Interaction of the 82-kDa subunit of the vaccinia virus early transcription factor heterodimer with the promoter core sequence directs downstream DNA binding of the 70-kDa subunit.

The vaccinia virus early transcription factor (VETF), a heterodimeric protein composed of 82- and 70-kDa subunits, interacts with viral early promoters at both a sequence-specific core region upstream and a sequence-independent region downstream of the RNA start site. To determine the VETF subunit-promoter interactions, 32P-labeled DNA targets were chemically synthesized with uniquely positioned phosphorothioates to which azidophenacyl bromide moieties were coupled. After incubating the derivatized promoter with VETF and exposing the complex to 302-nm light, the protein was denatured and the individual subunits with or without covalently bound DNA were isolated with specific antiserum and analyzed by SDS/polyacrylamide gel electrophoresis. Using a set of 26 duplex probes, with uniquely positioned aryl azide moieties on the coding or template strands, we found that the 82-kDa subunit interacted primarily with the core region of the promoter, whereas the 70-kDa subunit interacted with the downstream region. Nucleotide substitutions in the core region that downregulate transcription affected the binding of both subunits: the 82-kDa subunit no longer exhibited specificity for upstream regions of the promoter but also bound to downstream regions, whereas the binding of the 70-kDa subunit was abolished even though the mutations were far upstream of its binding site. These results suggested mechanisms by which the interaction of the 82-kDa subunit with the core sequence directs binding of the 70-kDa subunit to DNA downstream.

Global compilation of benthic data sets I

Approaches to quantify the organic carbon accumulation on a global scale generally do not consider the small-scale variability of sedimentary and oceanographic boundary conditions along continental margins. In this study, we present a new approach to regionalize the total organic carbon (TOC) content in surface sediments (<5 cm sediment depth). It is based on a compilation of more than 5500 single measurements from various sources. Global TOC distribution was determined by the application of a combined qualitative and quantitative-geostatistical method. Overall, 33 benthic TOC-based provinces were defined and used to process the global distribution pattern of the TOC content in surface sediments in a 1°x1° grid resolution. Regional dependencies of data points within each single province are expressed by modeled semi-variograms. Measured and estimated TOC values show good correlation, emphasizing the reasonable applicability of the method. The accumulation of organic carbon in marine surface sediments is a key parameter in the control of mineralization processes and the material exchange between the sediment and the ocean water. Our approach will help to improve global budgets of nutrient and carbon cycles.