Geochemical analyses of secondary minerals from ODP Leg 115 basalts (Tables 1+2)

Basalts recovered along the Reunion hotspot track on Ocean Drilling Program (ODP) Leg 115 range in age from 34 Ma at Site 706 to 64 Ma at Site 707. They have undergone various degrees of secondary alteration. Within single holes the amount of alteration can vary from a few percent to near complete replacement of phenocrysts and groundmass by secondary minerals. Olivine appears to be the most susceptible to alteration and in some sections it is the only mineral altered. In other sections, olivine, pyroxene and plagioclase phenocrysts, and groundmass have been completely replaced by secondary minerals. Clays are the predominant form of secondary mineralization. In addition to replacing olivine, pyroxene, glass, and groundmass, clays have filled veins, vesicles, and voids. Minor amounts of calcite, zeolites, and K-feldspar were also detected. The clays that filled vesicles and veins often show color zonations of dark, opaque bands near the edges that grade into tan or green transparent regions in the centers of the veins. The electron microprobe was used to obtain chemical analyses of these veins as well as to characterize isolated clays that replaced specific minerals and filled voids and vesicles.

Endocarditis infecciosa : significado de la disfunción renal

Objetivo: Determinar la significación clínica y pronóstica de la disfunción renal en pacientes con Endocarditis Infecciosa (EI) Material y método: Estudio protocolizado, descriptivo, observacional y transversal de pacientes con EI diagnosticados según criterios de Duke. Se realizó un análisis comparativo entre los pacientes con EI sin (Grupo Sin) y con Disfunción Renal (Grupo DR), que se definió en base a uremia > 0.60 g/l y/o creatininemia > 1.5 mg/dl y/o hematuria o proteinuria. Fueron analizados en EPI info 6.04. Resultados: De un total de 110 EI incluidas, 58 (52.7%) presentaron DR principalmente secundaria a glomerulonefritis (n 22), sepsis (n 14), insuficiencia renal crónica (n 5), insuficiencia cardíaca, nefropatía diabética y nefrotoxicidad (n 4 cada una) y embólica (n 1). No hubo diferencias en la permanencia media hospitalaria (32 DS±23.3 vs 26.32 DS±17.28 días), el sexo (masculino: 60.3 vs 71.25%) y la demora diagnóstica (5.5 (DS±7.23) vs. 5.4 (DS±7.64 días)(pNS). La edad media fue mayor en el grupo DR en el LS (49.62 DS±15.71 vs 43.53 DS±17.94 años). El Grupo DR tuvo mas frecuentemente EI Definida (87.9 vs 67.3%) (p=0.0089) y no hubo diferencias en la localización Mitral (48.3 vs 48.1%) y Aórtica (44.8 vs 34.6%). La valvulopatía degenerativa se presentó en el LS en DR (34.5 VS 19.6%)(p=0.07). No hubo diferencias en la presencia de comórbidas (62.1 vs 71.2%) (pNS) pero la enfermedad últimamente fatal ocurrió mas frecuentemente en DR (51.4 vs 21.6%)(p=0.05). Al ingreso sólo la presencia de rales pulmonares (53.4 vs 32.7%) y púrpura cutánea (27.6 vs 13.5%) fueron más frecuentes en DR (p=0.05). La sepsis no controlada (34.5 vs 15.7%), insuficiencia cardíaca (51.7 vs 32.7%), encefalopatía (50 vs 27.5%), shock séptico (24.1 vs 7.8%) y fallo multiorgánico (34.5 vs 3.9%) fueron complicaciones más frecuentes en DR (p<0.05). La fiebre persistente se encontró en el LS en el grupo de DR (48.3 vs 32.7%)(p=0.09). No hubo diferencias en el hallazgo de vegetaciones por ecocardiografía (83.3 vs 75.6%). La anemia (Hb<9 mg/dl) (31.86 DS±53.41 vs 35.21 DS±7.85)(p=0.009), hipergammaglobulinemia (58.5 vs 29.8)(p=0.006) e hiperglucemia (36.1 vs 18.5)(p=0.03) se asociaron a DR. En el grupo con DR fue mas común la EI con cultivos negativos (31.5 vs 0%)(p=0.001) y el predominio de las infecciones por S. aureus Meticilino Resistente (MRSA)(21.6 vs 2.7%) (p=0.02). No hubo diferencias en la indicación de cirugía (31 vs 36.5%). La mortalidad hospitalaria fue significativamente mayor en DR (51.7 vs 25%)(p=0.0041)(OR 3.2, IC95%1.42-7.24). Conclusión: En los pacientes con EI la disfunción renal resultó ser un indicador de desarrollo de complicaciones infecciosas y cardíacas, de infección por MRSA y de mortalidad cruda hospitalaria.-

Significado de la pérdida de peso en pacientes hospitalizados

La pérdida involuntaria de peso es un predictor independiente de morbimortalidad, especialmente en ancianos, pacientes con cáncer, SIDA y postoperatorios. Con el objeto de determinar la significación clínica de la pérdida de peso en pacientes internados, se estudiaron 100 pacientes. La edad media fue de 57.6 años (DS±11.04); 38% mayores de 65 años y 62% hombres. La permanencia hospitalaria media fue de 13 días, superior a la media del servicio (7,3 días). El 61% pertenecían a clase social baja y 25% eran desocupados. En el 100% fue involuntaria y en ninguno fue causa de hospitalización. Tenían hiporexia 61 pacientes y 57 malnutrición. El IMC fue inferior a 20 en el 50% de los casos. La causa fue determinada en el 70% y en 72% se relacionó con la enfermedad de base, en 27% con trastornos alimentarios y con fármacos en 1%. Las etiologías más frecuentes fueron: neoplasias (34 pacientes), enfermedades crónicas (24), TBC (3) y SIDA (3). El 46% desarrollaron infecciones nosocomiales y el 100% tenían comórbidas (alcoholismo 26%, depresión 22%, diabetes 20%, EPOC 11%, insuficiencia cardiaca, cirrosis y demencia 8% c/u e insuficiencia renal 6%). La mortalidad fue del 18% y las causas más frecuentes fueron sepsis severa, fallo multiorgánico y neoplasias. Conclusiones: La pérdida significativa de peso en el paciente hospitalizado se caracterizó por ser involuntaria, asociada a clase social baja, a malnutrición, a alta taza de comorbilidad, a predisposición a infecciones nosocomiales, secundaria a enfermedades crónicas, neoplasias, tuberculosis y SIDA y a una tasa de mortalidad elevada.

Composition of sediments and cores from DSDP Legs 54 and 61-63

The monograph gives results of studies of sediments and rocks collected from D/S Glomar Challenger in the Pacific Ocean. These studies have been based on the lithological facial analysis applied for the first time for identificating genesis of ocean sediments. These results include new ideas on formation of the Earth's sedimentary cover and can be used for constructing regional and global schemes of ocean paleogeography, reconstructing some structures, correlating sedimentation on continents and in oceans, estimating perspectives of oil- and gas-bearing deposits and ore formation. The monograph also gives the first petrographic classification of organic matter in black shales.

Curie temperatures and hysteresis properties of ODP Leg 183 sites, Kerguelen Plateau and Broken Ridge

In this manuscript, we present rock magnetic results of samples recovered during Leg 183. The Leg 183 cores were recovered from six drill sites and display variable rock magnetic properties. The differences in the rock magnetic properties are a function of mineralogy and alteration. Cretaceous subaerial basalt samples with titanomagnetite exhibit a strong Verwey transition in the vicinity of 110 K and have frequency-dependent susceptibility curves that resemble those of synthetic (titano) magnetites. These results are in good agreement with the thermomagnetic characteristics where titanomagnetites with Curie temperatures of ~580°C were identified. The hysteresis ratios suggest that the bulk magnetic grain size is in the psuedo-single-domain boundary. These subaerial basalts experienced high-temperature oxidation and maintained reliable paleomagnetic records. In contrast, the 34-Ma submarine pillow basalts do not show the Verwey transition during the low-temperature experiments. Thermomagnetic analysis shows that the remanent magnetization in this group is mainly carried by a thermally unstable mineral titanomaghemite. The frequency-dependent relationships are opposite of those from the first group and show little sign of titanomagnetite characteristics. Rocks from the third group are oxidized titanomagnetites and have multiple magnetic phases. They have irreversible thermaomagnetic curves and hysteresis ratios clustering toward the multidomain region (with higher Hcr/Hc ratios). The combined investigation suggests that variations in magnetic properties correlate with changes in lithology, which results in differences in the abundance and size of magnetic minerals. The rock magnetic data on Leg 183 samples clearly indicate that titanomagnetite is the dominant mineral and the primary remanence carrier in subaerial basalt. The generally good magnetic stability and other properties exhibited by titanomagnetite-bearing rocks support the inference that the ChRM isolated from the Cretaceous sites were acquired during the Cretaceous Normal Superchron. The stable inclinations identified from these samples are therefore useful for future tectonic studies.

Chemical and isotopical analsyes of DSDP Hole 34-321 basalts

A blue-green smectite (iron-rich saponite) and green mica (celadonite) are the dominant sheet silicates in veins within the 10.5 m of basalt cored during DSDP Leg 34, Site 32l, in the Nazca plate. Oxygen isotopic analyses of these clays, and associated calcite, indicate a formation temperature of <25°C. Celadonite contains appreciable Fe2O3, K2O and SiO2, intermediate MgO, and very little Al2O3. Celadonite is commonly associated with goethite and hematite, which suggests that this phase formed by precipitation within a dominantly oxygenated environment of components leached from basalt and provided by seawater. A mass balance estimate indicates that celadonite formation can remove no more than 15% of the K annually transported to the oceans by rivers. In contrast, iron-rich saponite containing significant Al2O3 appears to have precipitated from a nonoxidizing, distinctly alkaline fluid containing a high Na/K ratio relative to unmodified seawater. Seawater-basalt interaction at low temperatures, resulting in the formation of celadonite and smectite may explain chemical gradients observed in interstitial waters of sediments overlying basalts.

Geochemistry of minerals at DSDP Holes 68-501 and 69-504B

The interaction of seawater with basalts in DSDP Hole 501 and the upper part of Hole 504B (Costa Rica Rift) produced oxidative alteration and a zonation of clay minerals along cracks. From rock edges to interiors in many cracks the following succession occurs, based on microscopic observations and microprobe analysis: iron hydroxides (red), "protoceladonite" (green), iddingsite (orange), and saponite (yellow). Clay minerals replace olivines and fill vesicles and cracks. Other secondary minerals are phillipsite, aragonite, and unidentified carbonates. Some glass is transformed to Mg-rich palagonite. Bulk rock chemistry is related to the composition of the secondary minerals. The zonation can be interpreted as a succession of postburial nonoxidative and oxidative diagenesis similar to that described in the Leg 34 basalts.

Geochemical characterizations of the Cretaceous formations at DSDP Holes 93-603B and 11-105

Geochemical characterizations of the Cretaceous formations at Site 603 are quite comparable with those at Site 105. In the Blake-Bahama and the Hatteras formations, the petroleum potential is medium (<5 kg HC/t of rock) to very low (<0.5 kg HC/t of rock), and the organic matter is mainly of type III origin, that is, terrestrial. At the top of the Hatteras Formation, there is a condensed series, which chiefly contains organic matter of type II origin, with up to 20 wt.% total organic carbon content in Core 603B-34 and 25 wt.% in Core 105-9. This accumulation corresponds to the Cenomanian/Turonian boundary event. An examination of dinoflagellates in the kerogen concentration assigns dates to the samples studied by organic geochemistry. The Cenomanian and Turonian age of the organic-matter-rich black claystones indicates a low rate of sedimentation, about 1 m/Ma. Furthermore, the occurrence of type II organic matter indicates an anoxic environment with insufficient oxygen renewal to oxidize the sinking hemipelagic organic matter. This organic enrichment is not related to local phenomena but to sedimentation over an extended area, because deposits are well known in various areas with different paleodepths in the North Atlantic.

Composition of post-Jurassic deposits from the Northwest Pacific and the Galapagos Rift, data of DSDP Legs 62, 65, and 70

The monogragh contains results of mineralogicai and geochemical studies of Mesozoic and Cenozoic deposits from the Pacific Ocean collected during Deep Sea Drilling Project. Special attention is paid on the aspects of geochemical history of post-Jurassic sedimentation in the central part of the Northwest Pacific, detailed characteristics of the main stages of sedimentary evolution are given: Early Cretaceons (protooceanic), Late Cretaceons (transitional) and Cenozoic (oceanic). Results of mineralogical and geochemical studies of hydrothermal deposits from the Galapagos Rift are given as well.