Regulation of myogenesis and suppression of {\it mck\/} 5$\sp\prime$ enhancer elements by TGF$\beta$ and RAS

The regulation of muscle differentiation, like cell differentiation in general, is only now beginning to be understood. Here are described several key features to myogenesis: a beginning, some intermediary events, and an endpoint. Muscle differentiation proceeds spontaneously when myoblasts are cultured in serum-poor medium. Transforming growth factor type $\beta$ (TGF$\beta$), a component of fetal serum, was found to potently suppress muscle differentiation. Prolonged blockade of differentiation required replenishing TGF$\beta$. When TGF$\beta$ was removed, cells rapidly differentiated. Both TGF$\beta$ and RAS, which also blocks myogenesis, suppress the genes for a series of muscle-specific proteins. Regions that regulate transcription of one such gene, muscle creatine kinase (mck), were located by linking progressively smaller parts of the mck 5$\sp\prime$ region to the marker gene cat and testing the constructs for regulated expression of cat in myoblasts and muscle cells. The mck promoter is not muscle-specific but requires activation. Two enhancers were found: a weak, developmentally regulated enhancer within the first intron, and a strong, compact, and tightly developmentally regulated enhancer about 1.2 Kb upstream of the transcription start site. Activity of this enhancer is eliminated by activated ras. Suppression of activated N-RAS restores potency to the upstream enhancer. Further deletion shows the mck 5$\sp\prime$ enhancer to contain an enhancer core with low but significant muscle-specific activity, and at least one peripheral element that augments core activity. The core and this peripheral element were comprised almost entirely of factor-binding motifs. The peripheral element was inactive as a single copy, but was constitutively active in multiple copies. Regions flanking the peripheral element augmented its activity and conferred partial muscle-specificity. The enhancer core is also modulated by its 5$\sp\prime$ flanking region in a complex manner. Site-specific mutants covering most of the enhancer core and interesting flanking sequences have been made; all mutants tested diminish the activity of the 5$\sp\prime$ enhancer. Alteration of the site to which MyoD1 is reported to bind completely inactivates the enhancer. A theoretical analysis of cooperativity is presented, through which the binding of a constitutively expressed nuclear factor is shown to have weak positive cooperativity. In summary, TGF$\beta$, RAS, and enhancer-binding factors are found to be initial, intermediary, and final regulators, respectively, of muscle differentiation. ^

Impact of BCR -ABL on DNA repair

The BCR-ABL fusion gene is the molecular hallmark of Philadelphia-positive leukemias. Normal Bcr is a multifunctional protein, originally localized to the cytoplasm. It has serine kinase activity and has been implicated in cellular signal transduction. Recently, it has been reported that Bcr can interact with xeroderma pigmentosum group B (XPB/ERCC3)—a nuclear protein active in UV-induced DNA repair. Two major Bcr proteins (p160 Bcr and p130Bcr) have been characterized, and our preliminary results using metabolic labeling and immunoblotting demonstrated that, while both the p160 and p130 forms of Bcr localized to the cytoplasm, the p130 form (and to a lesser extent p160) could also be found in the nucleus. Furthermore, electron microscopy confirmed the presence of Bcr in the nucleus and demonstrated that this protein associates with metaphase chromatin as well as condensed interphase heterochromatin. Since serine kinases that associate with condensed DNA are often cell cycle regulatory, these observations suggested a novel role for nuclear Bcr in cell cycle regulation and/or DNA repair. However, cell cycle synchronization analysis did not demonstrate changes in levels of Bcr throughout the cell cycle. Therefore we hypothesized that BCR serves as a DNA repair gene, and its function is altered by formation of BCR-ABL. This hypothesis was investigated using cell lines stably transfected with the BCR-ABL gene, and their parental counterparts (MBA-1 vs. M07E and Bcr-AblT1 vs. 4A2+pZAP), and several DNA repair assays: the Comet assay, a radioinimunoassay for UV-induced cyclobutane pyrimidine dimers (CPDs), and clonogenic assays. Comet assays demonstrated that, after exposure to either ultraviolet (UV)-C (0.5 to 10.0 joules m −2) or to gamma radiation (200–1000 rads) there was greater efficiency of DNA repair in the BCR-ABL-transfected cells compared to their parental controls. Furthermore, after UVC-irradiation, there was less production of CPDs, and a more rapid disappearance of these adducts in BCR-ABL-bearing cells. UV survival, as reflected by clonogenic assays, was also greater in the BCR-ABL-transfected cells. Taken together, these results indicate that, in our systems, BCR-ABL confers resistance to UVC-induced damage in cells, and increases DNA repair efficiency in response to both UVC- and gamma-irradiation. ^

Geochemistry of bulk samples and various minerals of sediment core CRP-1 from the Ross Sea, Antarctica

Thirty-nine medium and fine grained sandstones from between 19,26 and 147,23 mbsf in the Cape Roberts-l core (CRP-1) were analysed for 10 major and 16 trace elements. Using whole-lock compositions, 9 samples were selected for analyses of mineral and glass grains by energy dispersive electron microscope. Laser-Ablation Mass-Spectrometry was used to determine rare earth elements and 14 additional trace elements in glass shards, pyroxenes and feldspars in order to examine their contribution to the bulk rock chemistry. Geochemical data reveal the major contribution played by the Granite Harbour Intrusives to the whole rock composition, even if a significant input is supplied by McMurdo volcanics and Ferrar dolerite pyroxenes McMurdo volcanics were studied in detail; they appeal to derive from a variety of litologies, and a dominant role of wind transpoitation from exposures of volcanic rocks may be inferred from the contemporary occurrence of different compositions at all depths. Only at 116.55 mbsf was a thin layer of tephra found, linked to an explosive eruption McMurdo volcanic rocks exhibit larger abundances at depths above 62 mbsf, in correspondence with the onset of volcanic activity in the McMurdo Sound area. From 62 mbsf to the bottom of the core, McMurdo volcanics are less abundant and probably issued from some centres in the McMurdo Sound region. However, available data do not allow the exclusion of wind transport from some eruptive centres active in north Victoria Land at the beginning of the Miocene Epoch.

Telurismo, Vanguardia y Tiempo Literario en Doña Bárbara

Para legitimar su propia modernidad, los escritores y críticos asociados al Boom solían describir a Rómulo Gallegos como un autor arcaico, neonaturalista o neorromántico, todavía activo en el siglo XX. Este artículo se propone reconstruir el horizonte de expectativas que cimentó el prestigio inicial de Doña Bárbara. Se argumenta que su éxito se debió al menos parcialmente a la proximidad —que después dejaría de percibirse con claridad— entre el regionalismo o mundonovismo y la estética de vanguardia. La comprensión del interés de Gallegos en la cinematografía resulta esencial para entender dichas afinidades.

Pollen profiles from 8 sediment cores from the Degersee, Southern Germany

The discovery of a neolithic pile field in the shallow water near the eastern shore of the Degersee confirmed earlier palynological and sedimentological studies stating that early man was active in the region since more than 6000 years. The already available off-site data were freshly assessed, completed by additional data from old and new cores and the interpretations revised. A common time scale for the off-site data and the on-site data was obtained by AMS dating of terrestrial macro remains of the neolithic section of off-site core De_I+De_H. The ages can thus be parallelled with AMS ages of construction timber on-site. Pollen analyses from all cores provide a further time scale. The continuously and densely sampled pollen profile of the profundal zone embracing the entire Late glacial and Holocene serves as a reference. From the Boreal onwards the relative ages are transformed by AMS ages and varve counts into calibrated and absolute. A transect cored close to the neolithic pile field across the lake marl-platform demonstrates its geological architecture in the shallow water since the Lateglacial. Studies of the microfabric of thin sections of drilled cores and of box cores from the excavations demonstrate that neolithic settlements now at 2-3,5 m water depth had been erected on lake marl freshly fallen dry, thus indicating earlier lake levels dropped by 1.5-2 m. The neolithic section of the highly resolved off-site profile in the lake=s profundal zone has laminated and calcareous zones alternating with massive ones. Assemblages of diatoms and concentrations of trace elements changing simultaneously characterise the calcareous sections as deposits of low lake levels that lasted between some 40 and more than 300 years. The ages of discovered lake shore dwellings fall into calcareous segments with low lake levels. From the end of the Upper Atlantic period (F VII) appear Secondary Forest Cycles in the beech forest, a man-made sequence of repeated vegetational development with an identical pattern: With a decrease of beech pollen appear pollen of grasses, herbs and cultural indicators. These are suppressed by the light demanding hazel and birch, those again by ash, and finally by the shade demanding beech forming a new pollen peak. Seven main Forest Cycles are identified In the upper Neolithic period each comprising some 250, 450 or 800 years. They are subdivided into subcycles that can be broken down by very dense sampling in even shorter cycles of decadal length. Farming settlers have caused minor patchy clearances of the beech-mixed-forest with the use of fire. The phases of clearance coincide with peaks of charcoal and low stands of the lake levels. The Secondary Forest Cycles and the continuous occurrence of charcoal prove a continued occupation of the region. Together with the repeated restoration of the beech climax forest they point to pulsating occupation probably associated with dynamic demography. The synchronism of the many palynological, sedimentological and archaeological data point to an external forcing as the climate that affects comprehensively all these proxies. The fluctuations of the activity of the sun as manifested in the residual d14C go largely along with the proxies. The initial clearances at the begin of the forest cycles are linked to low lake levels and negative values of d14C that point to dry and warm phases of a more continental climate type. The subcycles exist independent from climatic changes, indicating that early man acted largely independent from external forces.

Thorium and radiocarbon measurements on sediment cores from the Northseast Atlantic

Radiocarbon and 230Thexcess data from six NE Atlantic box cores are considered. The cores form a transect from the Porcupine Abyssal Plain over the East Thulean Rise to the southern end of Feni Drift. The chronology for the cores is established from bulk sediment carbonate radiocarbon data and reveals that sections exhibiting constant accumulation rates can be identified in all the cores, with rates of 3.0-3.5 cm/kyr on the plain through the Holocene and late Holocene rates of 4.3-6.6 cm/kyr elsewhere. Five out of the six cores show accumulations of more 230Thexcess than is produced in the overlying water column, with the greatest inventories (up to 225% of production) in the cores from the rise and drift. A size fraction comparison between two cores from the plain and rise reveals that the higher overall accumulation rates and 230Thexcess inventories in the off-plain cores are due to an increased fine (<5 µm) component fraction, whereas the flux of coarser material is similar to that received on the plain. This suggests that the higher fluxes of materials observed are physically (rather than biogeochemically) driven and also that drift formation has been continuously active in the late Holocene. Sections of all the cores where regular accumulation is defined by the radiocarbon data are modeled first by a linear radiocarbon age/depth model and second by a constant rain (230Thexcess)0 model prorated for the observed core inventories. These modeling approaches yield historical mass accumulation rate estimates which are generally in reasonable agreement (±30%), but the differences observed appear to be well organized in time rather than random.

Benthic foraminiferal composition at the inner wall of the Middle America Trench, Costa Rica

The sediments of Deep Sea Drilling Project Site 565 and University of Texas Marine Science Institute Cores IG-24-7-38 to -42 taken on the landward slope of the Middle America Trench exhibit characteristics of material subject to reworking during downslope mass flow. These characteristics include a generally homogeneous texture, lack of sedimentary structures, pervasive presence of a penetrative scaly fabric, and presence of transported benthic foraminifers. Although these features occur throughout the sediments examined, trends in bulk density, porosity, and water content, and abrupt shifts in these index physical properties and in sediment magnetic properties at Site 565 indicate that downslope sediment creep is presently most active in the upper 45 to 50 m of sediment. It cannot be determined whether progressive dewatering of sediment has brought the material at this depth to a plastic limit at which sediment can no longer flow (thus resulting in its accretion to the underlying sediments) or whether this depth represents a surface along which slumping has occurred. We suspect both are true in part, that is, that mass movements and downslope reworking accumulate sediments in a mobile layer of material that is self-limiting in thickness.

Bajo los adoquines está la Pachamama : Territorialidad andina en el Gran La Plata [2008-2011]

Desde hace aproximadamente 20 años, se está viviendo un resurgimiento del movimiento indígena a nivel mundial y continental. El territorio juega un papel esencial para las numerosas organizaciones y comunidades que lo componen, en tanto articula el accionar de estos sujetos al espacio en un sentido procesual y relacional, a través de una concepción en la que la tríada territorio-territorialidad-territorialización, niega la dualidad cartesiana entre materia y espíritu y afirma que toda apropiación material es a la vez simbólica. Según la Encuesta Complementaria de Pueblos Indígenas 2004-2005, complementaria del Censo Nacional de Población, Hogares y Viviendas 2001 del INdEC, el 54 de las 600.329 personas que se autoreconocen como parte de alguno de los más de treinta pueblos aborígenes que habitan en Argentina, se encuentra en áreas urbanas. El interés de este trabajo es el entender cuáles son las modalidades de apropiación material y simbólica del espacio que llevan adelante la Organización Quechua-Aymara Hijos del Cóndor [Kunthurpa Churinkuna] en conjunto con la Academia Mayor de la Lengua Quechua de Cusco-Filial Regional Internacional "Berisso" [Qheswasimi Jamutána Kuraq Suntur Qosqo-Perusuyu], y la Comunidad Qolla Gran La Plata, todas pertenecientes al universo cultural andino, y activas en el ámbito de la capital bonaerense. Es decir, qué territorialidad específica construyen en el espacio urbano, en función de la recreación de su cultura ancestral [analizada a través del enfoque del control cultural], y atendiendo a su relación con sus estrategias políticas y sus condiciones socioeconómicas, que se ponen en juego en la configuración de determinados espacios de socialización. Se trata de una investigación que emplea el método etnográfico, con técnicas tales como la observación participante y la entrevista en profundidad

Bajo los adoquines está la Pachamama : Territorialidad andina en el Gran La Plata [2008-2011]

Desde hace aproximadamente 20 años, se está viviendo un resurgimiento del movimiento indígena a nivel mundial y continental. El territorio juega un papel esencial para las numerosas organizaciones y comunidades que lo componen, en tanto articula el accionar de estos sujetos al espacio en un sentido procesual y relacional, a través de una concepción en la que la tríada territorio-territorialidad-territorialización, niega la dualidad cartesiana entre materia y espíritu y afirma que toda apropiación material es a la vez simbólica. Según la Encuesta Complementaria de Pueblos Indígenas 2004-2005, complementaria del Censo Nacional de Población, Hogares y Viviendas 2001 del INdEC, el 54 de las 600.329 personas que se autoreconocen como parte de alguno de los más de treinta pueblos aborígenes que habitan en Argentina, se encuentra en áreas urbanas. El interés de este trabajo es el entender cuáles son las modalidades de apropiación material y simbólica del espacio que llevan adelante la Organización Quechua-Aymara Hijos del Cóndor [Kunthurpa Churinkuna] en conjunto con la Academia Mayor de la Lengua Quechua de Cusco-Filial Regional Internacional "Berisso" [Qheswasimi Jamutána Kuraq Suntur Qosqo-Perusuyu], y la Comunidad Qolla Gran La Plata, todas pertenecientes al universo cultural andino, y activas en el ámbito de la capital bonaerense. Es decir, qué territorialidad específica construyen en el espacio urbano, en función de la recreación de su cultura ancestral [analizada a través del enfoque del control cultural], y atendiendo a su relación con sus estrategias políticas y sus condiciones socioeconómicas, que se ponen en juego en la configuración de determinados espacios de socialización. Se trata de una investigación que emplea el método etnográfico, con técnicas tales como la observación participante y la entrevista en profundidad

Bajo los adoquines está la Pachamama : Territorialidad andina en el Gran La Plata [2008-2011]

Desde hace aproximadamente 20 años, se está viviendo un resurgimiento del movimiento indígena a nivel mundial y continental. El territorio juega un papel esencial para las numerosas organizaciones y comunidades que lo componen, en tanto articula el accionar de estos sujetos al espacio en un sentido procesual y relacional, a través de una concepción en la que la tríada territorio-territorialidad-territorialización, niega la dualidad cartesiana entre materia y espíritu y afirma que toda apropiación material es a la vez simbólica. Según la Encuesta Complementaria de Pueblos Indígenas 2004-2005, complementaria del Censo Nacional de Población, Hogares y Viviendas 2001 del INdEC, el 54 de las 600.329 personas que se autoreconocen como parte de alguno de los más de treinta pueblos aborígenes que habitan en Argentina, se encuentra en áreas urbanas. El interés de este trabajo es el entender cuáles son las modalidades de apropiación material y simbólica del espacio que llevan adelante la Organización Quechua-Aymara Hijos del Cóndor [Kunthurpa Churinkuna] en conjunto con la Academia Mayor de la Lengua Quechua de Cusco-Filial Regional Internacional "Berisso" [Qheswasimi Jamutána Kuraq Suntur Qosqo-Perusuyu], y la Comunidad Qolla Gran La Plata, todas pertenecientes al universo cultural andino, y activas en el ámbito de la capital bonaerense. Es decir, qué territorialidad específica construyen en el espacio urbano, en función de la recreación de su cultura ancestral [analizada a través del enfoque del control cultural], y atendiendo a su relación con sus estrategias políticas y sus condiciones socioeconómicas, que se ponen en juego en la configuración de determinados espacios de socialización. Se trata de una investigación que emplea el método etnográfico, con técnicas tales como la observación participante y la entrevista en profundidad

Chemical measurements from the EPICA Dome C core

Sea ice and dust flux increased greatly in the Southern Ocean during the last glacial period. Palaeorecords provide contradictory evidence about marine productivity in this region, but beyond one glacial cycle, data were sparse. Here we present continuous chemical proxy data spanning the last eight glacial cycles (740,000 years) from the Dome C Antarctic ice core. These data constrain winter sea-ice extent in the Indian Ocean, Southern Ocean biogenic productivity and Patagonian climatic conditions. We found that maximum sea-ice extent is closely tied to Antarctic temperature on multi-millennial timescales, but less so on shorter timescales. Biological dimethylsulphide emissions south of the polar front seem to have changed little with climate, suggesting that sulphur compounds were not active in climate regulation. We observe large glacial-interglacial contrasts in iron deposition, which we infer reflects strongly changing Patagonian conditions. During glacial terminations, changes in Patagonia apparently preceded sea-ice reduction, indicating that multiple mechanisms may be responsible for different phases of CO2 increase during glacial terminations. We observe no changes in internal climatic feedbacks that could have caused the change in amplitude of Antarctic temperature variations observed 440,000 years ago.

Principal petrographic characteristics and K-Ar isotope-geochronological data on samples from the Keli Volcanic Highland, Greater Caucasus

The paper reports newly obtained stratigraphic, petrographic, and isotope geochronology data on modern moderately acid lavas from the Keli Highland of the Greater Caucasus and presents a geological map of the territory, in which 35 volcanoes active in Late Quaternary time were documented by the authors. Total duration of volcanic activity at the highland was estimated at 250 ka. Volcanic activity was discrete and occurred in three phases: Middle Neopleistocene (245-170 ka), Late Neopleistocene (135-70 ka), and Late Neopleistocene-Holocene (<30 ka). Newly obtained lines of evidence indicate that certain volcanoes erupted in the latest Neopleistocene-Holocene. The first phase of volcanic activity was connected mainly with lava volcanoes, and eruptions during the later phases of volcanic activity in this part of the Greater Caucasus produced mainly lavas. The most significant eruptions are demonstrated to occur in the territory during the second phase. The major evolutionary trends of volcanic processes during the final phase in the Keli Highland are determined. It was also determined that overwhelming majority of volcanoes that were active less than 30 ka BP are spatially restricted to long-liven local magmatic zones, which were active during either all three or only the final two phases of activity. These parts of the territory are, perhaps, the most hazardous in terms of volcanic activity.

Composition of bottom sediments, rocks, and ores from the Tropical Atlantic

Geological features of some areas of the Tropical Atlantic (stratigraphy, tectonic structure, lithology, distribution of ore components in bottom sediments, petrography of bedrocks, etc.) are under consideration in the book. Regularities of concentration of trace elements in iron-manganese nodules, features of these nodules in bottom sediments, distribution of phosphorite nodules and other phosphorites have been studied. Much attention is paid to rocks of the ocean crust. A wide range of mineralization represented by magnetite, chromite, chalcopyrite, pyrite, pentlandite, and other minerals has been found.

Minerals and geochemistry abundance and occurance, as well as K-Ar determinations for DSDP Site 92-597 basalts

Preliminary studies of hydrothermally altered massive basalts formed at the fast-spreading Mendoza Rise and recovered from DSDP Holes 597B and 597C indicate the presence of three secondary mineral assemblages which formed in the following order: (1) trioctahedral chlorite and talc, (2) goethite and smectite, and (3) calcite and celadonite. The sequential precipitation of these mineral assemblages denotes high water:rock ratios and time-varying conditions of temperature (early >200°C to late <30°C) and state of oxidation (early nonoxidative to late oxidative). A decrease in the relative proportion of oxidative mineral assemblages with depth to 70 m in Site 597 basement indicates a zone of oxidative alteration that became shallower with time as the deeper, more constricted fracture systems were filled by secondary mineralization. In this report we present the first results of the K-Ar dating of celadonite formation age; celadonite formation reflects end-stage hydrothermal alteration in Site 597 basement. Three celadonite dates obtained from Site 597 samples include 13.1 ± 0.3 m.y. from 17 m basement depth (Hole 597B), 19.9 ± 0.4 m.y. from 18 m basement depth (Hole 597C), and 19.3 ± 1.6 m.y. from 60 m basement depth (Hole 597C). The age of host rock crystallization (28.6 m.y.) and the K-Ar dates of celadonite formation establish that hydrothermal alteration in the upper 70 m of Site 597 basement continued for at least 10 m.y. and possibly as long as 16 m.y. after basalt crystallization at the ridge crest. Assuming a half-spreading rate of 55 km/m.y., we calculate that hydrothermal circulation was active in shallow basement at a distance of at least 550 km off ridge crest and possibly as far as 1000 km off ridge crest.

(Table 1) Results of X-ray radiographic analyses of authigenic phosphorites from the Southwest Africa shelf

In the biologically productive area on the Southwest Africa shelf a current process of diagenetic phosphorite formation occurs. Remains of phytoplankton are the main source of phosphorus in host bottom sediments. Phosphorus concentrates in nodules due to its redistribution in bottom sediments and precipitation from interstitial waters. Accumulation of the phosphate nodules, as well as of scattered fish bone debris in sediments occurs at sudden change in hydrological conditions and removal of fine sediment fractions due to increased bottom currents or during transgressions.