), l’exode rural et le fonctionnariat (1980) et la transition démocratique (1990). Ces évènements influent sur les pratiques architecturales et sur les discours identitaires qui en sont les corolaires.
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This note is concerned with fish remains from Upper Neogene beds at Farol das Lagostas (and nearby quarry of SECIL) and Baía Farta, mainly recovered by the author in 1960, 1961, 1963 and 1967. For further data see ANTUNES, 1964, pp. 213-215. All the forms identified until now (many of them for the first time) are show in «tableau I». Smaller ones are poorly represented. I. benedeni is provisorily accepted as a distinct species, though it may correspond to a dental morphotype that does exist equally in the extant I. oxyrhinchus (see text): therefore I. benedeni from Farol das Lagostas may after all represent only some dental variations that really belong in the form described as I. cf. oxyrhinchus. The presence of Aprionodon and Hypoprion could not be ascertained: Procarcharodon megalodon, Carcharodon carcharias, Isurus benedeni. Galeocerdo cuvieri, and Carcharhinus sp. I and sp. II are specially discussed. The whole fauna does not correspond either to a very shallow and coastal environment, or to deep waters far away from the coast. It clearly points out to warm waters: an acceptable model would be the fauna from the tropical Atlantic between Northern Angola and Senegal-Cape Verde. The age of this fauna was long regarded as Burdigalian. The data formerly presented (ANTUNES, 1963) that allowed us to ascribe a pliocene age to the uppermost Neogene beds of Farol das Lagostas (Neogene III, ANTUNES, 1964) are reviewed and developed in this paper. This view is corroborated by planctonic foraminifera and stratigraphical data which provide further evidence to prove the presence of miocene beds much younger than Burdigalian, and that some deposits previously correlated to this stage have instead a Plio-Pleistocene age. Fish fauna from Farol das Lagostas is very characteristic, with giant P. megalodon in association with C. carcharias (which predominates, and whose stratigraphical distribution is particularly discussed), and with other very advanced forms like the extant tiger shark, G. cuvieri, enormous I. Benedeni, Hemipristis, and Carcharhinus (whose size largely exceeds the maximum observed with miocene material). With the exception of P. megalodon (extinct) all the other forms show very close affinities, or even identity with modern species. Comparisons with very similar faunas from some South African localities that may also have a Pliocene age are also presented.
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This note is concerned with fish remains from upper Neogene beds at Farol das Lagostas (and nearby quarry of SECIL) and Baía Farta, mainly recovered by the author in 1960, 1961, 1963 and 1967. For further data see ANTUNES, 1964, pp. 213-215. All the forms identified until now (many of them for the first time) are show in «tableau I». Smaller ones are poorly represented. I. benedeni is provisorily accepted as a distinct species, though it may correspond to a dental morphotype that does exist equally in the extant I. oxyrhinchus (see text): therefore I. benedeni from Farol das Lagostas may after all represent only some dental variations that really belong in the form described as I. cf. oxyrhinchus. The presence of Aprionodon and Hypoprion could not be ascertained: Procarcharodon megalodon, Carcharodon carcharias, Isurus benedeni. Galeocerdo cuvieri, and Carcharhinus sp. I and sp. II are specially discussed. The whole fauna does not correspond either to a very shallow and coastal environment, or to deep waters far away from the coast. It clearly points out to warm waters: an acceptable model would be the fauna from the tropical Atlantic between Northern Angola and Senegal-Cape Verde. The age of this fauna was long regarded as Burdigalian. The data formerly presented (ANTUNES, 1963) that allowed us to ascribe a pliocene age to the uppermost Neogene beds of Farol das Lagostas (Neogene III, ANTUNES, 1964) are reviewed and developed in this paper. This view is corroborated by planctonic foraminifera and stratigraphical data which provide further evidence to proove the presence of miocene beds much younger than Burdigalian, and that some deposits previously correlated to this stage have instead a Plio-Pleistocene age. Fish fauna from Farol das Lagostas is very characteristic, with giant P. megalodon in association with C. carcharias (which predominates, and whose stratigraphical distribution is particularly discussed), and with other very advanced forms like the extant tiger shark, G. cuvieri, enormous I. Benedeni, Hemipristis, and Carcharhinus (whose size largely exceeds the maximum observed with miocene material). With the exception of P. megalodon (extinct) all the other forms show very close affinities, or even identity with modern species. Comparisons with very similar faunas from some South African localities that may also have a Pliocene age are also presented.
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The Mid Miocene marine formations of Salles area (former "Sallomacian" stage) have been studied again from numerous outcrops and cores. The deep structural framework influences notably of the characteristics and distribution of the deposits, which are neritic. The stratigraphy is stated precisely thanks to the planktonic fauna and floradetailed examination (probably Serravallian zones NN6 - N12). Several paleobiofacies are reconstituted from the rich invertebrate faunas, which give also paleoclimatic data.
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En lisant cet extrait de journal qui ouvre le livre « Le Sacrifice humain en Grèce ancienne » de Pierre Bonnechère, on peut se rendre compte que l’homme a toujours éprouvé, face au sacrifice humain, une sorte de mélange entre horreur, mystère et attraction, une « fascination étrange » 1 qui a amené les intellectuels, les écrivains et les artistes du monde entier à chercher à comprendre comment et pourquoi, hier comme aujourd’hui, le sacrifice humain continue à être une composante des pratiques rituelles des différents cultes, religieux ou pas, puisqu’il existe toujours des réminiscences de ces pratiques.
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1828 t.1
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1831 t.4
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1829 t.2
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1830 t.3
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1832 t.5
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1833 t.6
