Strongly correlated electron systems often exhibit very strong interactions between structural and electronic degrees of freedom that lead to complex and interesting phase diagrams. For technological applications of these materials it is important to learn how to drive transitions from one phase to another. A key question here is the ultimate speed of such phase transitions, and to understand how a phase transition evolves in the time domain. Here we apply time-resolved X-ray diffraction to directly measure the changes in long-range order during ultrafast melting of the charge and orbitally ordered phase in a perovskite manganite. We find that although the actual change in crystal symmetry associated with this transition occurs over different timescales characteristic of the many electronic and vibrational coordinates of the system, the dynamics of the phase transformation can be well described using a single time-dependent 'order parameter' that depends exclusively on the electronic excitation.

The chicken beta-globin 5'HS4 insulator element acts as a barrier to the encroachment of chromosomal silencing. Endogenous 5'HS4 sequences are highly enriched with histone acetylation and H3K4 methylation regardless of neighboring gene expression. We report here that 5'HS4 elements recruit these histone modifications when protecting a reporter transgene from chromosomal silencing. Deletion studies identified a single protein binding site within 5'HS4, footprint IV, that is necessary for the recruitment of histone modifications and for barrier activity. We have determined that USF proteins bind to footprint IV. USF1 is present in complexes with histone modifying enzymes in cell extracts, and these enzymes specifically interact with the endogenous 5'HS4 element. Knockdown of USF1 expression leads to a loss of histone modification recruitment and subsequent encroachment of H3K9 methylation. We propose that barrier activity requires the constitutive recruitment of H3K4 methylation and histone acetylation at multiple residues to counteract the propagation of condensed chromatin structures.

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[1] Using Cluster data, we investigate the electric structure of a dipolarization front (DF) -the ion inertial length (c/w pi ) scale boundary in the Earth's magnetotail formed at the front edge of an earthward propagating flow with reconnected magnetic flux. We estimate the current density and the electron pressure gradient throughout the DF by both single-spacecraft and multi-spacecraft methods. Comparison of the results from the two methods shows that the single-spacecraft analysis, which is capable of resolving the detailed structure of the boundary, can be applied for the DF we study. Based on this, we use the current density and the electron pressure gradient from the single-spacecraft method to investigate which terms in the generalized Ohm's law balance the electric field throughout the DF. We find that there is an electric field at ion inertia scale directed normal to the DF; it has a duskward component at the dusk flank of DF but a dawnward component at the dawn flank of DF. This electric field is balanced by the Hall (j  B/ne) and electron pressure gradient (r P e /ne) terms at the DF, with the Hall term being dominant. Outside the narrow DF region, however, the electric field is balanced by the convection (V i  B) term, meaning the frozen-in condition for ions is broken only at the DF itself. In the reference frame moving with the DF the tangential electric field is almost zero, indicating there is no flow of plasma across the DF and that the DF is a tangential discontinuity. The normal electric field at the DF constitutes a potential drop of $1 keV, which may reflect and accelerate the surrounding ions. Citation: Fu, H. S., Y. V. Khotyaintsev, A. Vaivads, M. André, and S. Y. Huang (2012), Electric structure of dipolarization front at sub-proton scale, Geophys. Res. Lett., 39, L06105,