Randomized controlled trial comparing a variable-thread novel tapered and a standard tapered implant: interim one-year results

STATEMENT OF PROBLEM: A tapered implant with continuously changing threads purported to provide stable tissue support and allow immediate function has been developed. Treatment success and stabilization of supporting tissues over time require documentation. PURPOSE: The purpose of this prospective, randomized, controlled, multicenter study was to evaluate changes in bone level and soft tissue behavior between the novel implant (NobelActive/NA) and a standard tapered implant (NobelReplace Tapered Groovy/NR) with regard to immediate function. MATERIAL AND METHODS: A total of 177 patients randomly allocated to 3 treatment groups (2 different test implant groups: NA Internal (n=117; internal connection) and External (n=82), and 1 standard treatment group, NR (n=126)) received 325 implants. Implants were placed into healed sites, and all but 6 implants were immediately nonocclusally loaded. Clinical and radiographic evaluations of treatment success, crestal bone levels, and soft tissue changes were performed at the time of placement and after 3, 6, and 12 months. Log-Rank test was used to analyze the differences in survival rate. Marginal bone level was compared using the Kruskal-Wallis test and Mann-Whitney U-test (alpha=.05). RESULTS: One-year cumulative survival rates were comparable (96.6% for NA Internal; 96.3% for NA External; 97.6% for NR; P=.852; Log-Rank). Mean (SD) change in bone level was -0.95 mm (1.37) for NA Internal, -0.64 mm (0.97) for NA External, and -0.63 mm (1.18) for NR (P=.589; Kruskal-Wallis). Stable soft tissues and significantly increased papilla scores (P<.001; Wilcoxon signed-rank) were observed for all implant types. CONCLUSIONS: The novel implants showed high survival rates as well as stable bone and soft tissue levels after 1 year, and may be recommended for clinical use, even under immediate function.

A 6'-Fluoro-Substituent in Bicyclo-DNA Increases Affinity to Complementary RNA Presumably by CF-HC Pseudohydrogen Bonds

The synthesis of a novel bicyclic thymidine analogue carrying a β-fluoro substituent at C6' (6'F-bcT) has been achieved. Key steps of the synthesis were an electrophilic fluorination/stereospecific hydrogenation sequence of a bicyclo sugar intermediate, followed by an N-iodo-succinimide-induced stereoselective nucleosidation. A corresponding phosphoramidite building block was then prepared and used for oligonucleotide synthesis. Tm measurements of oligonucleotides with single and double incorporations showed a remarkable stabilization of duplex formation particularly with RNA as complement without compromising pairing selectivity. Increases in Tm were in the range of +1-2 °C compared to thymidine and +1-3 °C compared to a standard bc-T residue. Structural investigations of the 6'F-bcT nucleoside by X-ray crystallography showed an in-line arrangement of the fluorine substituent with H6 of thymine, however, with a distance that is relatively long for a nonclassical CF-HC hydrogen bond. In contrast, structural investigations in solution by (1)H and (13)C NMR clearly showed scalar coupling of fluorine with H6 and C6 of the nucleobase, indicating the existence of at least weak electrostatic interactions. On the basis of these results, we put forward the hypothesis that these weak CF-HC6 electrostatic interactions increase duplex stability by orienting and partially freezing torsion angle χ of the 6'F-bcT nucleoside.

Mass-movement and flood-induced deposits in Lake Ledro, southern Alps, Italy: implications for Holocene palaeohydrology and natural hazards

High-resolution seismic profiles and sediment cores from Lake Ledro combined with soil and riverbed samples from the lake's catchment area are used to assess the recurrence of natural hazards (earthquakes and flood events) in the southern Italian Alps during the Holocene. Two well-developed deltas and a flat central basin are identified on seismic profiles in Lake Ledro. Lake sediments have been finely laminated in the basin since 9000 cal. yr BP and frequently interrupted by two types of sedimentary events (SEs): light-coloured massive layers and dark-coloured graded beds. Optical analysis (quantitative organic petrography) of the organic matter present in soil, riverbed and lacustrine samples together with lake sediment bulk density and grain-size analysis illustrate that light-coloured layers consist of a mixture of lacustrine sediments and mainly contain algal particles similar to the ones observed in background sediments. Light-coloured layers thicker than 1.5 cm in the main basin of Lake Ledro are synchronous to numerous coeval mass-wasting deposits remoulding the slopes of the basin. They are interpreted as subaquatic mass-movements triggered by historical and pre-historical regional earthquakes dated to AD2005, AD1891, AD1045 and 1260, 2545, 2595, 3350, 3815, 4740, 7190, 9185 and 11 495 cal. yr BP. Darkcoloured SEs develop high-amplitude reflections in front of the deltas and in the deep central basin. These beds are mainly made of terrestrial organic matter (soils and lignocellulosic debris) and are interpreted as resulting from intense hyperpycnal flood event. Mapping and quantifying the amount of soil material accumulated in the Holocene hyperpycnal flood deposits of the sequence allow estimating that the equivalent soil thickness eroded over the catchment area reached up to 5mm during the largest Holocene flood events. Such significant soil erosion is interpreted as resulting from the combination of heavy rainfall and snowmelt. The recurrence of flash flood events during the Holocene was, however, not high enough to affect pedogenesis processes and highlight several wet regional periods during the Holocene. The Holocene period is divided into four phases of environmental evolution. Over the first half of the Holocene, a progressive stabilization of the soils present through the catchment of Lake Ledro was associated with a progressive reforestation of the area and only interrupted during the wet 8.2 event when the soil destabilization was particularly important. Lower soil erosion was recorded during the mid-Holocene climatic optimum (8000-4200 cal. yr BP) and associated with higher algal production. Between 4200 and 3100 cal. yr BP, both wetter climate and human activities within the drainage basin drastically increased soil erosion rates. Finally, from 3100 cal. yr BP to the present-day, data suggest increasing and changing human land use.

Long-term climate change commitment and reversibility: An EMIC Intercomparison

This paper summarizes the results of an intercomparison project with Earth System Models of Intermediate Complexity (EMICs) undertaken in support of the Intergovernmental Panel on Climate Change (IPCC) Fifth Assessment Report (AR5). The focus is on long-term climate projections designed to 1) quantify the climate change commitment of different radiative forcing trajectories and 2) explore the extent to which climate change is reversible on human time scales. All commitment simulations follow the four representative concentration pathways (RCPs) and their extensions to year 2300. Most EMICs simulate substantial surface air temperature and thermosteric sea level rise commitment following stabilization of the atmospheric composition at year-2300 levels. The meridional overturning circulation (MOC) is weakened temporarily and recovers to near-preindustrial values in most models for RCPs 2.6-6.0. The MOC weakening is more persistent for RCP8.5. Elimination of anthropogenic CO2 emissions after 2300 results in slowly decreasing atmospheric CO2 concentrations. At year 3000 atmospheric CO2 is still at more than half its year-2300 level in all EMICs for RCPs 4.5-8.5. Surface air temperature remains constant or decreases slightly and thermosteric sea level rise continues for centuries after elimination of CO2 emissions in all EMICs. Restoration of atmospheric CO2 from RCP to preindustrial levels over 100-1000 years requires large artificial removal of CO2 from the atmosphere and does not result in the simultaneous return to preindustrial climate conditions, as surface air temperature and sea level response exhibit a substantial time lag relative to atmospheric CO2.

COP 9 SIGNALOSOME SUBUNIT 6 STABILIZES COP1, A NOVEL E3 UBIQUITIN LIGASE FOR 14-3-3σ

14-3-3σ, a gene upregulated by p53 in response to DNA damage, exists as part of a positive-feedback loop which activates p53 and is a human cancer epithelial marker downregulated in various cancer types. 14-3-3σ levels are critical for maintaining p53 activity in response to DNA damage and regulating signal mediator such as Akt. Here, we identify Mammalian Constitutive Photomorphogenic 1 (COP1) as a novel E3 ubiquitin ligase for targeting 14-3-3σ through proteasome degradation. We show for the first time that COP9 signalosome subunit 6 (CSN6) associates with COP1 and is involved in 14-3-3σ ubiquitin-mediated degradation. Mechanistic studies show that CSN6 expression leads to stabilization of COP1 through reducing COP1 self-ubiquitination and decelerating COP1’s turnover rate. We also show that CSN6-mediated 14-3-3σ ubiquitination is compromised when COP1 is knocked down. Thus, CSN6 mediates 14-3-3σ ubiquitination through enhancing COP1 stability. Subsequently, we show that CSN6 causes 14-3-3σ downregulation, thereby activating Akt and promoting cell survival by suppressing FOXO, an Akt target, transcriptional activity. Also, CSN6 overexpression leads to increased cell growth, transformation and promotes tumorigenicity. Significantly, 14-3-3σ expression can correct the abnormalities mediated by CSN6 expression. These data suggest that the CSN6-COP1 axis is involved in 14-3-3σ degradation, and that deregulation of this axis will promote cell growth and tumorigenicity.

Mechanisms regulating the p120-catenin/Kaiso pathway

The Wnt pathways contribute to many processes in cancer and developmental biology, with β-catenin being a key canonical component. P120-catenin, which is structurally similar to β-catenin, regulates the expression of certain Wnt target genes, relieving repression conferred by the POZ/ zinc-finger transcription factor Kaiso. In my first project, employing Xenopus embryos and mammalian cell lines, I found that the degradation machinery of the canonical Wnt pathway modulates p120-catenin protein stability, especially p120 isoform-1, through mechanisms shared with b-catenin. Exogenous expression of destruction-complex components such as GSK3b or Axin promotes p120-catenin degradation, and consequently, is able to rescue developmental phenotypes resulting from p120 over-expression during early Xenopus embryonic development. Conversely, as predicted, the in vivo depletion of either Axin or GSK3b coordinately increased p120 and b-catenin levels, while p120 levels decreased upon LRP5/6 depletion, which are positive modulators in the canonical Wnt pathway. At the primary sequence level, I resolved conserved GSK3b phosphorylation sites in p120’s (isoform 1) amino-terminal region. Point-mutagenesis of these residues inhibited the association of destruction complex proteins including those involved in ubiquitination, resulting in p120-catenin stabilization. Importantly, we found that two additional p120-catenin family members, ARVCF-catenin and d-catenin, in common with b-catenin and p120, associate with Axin, and are degraded in Axin’s presence. Thus, by similar means, it appears that canonical Wnt signals coordinately modulate multiple catenin proteins having roles in development and conceivably disease states. In my second project, I found that the Dyrk1A kinase exhibits a positive effect upon p120-catenin levels. That is, unlike the negative regulator GSK3b kinase, a candidate screen revealed that Dyrk1A kinase enhances p120-catenin protein levels via increased half-life. Dyrk1A is encoded by a gene located within the trisomy of chromosome 21, which contributes to mental retardation in Down Syndrome patients. I found that Dyrk1A expression results in increased p120 protein levels, and that Dyrk1A specifically associates with p120 as opposed to other p120-catenin family members or b-catenin. Consistently, Dyrk1A depletion in mammalian cell lines and Xenopus embryos decreased p120-catenin levels. I further confirmed that Dyrk overexpression and knock-down modulates both Siamois and Wnt11 gene expression in the expected manner based upon the resulting latered levels of p120-catenin. I determined that Dyrk expression rescues Kaiso depletion effects (gastrulation failure; increased endogenous Wnt11 expression), and vice versa. I then identified a putative Dyrk phosphorylation region within the N-terminus of p120-catenin, which may also be responsible for Dyrk1A association. I went on to make a phosphomimic mutant, which when over-expressed, had the predicted enhanced capacity to positively modulate endogenous Wnt11 and Siamois expression, and thereby generate gastrulation defects. Given that Dyrk1A modulates Siamois expression through stabilization of p120-catenin, I further observed that ectopic expression of Dyrk can positively influence b-catenin’s capacity to generate ectopic dorsal axes when ventrally expressed in early Xenopus embryos. Future work will investigate how Dyrk1A modulates the Wnt signaling pathway through p120-catenin, and possibly begin to address how dysfunction of Dyrk1A with respect to p120-catenin might relate to aspects of Down syndrome. In summary, the second phase of my graduate work appears to have revealed a novel aspect of Dyrk1A/p120-catenin action in embryonic development, with a functional linkage to canonical Wnt signaling. What I have identified as a “Dyrk1A/p120-catenin/Kaiso pathway” may conceivably assist in our larger understanding of the impact of Dyrk1A dosage imbalance in Down syndrome.

c-{\it mos\/} RNA expression in somatic cells and its physiological significance in cell cycle progression

The c-mos proto-oncogene, which is expressed at relatively high levels in male and female germ cells, plays a key role in oocyte meiotic maturation. The c-mos gene product in oocytes (p39$\sp{\rm c-mos}$) is necessary and sufficient to initiate meiosis. p39$\sp{\rm c-mos}$ is also an essential component of the cytostatic factor, which is responsible for arresting vertebrate oocytes at the second meiotic metaphase by stabilizing the maturation promoting factor (MPF). MPF is a universal regulator of both meiosis and mitosis. Much less is understood about c-mos expression and function in somatic cells. In addition to gonadal tissues, c-Mos has been detected in some somatic tissues and non-germ cell lines including NIH 3T3 cells as a protein termed p43$\sp{\rm c-mos}$. Since c-mos RNA transcripts were not previously detected in this cell line by Northern blot or S1 protection analyses, a search was made for c-mos RNA in NIH 3T3 cells. c-mos transcripts were detected using the highly sensitive RNA-PCR method and RNase protection assays. Furthermore, cell cycle analyses indicated that expression of c-mos RNA is tightly controlled in a cell cycle dependent manner with highest levels of transcripts (approximately 5 copies/cell) during the G2 phase.^ In order to determine the physiological significance of c-mos RNA expression in somatic cells, antisense mos was placed under the control of an inducible promoter and introduced into either NIH 3T3 cells or C2 cells. It was found that a basal level of expression of antisense mos resulted in interference with mitotic progression and growth arrest. Several nuclear abnormalities were observed, especially the appearance of binucleated and multinucleated cells as well as the extrusion of microvesicles containing cellular material. These results indicate that antisense mos expression results in a block in cytokinesis. In summary, these results establish that c-mos expression is not restricted to germ cells, but instead indicate that c-mos RNA expression occurs during the G2 stage of the cell cycle. Furthermore, these studies demonstrate that the c-mos proto-oncogene plays an important role in cell cycle progression. As in meiosis, c-mos may have a similar but not identical function in regulating cell cycle events in somatic cells, particularly in controlling mitotic progression via activation/stabilization of MPF. ^

Fractures in Children and Adolescents

Fractures of the growing bone require fixation techniques, which preclude any injury to the growth plate regions. This requirement is met by Elastic Stable Intramedullary Nails (ESIN) which are positioned between both metaphyseal regions. Pronounced malposition and/or shortening, open fractures and fractures with impending skin perforation are indications for clavicle nailing in adolescents. Retrograde nailing with two elastic nails, inserted from lateral, is the method of choice for stabilization of humerus fractures. In radial neck fractures with severe tilting of the radial head, a retrograde nail may reduce and fix the head. In Monteggia lesions, the ulna fracture is reduced and fixed with an antegrade nail. Forearm fractures with unacceptable axial deviation are reduced and fixed with one antegrade nail in the ulna and a retrograde nail in the radius. Ascending elastic nailing is done for femur shaft and proximal femur fractures. The medial and lateral entry sites are located above the distal physis. End caps are used to prevent shortening in spiral and multiple segment fractures. Fractures of the distal third of the femur are nailed in a descending technique. The entry sites of two nails are located on the lateral cortex below the greater trochanter. Combined tibia and fibula fractures, open fractures and unstable fracture types such as spiral and multifragmental tibia fractures are good indications for ESIN. Descending nailing is the method of choice. The nail entry points are medially and laterally distal to the apophysis of the proximal tibia. Thorough knowledge of each fracture type, fracture location and age specific healing pattern is necessary for safe and effective treatment of pediatric fractures

Tracing reinforcement through asymmetrical partner preference in the European common vole Microtus arvalis

Background The mechanistic basis of speciation and in particular the contribution of behaviour to the completion of the speciation process is often contentious. Contact zones between related taxa provide a situation where selection against hybridization might reinforce separation by behavioural mechanisms, which could ultimately fully isolate the taxa. One of the most abundant European mammals, the common vole Microtus arvalis, forms multiple natural hybrid zones where rapidly diverging evolutionary lineages meet in secondary contact. Very narrow zones of hybridization spanning only a few kilometres and sex-specific gene flow patterns indicate reduced fitness of natural hybrids and incipient speciation between some of the evolutionary lineages. In this study, we examined the contribution of behavioural mechanisms to the speciation process in these rodents by fine-mapping allopatric and parapatric populations in the hybrid zone between the Western and Central lineages and experimental testing of the partner preferences of wild, pure-bred and hybrid female common voles. Results Genetic analysis based on microsatellite markers revealed the presence of multiple parapatric and largely non-admixed populations at distances of about 10 km at the edge of the area of natural hybridization between the Western and Central lineages. Wild females from Western parapatric populations and lab-born F1 hybrids preferred males from the Western lineage whereas wild females of Central parapatric origin showed no measurable preference. Furthermore, wild and lab-born females from allopatric populations of the Western or Central lineages showed no detectable preference for males from either lineage. Conclusions The detected partner preferences are consistent with asymmetrical reinforcement of pre-mating reproductive isolation mechanisms in the European common vole and with earlier results suggesting that hybridization is more detrimental to the Western lineage. As a consequence, these differences in behaviour might contribute to a further geographical stabilization of this moving hybrid zone. Such behavioural processes could also provide a mechanistic perspective for frequently-detected asymmetrical introgression patterns in the largely allopatrically diversifying Microtus genus and other rapidly speciating rodents.

Solvation-Driven Charge Transfer and Localization in Metal Complexes

In any physicochemical process in liquids, the dynamical response of the solvent to the solutes out of equilibrium plays a crucial role in the rates and products: the solvent molecules react to the changes in volume and electron density of the solutes to minimize the free energy of the solution, thus modulating the activation barriers and stabilizing (or destabilizing) intermediate states. In charge transfer (CT) processes in polar solvents, the response of the solvent always assists the formation of charge separation states by stabilizing the energy of the localized charges. A deep understanding of the solvation mechanisms and time scales is therefore essential for a correct description of any photochemical process in dense phase and for designing molecular devices based on photosensitizers with CT excited states. In the last two decades, with the advent of ultrafast time-resolved spectroscopies, microscopic models describing the relevant case of polar solvation (where both the solvent and the solute molecules have a permanent electric dipole and the mutual interaction is mainly dipole−dipole) have dramatically progressed. Regardless of the details of each model, they all assume that the effect of the electrostatic fields of the solvent molecules on the internal electronic dynamics of the solute are perturbative and that the solvent−solute coupling is mainly an electrostatic interaction between the constant permanent dipoles of the solute and the solvent molecules. This well-established picture has proven to quantitatively rationalize spectroscopic effects of environmental and electric dynamics (time-resolved Stokes shifts, inhomogeneous broadening, etc.). However, recent computational and experimental studies, including ours, have shown that further improvement is required. Indeed, in the last years we investigated several molecular complexes exhibiting photoexcited CT states, and we found that the current description of the formation and stabilization of CT states in an important group of molecules such as transition metal complexes is inaccurate. In particular, we proved that the solvent molecules are not just spectators of intramolecular electron density redistribution but significantly modulate it. Our results solicit further development of quantum mechanics computational methods to treat the solute and (at least) the closest solvent molecules including the nonperturbative treatment of the effects of local electrostatics and direct solvent−solute interactions to describe the dynamical changes of the solute excited states during the solvent response.

The Interplay between Melting, Refertilization and Carbonatite Metasomatism in Off-Cratonic Lithospheric Mantle under Zealandia: an Integrated Major, Trace and Platinum Group Element Study

It is widely accepted that stabilization of the continental crust requires the presence of sub-continental lithospheric mantle. However, the degree of melt depletion required to stabilize the lithosphere and whether widespread refertilization is a significant process remain unresolved. Here, major and trace element, including platinum group elements (PGE), characterization of 40 mantle xenoliths from 13 localities is used to constrain the melt depletion, refertilization and metasomatic history of lithospheric mantle underneath the micro-continent Zealandia. Our previously published Re–Os isotopic data for a subset of these xenoliths indicate Phanerozoic to Paleoproterozoic ages and, reinterpreted with the new major and trace element data presented here, demonstrate that a large volume (>2 million km3) of lithospheric mantle with an age of 1·99 ± 0·21 Ga is present below the much younger crust of Zealandia. A peritectic melting model using moderately incompatible trace elements (e.g. Yb) in bulk-rocks demonstrates that these peridotites experienced a significant range of degrees of partial melting, between 3 and 28%. During subsolidus equilibration clinopyroxene gains significant rare earth elements (REE), which then leads to the underestimation of the degree of partial melting by ≤12% in fertile xenoliths. A new approach taking into account the effects of subsolidus re-equilibration on clinopyroxene composition effectively removes discrepancies in the calculated degree of melting and provides consistent estimates of between 4 and 29%. The estimated amount of melting is independent of the Re–Os model ages of the samples. The PGE patterns record simple melt depletion histories and the retention of primary base metal sulfides in the majority of the xenoliths. A rapid decrease in Pt/IrN observed at c. 1·0 wt % Al2O3 is a direct result of the exhaustion of sulfide in the mantle residue at c. 20–25% partial melting and the inability of Pt to form a stable alloy phase. Major elements preserve evidence for refertilization by a basaltic component that resulted in the formation of secondary clinopyroxene and low-forsterite olivine. The majority of xenoliths show the effects of cryptic metasomatic overprinting, ranging from minor to strong light REE enrichments in bulk-rocks (La/YbN = 0·16–15·9). Metasomatism is heterogeneous, with samples varying from those with weak REE enrichment and notable positive Sr and U–Th anomalies and negative Nb–Ta anomalies in clinopyroxene to those that have extremely high concentrations of REE, Th–U and Nb. Chemical compositions are consistent with a carbonatitic component contributing to the metasomatism of the lithosphere under Zealandia. Notably, the intense metasomatism of the samples did not affect the PGE budget of the peridotites as this was controlled by residual sulfides.

Cell mixing induced by myc is required for competitive tissue invasion and destruction

Cell-cell intercalation is used in several developmental processes to shape the normal body plan. There is no clear evidence that intercalation is involved in pathologies. Here we use the proto-oncogene myc to study a process analogous to early phase of tumour expansion: myc-induced cell competition. Cell competition is a conserved mechanism driving the elimination of slow-proliferating cells (so-called 'losers') by faster-proliferating neighbours (so-called 'winners') through apoptosis and is important in preventing developmental malformations and maintain tissue fitness. Here we show, using long-term live imaging of myc-driven competition in the Drosophila pupal notum and in the wing imaginal disc, that the probability of elimination of loser cells correlates with the surface of contact shared with winners. As such, modifying loser-winner interface morphology can modulate the strength of competition. We further show that elimination of loser clones requires winner-loser cell mixing through cell-cell intercalation. Cell mixing is driven by differential growth and the high tension at winner-winner interfaces relative to winner-loser and loser-loser interfaces, which leads to a preferential stabilization of winner-loser contacts and reduction of clone compactness over time. Differences in tension are generated by a relative difference in F-actin levels between loser and winner junctions, induced by differential levels of the membrane lipid phosphatidylinositol (3,4,5)-trisphosphate. Our results establish the first link between cell-cell intercalation induced by a proto-oncogene and how it promotes invasiveness and destruction of healthy tissues.

The p120-catenin/Kaiso signaling pathway

The canonical and non-canonical Wnt signaling pathways appear to interact with one another as a network in development, or when hyper-activated, in the progression of disease. A much studied key mediator of the canonical Wnt pathway, β-catenin, is characterized by a central armadillo-repeat domain that engages in multiple protein-protein interactions, such as those with cadherins functioning at cell-cell contact regions. In the nucleus, β-catenin forms a complex with the repressor TCF/LEF, promoting the activation of genes participating in processes such as proliferation, differentiation and stem cell survival. Somewhat similarly, the p120-catenin binds the distinct transcriptional repressor Kaiso, relieving Kaiso-mediated repression to promote gene activation. Here, employing Xenopus laevis, I report upon both downstream and upstream aspects of the p120-catenin/Kaiso pathway which was previously poorly understood. I first show that Kaiso, a BTB/POZ zinc-finger family member, directly represses canonical Wnt gene targets (Siamois, c-Fos, Cyclin-D1 and c-Myc) in conjunction with TCF. Depletion or dominant-negative inhibition of xKaiso results in Siamois de-repression, while xKaiso over-expression induces additional Siamois repression through recruitment of N-CoR co-repressor and chromatin modifications. Functional interdependencies are further corroborated by the capacity of Kaiso to suppress β-catenin-induced axis duplication. Thus, my work inter-relates the p120-catenin/Kaiso and β-catenin/TCF pathways at the level of specific gene promoters important in development and cancer progression. Regarding upstream aspects of the p120-catenin/Kaiso pathway, I collaboratively identified p120 in association with Frodo, a protein previously identified as a component of the canonical (β-catenin dependent) Wnt pathway. I determined that canonical Wnt signals result in Frodo-mediated stabilization of p120-catenin, resulting in the sequestration of Kaiso to the cytoplasm and thereby the activation (relief of repression) of gene targets. Developmental evidence supporting this view included findings that Frodo has the capacity to partially rescue Kaiso over-expression phenotypes in early Xenopus embryos. Taken together, my studies point to the convergence of p120-catenin/Kaiso and β-catenin/TCF signaling pathways at the level of gene transcription as well as at more upstream points during vertebrate development. ^

Vital function for PRELI and essential requirement for its LEA motif

Proteins containing the late embryogenesis abundant (LEA) motif comprise an evolutionarily conserved family, long postulated to protect plant embryos from stress and death. However, the significance of LEA-containing proteins and the mechanisms behind their function remain undetermined. Here we show that PRELI, a mammalian protein that possesses tandem repeats of the LEA motif, can protect cells against staurosporine, TNF-α or UV irradiation-induced apoptosis. We found that key to PRELI-dependent mechanisms that promote cell resistance to death are the stabilization of the respiratory chain, upholding of mitochondrial membrane potential and retention of apoptogenic molecules. By in vitro and in vivo studies, we also show that the expression of mutant PRELI/LEA- proteins lacking the LEA motif, results in the complete loss of PRELI's anti-apoptotic functions. Collectively, our data uncover a new molecular player in the control of apoptosis and support the hypothesis that LEA-containing proteins are evolutionarily conserved cell protectors against stress and death. ^

Age determinations from Bykovsky Peninsula, Siberia

A wide variety of environmental records is necessary for analysing and understanding the complex Late Quaternary dynamics of permafrost-dominated Arctic landscapes. A NE Siberian periglacial key region was studied in detail using sediment records, remote sensing data, and terrain modelling, all incorporated in a geographical information system (GIS). The study area consists of the Bykovsky Peninsula and the adjacent Khorogor Valley in the Kharaulakh Ridge situated a few kilometres southeast of the Lena Delta. In this study a comprehensive cryolithological database containing information from 176 sites was compiled. The information from these sites is based on the review of previously published borehole data, outcrop profiles, surface samples, and our own field data. These archives cover depositional records of three periods: from Pliocene to Early Pleistocene, the Late Pleistocene and the Holocene. The main sediment sequences on the Bykovsky Peninsula consist of up to 50 m thick ice-rich permafrost deposits (Ice Complex) that were accumulated during the Late Pleistocene. They were formed as a result of nival processes around extensive snowfields in the Kharaulakh Ridge, slope processes in these mountains (such as in the Khorogor Valley), and alluvial/proluvial sedimentation in a flat accumulation plain dominated by polygonal tundra in the mountain foreland (Bykovsky Peninsula). During the early to middle Holocene warming, a general landscape transformation occurred from an extensive Late Pleistocene accumulation plain to a strongly thermokarst-dominated relief dissected by numerous depressions. Thermokarst subsidence had an enormous influence on the periglacial hydrological patterns, the sediment deposition, and on the composition and distribution of habitats. Climate deterioration, lake drainage, and talik refreezing occurred during the middle to late Holocene. The investigated region was reached by the post-glacial sea level rise during the middle Holocene, triggering thermo-abrasion of ice-rich coasts and the marine inundation of thermokarst depressions.