Annualis ordo recitandi et celebrandi juxta rubricas Breviarii et Misalis Romani ac S.R.C. decreta in sancta cathedrali tota que Jacobo politana Chilensi, 1826, 28, 31-33, 36, 38-42, 44, 46, 47, 49, 50.

Mode of access: Internet.

Memoires pour servir a l'histoire de la vie de Cesar Borgia, duc de Valentinois, fils du pape Alexandre VI. contenant diverses choses très remarquables concernant l'histoire de ce pape, & de son pontificat &c.

Fictitious imprint.

Historical collections of Virginia : containing a collection of the most interesting facts, traditions, biographical sketches, anecdotes, &c., relating to its history and antiquities, together with geographical and statistical descriptions : to which is appended, an historical and descriptive sketch of the District of Columbia : illustrated by over 100 engravings, giving views of the principal towns, seats of eminent men, public buildings, relics of antiquity, historic localities, natural scenery, etc., etc. /

Illustrated by J.W. Barber.

Tower AB-216/U, tower section set AB-298/U, guy kit MK-99/U, accessory kit MK-100/U, guy kit MK-101/U.

"June 1956."

Na 1 Nachlass Max Horkheimer, 803 - "Dialektik der Aufklärung" von Max Horkheimer und Theodor W. Adorno (p. XI 6.43 - XI 6.106)

43. - 62. Sammlung B: "Konzepte als Zugabe zur Festschrift für Friedrich Pollock" [GS 12, S. 250 - 295]. 64 Blatt; 43. "Zum Problem der Bedürfnisse". Typoskript, 6 Blatt; 44. "Dichtung und Moral". Typoskript, 5 Blatt; 45. "Geschichte der amerikanischen Arbeiterschaft". Typoskript, 1 Blatt; 46. "Kein Weg zur Wahrheit". Typoskript, 1 Blatt; 47. "Zur Rechtsphilosophie". Typoskript mit eigenen Korrekturen, 2 Blatt; 48. "Strafgefangene". Typoskript, 1 Blatt; 49. "Jüdischer Charakter". Typoskript, 1 Blatt; 50. "Solidarität". Typoskript, 2 Blatt; 51. "Unmöglichkeit der Dichtung". Typoskript, 1 Blatt; 52. "Theorie des Verbrechers". Typoskript, 14 Blatt; 53. "Erbsünde und Kopula". Typoskript, 2 Blatt; 54. "Feind". Typoskript, 2 Blatt; 55. "Haupt- und Nebensatz". Typoskript, 3 Blatt; 56. "Bewußtsein". Typoskript, 1 Blatt; 57. "Kampf und Gewaltlosigkeit". Typoskript, 6 Blatt; 58. "Umschlag der idealistischen Dialektik". Typoskript, 1 Blatt; 59. "Die Rackets und der Geist". Typoskript, 7 Blatt; 60. "Altmodische Probleme". Typoskript mit eigenen Korrekturen, 2 Blatt; 61. "Physiognomik". Typoskript, 1 Blatt; 62. "Religionspsychologie". Typoskript, 2 Blatt; 63. - 106. Sammlung C: "New Yorker Notizen [I]"; 63. "Dialektik der Aufklärung Nr. 7". Typoskript mit eigenen Korrekturen, 12 Blatt; 64. Aus der "Dialektik der Aufklärung"; Kapitel: "Elemente des Antisemitismus", Abschitt VII:; 64a) Typoskript mit eigenen Korrekturen, 11 Blatt; 64b) Teilstück, Typoskript, 2 Blatt; 64c) Teilstück, Typoskript, 1 Blatt; 64d) Teilstück, Typoskript, 1 Blatt; 65. "Bemerkungen zu These VII" [zu: 64]; Über Antisemitismus und Stalinismus, [von Theodor W. Adorno]. Typoskript, 3 Blatt; 66. "Verwandlung der Idee in Gesinnung":; 66a) Typoskript, 5 Blatt; 66b) Typoskript mit eigenen Korrekturen, 4 Blatt; 66c) Typoskript, 5 Blatt; 67. "Zum Problem der Bedürfnisse". Typoskript mit eigenen Korrekturen, 6 Blatt; 68. "Dichtung und Moral":; 68a) Typoskript, 5 Blatt; 68b) Typoskript mit eigenen Korrekturen, 4 Blatt; 68c) Typoskript mit eigenen Korrekturen, 4 Blatt; 68d) Typoskript mit eigenen Korrekturen, 5 Blatt; 69. "Geschichte der amerikanischen Arbeiterschaft":; 69a) Typoskript, 1 Blatt; 69b) Typoskript; 1 Blatt; 70. "Straftheorie. Zur Rechtsphilosophie":; 70a) Typoskript mit eigenen Korrekturen, 3 Blatt; 70b) Typoskript mit eigenen Korrekturen, 3 Blatt; 70c) Typoskript mit eigenen Korrekturen, 3 Blatt; 70d) Typoskript, 3 Blatt; 71. "Jüdischer Charakter". Typoskript, 1 Blatt; 72. "Solidarität". Typoskript, 2 Blatt; 73. "Theorie des Verbrechens". Typoskript mit eigenen Korrekturen, 17 Blatt; 74. "Erbsünde und Copula":; 74a) Typoskript, 2 Blatt; 74b) Typoskript mit eigenen Korrekturen, 3 Blatt; 75. "Geschichtsphilosophischer Exkurs zur Odysee" [von Theodor W. Adorno ?]. Teilstück, Typoskript, 1 Blatt; 76. "Feind":; 76a) Typoskript, 2 Blatt; 76b) Typoskript, 2 Blatt; 76c) Typoskript, 2 Blatt; 76d) Entwurf, englisch, Typoskript mit eigenen Korrekturen, 2 Blatt; 77. "Haupt- und Nebensatz":; 77a) Typoskript, 2 Blatt; 77b) Typoskript mit eigenen Korrekturen, 2 Blatt; 77c) Typoskript mit eigenen Korrekturen, 2 Blatt; 77d) Typoskript mit eigenen Korrekturen, 3 Blatt; 78. "Bewußtsein":; 78a) Typoskript, 1 Blatt; 78b) Typoskript mit eigenen Korrekturen, 1 Blatt; 79. "Kampf und Gewaltlosigkeit":; 79a) Typoskript, 6 Blatt; 79b) Typoskript, 6 Blatt; 79c) Teilstücke, Typoskript mit eigenen Korrekturen, 6 Blatt; 79d) Typoskript mit eigenen Korrekturen, 5 Blatt; 79e) Typoskript, 5 Blatt; 79f) Teilstück, Typoskript mit eigenen Korrekturen, 2 Blatt; 80. "Die Rackets und der Geist":; 80a) Typoskript mit eigenen Korrekturen, 2 Blatt; 80b) Typoskript mit eigenen Korrekturen, 6 Blatt; 81. "Altmodisches Problem". Typoskript, 2 Blatt; 82. "Physiognomik". Typoskript, 1 Blatt; 83. "Religionspsychologie":; 83a) Typoskript mit eigenen Korrekturen, 2 Blatt; 83b) Typoskript mit eigenen Korrekturen, 2 Blatt; 84. "Leeres Erschrecken":; 84a) Typoskript mit eigenen Korrekturen, 2 Blatt; 84b) Typoskript, 2 Blatt; 84c) Typoskript mit eigenen Korrekturen, 2 Blatt; 85. "Philosophie und Arbeitsteilung":; 85a) Typoskript mit eigenen Korrekturen, 3 Blatt; 85b) Typoskript mit eigenen Korrekturen, 3 Blatt; 85c) Typoskript, 3 Blatt; 85d) Typoskript mit handschriftlichen Korrekturen, 3 Blatt; 86. "Vorrede" zur Dialektik der Aufklärung. Typoskript mit eigenen Korrekturen, 11 Blatt; 87. ["Umschlag der idealistischen Dialektik"] Typoskript, 1 Blatt; 88. Über Erkenntnis und Sprache. Typoskript mit eigenen Korrekturen, 1 Blatt; 89. "Zur Kritik der Geschichtsphilosophie". Typoskript mit eigenen Korrekturen, 3 Blatt; 90. "Mensch und Tier":; 90a) Typoskript mit eigenen und handschriftlichen Korrekturen, 12 Blatt; 90b) Typoskript mit eigenen Korrekturen, 3 Blatt; 90c) Typoskript mit eigenen Korrekturen, 4 Blatt; 90d) Typoskript mit eigenen Korrekturen, 3 Blatt; 90e) Typoskript mit eigenen Korrekturen, 10 Blatt; 91. "Massengesellschaft". Typoskript, 1 Blatt; 92. "Zwei Welten". Typoskript, 2 Blatt; 93. "Zur Theorie der Gespenster":; 93a) Typoskript, 1 Blatt; 93b) Typoskript mit eigenen Korrekturen, 1 Blatt; 94. "Interesse am Körper":; 94a) Typoskript mit eigenen Korrekturen, 6 Blatt; 94b) Typoskript mit eigenen Korrekturen, 7 Blatt; 94c) Typoskript, 2 Blatt; 94d) Typoskript, 6 Blatt; 95. "Unmöglichkeit der Dichtung". Typoskript, 1 Blatt; 96. "Die Einseitigkeit der Negativität":; 96a) Typoskript, 2 Blatt; 96b) Typoskript mit eigenen Korrekturen, 2 Blatt; 96c) Typoskript, 2 Blatt; 97. "Widersprüche":; 97a) Typoskript, 4 Blatt; 97b) Typoskript mit eigenen Korrekturen, 4 Blatt; 98. "Zur Theorie der Dummheit":; 98a) Typoskript, 3 Blatt; 98b) Typoskript mit eigenen Korrekturen, 3 Blatt.; 99. "Gezeichnet". Typoskript, 2 Blatt; 100. "Quand-même":; 100a) Typoskript, 2 Blatt; 100b) Typoskript mit eigenen Korrekturen, 2 Blatt; 101. "Isolierung durch Verkehr":; 101a) Typoskript mit eigenen Korrekturen, 1 Blatt; 101b) Typoskript, 1 Blatt; 102. "Gegen Gescheitheit". Typoskript mit eigenen Korrekturen, 1 Blatt; 103. "Propaganda":; 103a) Typoskript mit eigenen Korrekturen, 2 Blatt; 103b) Typoskript, 2 Blatt; 103c) Typoskript mit eigenen Korrekturen, 2 Blatt; 104. "Der Gedanke". Typoskript mit eigenen Korrekturen, 1 Blatt; 105. Fragment aus der "Dialektik der Aufklärung", Exkurs II. Typoskript mit eigenen Korrekturen, 3 Blatt; 106. Zum Begriff des Individuums bei Leibniz und Hegel [GS 12, S. 314 - 315]. Typoskript mit eigenen Korrekturen, 2 Blatt;

A IMPORTÂNCIA DAS TICS E DA EDUCAÇÃO COMO PROCESSO COMUNICACIONAL DIALÓGICO NO ENSINO SUPERIOR: Um Estudo da Universidade Estadual de Mato Grosso do Sul

Esta tese teve por objetivo saber como o corpo docente da Universidade Estadual de Mato Grosso do Sul (UEMS) percebe, entende e reage ante a incorporação e utilização das Tecnologias de Informação e Comunicação (TICs) nos cursos de graduação dessa Instituição, considerando os novos processos comunicacionais dialógicos que elas podem proporcionar na sociedade atual. Metodologicamente, a tese é composta por pesquisa bibliográfica, buscando fundamentar as áreas da Educação e Comunicação, assim como a Educomunicação; pesquisa documental para contextualização do lócus da pesquisa e de uma pesquisa exploratória a partir da aplicação de um questionário online a 165 docentes da UEMS, que responderam voluntariamente. Verificou-se que os professores utilizam as TICs cotidianamente nas atividades pessoais e, em menor escala, nos ambientes profissionais. Os desafios estão em se formar melhor esse docente e oferecer capacitação continuada para que utilizem de forma mais eficaz as TICs nas salas de aula. Destaca-se ainda que os avanços em tecnologia e os novos ecossistemas comunicacionais construíram novas e outras realidades, tornando a aprendizagem um fator não linear, exigindo-se revisão nos projetos pedagógicos na educação superior para que estes viabilizem diálogos propositivos entre a comunicação e a educação. A infraestrutura institucional para as TICs é outro entrave apontado, tanto na aquisição como na manutenção desses aparatos tecnológicos pela Universidade. Ao final, propõe-se realizar estudos e pesquisas que possam discutir alterações nos regimes contratuais de trabalho dos docentes, uma vez que, para atuar com as TICs de maneira apropriada, exige-se mais tempo e dedicação do docente.

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.

Foraminiferal faunal estimates of paleotemperature: Circumventing the no-analog problem yields cool ice age tropics

The sensitivity of the tropics to climate change, particularly the amplitude of glacial-to-interglacial changes in sea surface temperature (SST), is one of the great controversies in paleoclimatology. Here we reassess faunal estimates of ice age SSTs, focusing on the problem of no-analog planktonic foraminiferal assemblages in the equatorial oceans that confounds both classical transfer function and modern analog methods. A new calibration strategy developed here, which uses past variability of species to define robust faunal assemblages, solves the no-analog problem and reveals ice age cooling of 5° to 6°C in the equatorial current systems of the Atlantic and eastern Pacific Oceans. Classical transfer functions underestimated temperature changes in some areas of the tropical oceans because core-top assemblages misrepresented the ice age faunal assemblages. Our finding is consistent with some geochemical estimates and model predictions of greater ice age cooling in the tropics than was inferred by Climate: Long-Range Investigation, Mapping, and Prediction (CLIMAP) [1981] and thus may help to resolve a long-standing controversy. Our new foraminiferal transfer function suggests that such cooling was limited to the equatorial current systems, however, and supports CLIMAP's inference of stability of the subtropical gyre centers.

Glacial North Atlantic: Sea surface conditions reconstructed by GLAMAP 2000

The response of the tropical ocean to global climate change and the extent of sea ice in the glacial nordic seas belong to the great controversies in paleoclimatology. Our new reconstruction of peak glacial sea surface temperatures (SSTs) in the Atlantic is based on census counts of planktic foraminifera, using the Maximum Similarity Technique Version 28 (SIMMAX-28) modern analog technique with 947 modern analog samples and 119 well-dated sediment cores. Our study compares two slightly different scenarios of the Last Glacial Maximum (LGM), the Environmental Processes of the Ice Age: Land, Oceans, Glaciers (EPILOG), and Glacial Atlantic Ocean Mapping (GLAMAP 2000) time slices. The comparison shows that the maximum LGM cooling in the Southern Hemisphere slightly preceeded that in the north. In both time slices sea ice was restricted to the north western margin of the nordic seas during glacial northern summer, while the central and eastern parts were ice-free. During northern glacial winter, sea ice advanced to the south of Iceland and Faeroe. In the central northern North Atlantic an anticyclonic gyre formed between 45° and 60°N, with a cool water mass centered west of Ireland, where glacial cooling reached a maximum of >12°C. In the subtropical ocean gyres the new reconstruction supports the glacial-to-interglacial stability of SST as shown by CLIMAP Project Members (CLIMAP) [1981]. The zonal belt of minimum SST seasonality between 2° and 6°N suggests that the LGM caloric equator occupied the same latitude as today. In contrast to the CLIMAP reconstruction, the glacial cooling of the tropical east Atlantic upwelling belt reached up to 6°-8°C during Northern Hemisphere summer. Differences between these SIMMAX-based and published U37[k]- and Mg/Ca-based equatorial SST records are ascribed to strong SST seasonalities and SST signals that were produced by different planktic species groups during different seasons.

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.

Physical oceanography from the northwestern Weddell Sea

We analyzed hydrographic data from the northwestern Weddell Sea continental shelf of the three austral winters 1989, 1997, and 2006 and two summers following the last winter cruise. During summer a thermal front exists at ~64° S separating cold southern waters from warm northern waters that have similar characteristics as the deep waters of the central basin of the Bransfield Strait. In winter, the whole continental shelf exhibits southern characteristics with high Neon (Ne) concentrations, indicating a significant input of glacial melt water. The comparison of the winter data from the shallow shelf off the tip of the Antarctic Peninsula, spanning a period of 17 yr, shows a salinity decrease of 0.09 for the whole water column, which has a residence time of <1 yr. We interpret this freshening as being caused by a combination of reduced salt input due to a southward sea ice retreat and higher precipitation during the late 20th century on the western Weddell Sea continental shelf. However, less salinification might also result from a delicate interplay between enhanced salt input due to sea ice formation in coastal areas formerly occupied by Larsen A and B ice shelves and increased Larsen C ice loss.