Beiträge zu v. Savigny's Geschichte des Römischen Rechts im Mittelalter : aus den Handschriften der Königlichen Bibliothek zu Königsberg /

Includes bibliographical footnotes.

Inventarnyĭ katalog kleĭm na amfornykh ruchkakh i gorlyshkakh i na cherepit︠s︡akh ėrmitazhnagʹo sobranīi︠a︡. S Z risunkami v teksti︠e︡, 15 fototipicheskimi i l avtotipicheskoi︠u︡ tablit︠s︡ami.

Romanized record.

Roman Catholicism, diplomacy, and the European communities, 1958-1964

This article investigates the Roman Catholic Church's role in the process of European integration from the first Hallstein Commission in 1958 to the failure of the Holy See's application to establish a diplomatic representation at the European Economic Community in 1964. The article focuses on the Church's response toward emerging European institutions and shows that local mobilization in Luxembourg, Strasbourg, and Brussels was instrumental in shaping relations between the Catholic Church and the European Communities (EC). The Church's position toward the EC, placing local communities as prime actors in dialogue with European institutions, reflected the sensitive nature of religion during the Cold War.

Data compilation on the biological response to ocean acidification: environmental and experimental context of data sets and related literature

The exponential growth of studies on the biological response to ocean acidification over the last few decades has generated a large amount of data. To facilitate data comparison, a data compilation hosted at the data publisher PANGAEA was initiated in 2008 and is updated on a regular basis (doi:10.1594/PANGAEA.149999). By January 2015, a total of 581 data sets (over 4 000 000 data points) from 539 papers had been archived. Here we present the developments of this data compilation five years since its first description by Nisumaa et al. (2010). Most of study sites from which data archived are still in the Northern Hemisphere and the number of archived data from studies from the Southern Hemisphere and polar oceans are still relatively low. Data from 60 studies that investigated the response of a mix of organisms or natural communities were all added after 2010, indicating a welcomed shift from the study of individual organisms to communities and ecosystems. The initial imbalance of considerably more data archived on calcification and primary production than on other processes has improved. There is also a clear tendency towards more data archived from multifactorial studies after 2010. For easier and more effective access to ocean acidification data, the ocean acidification community is strongly encouraged to contribute to the data archiving effort, and help develop standard vocabularies describing the variables and define best practices for archiving ocean acidification data.

Expanded GHOST database

In this study we review a global set of alkenone- and foraminiferal Mg/Ca-derived sea surface temperatures (SST) records from the Holocene and compare them with a suite of published Eemian SST records based on the same approach. For the Holocene, the alkenone SST records belong to the actualized GHOST database (Kim, J.-H., Schneider R.R., 2004). The actualized GHOST database not only confirms the SST changes previously described but also documents the Holocene temperature evolution in new oceanic regions such as the Northwestern Atlantic, the eastern equatorial Pacific, and the Southern Ocean. A comparison of Holocene SST records stemming from the two commonly applied paleothermometry methods reveals contrasting - sometimes divergent - SST evolution, particularly at low latitudes where SST records are abundant enough to infer systematic discrepancies at a regional scale. Opposite SST trends at particular locations could be explained by out-of-phase trends in seasonal insolation during the Holocene. This hypothesis assumes that a strong contrast in the ecological responses of coccolithophores and planktonic foraminifera to winter and summer oceanographic conditions is the ultimate reason for seasonal differences in the origin of the temperature signal provided by these organisms. As a simple test for this hypothesis, Eemian SST records are considered because the Holocene and Eemian time periods experienced comparable changes in orbital configurations, but had a higher magnitude in insolation variance during the Eemian. For several regions, SST changes during both interglacials were of a similar sign, but with higher magnitudes during the Eemian as compared to the Holocene. This observation suggests that the ecological mechanism shaping SST trends during the Holocene was comparable during the penultimate interglacial period. Although this "ecology hypothesis" fails to explain all of the available results, we argue that any other mechanism would fail to satisfactorily explain the observed SST discrepancies among proxies.

La synthèse philosophico-juridique de V.S. Soloviev : élaboration et mise en œuvre d’un cadre théorique

Vladimir S. Soloviev (1853-1900) était un philosophe russe, poète et dissident de la période prérévolutionnaire. Comme celle de beaucoup de ses contemporains prérévolutionnaires russes, la pensée de Soloviev fut constamment sollicitée par la réfection imminente de l’État russe dans un futur très proche. Dans le contexte de cette époque, un examen des fondements théoriques du système juridique était peut-être inévitable. Néanmoins, dans la pensée russe, c’est seulement avec Soloviev que le droit cessa d’être un sujet spécialisé dans le domaine de l’administration, ne concernant guère les grands enjeux de société, et devint intimement lié au développement même de la philosophie morale et sociale. Au sein du projet philosophique systématique que propose Soloviev, le concept de l’unitotalité est envahissant, en termes épistémologique et social. Une pierre d’assise également fondamentale est le concept philosophico-religieux de la divino-humanité, à travers lequel la source de la dignité humaine est ultimement exprimée. La philosophie juridique de Soloviev, contenue pour l’essentiel dans un traité intitulé La Justification du bien : essai de philosophie morale (1897), a pour principal objet l’interaction entre le droit et la morale. Alors que l’objet et la portée du droit peuvent être directement déduits de principes moraux, le droit ne peut pas coïncider exactement avec la morale, compte tenu de son caractère plus limité, fini et coercitif. Pour Soloviev, le droit doit imposer un niveau minimum du bien en fournissant les conditions de base (par ex. la primauté du droit, le droit à une existence digne, la liberté de conscience) pour le libre développement des facultés humaines sans transposer directement en lui la plénitude complète du bien. La principale motivation de Soloviev réside dans la prémisse théologique sous-jacente que le bien ne peut jamais être complètement subsumé sauf par un acte conscient de liberté personnelle. En tandem, Soloviev souligne le rôle progressiste de l’État pour favoriser le libre perfectionnement humain. En tant que tel, Soloviev nous fournit certaines voies innovatrices dans le façonnement de la relation tant théorique que pratique entre le droit et la religion. À l’encontre d’un compromis entre objets, c’est-à-dire un arrangement de type interculturel situé entre fragmentation culturelle (multiculturalisme idéologique) et assimilation antireligieuse (laïcité militante), l’analyse de Soloviev présente la nécessité d’une conciliation temporelle, dans une perspective historique beaucoup plus large, où la laïcité est considérée non pas comme une finalité ontologique en soi, figée dans le temps, mais comme un moyen au service d’une destinée humaine en cours d’actualisation. Le cadre philosophico-juridique de Soloviev peut être utilement mis en dialogue avec des auteurs contemporains comme Stephen L. Carter, Charles Taylor, John Witte Jr, Ronald Dworkin et Jürgen Habermas. La contribution potentielle de Soloviev sur la place de la religion dans la société russe contemporaine est également mentionnée, avec un accent particulier sur le réexamen critique de l’héritage durable de la notion byzantine de la symphonie entre l’Église et l’État. Enfin, une théorie du fédéralisme inspirée par Soloviev est développée en appliquant, sur une base comparative, des avancées théoriques dans le domaine de l’histoire juridique global à l’évolution constitutionnelle du Canada et d’Israël.

Annotated record of the detailed examination of Mn deposits from BLM Leg Alpha Cruise, R/V Kana Keoki off the south-western coastal area of the Gulf of Mexico off Texas

The BLM-OCS (Bureau of Land Management-Outer Continental Shelf) program was designed to establish chemical, biological, and geological baseline on the South Texas Continental Shelf. The focus for the geological program was to establish the nature and amount of the suspended sediment in the water column, of the Holocene sediments on the shelf, and to identify and locate regions of geology conditions which may be hazardous to OCS operations. To accomplish these goals three cruises were planned. The report constitutes results of the first cruise. The results of these cruises associated with the subsequent laboratory analysis, enabled to establish a detailed baseline in order to provide significant geologic and biologic data for environmental assessment. Dredges recovered are available at University of Texas (see: BLM/OCS South Texas Outer Continental Shelf (STOCS) Project Sediment Data http://www.ngdc.noaa.gov/docucomp/page?xml=NOAA/NESDIS/NGDC/MGG/Geology/iso/xml/G02888.xml&view=getDataView&header=none).

Annotated record and chemical analysis of manganese nodules from R/V Moana Wave Cruise Mn-74-01 and Mn-74-02 stations

Cruise Mn-74-02 of the R/V MOANA WAVE was the second part of the field work of the NSF/IDOE Inter-University Ferromanganese Research Program in 1974, and we gratefully acknowledge the support of the office for the International Decade of Ocean Exploration and the Office of Oceanographic Facilities and Support. This program was designed to investigate the origin, growth, and distribution of copper/nickel-rich manganese nodules in the Pacific Ocean. The field effort was designed to satisfy sample requirements of the fifteen principal investigators, while increasing general knowledge of the copper/nickel-rich nodule deposits of the equatorial Pacific. This report is the second of a series of cruise reports designed to assist sample requests for documented nodules, sediment, and water samples so that laboratory results can be realistically compared and related to the environment of nodule growth. Nodule samples and bathymetric and navigational data are archived at the Hawaii Institute of Geophysics, University of Hawaii. Bulk chemical analyses of nodules and reduction of survey data were carried out at Hawaii. Sediment cores were stored at the University of Hawaii and at Scripps Institution of Oceanography. The SIO analytical facility provided stratigraphic data on sediment chemistry.

Fossil associations from the middle and upper Eocene strata of the Pamplona Basin and surrounding areas (Navarre, western Pyrenees)

Fossil associations from the middle and upper Eocene (Bartonian and Priabonian) sedimentary succession of the Pamplona Basin are described. This succession was accumulated in the western part of the South Pyrenean peripheral foreland basin and extends from deep-marine turbiditic (Ezkaba Sandstone Formation) to deltaic (Pamplona Marl, Ardanatz Sandstone and Ilundain Marl formations) and marginal marine deposits (Gendulain Formation). The micropalaeontological content is high. It is dominated by foraminifera, and common ostracods and other microfossils are also present. The fossil ichnoasssemblages include at least 23 ichnogenera and 28 ichnospecies indicative of Nereites, Cruziana, Glossifungites and ?Scoyenia-Mermia ichnofacies. Body macrofossils of 78 taxa corresponding to macroforaminifera, sponges, corals, bryozoans, brachiopods, annelids, molluscs, arthropods, echinoderms and vertebrates have been identified. Both the number of ichnotaxa and of species (e. g. bryozoans, molluscs and condrichthyans) may be considerably higher. Body fossil assemblages are comparable to those from the Eocene of the Nord Pyrenean area (Basque Coast), and also to those from the Eocene of the west-central and eastern part of South Pyrenean area (Aragon and Catalonia). At the European scale, the molluscs assemblages seem endemic from the Pyrenean area, although several Tethyan (Italy and Alps) and Northern elements (Paris basin and Normandy) have been recorded. Palaeontological data of studied sedimentary units fit well with the shallowing process that throughout the middle and late Eocene occurs in the area, according to the sedimentological and stratigraphical data.