Chemical composition of samples from DSDP Holes 16-163 and 17-164

Considerable postsedimentational alteration of fine dispersed minerals in Cretaceous sedimentary sequences was found in three deep-sea drillholes (163, 164, 169). Original Fe-montmorillonites formed from basalts were converted during lithification to mixed-layer montmorillonite-hydromicas and then to pure hydromicas (celadonites). An assumption that the minerals were originally of authigenic-diagenetic composition is based on a broad spectrum of other diagenetic minerals present: silica group from opal A to opal CT and quartz, clinoptilolite and palygorskite. In addition, quartz-hydromica ratio is strikingly atypical of aeolian transport.

Oxygen, hydrogen, and carbon isotopic compositions in deep sea cherts, porcellanites, and coexisting carbonates from DSDP Legs 2, 3, 6, 7, 11, 14, 16, 17, and 20

Seventy four samples of DSDP recovered cherts of Jurassic to Miocene age from varying locations, and 27 samples of on-land exposed cherts were analyzed for the isotopic composition of their oxygen and hydrogen. These studies were accompanied by mineralogical analyses and some isotopic analyses of the coexisting carbonates. d18O of chert ranges between 27 and 39%. relative to SMOW, d18O of porcellanite - between 30 and 42%. The consistent enrichment of opal-CT in porcellanites in 18O with respect to coexisting microcrystalline quartz in chert is probably a reflection of a different temperature (depth) of diagenesis of the two phases. d18O of deep sea cherts generally decrease with increasing age, indicating an overall cpoling of the ocean bottom during the last 150 m.y. A comparison of this trend with that recorded by benthonic foraminifera (Douglas and Savin, 1975; http://www.deepseadrilling.org/32/volume/dsdp32_15.pdf) indicates the possibility of d18O in deep sea cherts not being frozen in until several tens of millions of years after deposition. Cherts of any Age show a spread of d18O values, increasing diagenesis being reflected in a lowering of d18O. Drusy quartz has the lowest d18O values. On-land exposed cherts are consistently depleted in 18O in comparison to their deep sea time equivalent cherts. Water extracted from deep sea cherts ranges between 0.5 and 1.4 wt %. dD of this water ranges between -78 and -95%. and is not a function of d18O of the cherts (or the temperature of their formation).

Composition of palygorskite-rich and montmorillonite-rich zeolite-containing sediments from DSDP Sites 164 and 196

Cretaceous, Tertiary, and Quaternary sediments from Deep Sea Drilling Project Sites 164 and 196 (13°12' N, 161°31' W and 30°07' N, 148°34' E, respectively) were analyzed for major chemical elements and mineralogy. Sediments from these sites contain large proportions of authigenic minerals: mainly palygorskite, clinoptilolite and chert in the Cretaceous, and montmorillonite, phillipsite and chert in the Tertiary. The montmorillonite-phillipsite assemblage is thought to be derived from volcanic ash or glass, and the palygorskite-clinoptilolite assemblage is thought to be derived by reaction of biogenic silica with volcanic ash or glass or with montmorillonite and phillipsite. Both assemblages have generally moderate Ti/Al ratios, ranging from 0.026 to 0.047, so most of the palygorskite, clinoptilolite, montmorillonite and phillipsite could not be derived in situ from alteration of basaltic material. Plagioclase compositions suggest that the volcanic precursors were silicic or intermediate, but it is also possible that the sediments have been extensively fractionated by redistribution from nearby seamounts. Available data on other Late Cretaceous sediments in the Pacific were analyzed. Clinoptilolite and chert are present nearly everywhere where palygorskite is abundant; phillipsite is rare where palygorskite is abundant. It is suggested that increased water temperatures during the Cretaceous increased reaction rates and determined the alteration products.

桂西那坡县种子植物区系初步研究

　　本文对桂西那坡县种子植物区系的成分进行了全面系统的的分析，以探讨区系的性质和特点，为研究广西植物区系和滇、越、桂植物区系提供宝贵的资料。 　　本区系有裸子植物9科、13属、17种，被植物164科、876属、2138种。科的分析表明以热带－亚热带分布居首位，次为热带分布。特征科有樟科、木兰科、壳斗科、金缕梅科、山茶科、茜草科、大戟科等共21科，它们也是我国热带、亚热带植物区系的特征科。 　　属的分析显示热带分布占70．75％，居首位;温带分布占18．6％;东亚分布占8．7％;我国特有分布占2．2％;缺乏中亚分布成分。热带分布中以印度－马来西亚成分居多，占27．6％，其次是泛带分布，占18．8％。 　　种的分析表明以中国特有分布居第一位，占45．1％;其次是热带亚洲分布，占31．6％;居第三位是东亚分布，占13．8％。 　　那坡植物区系特有现象十分显著，共计东亚特有科有8个，中国特有属有17个，中国特有种有774个，其中56种为那坡特有种。 　　分析结果表明那坡种了植物区系具有以下特征：（1）热带北缘性质，具有很强的热带向亚热带的过渡性;（2）特有现象显著;（3）岩溶特性明显;（4）地理成分复杂;（5）起源古老。 　　本区系分析所依据的植物名录由作者汇编而成，绝大部分种名有标本引证，且经专家审定，同时还溶进作者两次野外考察的心得，为到目前为止，最完整的一份该地区的植物名录。

O Regresso a Casa

Assistimos, actualmente, a uma política de cuidados de saúde hospitalares orientada essencialmente para o tratamento da doença e reabilitação da Pessoa, em que se preconizam os internamentos hospitalares cada vez mais curtos e o regresso precoce a casa. O regresso a casa é uma realidade. Uma realidade que pressupõe: acessibilidade aos cuidados de saúde; avaliação das necessidades globais; organização e prática do trabalho interdisciplinar e em parceria; adequação ao tipo e grau das limitações; focalização na reabilitação e autonomia; respeito pelos direitos, dignidade e individualidade e o envolvimento da Pessoa e família. Deste modo, várias questões se levantam ao reflectirmos sobre esta problemática: Como podemos preparar o regresso de alguém a casa se não o enquadrarmos no seu processo de reabilitação e no seu contexto familiar, reconhecendo o seu lugar, as suas interacções e as suas potencialidades? Como podemos integrar e habilitar a família para a prestação de cuidados sem a conhecermos e sem identificarmos as suas necessidades? Como pode a família cuidar, se não for cuidada?

Facteurs de risque de sévérité de la papillomatose respiratoire juvénile

La papillomatose respiratoire récurrente (PRR) juvénile est causée par les génotypes 6 et 11 du virus du papillome humain (VPH). Cette maladie est caractérisée par des verrues récurrentes généralement au larynx. La forme sévère peut avoir un impact dévastateur sur la santé et la qualité de vie de l’enfant atteint et de sa famille en raison des conséquences des multiples chirurgies nécessaires et du risque d'obstruction des voies respiratoires. Objectif: Examiner les facteurs de risque associés aux manifestations sévères de la PRR. Méthode: Étude rétrospective des 31 cas diagnostiqués entre janvier 1995 et décembre 2008. Les données démographiques, cliniques, génétiques et virologiques ont été évaluées. Des régressions logistiques furent effectuées afin d'évaluer le rôle des variables indépendantes sur la sévérité de la maladie. Résultats: Nos données suggèrent que les facteurs de risque de sévérité de la PRR seraient associés au genre féminin (Rapport de cotes (RC)=2.60, intervalles de confiance (IC) 95% : 0.44-15.44), au fait d’être premier-né (RC=3.51, IC 95% : 0.17-72.32), à un statut économique faible (RC=5.31, IC 95% : 0.17-164.19), à un jeune âge (RC=0.83, IC 95% : 0.68-1.01), à une charge virale élevée (RC=3.81, IC 95% : 0.23-63.16) et aux condylomes chez la mère pendant la grossesse (RC=12.05, IC 95% : 0.97-149.85). Conclusion: La sévérité de la PRR serait le résultat d'une combinaison de déterminants qui favoriseraient la croissance cellulaire particulièrement chez les jeunes enfants. Des mesures préventives et thérapeutiques visant à restreindre la contamination et la réplication du virus pourraient réduire le fardeau de la maladie.

Experiencia en nefrectomía: serie de casos de cuatro años

Introducción: Las indicaciones por las cuales un paciente requiere una nefrectomía son múltiples: las neoplasias, la hidronefrosis y la exclusión funcional son las principales. En manos expertas la nefrectomía es un procedimiento seguro, especialmente porque en la actualidad el abordaje por excelencia es realizar una técnica mínimamente invasiva con conservación de nefronas. Se presenta el análisis de la experiencia en Mederi, Hospital Universitario Mayor en esta intervención. Metodología: Se realizó una serie de casos de pacientes llevados a nefrectomía entre mayo de 2008 y mayo de 2012. Se incluyeron la totalidad de los casos. Resultados: Se analizaron 72 registros, 49 mujeres y 25 hombres; 13 de ellas fueron laparoscópicas. La edad promedio fue de 58,6 años. El tiempo medio operatorio fue 169,23 minutos (118-220 minutos). El sangrado operatorio promedio fue de 680,63 ml (IC95%: 2,83-1358 ml). El tiempo de hospitalización promedio fue de 4,88 días IC95%. La mayoría de los pacientes se distribuyeron en estadios medios de la enfermedad tumoral, con poco compromiso ganglionar y metástasis; el diagnóstico histológico y estadio dominante fueron el carcinoma de células renales grado 3 de Fuhrman respectivamente. Se reportan 13 casos de compromiso de la capsula de Gerota y 11 con compromiso del hilio. Discusión: La experiencia en nefrectomía de la institución es muy positiva por el bajo número de mortalidad y complicaciones. En cuanto a la técnica, es importante promover la técnica laparoscópica

(Table DR1) Biogenic silica and chert in the Pacific Ocean, DSDP and ODP data

Evidence for the dissolution of biogenic silica at the base of pelagic sections supports the hypothesis that much of the chert formed in the Pacific derives from the dissolution and reprecipitation of this silica by hydrothermal waters. As ocean bottom waters flow into and through the crust, they become warmer. Initially they remain less saturated with respect to dissolved silica than pore water in the overlying sediments. With the diffusion of heat, dissolved ions, and to some extent the advection of water itself, biogenic silica in the basal part of the sedimentary section is dissolved. Upon conductively cooling, these pore waters precipitate chert layers. The most common thickness for the basal silica-free zone (20 m) lies below the most common height of the top of the chert interval above basement (50 m). This mode of chert formation explains the frequent occurrence of chert layers at very shallow subbottom depths in pelagic sections of the Pacific. It is also consistent with the common occurrence of cherts

Occurrence of hiatuses PH and NH 1 through NH 7 in DSDP holes

Miocene paleoceanographic evolution exhibits major changes resulting from the opening and closing of passages, the subsequent changes in oceanic circulation, and development of major Antarctic glaciation. The consequences and timing of these events can be observed in variations in the distribution of deep-sea hiatuses, sedimentation patterns, and biogeographic distribution of planktic organisms. The opening of the Drake Passage in the latest Oligocene to early Miocene (25-20 Ma) resulted in the establishment of the deep circumpolar current, which led to thermal isolation of Antarctica and increased global cooling. This development was associated with a major turnover in planktic organisms, resulting in the evolution of Neogene assemblages and the eventual extinction of Paleogene assemblages. The erosive patterns of two widespread hiatuses (PH, 23.0-22.5 Ma; and NH 1, 20-18 Ma) indicate that a deep circumequatorial circulation existed at this time, characterized by a broad band of carbonate-ooze deposition. Siliceous sedimentation was restricted to the North Atlantic and a narrow band around Antarctica. A major reorganization in deep-sea sedimentation and hiatus distribution patterns occurred near the early/middle Miocene boundary, apparently resulting from changes in oceanic circulation. Beginning at this time, deep-sea erosion occurred throughout the Caribbean (hiatus NH 2, 16-15 Ma), suggesting disruption of the deep circumequatorial circulation and northward deflection of deep currents, and/or intensification of the Gulf Stream. Sediment distribution patterns changed dramatically with the sudden appearance of siliceous-ooze deposition in the marginal and east equatorial North Pacific by 16.0 to 15.5 Ma, coincident with the decline of siliceous sedimentation in the North Atlantic. This silica switch may have been caused by the introduction of Norwegian Overflow Water into the North Atlantic acting as a barrier to outcropping of silica-rich Antarctic Bottom Water. The main aspects of the present oceanic circulation system and sediment distribution pattern were established by 13.5 to 12.5 Ma (hiatus NH 3), coincident with the establishment of a major East Antarctic ice cap. Antarctic glaciation resulted in a broadening belt of siliceous-ooze deposition around Antarctica, increased siliceous sedimentation in the marginal and east equatorial North Pacific and Indian Oceans, and further northward restriction of siliceous sediments in the North Atlantic. Periodic cool climatic events were accompanied by lower eustatic sea levels and widespread deep-sea erosion at 12 to 11 Ma (NH 4), 10 to 9 Ma (NH 5), 7.5 to 6.2 Ma (NH 6), and 5.2 to 4.7 Ma (NH 7).

Paleoelevations in the Pacific Ocean 35 million years ago

Data from deep sea drilling, linear magnetic anomalies and bathymetric measurements together with age and morphometric characteristics of seamounts have been used to construct a paleobathymetric map of the oceans 35 million years ago. A brief analysis of these results is presented.