Disputatio philosophica in que refutatur axioma illud Aristotelicum, quo asseritur nihil esse in intellectu, quod non prius fuerit in sensu.

Diss.--Hanover, Martinus Iber, respondent.

Philologiae sacrae : qua totius sacro sanctae Veteris & Novi Testamenti scripturae, tum stylus & literatura, tum sensus & genuinae interpretationis ratio expenditur, libri quinque, quorum I. & II. Generalia de Sacrae Scripturae stylo & sensu, III. & IV. Grammatica sacra, V. Rhetorica sacra comprehenduntur /

Errata on last p.

Vota decisiva a Francisco Maria Constantino nobili Asculano, celebratissimo juris utriusque consulto, ac Romanae Curiae advocato elucubrata in causis, in quibus ... vel definitivè pronunciavit, aùt in sensu veritatis respondit, nunc vero primum a J.U.D. Cosmo Mathia Constantino authoris pridem defuncti pronepote in lucem edita ... tomus II.

Mode of access: Internet.

Vota decisiva a Francisco Maria Constantino nobili Asculano, celebratissimo juris utriusque consulto, ac Romanae Curiae advocato elucubrata in causis, in quibus ... vel definitivè pronunciavit, aùt in sensu veritatis respondit, nunc vero primum a J.U.D. Cosmo Mathia Constantino authoris pridem defuncti pronepote in lucem edita ... tomus I.

Mode of access: Internet.

Speciation of Antechinus stuartii and A. subtropicus (Marsupialia : Dasyuridae) in eastern Australia: molecular and morphological evidence

This paper evaluates the systematic status of the Antechinus populations of northern New South Wales and southern Queensland, using a combined morphological and molecular (allozymes and mitochondrial DNA) approach. Analysis of the d-loop section of the mitochondrial DNA control region revealed two highly supported clades within A. stuartii sensu lato that were sympatric in the Border Ranges of northern New South Wales. However, genetic distances between these clades were small ( approximately 3%), indicating that time of divergence was probably relatively recent. Allozyme electrophoresis also showed very small differences between clades/ species. Analyses of cranial and dental characters showed that the members of each of these clades differed morphologically and that the clades corresponded to A. stuartii and the recently described A. subtropicus. The combined results support the species status of A. stuartii and A. subtropicus, and suggest that speciation was likely a result of a recent vicariant event.

Comparison of Ba/Ca and d18OWATER as freshwater proxies: a multi-species core-top study on planktonic foraminifera from the vicinity of the Orinoco River mouth

Past river run-off is an important measure for the continental hydrological cycle and the as-sessment of freshwater input into the ocean. However, paleosalinity reconstructions applying different proxies in parallel often show offsets between the respective methods. Here, we compare the established foraminiferal Ba/Ca and d18OWATER salinity proxies for their capability to record the highly seasonal Orinoco freshwater plume in the eastern Caribbean. For this purpose we obtained a data set comprising Ba/Ca and d18OWATER determined on multiple spe-cies of planktonic foraminifera from core tops distributed around the Orinoco river mouth. Our findings indicate that interpretations based on either proxy could lead to different conclu-sions. In particular, Ba/Ca and d18OWATER diverge in their spatial distribution due to different governing factors. Apparently, the Orinoco freshwater plume is best tracked by Ba/Ca ratios of G. ruber (pink and sensu lato morphotypes), while d18OWATER based on the same species is more related to the local precipitation-evaporation balance overprinting the riverine freshwater contribution. Other shallow dwelling species (G. sacculifer, O. universa) show a muted response to the freshwater discharge, most likely due to their ecological and habitat prefer-ences. Extremely high Ba/Ca ratios recorded by G. ruber are attributed to Ba2+-desorption from suspended matter derived from the Orinoco. Samples taken most proximal to the freshwater source do not show pronounced Ba/Ca or d18OWATER anomalies. Here, the suspension loaded freshwater lid developing during maximum discharge suppresses foraminiferal populations. Both proxies are therefore biased towards dry season conditions at these sites, when surface salinity is only minimally reduced.

(Table 1) Planktonic foraminifera counts and stable oxygen isotope ratios of Pacific Ocean surface sediments

Core-top samples from the eastern tropical Pacific (10°N to 20°S) were used to test whether the ratio between Globorotalia menardii cultrata and Neogloboquadrina dutertrei abundance (Rc/d) and the oxygen isotope composition (?18O) of planktonic foraminifera can be used as proxies for the latitudinal position of the Equatorial Front. Specifically, this study compares the ?18O values of eight species of planktonic foraminifera (Globigerinoides ruber sensu stricto (ss) and sensu lato (sl), Globigerinoides sacculifer, Globigerinoides triloba, Pulleniatina obliquiloculata, Neogloboquadrina dutertrei, Globorotalia menardii menardii, Globorotalia menardii cultrata and Globorotalia tumida) with the seasonal hydrography of the region, and evaluates the application of each species or combination of species for paleoceanographic reconstructions. The results are consistent with sea surface temperature and water column stratification patterns. We found that in samples north of 1°N, the Rc/d values tend to be higher and d18O values of G. ruber, G. sacculifer, G. triloba, P. obliquiloculata, N. dutertrei, and G. menardii cultrata tend to be lower than those from samples located south of 1°N. We suggest that the combined use of Rc/d and the d18O difference between G. ruber and G. tumida or between P. obliquiloculata and G. tumida are the most suitable tools for reconstructing changes in the latitudinal position of the Equatorial Front and changes in the thermal stratification of the upper water column in the eastern tropical Pacific.

Planktic foraminifera isotopes, temperature and d18O of seawater at the central Walvis Ridge for Termination II (MIS 6 to 5), sediment core 64PE-174P13

Salty and warm Indian Ocean waters enter the South Atlantic via the Agulhas leakage, south of Africa. Model simulations and proxy evidence of Agulhas leakage strengthening during glacial terminations led to the hypothesis that it was an important modulator of the Atlantic Ocean circulation. Yet, the fate of the leakage salinity and temperature anomalies remains undocumented beyond the southern tip of Africa. Downstream of the leakage, new paleoceanographic evidence from the central Walvis Ridge (southeast Atlantic) shows that salinity increased at the thermocline, and less so at the surface, during glacial termination II. Thermocline salinity change coincided with higher frequency of Agulhas rings passage at the core location and with salinity maxima in the Agulhas leakage area, suggesting that leakage waters were incorporated in the Atlantic circulation through the thermocline. Hydrographic changes at the Walvis Ridge and in the leakage area display a distinct two-step structure, with a reversal at ca. 134 ka. This matched a wet interlude within the East Asia weak monsoon interval of termination II, and a short-lived North Atlantic warming. Such concurrence points to a Bølling-Allerød-like recovery of the Atlantic circulation amidst termination II, with a northward shift of the Intertropical Convergence Zone and Southern Hemisphere westerlies, and attendant curtailment of the interocean connection south of Africa.

Planktonic foraminiferal flux and shell geochemistry data in the sediment trap time series JAM 1-3 off south Java

Results from sediment trap experiments conducted in the seasonal upwelling area off south Java from November 2000 until July 2003 revealed significant monsoon-, El Niño-Southern Oscillation-, and Indian Ocean Dipole-induced seasonal and interannual variations in flux and shell geochemistry of planktonic foraminifera. Surface net primary production rates together with total and species-specific planktonic foraminiferal flux rates were highest during the SE monsoon-induced coastal upwelling period from July to October, with three species Globigerina bulloides, Neogloboquadrina pachyderma dex., and Globigerinita glutinata contributing to 40% of the total foraminiferal flux. Shell stable oxygen isotopes (d18O) and Mg/Ca data of Globigerinoides ruber sensu stricto (s.s.), G. ruber sensu lato (s.l.), Neogloboquadrina dutertrei, Pulleniatina obliquiloculata, and Globorotalia menardii in the sediment trap time series recorded surface and subsurface conditions. We infer habitats of 0-30 m for G. ruber at the mixed layer depth, 60-80 m (60-90 m) for P. obliquiloculata (N. dutertrei) at the upper thermocline depth, and 90-110 m (100-150 m) for G. menardii in the 355-500 mm (>500 µm) size fraction corresponding to the (lower) thermocline depth in the study area. Shell Mg/Ca ratio of G. ruber (s.l. and s.s.) reveals an exponential relationship with temperature that agrees with published relationships particularly with the Anand et al. (2003) equations. Flux-weighted foraminiferal data in sediment trap are consistent with average values in surface sediment samples off SW Indonesia. This consistency confirms the excellent potential of these proxies for reconstructing past environmental conditions in this part of the ocean realm.

Anatomy and variability of "Cuvierichelys parisiensis", a geoemydid turtle that crosses the Eocene-Oligocene boundary in Belgium

Abundant material of turtles from the early Oligocene site of Boutersem-TGV (Boutersem, Belgium), is presented here. No information on the turtles found there was so far available. All the turtle specimens presented here are attributable to a single freshwater taxon that is identified as a member of Geoemydidae, Cuvierichelys. It is the first representative of the ‘Palaeochelys s. l.–Mauremys’ group recognized in the Belgian Paleogene record. This material, which allows to know all the elements of both the carapace and the plastron of the taxon, cannot be attributed to the only species of the genus Cuvierichelys so far identified in the Oligocene, the Spanish form Cuvierichelys iberica. The taxon from Boutersem is recognized as Cuvierichelys parisiensis. Thus, both the paleobiogeographic and the biostratigraphic distributions of Cuvierichelys parisiensis are extended, its presence being confirmed for the first time outside the French Eocene record. The validity of some European forms is refuted, and several characters previously proposed as different between Cuvierichelys iberica and Cuvierichelys parisiensis are recognized as subjected to intraspecific variability.

A estrutura de poder tradicional no stricto sensu: o caso do mestrado profissional em Administração Pública em Rede Nacional - PROFIAP

This study approaches bureaucratic organizational structures with the aim to understand the adherence procedure to virtual technologies in the stricto sensu educational administrative process. Thus, the author navigates through the formation of these organizations in Brazil with the intent to demonstrate the bureaucratic organizational culture and the consequent form of domination of those who detain power. In this epistemological construction, the author explores the culture s bureaucratic environment and the organizational power. In the analyses, it was observed the technological phenomenon in the ODL s administrative environment, which can explain the adherence procedure to structures and technological instruments for stricto sensu courses that, hypothetically, dilutes the traditional inherited organizational axiom. Therefore, it was utilized as object of study the Professional Master s degree in National Scale Public Administration PROFIAP, hence analyzing the documental content and the legislation related to institutionalization as well as the positioning of professors/coordinators and of the director of CAPES/MEC. Considering this axioms, it was concluded that the bureaucratic structures can admit ODL in the stricto sensu s environment. However, this can only be done as long as the adherence does not imply in a dilution of the traditional forms of power and institutional bureaucratic inherited dominance, as well as the alleged hegemony of the governmental structure in the educational administration adopted in person by the stricto sensu courses in Brazil

CONTORNOS DA CIÊNCIA DA INFORMAÇÃO NO BRASIL: um estudo dos programas de pós-graduação stricto sensu

Aborda a Ciência da Informação através das articulações entre os seus sistemas de pós-graduação. Mostra a evolução da representação dos programas de pós-graduação em Ciência da Informação no Brasil através do portal da CAPES. Examina como essa área vem reagindo no Brasil aos desafios do crescimento e estabilidade. Pretende então, entender como os programas de Pós-graduação estão respondendo ás demandas de diversas naturezas que a sociedade lhe coloca, no que diz respeito á formação de docentes e pesquisadores. Focaliza também as linhas de pesquisa dos cursos de Ciência da Informação. Com essa perspectiva, a pesquisa foi estruturada nas seguintes partes: introdução, referencial teórico e procedimentos metodológicos.

A INTERNACIONALIZAÇÃO DOS PROGRAMAS DE PÓS-GRADUAÇÃO STRICTO SENSU DA ÁREA INTERDISCIPLINAR

A  temática da internacionalização já é muito difundida no âmbito das organizações, em que de forma pragmática está interligada ao processo capitalista e da competitividade. Entretanto é possível também empregá-la em outras áreas, como a de ensino e conhecimento. Dentro do contexto da competitividade, as universidades precisam ampliar seu campo de atuação, e a internacionalização pode ser uma importante estratégia ou ferramenta de auxílio nessa caminhada, visto que existe uma preocupação de que as instituições de ensino invistam na internacionalização,  já que ela pode trazer inúmeros benefícios, dentre eles o aumento do número de publicações. Nesse momento se destaca a necessidade de aprofundar os estudos sobre a internacionalização para que as instituições de ensino possam melhorar seu desempenho. Esta pesquisa enfoca os programas de pós-graduação stricto sensu da área interdisciplinar com a busca por apresentar o grau de internacionalização dos programas selecionados e avaliar se os programas mais internacionalizados refletem uma melhor nota da CAPES.

Studio geologico-geomorfologico per la soluzione di problematiche tecnico-applicative nelle località Terra Murata (borgo medievale e costone lato Marina Corricella) e Centane-Panoramica (Isola di Procida, Golfo di Napoli)

Nel presente rapporto tecnico viene illustrato uno studio del dissesto geomorfologico in due aree selezionate dell’Isola di Procida, rispettivamente ubicate nella zona storica di Procida (borgo medievale di Terra Murata lungo la Via Salita Castello-altezza Via S. Domenico) e nell’area costiera che raccorda Punta Pizzaco con Punta Solchiaro (comprensorio Centane-Panoramica). In generale le finalità del rapporto tecnico sono quelle di fornire un inquadramento di queste due zone da un punto di vista geologico, che si differenziano negli aspetti particolari. Infatti, nella zona di Terra Murata, sia nella zona alta del borgo medievale (piazzale oltre le mura) che lungo il costone tufaceo antistante la Marina Corricella (salita Castello all’altezza di Via S. Domenico) sono documentate copiose perdite d’acqua attraverso i terreni vulcanici di natura tufacea e pozzolanica che affiorano nell’area. Tali perdite d’acqua attraverso i terreni interessano anche numerose abitazioni, creando disagi che rendono necessario l’ulteriore accertamento tecnico al fine di individuare, anche tentativamente, le cause di tali dissesti e di proporre soluzioni tecnicamente soddisfacenti a tali problematiche attraverso uno studio approfondito.