Crystallization screens: compatibility with the lipidic cubic phase for in meso crystallization of membrane proteins.

The in meso method for growing crystals of membrane proteins uses a spontaneously forming lipidic cubic mesophase. The detergent-solubilized protein is dispersed with lipid, typically monoolein, and in so doing the cubic phase self-assembles. A precipitant is added to trigger crystal nucleation and growth. The commercial screen solution series are convenient for use in crystallization trials. The aim of this study was to determine which of the Hampton Screen and Screen 2 series of solutions are compatible with the in meso method. These screens contain components any of which could destroy the cubic phase. X-ray diffraction was used for phase identification and for microstructure characterization. The study was done at 4 degrees C and at 20 degrees C. Two types of sample preparations were examined. One used an excess of half-strength screen solution (Prep. 1). The other used a limiting quantity of undiluted screen solution (Prep. 2). At 20 degrees C, over 90% of the screen solutions produced the cubic phase with Prep. 1. This figure dropped to 50% with Prep. 2. In contrast, 50 to 60% of the screens were cubic phase compatible at 4 degrees C under Prep. 1 conditions. The figure fell to 25% with Prep. 2. The mode of action of the diverse screen components are explained on the basis of the phase properties of the monoolein/water system

Consistently dated Atlantic sediment cores over the last 40 thousand years

Abstract: Rapid changes in ocean circulation and climate have been observed in marine-sediment and ice cores over the last glacial period and deglaciation, highlighting the non-linear character of the climate system and underlining the possibility of rapid climate shifts in response to anthropogenic greenhouse gas forcing. To date, these rapid changes in climate and ocean circulation are still not fully explained. One obstacle hindering progress in our understanding of the interactions between past ocean circulation and climate changes is the difficulty of accurately dating marine cores. Here, we present a set of 92 marine sediment cores from the Atlantic Ocean for which we have established age-depth models that are consistent with the Greenland GICC05 ice core chronology, and computed the associated dating uncertainties, using a new deposition modeling technique. This is the first set of consistently dated marine sediment cores enabling paleoclimate scientists to evaluate leads/lags between circulation and climate changes over vast regions of the Atlantic Ocean. Moreover, this data set is of direct use in paleoclimate modeling studies