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.

Gas hydrates of nonpressurized (GC) and pressurized (DAPC) sediment cores from the Hakon Mosby Mud Volcano, SW Barents Sea

The occurrence of gas hydrates at submarine mud volcanoes (MVs) located within the gas hydrate stability zone (GHSZ) is controlled by upward fluid and heat flux associated with MV activity. Determining the spatial distribution of gas hydrates at MVs is crucial to evaluate their sensitivity to known episodic changes in volcanic activity. We determined the hydrocarbon inventory and spatial distribution of hydrates at an individual MV structure. The Håkon Mosby Mud Volcano (HMMV), located at 1,250 m water depth on the Barents Sea slope, was investigated by combined pressure core sampling, heat flow measurements, and pore water chemical analysis. Quantitative pressure core degassing revealed gas-sediment ratios between 3.1 and 25.7, corresponding to hydrate concentrations of up to 21.3% of the pore volume. Hydrocarbon compositions and physicochemical conditions imply that gas hydrates incipiently crystallize as structure I hydrate, with a dissociation temperature of around 13.8°C at this water depth. Based on numerous in situ measurements of the geothermal gradient in the seabed, pore water sulfate profiles and microbathymetric data, we show that the thickness of the GHSZ increases from less than 1 m at the warm center to around 47 m in the outer parts of the HMMV. We estimate the total mass of hydrate-bound methane stored at the HMMV to be about 102.5 kt, of which 2.8 kt are located within the morphological Unit I around the center and thus are likely to be dissociated in the course of a large eruption.

Biomass of large protists from the Infrakingdom Rhizaria in the global ocean

The present data set is a worldwide compilation from 11 oceanographic expeditions during which an underwater vision profiler (UVP) was deployed in situ to determine the vertical distribution (biomass) of 4 taxonomic groups of plankton larger than 600 µm, belonging to the Infrakingdom Rhizaria, including Collodaria, Acantharia, Phaeodaria and other Rhizaria. Vertical distributions are binned in four layers: 0-100, 0-200, 100-500 and 0-500 m.

Physical oceanography from CTD during Maria S. Merian cruise MSM20/4 in spring 2012

With an extension of > 40 km**2 the recently discovered Campeche cold-water coral province located at the northeastern rim of the Campeche Bank in the southern Gulf of Mexico belongs to the largest coherent cold-water coral areas discovered so far. The Campeche province consists of numerous 20-40 m-high elongated coral mounds that are developed in intermediate water depths of 500 to 600 m. The mounds are colonized by a vivid cold-water coral ecosystem that covers the upper flanks and summits. The rich coral community is dominated by the framework-building Scleractinia Enallopsammia profunda and Lophelia pertusa, while the associated benthic megafauna shows a rather scarce occurrence. The recent environmental setting is characterized by a high surface water production caused by a local upwelling center and a dynamic bottom-water regime comprising vigorous bottom currents, obvious temporal variability, and strong density contrasts, which all together provide optimal conditions for the growth of cold-water corals. This setting - potentially supported by the diel vertical migration of zooplankton in the Campeche area - controls the delivering of food particles to the corals. The Campeche cold-water coral province is, thus, an excellent example highlighting the importance of the oceanographic setting in securing the food supply for the development of large and vivid cold-water coral ecosystems.

Opinion: Can coalescent models explain deep divergences in the diatoms and argue for the acceptance of paraphyletic taxa at all taxonomic hierarchies?

Although ancestral polymorphisms and incomplete lineage sorting are commonly used at the population level, increasing reports of these models have been invoked and tested to explain deep radiations. Hypotheses are put forward for ancestral polymorphisms being the likely reason for paraphyletic taxa at the class level in the diatoms based on an ancient rapid radiation of the entire groups. Models for ancestral deep coalescence are invoked to explain paraphyly and molecular evolution at the class level in the diatoms. Other examples at more recent divergences are also documented. Discussion as to whether or not paraphyletic groups seen in the diatoms at all taxonomic levels should be recognized is provided. The continued use of the terms centric and pennate diatoms is substantiated with additional evidence produced to support their use in diatoms both as descriptive terms for both groups and as taxonomic groups for the latter because new morphological evidence from the auxospores justifies the formal classification of the basal and core araphids as new subclasses of pennate diatoms in the Class Bacillariophyceae. Keys for higher levels of the diatoms showing how the terms centrics and araphid diatoms can be defined are provided.

Opinion: Can coalescent models explain deep divergences in the diatoms and argue for the acceptance of paraphyletic taxa at all taxonomic hierarchies?

Although ancestral polymorphisms and incomplete lineage sorting are commonly used at the population level, increasing reports of these models have been invoked and tested to explain deep radiations. Hypotheses are put forward for ancestral polymorphisms being the likely reason for paraphyletic taxa at the class level in the diatoms based on an ancient rapid radiation of the entire groups. Models for ancestral deep coalescence are invoked to explain paraphyly and molecular evolution at the class level in the diatoms. Other examples at more recent divergences are also documented. Discussion as to whether or not paraphyletic groups seen in the diatoms at all taxonomic levels should be recognized is provided. The continued use of the terms centric and pennate diatoms is substantiated with additional evidence produced to support their use in diatoms both as descriptive terms for both groups and as taxonomic groups for the latter because new morphological evidence from the auxospores justifies the formal classification of the basal and core araphids as new subclasses of pennate diatoms in the Class Bacillariophyceae. Keys for higher levels of the diatoms showing how the terms centrics and araphid diatoms can be defined are provided.

Prevalencia del síndrome de cementación ósea en pacientes de artroplastia de cadera, Hospital Universitario Mayor Méderi 2014

Resumen Introducción: Con el fin de estimar la prevalencia del síndrome de cementación ósea (SICO) en pacientes llevados a artroplastia de cadera cementada en el Hospital Universitario Mayor Méderi 2014. Materiales y métodos: Se realizó un estudio observacional, descriptivo, de corte transversal, se evaluaron los registros de historia clínica de los pacientes llevados a artroplastia cementada de cadera desde enero a diciembre de 2014. Se estimó la prevalencia del número total de casos de SICO sobre el total de intervenidos y la mortalidad del número de muertes intraoperatorias sobre el total de pacientes que desarrollaron el SICO. Resultados: Se encontraron 102 pacientes llevados a artroplastia cementada de cadera; 73,5% de género femenino, la mediana de edad fue 82 años, la prevalencia de SICO fue de 0,96 x 100 procedimientos y la mortalidad de 7,14 x 100 eventos (1 caso), el evento más frecuentemente relacionado fue las Perdida sanguínea < 300ml (p.valor: 0,006), el resto de diferencias entre los factores de riesgo reconocidos no fueron estadísticamente significativas. Discusión Se encontró una baja frecuencia del evento, con una muerte relacionada, se requieren estudios prospectivos para explorar desenlaces en el tiempo para la presentación de SICO y factores de riesgo adicionales. Palabras clave: "Hipotensión/Diagnóstico", "Prevalencia", "Artroplastia de Reemplazo de Cadera/Efectos Adversos", "Cementos Óseos/Efectos Adversos", "Complicaciones Postoperatorias/Etiología" y "Complicaciones Postoperatorias/Inducido Químicamente"

Sonata No. 4 in C, Op. 102, No. 1

Soitinnus: Sello, piano.

Na 1 Nachlass Max Horkheimer, 38 - Korrespondenzen u.a. mit Arthur E. Nadel (p. I 19, 1-102)

40 Briefe zwischen Arthur E. Nadel und Max Horkheimer, 1934-1939; 1 Brief von Arthur E. Nadel an Armin Hodler, 02.02.1939; 18 Briefe zwischen Otto Nathan und Max Horkheimer, 1934-1940; 1 Brief von Friedrich Pollock an Paul Tillich, 12.11.1938; 5 Briefe zwischen dem National Council of Jewish Women New York Section und Max Horkheimer, 1937-1939; 1 Brief vom National Council of Parent Education Poughkeepsie, New York an Max Horkheimer, 17.06.1940; 1 Brief vom National Research Council Washington an Max Horkheimer, 15.02.1941; 2 Briefe zwischen dem National Roster of Scientific and Specialized Personnel Washington und Max Horkheimer, 1940; 2 Briefe zwischen Lisel Nädele und Max Horkheimer, 11.12.1939, 22.01.1940; 1 Brief von Benjamin Nathaniel Nelson an Max Horkheimer, 20.04.1938 sowie Briefwechsel mit der C.R.B. Educational Foundation, New York; 2 Briefe zwischen der C.R.B. Educational Foundation, New York und Max Horkheimer, 16.12.1937; 1 Brief von Max Horkheimer an Neumann, 08.07.1934; 3 Briefe und Beilage zwischen Fritz Neumark, Jenny Neumark und Max Horkheimer, 08.08.1939 sowie Briefwechsel mit Otto Strauß; 2 Briefe zwischen Otto Strauß vom Selfhelp for German Emigree New York und Max Horkheimer, 01.08.1939, 04.08.1939;